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Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36168313/Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.; Jordá-Pardo...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.;  Jordá-Pardo, J.; Martín-Lerma, I.; Sesé, C. & Valdivia, J. (2018): Recurrent Magdalenian occupation in the interior of the Iberian<br />Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences<br /><a href="https://doi.org/10.1007/s12520-018-0620-z" rel="nofollow">https://doi.org/10.1007/s12520-018-0620-z</a><br /><br />Abstract<br />The occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic.We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36168313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36168313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36168313; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36168313]").text(description); $(".js-view-count[data-work-id=36168313]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36168313; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36168313']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36168313, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36168313]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36168313,"title":"Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)","translated_title":"","metadata":{"abstract":"Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.; Jordá-Pardo, J.; Martín-Lerma, I.; Sesé, C. \u0026 Valdivia, J. (2018): Recurrent Magdalenian occupation in the interior of the Iberian\nPeninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences\nhttps://doi.org/10.1007/s12520-018-0620-z\n\nAbstract\nThe occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). 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Archaeological and Anthropological Sciences\nhttps://doi.org/10.1007/s12520-018-0620-z\n\nAbstract\nThe occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic.We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.\n\n\n","internal_url":"https://www.academia.edu/36168313/Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_","translated_internal_url":"","created_at":"2018-03-15T01:37:49.930-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Peña_de_Estebanvela_Segovia_Spain_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":1624,"name":"Zooarchaeology","url":"https://www.academia.edu/Documents/in/Zooarchaeology"},{"id":4548,"name":"Palaeolithic Archaeology","url":"https://www.academia.edu/Documents/in/Palaeolithic_Archaeology"},{"id":15780,"name":"Taphonomy","url":"https://www.academia.edu/Documents/in/Taphonomy"},{"id":22571,"name":"Iberian Prehistory (Archaeology)","url":"https://www.academia.edu/Documents/in/Iberian_Prehistory_Archaeology_"},{"id":49708,"name":"Magdalenian","url":"https://www.academia.edu/Documents/in/Magdalenian"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="36029151"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior"><img alt="Research paper thumbnail of El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior">El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-F...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé,  C. & Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.  En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. & Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. <br /> <br />Resumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales  y paleofaunísticas  y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las  cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior. <br />Palabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente <br />Abstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian.    <br />Key Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36029151"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36029151"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36029151; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36029151]").text(description); $(".js-view-count[data-work-id=36029151]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36029151; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36029151']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36029151, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36029151]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36029151,"title":"El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.","translated_title":"","metadata":{"abstract":"Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior. En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. \r\n\r\nResumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales y paleofaunísticas y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior.\r\nPalabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente\r\nAbstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian. \r\nKey Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment\r\n\r\n"},"translated_abstract":"Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior. En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. \r\n\r\nResumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales y paleofaunísticas y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior.\r\nPalabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente\r\nAbstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian. \r\nKey Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment\r\n\r\n","internal_url":"https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior","translated_internal_url":"","created_at":"2018-02-27T03:42:35.857-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Coímbre_Peñamellera_Alta_Asturias_durante_el_Pleistoceno_Superior","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":7075,"name":"Paleoenvironment","url":"https://www.academia.edu/Documents/in/Paleoenvironment"},{"id":7101,"name":"Paleoecology","url":"https://www.academia.edu/Documents/in/Paleoecology"},{"id":77508,"name":"Late Pleistocene","url":"https://www.academia.edu/Documents/in/Late_Pleistocene"},{"id":116250,"name":"Cantabrian Region","url":"https://www.academia.edu/Documents/in/Cantabrian_Region"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="36017448"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_"><img alt="Research paper thumbnail of Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_">Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yac...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. & Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259. <br /> <br />Resumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior,  datado en 15.680 - 14.230 cal BP,  hasta el nivel 6, del Gravetiense final,  con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S.  araneus – S.  coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M.  arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A.  sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos,  y actualmente vive en regiones más  septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere  un clima templado. <br />Abstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the  level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S.  araneus – S.  coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M.  arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and  Apodemus gr. A.  sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and  nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36017448"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36017448"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36017448; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36017448]").text(description); $(".js-view-count[data-work-id=36017448]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36017448; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36017448']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36017448, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36017448]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36017448,"title":"Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)","translated_title":"","metadata":{"abstract":"Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259.\r\n\r\nResumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior, datado en 15.680 - 14.230 cal BP, hasta el nivel 6, del Gravetiense final, con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A. sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos, y actualmente vive en regiones más septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere un clima templado. \r\nAbstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and Apodemus gr. A. sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate. "},"translated_abstract":"Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259.\r\n\r\nResumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior, datado en 15.680 - 14.230 cal BP, hasta el nivel 6, del Gravetiense final, con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A. sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos, y actualmente vive en regiones más septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere un clima templado. \r\nAbstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and Apodemus gr. A. sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate. ","internal_url":"https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_","translated_internal_url":"","created_at":"2018-02-26T02:52:39.138-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Los_micromamíferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Coímbre_Asturias_España_","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":77508,"name":"Late Pleistocene","url":"https://www.academia.edu/Documents/in/Late_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"},{"id":969133,"name":"North Spain","url":"https://www.academia.edu/Documents/in/North_Spain"},{"id":975805,"name":"Erinaceomorpha","url":"https://www.academia.edu/Documents/in/Erinaceomorpha"},{"id":975810,"name":"Soricomorpha","url":"https://www.academia.edu/Documents/in/Soricomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="35935814"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/35935814/Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Co%C3%ADmbre_Cave_Pe%C3%B1amellera_Alta_Asturias_"><img alt="Research paper thumbnail of Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias)." class="work-thumbnail" src="https://attachments.academia-assets.com/55817916/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/35935814/Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Co%C3%ADmbre_Cave_Pe%C3%B1amellera_Alta_Asturias_">Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias).</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.: Arrizabalaga...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.:  Arrizabalaga, A.; Jordá Pardo,  J. F.; Elorza, M.; Iriarte‐Chiapusso, M. J.; Sesé, C.; Uzquiano, P. (2017): Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias). Oxford Journal of Archaeology, 36 (4): 331-354.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="aba124b5276ac2cef122999235e80063" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":55817916,"asset_id":35935814,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/55817916/download_file?st=MTczMjgwMTM2NCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="35935814"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="35935814"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 35935814; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=35935814]").text(description); $(".js-view-count[data-work-id=35935814]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 35935814; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='35935814']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 35935814, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "aba124b5276ac2cef122999235e80063" } } $('.js-work-strip[data-work-id=35935814]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":35935814,"title":"Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="35671362"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_"><img alt="Research paper thumbnail of Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria)." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_">Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria).</a></div><div class="wp-workCard_item"><span>C. Sesé (2017). Estudios Geológicos 73(2): e072.</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. <br />Palabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.<br />ABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. <br />Keywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="35671362"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="35671362"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 35671362; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=35671362]").text(description); $(".js-view-count[data-work-id=35671362]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 35671362; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='35671362']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 35671362, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=35671362]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":35671362,"title":"Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria).","translated_title":"","metadata":{"doi":"10.3989/ egeol.41589.471.","abstract":"RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. \nPalabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.\nABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. \nKeywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.\n","location":"http://hdl.handle.net/10261/159027","more_info":"http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/966","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"C. Sesé (2017). Estudios Geológicos 73(2): e072."},"translated_abstract":"RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. \nPalabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.\nABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. \nKeywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.\n","internal_url":"https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_","translated_internal_url":"","created_at":"2018-01-15T05:36:10.569-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Los_micromamíferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":292,"name":"Palaeoclimatology","url":"https://www.academia.edu/Documents/in/Palaeoclimatology"},{"id":17472,"name":"Palaeoecology","url":"https://www.academia.edu/Documents/in/Palaeoecology"},{"id":53800,"name":"Pleistocene mammals","url":"https://www.academia.edu/Documents/in/Pleistocene_mammals"},{"id":87213,"name":"Vertebrate taphonomy","url":"https://www.academia.edu/Documents/in/Vertebrate_taphonomy"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"}],"urls":[{"id":8443634,"url":"http://hdl.handle.net/10261/159027"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="34555405"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A"><img alt="Research paper thumbnail of New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. & Pérez-González, A." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A">New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. & Pérez-González, A.</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews </span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape <br />and climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher <br />than at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="34555405"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="34555405"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 34555405; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=34555405]").text(description); $(".js-view-count[data-work-id=34555405]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 34555405; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='34555405']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 34555405, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=34555405]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":34555405,"title":"New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. \u0026 Pérez-González, A.","translated_title":"","metadata":{"volume":"173","abstract":"In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape\r\nand climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher\r\nthan at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.\r\n","page_numbers":"78-91","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Quaternary Science Reviews "},"translated_abstract":"In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape\r\nand climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher\r\nthan at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.\r\n","internal_url":"https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A","translated_internal_url":"","created_at":"2017-09-13T01:04:52.312-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_García_M_J_Sesé_C_Santonja_M_and_Pérez_González_A","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="34015262"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living"><img alt="Research paper thumbnail of The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living." class="work-thumbnail" src="https://attachments.academia-assets.com/53959609/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living">The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living.</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/EduardoGarc%C3%ADaS%C3%A1nchez">Eduardo García Sánchez</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/JFJorda">Jesús F. Jordá</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/Mar%C3%ADadeAndr%C3%A9sHerrero">María de Andrés Herrero</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/MariaJoseIriarteChiapusso">Maria-Jose Iriarte-Chiapusso</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/%C3%93scarFuente">Óscar Fuente Fernández</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/PabloLopezCisneros">Pablo Lopez Cisneros</a></span></div><div class="wp-workCard_item"><span>Conference: Hugo Obermaier-Gesellschaft für Erforschung des Eizeitalters und der Steinzeit e V. 57th Annual Meeting in Heidenheim, 2015, Volume: 57th Annual Meeting in Heidenheim. Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).<br /><br />Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.<br />Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.<br />This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44f29afe83ef5308ea9f237dd6b254f1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53959609,"asset_id":34015262,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53959609/download_file?st=MTczMjgwMTM2NCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="34015262"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="34015262"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 34015262; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=34015262]").text(description); $(".js-view-count[data-work-id=34015262]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 34015262; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='34015262']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 34015262, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44f29afe83ef5308ea9f237dd6b254f1" } } $('.js-work-strip[data-work-id=34015262]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":34015262,"title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living.","translated_title":"","metadata":{"volume":"57","abstract":"Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).\n\nCoímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.\nMoreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.\nThis work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.\n","page_numbers":"15-16","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Conference: Hugo Obermaier-Gesellschaft für Erforschung des Eizeitalters und der Steinzeit e V. 57th Annual Meeting in Heidenheim, 2015, Volume: 57th Annual Meeting in Heidenheim. Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age"},"translated_abstract":"Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).\n\nCoímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.\nMoreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.\nThis work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.\n","internal_url":"https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living","translated_internal_url":"","created_at":"2017-07-24T02:37:45.919-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2497886,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":29838809,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":352134,"co_author_invite_id":null,"email":"d***z@ucm.es","affiliation":"Universidad Complutense de Madrid","display_order":1,"name":"David Álvarez-Alonso","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). 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A symbolic place, a place for living."},{"id":29838815,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":467560,"co_author_invite_id":null,"email":"j***o@terra.es","affiliation":"Universidad Nacional de Educación a Distancia","display_order":7,"name":"Julio Rojo","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838816,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":372428,"co_author_invite_id":null,"email":"m***e@ehu.es","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":8,"name":"Maria-Jose Iriarte-Chiapusso","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838817,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":4287495,"co_author_invite_id":null,"email":"c***e@mncn.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":9,"name":"Carmen Sesé","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838818,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":1256507,"co_author_invite_id":null,"email":"p***o@hotmail.com","display_order":10,"name":"Paloma Uzquiano Ollero","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838819,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":2788011,"co_author_invite_id":null,"email":"m***a@hotmail.com","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":11,"name":"Martin Arriolabengoa","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838820,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":490382,"co_author_invite_id":null,"email":"i***i@hotmail.com","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":12,"name":"Irantzu Elorrieta-Baigorri","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="33992028"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33992028/Subsistencia_movilidad_y_adaptaci%C3%B3n_al_medio_de_los_cazadores_recolectores_gravetienses_en_el_sector_occidental_de_la_regi%C3%B3n_cant%C3%A1brica_la_cueva_de_Co%C3%ADmbre_Asturias_"><img alt="Research paper thumbnail of Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)" class="work-thumbnail" src="https://attachments.academia-assets.com/53942206/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33992028/Subsistencia_movilidad_y_adaptaci%C3%B3n_al_medio_de_los_cazadores_recolectores_gravetienses_en_el_sector_occidental_de_la_regi%C3%B3n_cant%C3%A1brica_la_cueva_de_Co%C3%ADmbre_Asturias_">Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/David%C3%81lvarezAlonso">David Álvarez-Alonso</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/JFJorda">Jesús F. Jordá</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/AlvaroArrizabalaga">Alvaro Arrizabalaga</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PalomaUzquianoOllero">Paloma Uzquiano Ollero</a></span></div><div class="wp-workCard_item"><span>Trabajos de Prehistoria</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Coímbre is one of the few Gravettian sites the middle- western part of Cantabria. It is one of th...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Coímbre is one of the few Gravettian sites the middle-<br />western part of Cantabria. It is one of the most interesting<br />sites for the analysis of the Gravettian close to the boundary of its western expansion in Europe. Zooarchaeological and taphonomical study of the faunal and archaeobotanical remains and the lithic industry and the interpretation of its AMS-dated archaeological and<br />sedimentological sequence make it possible to analyse<br />the Gravettian settlement in Coímbre cave using a territorial<br />perspective. The subsistence strategies developed<br />in Coímbre have been determinant in the interpretation<br />of its occupation patterns. Thus, we can assess the existence<br />of the specific mobility and subsistence patterns<br />developed by these human groups in the framework of<br />Cantabria. This pattern shows an ephemeral logistic and<br />punctual occupation of the cave, probably linked to an<br />eastern-western corridor. This is one of the paper’s most<br />interesting contributions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6ada514d59db5f37f8f7a85fb68cb623" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53942206,"asset_id":33992028,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53942206/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33992028"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33992028"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33992028; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33992028]").text(description); $(".js-view-count[data-work-id=33992028]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33992028; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33992028']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33992028, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "6ada514d59db5f37f8f7a85fb68cb623" } } $('.js-work-strip[data-work-id=33992028]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33992028,"title":"Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)","translated_title":"","metadata":{"issue":"1","volume":"74","abstract":"Coímbre is one of the few Gravettian sites the middle-\nwestern part of Cantabria. 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class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_"><img alt="Research paper thumbnail of Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/53856315/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_">Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)</a></div><div class="wp-workCard_item"><span>Spanish Journal of Paleontology</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. & Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burg...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. &  Morales, J. (2017).  Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.<br />Abstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.<br />Keywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.<br />Resumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.<br />Palabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7129c09a041b1d9d97c677b57ad914c7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53856315,"asset_id":33880579,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33880579"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33880579"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33880579; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33880579]").text(description); $(".js-view-count[data-work-id=33880579]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33880579; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33880579']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33880579, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "7129c09a041b1d9d97c677b57ad914c7" } } $('.js-work-strip[data-work-id=33880579]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33880579,"title":"Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)","translated_title":"","metadata":{"issue":"1","volume":"32","abstract":"Sesé, C. \u0026 Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.\nAbstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.\nKeywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.\nResumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.\nPalabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.\n\n","page_numbers":"63-78","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Spanish Journal of Paleontology"},"translated_abstract":"Sesé, C. \u0026 Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.\nAbstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.\nKeywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.\nResumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.\nPalabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.\n\n","internal_url":"https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_","translated_internal_url":"","created_at":"2017-07-14T02:26:55.903-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":29717169,"work_id":33880579,"tagging_user_id":4287495,"tagged_user_id":2992261,"co_author_invite_id":null,"email":"j***1@gmail.com","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":1,"name":"Jorge Morales","title":"Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)"}],"downloadable_attachments":[{"id":53856315,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53856315/thumbnails/1.jpg","file_name":"Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos.pdf","download_url":"https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Late_Aragonian_mammal_sites_of_Cuesta_de.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53856315/Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos-libre.pdf?1500024541=\u0026response-content-disposition=attachment%3B+filename%3DLate_Aragonian_mammal_sites_of_Cuesta_de.pdf\u0026Expires=1732804965\u0026Signature=Y~S59qtkugkHksSb~~gPgfQpWmkYoXUzbq06S7e-KTG3FNdSMKH98kF8Rd4g1hXKkerYB8cpM9wnYFuD9zW9LWAajx5QSzl8y5YNjrtqNUheCG4inIUq6Eg38ca6OIGP-6TS1kqwpLS5QeIfBHC8Amg8umUwDyCqQPFST~BuTYSSYURyJ8mcKeStVSenLSffelLR~lnIzJUXp~pC0ub14OYmwiyeCSaAasJPLrnDiw2pXAmXVzaHRqaSO9PZnVHNQZ8hK9OPJEUlY~dZqRe5YX0kyGe9xx1zlnaeiLMDR4H1MVmyGfDkXV4pUtw9lY-FUpEBGxsMXxFwJTEmNmeEQA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_","translated_slug":"","page_count":16,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":53856315,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53856315/thumbnails/1.jpg","file_name":"Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos.pdf","download_url":"https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Late_Aragonian_mammal_sites_of_Cuesta_de.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53856315/Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos-libre.pdf?1500024541=\u0026response-content-disposition=attachment%3B+filename%3DLate_Aragonian_mammal_sites_of_Cuesta_de.pdf\u0026Expires=1732804965\u0026Signature=Y~S59qtkugkHksSb~~gPgfQpWmkYoXUzbq06S7e-KTG3FNdSMKH98kF8Rd4g1hXKkerYB8cpM9wnYFuD9zW9LWAajx5QSzl8y5YNjrtqNUheCG4inIUq6Eg38ca6OIGP-6TS1kqwpLS5QeIfBHC8Amg8umUwDyCqQPFST~BuTYSSYURyJ8mcKeStVSenLSffelLR~lnIzJUXp~pC0ub14OYmwiyeCSaAasJPLrnDiw2pXAmXVzaHRqaSO9PZnVHNQZ8hK9OPJEUlY~dZqRe5YX0kyGe9xx1zlnaeiLMDR4H1MVmyGfDkXV4pUtw9lY-FUpEBGxsMXxFwJTEmNmeEQA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="33272836"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33272836/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_"><img alt="Research paper thumbnail of Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/53341269/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33272836/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/LydiaZapata">Lydia Zapata</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/M%C3%B3nicaRuizAlonso">Mónica Ruiz-Alonso</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula cur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440e21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770e12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural<br />resources may have been used. The faunal remains represented at this site reflect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality fix the occupation of levels IeIII from the spring to the autumn. Certain types of wood were collected for use as firewood. Other elements found in the record (personal ornaments, mobiliary art and raw materials) provide evidence that the people that occupied the site moved over a more extensive territory.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d74023c6760eecc9d5b89cefe9de4589" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53341269,"asset_id":33272836,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53341269/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33272836"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33272836"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33272836; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33272836]").text(description); $(".js-view-count[data-work-id=33272836]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33272836; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33272836']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33272836, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d74023c6760eecc9d5b89cefe9de4589" } } $('.js-work-strip[data-work-id=33272836]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33272836,"title":"Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)","translated_title":"","metadata":{"abstract":"The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440e21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770e12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). 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href="https://www.academia.edu/32637472/El_aprovechamiento_de_lagomorfos_en_el_Paleol%C3%ADtico_superior_cant%C3%A1brico_Nuevas_perspectivas_desde_la_cueva_de_Co%C3%ADmbre_Asturias_"><img alt="Research paper thumbnail of El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias)." class="work-thumbnail" src="https://attachments.academia-assets.com/52807453/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32637472/El_aprovechamiento_de_lagomorfos_en_el_Paleol%C3%ADtico_superior_cant%C3%A1brico_Nuevas_perspectivas_desde_la_cueva_de_Co%C3%ADmbre_Asturias_">El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias).</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. & Sesé, C. 2017: El aprovecha...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. & Sesé, C. 2017: El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias). Arqueobiología durante el Greenland Stadial 2 en la Región Cantábrica (CA. 22000-15000 CAL BP). Salamanca 20-21 de abril 2017. Universidad de Salamanca: p. 5<br /><br />Resumen: En la mayor parte de los yacimientos del norte peninsular, estos animales son escasos o excepcionales y prácticamente sus restos son testimoniales. Sin embargo, en los niveles del Magdaleniense superior de la zona B de la cueva de Coímbre (Peñamellera Alta,<br />Asturias) ha aparecido una importante concentración de restos de conejo que merecen la pena<br />ser analizados en cierto detalle. Con este estudio, presentamos los resultados del análisis tafonómico de los conejos del yacimiento. Desde una perspectiva taxonómica los lagomorfos<br />suponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las<br />especies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,<br />otros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia<br />tafonómica compleja con individuos aportados por el ser humano frente a otros con aportes<br />biológicos no humanos. En todo caso las evidencias registradas en la cueva de Coímbre deben<br />ser consideradas y tenidas en cuenta a la hora de reflexionar por qué en los otros contextos<br />cantábricos son tan escasos estos animales.<br /><br />Palabras clave: Tafonomía, Lagomorfos, Paleolítico superior, Pleistoceno superior, Yacimiento de la cueva de Coímbre, Asturias, Región Cantábrica, Norte de España.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="094c8c6b4f025401437eb78ba683f651" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52807453,"asset_id":32637472,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52807453/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32637472"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32637472"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32637472; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32637472]").text(description); $(".js-view-count[data-work-id=32637472]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32637472; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32637472']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32637472, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "094c8c6b4f025401437eb78ba683f651" } } $('.js-work-strip[data-work-id=32637472]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32637472,"title":"El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias).","translated_title":"","metadata":{"abstract":"Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. \u0026 Sesé, C. 2017: El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias). Arqueobiología durante el Greenland Stadial 2 en la Región Cantábrica (CA. 22000-15000 CAL BP). Salamanca 20-21 de abril 2017. Universidad de Salamanca: p. 5\n\nResumen: En la mayor parte de los yacimientos del norte peninsular, estos animales son escasos o excepcionales y prácticamente sus restos son testimoniales. Sin embargo, en los niveles del Magdaleniense superior de la zona B de la cueva de Coímbre (Peñamellera Alta,\nAsturias) ha aparecido una importante concentración de restos de conejo que merecen la pena\nser analizados en cierto detalle. Con este estudio, presentamos los resultados del análisis tafonómico de los conejos del yacimiento. Desde una perspectiva taxonómica los lagomorfos\nsuponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las\nespecies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,\notros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia\ntafonómica compleja con individuos aportados por el ser humano frente a otros con aportes\nbiológicos no humanos. En todo caso las evidencias registradas en la cueva de Coímbre deben\nser consideradas y tenidas en cuenta a la hora de reflexionar por qué en los otros contextos\ncantábricos son tan escasos estos animales.\n\nPalabras clave: Tafonomía, Lagomorfos, Paleolítico superior, Pleistoceno superior, Yacimiento de la cueva de Coímbre, Asturias, Región Cantábrica, Norte de España.\n\n\n"},"translated_abstract":"Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. \u0026 Sesé, C. 2017: El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias). Arqueobiología durante el Greenland Stadial 2 en la Región Cantábrica (CA. 22000-15000 CAL BP). Salamanca 20-21 de abril 2017. Universidad de Salamanca: p. 5\n\nResumen: En la mayor parte de los yacimientos del norte peninsular, estos animales son escasos o excepcionales y prácticamente sus restos son testimoniales. Sin embargo, en los niveles del Magdaleniense superior de la zona B de la cueva de Coímbre (Peñamellera Alta,\nAsturias) ha aparecido una importante concentración de restos de conejo que merecen la pena\nser analizados en cierto detalle. Con este estudio, presentamos los resultados del análisis tafonómico de los conejos del yacimiento. Desde una perspectiva taxonómica los lagomorfos\nsuponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las\nespecies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,\notros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia\ntafonómica compleja con individuos aportados por el ser humano frente a otros con aportes\nbiológicos no humanos. En todo caso las evidencias registradas en la cueva de Coímbre deben\nser consideradas y tenidas en cuenta a la hora de reflexionar por qué en los otros contextos\ncantábricos son tan escasos estos animales.\n\nPalabras clave: Tafonomía, Lagomorfos, Paleolítico superior, Pleistoceno superior, Yacimiento de la cueva de Coímbre, Asturias, Región Cantábrica, Norte de España.\n\n\n","internal_url":"https://www.academia.edu/32637472/El_aprovechamiento_de_lagomorfos_en_el_Paleol%C3%ADtico_superior_cant%C3%A1brico_Nuevas_perspectivas_desde_la_cueva_de_Co%C3%ADmbre_Asturias_","translated_internal_url":"","created_at":"2017-04-25T01:28:17.272-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52807453,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52807453/thumbnails/1.jpg","file_name":"Yravedra_et_al_2017_El_aprovechamiento_de_lagomorfos_en_el_Paleolitico_superior_cantabrico.pdf","download_url":"https://www.academia.edu/attachments/52807453/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"El_aprovechamiento_de_lagomorfos_en_el_P.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52807453/Yravedra_et_al_2017_El_aprovechamiento_de_lagomorfos_en_el_Paleolitico_superior_cantabrico-libre.pdf?1493108992=\u0026response-content-disposition=attachment%3B+filename%3DEl_aprovechamiento_de_lagomorfos_en_el_P.pdf\u0026Expires=1732804965\u0026Signature=ahs1IdXtdLw1Wslzkg63IA9fvvdPjGZgwg~4VqNicaCtrkBz6iJR-mYOypbEmuQSgsIMhsANQTYur3-rF~49pqbqV0nO12oS~i4tRLQpQnd9mOdJwe0SbJZkUsqFwvQq5Vpqm60GzdKCfJHXUJ6Sxu1HNB1U-9zByQJ5ci7lVve1EibKQ4wH5zjcs7~-VSHRfG1SW9M8ZbXGPOCZNDMjjpHewm2zfKjTXYBIo7arY85Y7kbQnfIy22480inyqN8I8T8FjOKumcooaITPQ3M2GBZ~BoAMSgebZX8e7V0-MHj52sgKhSGIoXOUJmbL0olv272elxuHbEYEIevR5Dup5Q__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"El_aprovechamiento_de_lagomorfos_en_el_Paleolítico_superior_cantábrico_Nuevas_perspectivas_desde_la_cueva_de_Coímbre_Asturias_","translated_slug":"","page_count":4,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52807453,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52807453/thumbnails/1.jpg","file_name":"Yravedra_et_al_2017_El_aprovechamiento_de_lagomorfos_en_el_Paleolitico_superior_cantabrico.pdf","download_url":"https://www.academia.edu/attachments/52807453/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"El_aprovechamiento_de_lagomorfos_en_el_P.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52807453/Yravedra_et_al_2017_El_aprovechamiento_de_lagomorfos_en_el_Paleolitico_superior_cantabrico-libre.pdf?1493108992=\u0026response-content-disposition=attachment%3B+filename%3DEl_aprovechamiento_de_lagomorfos_en_el_P.pdf\u0026Expires=1732804965\u0026Signature=ahs1IdXtdLw1Wslzkg63IA9fvvdPjGZgwg~4VqNicaCtrkBz6iJR-mYOypbEmuQSgsIMhsANQTYur3-rF~49pqbqV0nO12oS~i4tRLQpQnd9mOdJwe0SbJZkUsqFwvQq5Vpqm60GzdKCfJHXUJ6Sxu1HNB1U-9zByQJ5ci7lVve1EibKQ4wH5zjcs7~-VSHRfG1SW9M8ZbXGPOCZNDMjjpHewm2zfKjTXYBIo7arY85Y7kbQnfIy22480inyqN8I8T8FjOKumcooaITPQ3M2GBZ~BoAMSgebZX8e7V0-MHj52sgKhSGIoXOUJmbL0olv272elxuHbEYEIevR5Dup5Q__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":15780,"name":"Taphonomy","url":"https://www.academia.edu/Documents/in/Taphonomy"},{"id":30825,"name":"Upper Paleolithic","url":"https://www.academia.edu/Documents/in/Upper_Paleolithic"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"},{"id":969133,"name":"North Spain","url":"https://www.academia.edu/Documents/in/North_Spain"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474865"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662687/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf">Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016.  Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas  (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. <br /><br />Resumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres<br />yacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment<br />and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="90c8ea538ad036e819e08e791ad2c15b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662687,"asset_id":32474865,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474865"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474865"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474865; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474865]").text(description); $(".js-view-count[data-work-id=32474865]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474865; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474865']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474865, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "90c8ea538ad036e819e08e791ad2c15b" } } $('.js-work-strip[data-work-id=32474865]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474865,"title":"Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. \n\nResumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres\nyacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.\n\nAbstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment\nand a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. \n\nResumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres\nyacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.\n\nAbstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment\nand a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:53:51.062-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662687,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662687/thumbnails/1.jpg","file_name":"Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Interpretacion_paleoambiental_de_los_mic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662687/Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria-libre.pdf?1492502142=\u0026response-content-disposition=attachment%3B+filename%3DInterpretacion_paleoambiental_de_los_mic.pdf\u0026Expires=1732591648\u0026Signature=AUxjzxEmfQQ-g4AbhmHYxc5vjUP-g41J~YCCOdPXUSCnefIK5ueLgrfcJK4gRIXxZJUjT7yLJ7TH2vL7m6uto7XNrn45NdiRLvP5VJpebZRMqmiuBb0gemcOpMYp9ilGa1h4SzozDxP-b0aOPFSuTl15mqlKMy16bD9bmo50oSIvWTTD77a9EZtVDKBbURo27UOohNA7ceNR9AzZiwTkOymKtX8oQdpIDHK9I2OC9pZhaxm1LByD6NTwwtQJBat7ncVNo4nnvwYky5SyYvWvfBGm~BH0BZOmdTDtmuoAiTZkn8WCgVt476p-50O1aOt-XCLeMkddr-0zkniN0Ap2sw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":48,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662687,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662687/thumbnails/1.jpg","file_name":"Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Interpretacion_paleoambiental_de_los_mic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662687/Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria-libre.pdf?1492502142=\u0026response-content-disposition=attachment%3B+filename%3DInterpretacion_paleoambiental_de_los_mic.pdf\u0026Expires=1732591648\u0026Signature=AUxjzxEmfQQ-g4AbhmHYxc5vjUP-g41J~YCCOdPXUSCnefIK5ueLgrfcJK4gRIXxZJUjT7yLJ7TH2vL7m6uto7XNrn45NdiRLvP5VJpebZRMqmiuBb0gemcOpMYp9ilGa1h4SzozDxP-b0aOPFSuTl15mqlKMy16bD9bmo50oSIvWTTD77a9EZtVDKBbURo27UOohNA7ceNR9AzZiwTkOymKtX8oQdpIDHK9I2OC9pZhaxm1LByD6NTwwtQJBat7ncVNo4nnvwYky5SyYvWvfBGm~BH0BZOmdTDtmuoAiTZkn8WCgVt476p-50O1aOt-XCLeMkddr-0zkniN0Ap2sw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":7075,"name":"Paleoenvironment","url":"https://www.academia.edu/Documents/in/Paleoenvironment"},{"id":27230,"name":"Chiroptera","url":"https://www.academia.edu/Documents/in/Chiroptera"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474804"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662596/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final d...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286<br /><br />Resumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa  europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f3e5235844801df9ae1ac01d19239ccd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662596,"asset_id":32474804,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474804"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474804"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474804; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474804]").text(description); $(".js-view-count[data-work-id=32474804]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474804; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474804']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474804, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f3e5235844801df9ae1ac01d19239ccd" } } $('.js-work-strip[data-work-id=32474804]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474804,"title":"Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286\n\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286\n\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:47:14.990-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662596,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662596/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662596/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria-libre.pdf?1492501763=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=AcHtWzpyqNdm0xtfdTBDtsnAsvn2va1WqC4deL-0YojaVQKa1Oz1JfvpsfJ~kL3ZR~TsUTLmJ64gwWy-mMsbko2DE7NHfB-ywWWMB30i-J-~XCnzlJoSrBcT7mwlvzduzEnE21Xgv0wGVkI4~Mq7A1irkAfnGMDfLoGXFcS12dkMeewI-M468yMAS9winfe4hOo0j2kn~5TXoXeSrM5Ka3V4RxgZX~18xOu63eO9zLkHg3v5bAzRrMdBoEh5QEbc9otqd5~bOzk8DP0SKkG5ik~mskYQEt66iCIX3Ts~H3ygK7grq6iW9bK--KV45C3QMTfX7FGjq0ZeQJJxDNcBoA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_España_pdf","translated_slug":"","page_count":38,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662596,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662596/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662596/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria-libre.pdf?1492501763=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=AcHtWzpyqNdm0xtfdTBDtsnAsvn2va1WqC4deL-0YojaVQKa1Oz1JfvpsfJ~kL3ZR~TsUTLmJ64gwWy-mMsbko2DE7NHfB-ywWWMB30i-J-~XCnzlJoSrBcT7mwlvzduzEnE21Xgv0wGVkI4~Mq7A1irkAfnGMDfLoGXFcS12dkMeewI-M468yMAS9winfe4hOo0j2kn~5TXoXeSrM5Ka3V4RxgZX~18xOu63eO9zLkHg3v5bAzRrMdBoEh5QEbc9otqd5~bOzk8DP0SKkG5ik~mskYQEt66iCIX3Ts~H3ygK7grq6iW9bK--KV45C3QMTfX7FGjq0ZeQJJxDNcBoA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":27230,"name":"Chiroptera","url":"https://www.academia.edu/Documents/in/Chiroptera"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474592"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662423/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated"> Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.<br /><br />Resumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,<br />Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus<br />agrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. <br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly<br />open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2888c2d016868011a23be981c8863030" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662423,"asset_id":32474592,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474592"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474592"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474592; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474592]").text(description); $(".js-view-count[data-work-id=32474592]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474592; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474592']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474592, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2888c2d016868011a23be981c8863030" } } $('.js-work-strip[data-work-id=32474592]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474592,"title":"Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf","translated_title":"","metadata":{"abstract":"\nSesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.\n\nResumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,\nMicrotus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus\nagrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. \n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly\nopen and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n\n"},"translated_abstract":"\nSesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.\n\nResumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,\nMicrotus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus\nagrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. \n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly\nopen and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n\n","internal_url":"https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:38:49.798-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662423,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662423/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662423/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria-libre.pdf?1492501251=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=YwlrsaXVlaMUGNlpYtw6giS3hbWkqplEHdZawpMttMCZepIey5CsHNmyN1R2T2paTFOKTI8RjrLukkjjr8bBS9fTzU0sJJAQjlegDS2m1~OU7NmBes8Mv~gkL64gKjEmyvV5PpMfsw31X2Z-gRVQJkSgQJ485XEtm0509F6AAItfrmf~Q0VQWXShslnMxGqnWvWWtZJwc2yUgn3dEYhK5w1Z00INTDg78iGLA~yIXSKUoo43~IMiZjNfOwY76Ag6ZrgSE4QajsX2wLb6WYfl-H8TC4T52cCMnMHyJ6K-ZfHAHsMIqJaItSdmr4rtEeMxO4CofZQl7nWln6lhzkiExg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":37,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662423,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662423/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662423/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria-libre.pdf?1492501251=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=YwlrsaXVlaMUGNlpYtw6giS3hbWkqplEHdZawpMttMCZepIey5CsHNmyN1R2T2paTFOKTI8RjrLukkjjr8bBS9fTzU0sJJAQjlegDS2m1~OU7NmBes8Mv~gkL64gKjEmyvV5PpMfsw31X2Z-gRVQJkSgQJ485XEtm0509F6AAItfrmf~Q0VQWXShslnMxGqnWvWWtZJwc2yUgn3dEYhK5w1Z00INTDg78iGLA~yIXSKUoo43~IMiZjNfOwY76Ag6ZrgSE4QajsX2wLb6WYfl-H8TC4T52cCMnMHyJ6K-ZfHAHsMIqJaItSdmr4rtEeMxO4CofZQl7nWln6lhzkiExg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474411"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662276/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016.  Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.<br />Resumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden  decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de<br />micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d73e1ce7866d2c915c22d59cc88074a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662276,"asset_id":32474411,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474411"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474411"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474411; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474411]").text(description); $(".js-view-count[data-work-id=32474411]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474411; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474411']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474411, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9d73e1ce7866d2c915c22d59cc88074a" } } $('.js-work-strip[data-work-id=32474411]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474411,"title":"Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de\nmicromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de\nmicromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:31:31.429-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662276,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662276/thumbnails/1.jpg","file_name":"Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana.pdf","download_url":"https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662276/Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana-libre.pdf?1492500765=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=VLBzKBTh4ivZV4tfM-DtAgGHF3EPxXyFM0kdh9YfQytBhL8rfHGqdr7wi-nXd1WhfD6FcV-Cx~9QvDENqX91PVcagQntb4Hu4L67vpscAZguLYC-0F3nkWLsekQNmTucFVFAiK4BQND8LTjdcwvtx3zaRIetO1gZ61BhpIuwYNVvVju56KsRN7q7qYW3RrtwUfxbsyRWqlFzYC-QgbWe0rkTlH3yehhgss~tyNCxCTGr7dPB6VQR99i37rd26Ky8LqwYwOaQXDw06t74gm1DWsau-tkoQ7YDyTcbpZomZghkZUNHhuloWX8hqg0H5ToEXMV0dn6UXa2lTBYH6OwnsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":38,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662276,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662276/thumbnails/1.jpg","file_name":"Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana.pdf","download_url":"https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662276/Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana-libre.pdf?1492500765=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=VLBzKBTh4ivZV4tfM-DtAgGHF3EPxXyFM0kdh9YfQytBhL8rfHGqdr7wi-nXd1WhfD6FcV-Cx~9QvDENqX91PVcagQntb4Hu4L67vpscAZguLYC-0F3nkWLsekQNmTucFVFAiK4BQND8LTjdcwvtx3zaRIetO1gZ61BhpIuwYNVvVju56KsRN7q7qYW3RrtwUfxbsyRWqlFzYC-QgbWe0rkTlH3yehhgss~tyNCxCTGr7dPB6VQR99i37rd26Ky8LqwYwOaQXDw06t74gm1DWsau-tkoQ7YDyTcbpZomZghkZUNHhuloWX8hqg0H5ToEXMV0dn6UXa2lTBYH6OwnsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); 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Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)" class="work-thumbnail" src="https://attachments.academia-assets.com/51731379/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/31349018/Patrimonio_geopaleontol%C3%B3gico_de_los_dep%C3%B3sitos_aluviales_situados_sobre_la_terraza_28_m_del_Jarama_Nuevos_datos_micropaleontol%C3%B3gicos_y_cronol%C3%B3gicos_Solar_de_la_Real_F%C3%A1brica_de_Pa%C3%B1os_de_San_Fernando_de_Henares_">Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://audema.academia.edu/JorgeMorindePablosLateAntiquityVisigothicKingdomandAlAndalusArchaeology">Jorge Morin de Pablos</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://uam.academia.edu/MarioLopezRecio">Mario Lopez Recio</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí,...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.;  Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. & Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. <br /><br /> Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). <br />Palabras clave: Micromamíferos, Jarama, Madrid, España. <br />Abstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). <br />Key words: Micromammals, Jarama, Madrid, Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="937dae8696ed6afd2aabb380b5decd27" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":51731379,"asset_id":31349018,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/51731379/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="31349018"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="31349018"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 31349018; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=31349018]").text(description); $(".js-view-count[data-work-id=31349018]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 31349018; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='31349018']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 31349018, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "937dae8696ed6afd2aabb380b5decd27" } } $('.js-work-strip[data-work-id=31349018]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":31349018,"title":"Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)","translated_title":"","metadata":{"abstract":"Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. \u0026 Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. \n\n Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). \nPalabras clave: Micromamíferos, Jarama, Madrid, España. \nAbstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). \nKey words: Micromammals, Jarama, Madrid, Spain."},"translated_abstract":"Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. \u0026 Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. \n\n Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). \nPalabras clave: Micromamíferos, Jarama, Madrid, España. \nAbstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). \nKey words: Micromammals, Jarama, Madrid, Spain.","internal_url":"https://www.academia.edu/31349018/Patrimonio_geopaleontol%C3%B3gico_de_los_dep%C3%B3sitos_aluviales_situados_sobre_la_terraza_28_m_del_Jarama_Nuevos_datos_micropaleontol%C3%B3gicos_y_cronol%C3%B3gicos_Solar_de_la_Real_F%C3%A1brica_de_Pa%C3%B1os_de_San_Fernando_de_Henares_","translated_internal_url":"","created_at":"2017-02-10T04:34:03.039-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":27519999,"work_id":31349018,"tagging_user_id":4287495,"tagged_user_id":687105,"co_author_invite_id":null,"email":"j***n@audema.com","affiliation":"AUDEMA","display_order":1,"name":"Jorge Morin de Pablos","title":"Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. 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(2016). Los micromam...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. & Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. <a href="http://dx.doi.org/10.3989/egeol.42424.405" rel="nofollow">http://dx.doi.org/10.3989/egeol.42424.405</a>.<br />Resumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.<br />Abstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. The climate would be of Mediterranean type, similar to the actual or perhaps a little milder and more humid.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b90c2989e9453261f9b3f44253fb42ac" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50798832,"asset_id":30346107,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50798832/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="30346107"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="30346107"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 30346107; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=30346107]").text(description); $(".js-view-count[data-work-id=30346107]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 30346107; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='30346107']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 30346107, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b90c2989e9453261f9b3f44253fb42ac" } } $('.js-work-strip[data-work-id=30346107]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":30346107,"title":"Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales","translated_title":"","metadata":{"abstract":"Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. \u0026 Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. http://dx.doi.org/10.3989/egeol.42424.405.\nResumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.\nAbstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. The climate would be of Mediterranean type, similar to the actual or perhaps a little milder and more humid."},"translated_abstract":"Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. \u0026 Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. http://dx.doi.org/10.3989/egeol.42424.405.\nResumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.\nAbstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. 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Rosas, A.; Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánche...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Rasilla, M. de la;  Rosas, A.;  Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.;  Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. E.; Valladas, H.; Mercier, N.; Tisnèrat-Laborde, N.; Grün, R.; Eggins, S.; Higham, T.; Wood, R. E.; Julià, R.; Soler, V.; Badal, E.;  Tarriño, A. & Alonso, J. (2016). El grupu neandertal de la Cueva d' El Sidrón (Borines, Piloña). Ciencies. 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C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.; Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. E.; Valladas, H.; Mercier, N.; Tisnèrat-Laborde, N.; Grün, R.; Eggins, S.; Higham, T.; Wood, R. E.; Julià, R.; Soler, V.; Badal, E.; Tarriño, A. \u0026 Alonso, J. (2016). El grupu neandertal de la Cueva d' El Sidrón (Borines, Piloña). Ciencies. Cartafueyos Asturianos de Ciencia y Teunoloxía, 6: 62-79."},"translated_abstract":"Rasilla, M. de la; Rosas, A.; Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.; Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. E.; Valladas, H.; Mercier, N.; Tisnèrat-Laborde, N.; Grün, R.; Eggins, S.; Higham, T.; Wood, R. E.; Julià, R.; Soler, V.; Badal, E.; Tarriño, A. \u0026 Alonso, J. (2016). El grupu neandertal de la Cueva d' El Sidrón (Borines, Piloña). Ciencies. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="28945890"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/28945890/New_data_from_Ambrona_Closing_the_hunting_versus_scavenging_debate"><img alt="Research paper thumbnail of New data from Ambrona Closing the hunting versus scavenging debate" class="work-thumbnail" src="https://attachments.academia-assets.com/49383844/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/28945890/New_data_from_Ambrona_Closing_the_hunting_versus_scavenging_debate">New data from Ambrona Closing the hunting versus scavenging debate</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/VillaPaola">Paola Villa</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uab.academia.edu/RMora">Rafael Mora</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavation...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavations at Ambrona (Spain), directed by Santonja and Pe´rez-Gonzaíez. The purpose of the new excavations was to achieve a better understanding of the stratigraphic sequence, general geology, sedimentary context and processes of accumulation of materials. Our objectives are to evaluate the opposing interpretations of the hominid subsistence activities at the site proposed by Freeman and Binford. The faunal and lithic remains are found in different sedimentary contexts: an alluvial fan, lacustrine muds, fluviatile clay–sands and channel deposits. Faunal remains in the lacustrine muds are often, but not always, in primary context. Remains of elephant and deer carcasses may be found in partial articulation or proximity and represent natural occurrences without any clear evidence of hominid intervention. In other contexts the faunal remains are occurrences of single anatomical elements either displaced by water or left isolated in situ. There are no carnivore marks; bones and stone artifacts show varying degrees of mechanical abrasion due to water transport. Limited evidence of human action on bones is provided by a few SEM verified cutmarks and some anthropic fractures. They document butchery of various animals, including elephants. We cannot prove hunting but we can definitely reject Binford's idea of marginal scavenging of medium-size ungulates from carnivore kills. Ambrona is a complex mix of natural and human components, the remnant of a natural landscape regularly visited by hominids, who transported some artifacts from nonlocal raw material sources and had an organized approach to meat acquisition. However, strong evidence of elephant hunting is provided only by sites younger than Ambrona.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="aaefd330ab10a81cf6e76a55f8052493" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49383844,"asset_id":28945890,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49383844/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="28945890"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="28945890"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 28945890; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=28945890]").text(description); $(".js-view-count[data-work-id=28945890]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 28945890; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='28945890']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 28945890, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "aaefd330ab10a81cf6e76a55f8052493" } } $('.js-work-strip[data-work-id=28945890]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":28945890,"title":"New data from Ambrona Closing the hunting versus scavenging debate","translated_title":"","metadata":{"abstract":"This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavations at Ambrona (Spain), directed by Santonja and Pe´rez-Gonzaíez. The purpose of the new excavations was to achieve a better understanding of the stratigraphic sequence, general geology, sedimentary context and processes of accumulation of materials. Our objectives are to evaluate the opposing interpretations of the hominid subsistence activities at the site proposed by Freeman and Binford. The faunal and lithic remains are found in different sedimentary contexts: an alluvial fan, lacustrine muds, fluviatile clay–sands and channel deposits. Faunal remains in the lacustrine muds are often, but not always, in primary context. Remains of elephant and deer carcasses may be found in partial articulation or proximity and represent natural occurrences without any clear evidence of hominid intervention. In other contexts the faunal remains are occurrences of single anatomical elements either displaced by water or left isolated in situ. There are no carnivore marks; bones and stone artifacts show varying degrees of mechanical abrasion due to water transport. Limited evidence of human action on bones is provided by a few SEM verified cutmarks and some anthropic fractures. They document butchery of various animals, including elephants. We cannot prove hunting but we can definitely reject Binford's idea of marginal scavenging of medium-size ungulates from carnivore kills. Ambrona is a complex mix of natural and human components, the remnant of a natural landscape regularly visited by hominids, who transported some artifacts from nonlocal raw material sources and had an organized approach to meat acquisition. However, strong evidence of elephant hunting is provided only by sites younger than Ambrona."},"translated_abstract":"This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavations at Ambrona (Spain), directed by Santonja and Pe´rez-Gonzaíez. The purpose of the new excavations was to achieve a better understanding of the stratigraphic sequence, general geology, sedimentary context and processes of accumulation of materials. Our objectives are to evaluate the opposing interpretations of the hominid subsistence activities at the site proposed by Freeman and Binford. The faunal and lithic remains are found in different sedimentary contexts: an alluvial fan, lacustrine muds, fluviatile clay–sands and channel deposits. Faunal remains in the lacustrine muds are often, but not always, in primary context. Remains of elephant and deer carcasses may be found in partial articulation or proximity and represent natural occurrences without any clear evidence of hominid intervention. In other contexts the faunal remains are occurrences of single anatomical elements either displaced by water or left isolated in situ. There are no carnivore marks; bones and stone artifacts show varying degrees of mechanical abrasion due to water transport. Limited evidence of human action on bones is provided by a few SEM verified cutmarks and some anthropic fractures. They document butchery of various animals, including elephants. We cannot prove hunting but we can definitely reject Binford's idea of marginal scavenging of medium-size ungulates from carnivore kills. Ambrona is a complex mix of natural and human components, the remnant of a natural landscape regularly visited by hominids, who transported some artifacts from nonlocal raw material sources and had an organized approach to meat acquisition. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="538868" id="papers"><div class="js-work-strip profile--work_container" data-work-id="36168313"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/36168313/Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_"><img alt="Research paper thumbnail of Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36168313/Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.; Jordá-Pardo...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.;  Jordá-Pardo, J.; Martín-Lerma, I.; Sesé, C. & Valdivia, J. (2018): Recurrent Magdalenian occupation in the interior of the Iberian<br />Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences<br /><a href="https://doi.org/10.1007/s12520-018-0620-z" rel="nofollow">https://doi.org/10.1007/s12520-018-0620-z</a><br /><br />Abstract<br />The occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic.We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36168313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36168313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36168313; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36168313]").text(description); $(".js-view-count[data-work-id=36168313]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36168313; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36168313']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36168313, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36168313]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36168313,"title":"Recurrent Magdalenian occupation in the interior of the Iberian Peninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain)","translated_title":"","metadata":{"abstract":"Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.; Jordá-Pardo, J.; Martín-Lerma, I.; Sesé, C. \u0026 Valdivia, J. (2018): Recurrent Magdalenian occupation in the interior of the Iberian\nPeninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences\nhttps://doi.org/10.1007/s12520-018-0620-z\n\nAbstract\nThe occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic.We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.\n\n\n"},"translated_abstract":"Yravedra, J.; Andrés-Chaín, M.; Cacho, C.; Martos, J. A.; Marquer, L.; Avezuela, B.; Jordá-Pardo, J.; Martín-Lerma, I.; Sesé, C. \u0026 Valdivia, J. (2018): Recurrent Magdalenian occupation in the interior of the Iberian\nPeninsula: new insights from the archaeological site of La Peña de Estebanvela (Segovia, Spain). Archaeological and Anthropological Sciences\nhttps://doi.org/10.1007/s12520-018-0620-z\n\nAbstract\nThe occupation of the Iberian Peninsula during the Upper Palaeolithic is mainly known from archaeological sites located in the Cantabrian and Mediterranean regions. Numerous sites have been excavated in these two regions when few sites are found in the interior of the peninsula. Several authors explain this scarcity of sites, in the inner region during the Upper Palaeolithic, by a decrease of human population resulting from a low capacity of human groups to adapt to the cold conditions of the Marine Isotopic Stage 2 (MIS 2), i.e. the effect of cold climate on human populations might have been stronger in the interior of the peninsula than in coastal areas. Recent studies underline the evidence of prehistoric occupation during this period in that region. It has been suggested that these occupations are isolated events limited to the warmest phases of the end of the MIS 2. The present study focuses on zooarchaeological and taphonomic aspects of the Magdalenian site of La Peña de Estebanvela (Segovia, Spain). Our results show that this site was recurrently occupied during the Magdalenian period, including warm and cold phases, which provide a new evidence of sustainable presence of human populations in the interior of the Iberian Peninsula at the end of the Upper Palaeolithic.We further propose hypotheses on the subsistence strategies (e.g. availability of hunting resources) developed at La Peña de Estebanvela and in a larger context including other Magdalenian sites of the inner region of the Peninsula.\n\n\n","internal_url":"https://www.academia.edu/36168313/Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_","translated_internal_url":"","created_at":"2018-03-15T01:37:49.930-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Recurrent_Magdalenian_occupation_in_the_interior_of_the_Iberian_Peninsula_new_insights_from_the_archaeological_site_of_La_Peña_de_Estebanvela_Segovia_Spain_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":1624,"name":"Zooarchaeology","url":"https://www.academia.edu/Documents/in/Zooarchaeology"},{"id":4548,"name":"Palaeolithic Archaeology","url":"https://www.academia.edu/Documents/in/Palaeolithic_Archaeology"},{"id":15780,"name":"Taphonomy","url":"https://www.academia.edu/Documents/in/Taphonomy"},{"id":22571,"name":"Iberian Prehistory (Archaeology)","url":"https://www.academia.edu/Documents/in/Iberian_Prehistory_Archaeology_"},{"id":49708,"name":"Magdalenian","url":"https://www.academia.edu/Documents/in/Magdalenian"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="36029151"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior"><img alt="Research paper thumbnail of El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior">El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-F...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé,  C. & Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.  En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. & Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. <br /> <br />Resumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales  y paleofaunísticas  y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las  cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior. <br />Palabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente <br />Abstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian.    <br />Key Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36029151"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36029151"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36029151; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36029151]").text(description); $(".js-view-count[data-work-id=36029151]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36029151; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36029151']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36029151, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36029151]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36029151,"title":"El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior.","translated_title":"","metadata":{"abstract":"Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior. En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. \r\n\r\nResumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales y paleofaunísticas y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior.\r\nPalabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente\r\nAbstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian. \r\nKey Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment\r\n\r\n"},"translated_abstract":"Iriarte-Chiapusso, M. J.; Yravedra Sainz de los Terreros, J.; David Álvarez-Alonso, D.; Alvarez-Fernández, E.; Aparicio, M. T.; Arrizabalaga, A.; Elorza, M.; Gabriel, S.; Jordá-Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. (2017): El contexto paleoambiental de las ocupaciones humanas de la cueva de Coímbre (Peñamellera Alta, Asturias) durante el Pleistoceno Superior. En: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 526-535. \r\n\r\nResumen: En este capítulo presentamos la síntesis paleoecológica y paleoambiental de la cueva de Coimbre obtenido a partir de las diferentes evidencias proporcionadas paleovegetales y paleofaunísticas y siguiendo los resultados de los estudios polínicos, antracológicas, macro- y micofaunísticos. Los resultados muestran un medio con paisajes abiertos y unas condiciones frías más o menos rigurosas según el momento bajo las cuales tuvieron lugar las ocupaciones humanas del Gravetiense y Magdaleniense inferior y medio. La secuencia arqueológica culmina con una fase más húmeda y una mayor diversidad del ecosistema durante el Magdaleniense superior.\r\nPalabras Clave: Pleistoceno superior, Cornisa Cantábrica, Paleoecología, Paleoambiente\r\nAbstract: In this chapter we offer a paleoecological and paleoenvironmental synthesis of the Coímbre cave using the evidence provided by plant and animal remains, as well as the results of the studies on pollen, wood charcoal, and microfauna. The result shows a milieu characterized by open landscapes and cold conditions of varying degrees of severity, depending on the time when the Gravettian and Lower and Middle Magdalenian human occupations took place. The archaeological sequence culminates in a more humid phase with a greater diversity of ecosystems during the Upper Magdalenian. \r\nKey Words: Upper Pleistocene, Cantabrian Mountains, Paleoecology, Paleoenvironment\r\n\r\n","internal_url":"https://www.academia.edu/36029151/El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Co%C3%ADmbre_Pe%C3%B1amellera_Alta_Asturias_durante_el_Pleistoceno_Superior","translated_internal_url":"","created_at":"2018-02-27T03:42:35.857-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"El_contexto_paleoambiental_de_las_ocupaciones_humanas_de_la_cueva_de_Coímbre_Peñamellera_Alta_Asturias_durante_el_Pleistoceno_Superior","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":7075,"name":"Paleoenvironment","url":"https://www.academia.edu/Documents/in/Paleoenvironment"},{"id":7101,"name":"Paleoecology","url":"https://www.academia.edu/Documents/in/Paleoecology"},{"id":77508,"name":"Late Pleistocene","url":"https://www.academia.edu/Documents/in/Late_Pleistocene"},{"id":116250,"name":"Cantabrian Region","url":"https://www.academia.edu/Documents/in/Cantabrian_Region"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="36017448"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_"><img alt="Research paper thumbnail of Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_">Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yac...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. & Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259. <br /> <br />Resumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior,  datado en 15.680 - 14.230 cal BP,  hasta el nivel 6, del Gravetiense final,  con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S.  araneus – S.  coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M.  arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A.  sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos,  y actualmente vive en regiones más  septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere  un clima templado. <br />Abstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the  level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S.  araneus – S.  coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M.  arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and  Apodemus gr. A.  sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and  nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="36017448"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36017448"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36017448; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36017448]").text(description); $(".js-view-count[data-work-id=36017448]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36017448; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36017448']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 36017448, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=36017448]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36017448,"title":"Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España)","translated_title":"","metadata":{"abstract":"Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259.\r\n\r\nResumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior, datado en 15.680 - 14.230 cal BP, hasta el nivel 6, del Gravetiense final, con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A. sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos, y actualmente vive en regiones más septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere un clima templado. \r\nAbstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and Apodemus gr. A. sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate. "},"translated_abstract":"Sesé. C. (2017): Los micromamíferos (Erinaceomorpha, Soricomorpha, Rodentia y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Coímbre (Asturias, España) In: La Cueva de Coímbre (Peñamellera Alta, Asturias). Ocupaciones humanas en el valle del Cares durante el Paleolítico superior (Álvarez-Alonso, D. \u0026 Yravedra Sainz de los Terreros, J., Dirs.). Investigación y Mecenazgo. Fundación María Cristina Masaveu Peterson. Asturias: 238-259.\r\n\r\nResumen: El material de micromamíferos del yacimiento del final del Pleistoceno Superior de la cueva de Coímbre procede de varios niveles, desde el nivel 1, del Magdaleniense superior, datado en 15.680 - 14.230 cal BP, hasta el nivel 6, del Gravetiense final, con una edad de 29.660 - 28.560 cal BP. La asociación de micromamíferos determinada en el yacimiento está compuesta por los siguientes taxones: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis y Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis y Apodemus gr. A. sylvaticus – A. flavicollis; y Lagomorpha: Oryctolagus cuniculus. La mayoría de estos taxones viven actualmente en la región donde se ubica el yacimiento, excepto Microtus oeconomus que se registra durante el Pleistoceno Superior en la mitad norte peninsular, desapareció de la Península Ibérica en tiempos históricos, y actualmente vive en regiones más septentrionales de Eurasia. Destaca en los subniveles 1a y 1b del Magdaleniense superior la abundancia relativa del conejo con respecto al resto de los micromamíferos, y en porcentajes muy similares, 21% y 23% respectivamente; lo que es bastante excepcional en la Región Cantábrica durante el Pleistoceno Superior, edad en la que el conejo fue muy escaso en dicha zona, tal como sucede actualmente, especialmente en Asturias. La asociación de micromamíferos de todos los niveles del yacimiento sugiere un clima templado. \r\nAbstract: The micromammal material of the Late Upper Pleistocene site of the Coímbre cave, comes from several levels, since the upper Magdalenian level 1, with an age of 15.680 - 14.230 cal BP, until the level 6, of the end of the Gravettian, with an age of 29.660 - 28.560 cal BP. The micromammal association of the Coímbre cave site is the following: Erinaceomorpha: Erinaceus europaeus; Soricomorpha: Sorex gr. S. araneus – S. coronatus, Talpa gr. T. europaea – T. occidentalis and Galemys pyrenaicus; Rodentia: Arvicola amphibius, Microtus gr. M. arvalis – M. agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis and Apodemus gr. A. sylvaticus – A. flavicollis; and Lagomorpha: Oryctolagus cuniculus. Most of these taxa live in the region at present days, except Microtus oeconomus that in the Upper Pleistocene is registered until the center of the Iberian Peninsula, but disappeared in historical times and nowadays is in northern euroasiatic regions. It is remarkable the abundance of the rabbit with respect to all the micromammals in the Upper Magdalenian levels 1a and 1b, with similar percentages, 21% y 23% respectively. This fact is very exceptional for the Cantabrian Region where the register of this taxa is very rare during the Upper Pleistocene, as it also happens nowadays, specially in Asturias. The micromammals association from all the levels of this site suggests a temperate climate. ","internal_url":"https://www.academia.edu/36017448/Los_micromam%C3%ADferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Co%C3%ADmbre_Asturias_Espa%C3%B1a_","translated_internal_url":"","created_at":"2018-02-26T02:52:39.138-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Los_micromamíferos_Erinaceomorpha_Soricomorpha_Rodentia_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Coímbre_Asturias_España_","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":77508,"name":"Late Pleistocene","url":"https://www.academia.edu/Documents/in/Late_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"},{"id":969133,"name":"North Spain","url":"https://www.academia.edu/Documents/in/North_Spain"},{"id":975805,"name":"Erinaceomorpha","url":"https://www.academia.edu/Documents/in/Erinaceomorpha"},{"id":975810,"name":"Soricomorpha","url":"https://www.academia.edu/Documents/in/Soricomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="35935814"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/35935814/Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Co%C3%ADmbre_Cave_Pe%C3%B1amellera_Alta_Asturias_"><img alt="Research paper thumbnail of Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias)." class="work-thumbnail" src="https://attachments.academia-assets.com/55817916/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/35935814/Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Co%C3%ADmbre_Cave_Pe%C3%B1amellera_Alta_Asturias_">Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias).</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.: Arrizabalaga...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.:  Arrizabalaga, A.; Jordá Pardo,  J. F.; Elorza, M.; Iriarte‐Chiapusso, M. J.; Sesé, C.; Uzquiano, P. (2017): Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias). Oxford Journal of Archaeology, 36 (4): 331-354.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="aba124b5276ac2cef122999235e80063" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":55817916,"asset_id":35935814,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/55817916/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="35935814"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="35935814"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 35935814; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=35935814]").text(description); $(".js-view-count[data-work-id=35935814]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 35935814; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='35935814']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 35935814, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "aba124b5276ac2cef122999235e80063" } } $('.js-work-strip[data-work-id=35935814]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":35935814,"title":"Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias).","translated_title":"","metadata":{"abstract":"Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.: Arrizabalaga, A.; Jordá Pardo, J. F.; Elorza, M.; Iriarte‐Chiapusso, M. J.; Sesé, C.; Uzquiano, P. (2017): Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias). Oxford Journal of Archaeology, 36 (4): 331-354."},"translated_abstract":"Yravedra, J.; Álvarez‐Alonso, D.; Estaca, V.; López‐Cisneros, P.; Andrés‐Chaín, M.: Arrizabalaga, A.; Jordá Pardo, J. F.; Elorza, M.; Iriarte‐Chiapusso, M. J.; Sesé, C.; Uzquiano, P. (2017): Selection and Exploitation of Macro-Vertebrate Resources during the Upper Palaeolithic in Northern Spain. New Evidence from Coímbre Cave (Peñamellera Alta, Asturias). Oxford Journal of Archaeology, 36 (4): 331-354.","internal_url":"https://www.academia.edu/35935814/Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Co%C3%ADmbre_Cave_Pe%C3%B1amellera_Alta_Asturias_","translated_internal_url":"","created_at":"2018-02-16T02:52:54.655-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":55817916,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/55817916/thumbnails/1.jpg","file_name":"Yravedra_et_al_2017_Selection_and_Explotation_of_MacroVertebrate_Resources_During_Upper_Palaeolithic_from_Coimbre.pdf","download_url":"https://www.academia.edu/attachments/55817916/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Selection_and_Exploitation_of_Macro_Vert.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/55817916/Yravedra_et_al_2017_Selection_and_Explotation_of_MacroVertebrate_Resources_During_Upper_Palaeolithic_from_Coimbre-libre.pdf?1518783040=\u0026response-content-disposition=attachment%3B+filename%3DSelection_and_Exploitation_of_Macro_Vert.pdf\u0026Expires=1732804964\u0026Signature=Z~9AoX12~IH5D1c~UP4E2IdjBe0l0oaXrXzHgRJqlaWf6RrtydXz7qYat0AmGb9lM3hlMS-61xG0M7dQXnbcD0mKS9RNPuy6HSRRrPj9XWdsOQhWvDEuvibtW-6zeRcOHcBJTuTx4JrNHZCKkc2XDosI2gwaPbBhEQbRdK7E5BjRg-A8WubCaZLROs9CxMQbb0KKbQLQofM04GagY4DrAJ3UyVJYaHlg4tsMv8YVKw9h6fEAEcd~8WOcM1ImCnyqy9XvLsGvWfIsJlfgRpkZQi~Pfd3cpa-cu3ByxMp~-yix5N1pfGz0mg~G40qOD80jHO3H8lElRmJaKp6yKelNlA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Selection_and_Exploitation_of_Macro_Vertebrate_Resources_during_the_Upper_Palaeolithic_in_Northern_Spain_New_Evidence_from_Coímbre_Cave_Peñamellera_Alta_Asturias_","translated_slug":"","page_count":24,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":55817916,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/55817916/thumbnails/1.jpg","file_name":"Yravedra_et_al_2017_Selection_and_Explotation_of_MacroVertebrate_Resources_During_Upper_Palaeolithic_from_Coimbre.pdf","download_url":"https://www.academia.edu/attachments/55817916/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Selection_and_Exploitation_of_Macro_Vert.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/55817916/Yravedra_et_al_2017_Selection_and_Explotation_of_MacroVertebrate_Resources_During_Upper_Palaeolithic_from_Coimbre-libre.pdf?1518783040=\u0026response-content-disposition=attachment%3B+filename%3DSelection_and_Exploitation_of_Macro_Vert.pdf\u0026Expires=1732804964\u0026Signature=Z~9AoX12~IH5D1c~UP4E2IdjBe0l0oaXrXzHgRJqlaWf6RrtydXz7qYat0AmGb9lM3hlMS-61xG0M7dQXnbcD0mKS9RNPuy6HSRRrPj9XWdsOQhWvDEuvibtW-6zeRcOHcBJTuTx4JrNHZCKkc2XDosI2gwaPbBhEQbRdK7E5BjRg-A8WubCaZLROs9CxMQbb0KKbQLQofM04GagY4DrAJ3UyVJYaHlg4tsMv8YVKw9h6fEAEcd~8WOcM1ImCnyqy9XvLsGvWfIsJlfgRpkZQi~Pfd3cpa-cu3ByxMp~-yix5N1pfGz0mg~G40qOD80jHO3H8lElRmJaKp6yKelNlA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1624,"name":"Zooarchaeology","url":"https://www.academia.edu/Documents/in/Zooarchaeology"},{"id":15780,"name":"Taphonomy","url":"https://www.academia.edu/Documents/in/Taphonomy"},{"id":29226,"name":"Archaeology of Hunting","url":"https://www.academia.edu/Documents/in/Archaeology_of_Hunting"},{"id":42252,"name":"Late Pleistocene to Early Holocene","url":"https://www.academia.edu/Documents/in/Late_Pleistocene_to_Early_Holocene"},{"id":788677,"name":"Rabbits","url":"https://www.academia.edu/Documents/in/Rabbits"},{"id":2893336,"name":"Macromammals","url":"https://www.academia.edu/Documents/in/Macromammals"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="35671362"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_"><img alt="Research paper thumbnail of Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria)." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_">Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria).</a></div><div class="wp-workCard_item"><span>C. Sesé (2017). Estudios Geológicos 73(2): e072.</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. <br />Palabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.<br />ABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. <br />Keywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="35671362"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="35671362"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 35671362; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=35671362]").text(description); $(".js-view-count[data-work-id=35671362]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 35671362; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='35671362']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 35671362, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=35671362]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":35671362,"title":"Los micromamíferos (Eulipotyphla, Chiroptera, Rodentia y Lagomorpha) del yacimiento del Pleistoceno Superior de la cueva de El Castillo (Cantabria).","translated_title":"","metadata":{"doi":"10.3989/ egeol.41589.471.","abstract":"RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. \nPalabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.\nABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. \nKeywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.\n","location":"http://hdl.handle.net/10261/159027","more_info":"http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/966","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"C. Sesé (2017). Estudios Geológicos 73(2): e072."},"translated_abstract":"RESUMEN: El material de micromamíferos del yacimiento del Pleistoceno Superior de la cueva de El Castillo, objeto de estudio detallado en este trabajo, proviene de los niveles auriñacienses 18b y 18c (datados en 40.000-45.000 BP), nivel 19, y niveles musterienses 20b, 20c, 20d, 20e (datados en 41.000-49.000 BP), 21a y 21b. La asociación de micromamíferos es la siguiente: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis y Lepus sp. La mayoría de estas especies están presentes en la fauna actual de Cantabria, excepto Pliomys lenki que se extinguió en el último tercio del Pleistoceno Superior, y Microtus oeconomus, que persistió en la península ibérica durante el Holoceno bien avanzado hasta su desaparición en tiempos históricos, y que actualmente está en regiones euroasiáticas más septentrionales. Hay una gran continuidad de la gran mayoría de los taxones en todos los niveles. La fauna en su conjunto parece indicar un medio predominantemente abierto, por lo general de praderas húmedas (y en mucha menor medida praderas secas) con una buena cobertura vegetal a nivel del suelo, en el que habría también algunas zonas arboladas o boscosas, y algún curso de agua. Los indicadores termófilos son escasos y poco abundantes, lo que podría indicar que el clima podría ser algo menos templado que en otros periodos del Pleistoceno Superior y quizás también que actualmente en la zona. \nPalabras clave: Micromamíferos; Pleistoceno Superior; Región Cantábrica; Tafonomía; Paleoecología; Paleoclimatología.\nABSTRACT: The micromammals remains from the Late Pleistocene site of the cave of El Castillo studied here in detail, came from the Aurignacian levels 18b and 18c (dated in 40.000-45.000 BP), level 19, and the Musterian levels 20b, 20c, 20d, 20e (dated in 41.000-49.000 BP), 21a and 21b. The micromammal association is the following: Erinaceus europaeus, Crocidura russula, Sorex coronatus, Sorex minutus, Neomys fodiens, Talpa europaea, Galemys pyrenaicus, cf. Miniopterus schreibersii, Chiroptera indet., Pliomys lenki, Microtus arvalis - Microtus agrestis, Microtus lusitanicus, Microtus oeconomus, Chionomys nivalis, Arvicola terrestris, Apodemus sylvaticus - Apodemus flavicollis and Lepus sp. Most of these species are in the present fauna of Cantabria, except Pliomys lenki that got extinct in the last third of the Upper Pleistocene, and Microtus oeconomus that disappeared from the Iberian Peninsula during the Holocene, in historical times, and is nowadays present in northern Euroasiatic regions. There is a great continuity of most of the taxa in all the levels. The faunal association seems to indicate a mainly open environment, in general with wet meadows (and few dry meadows), with good vegetation cover in the soil, with perhaps also some tree-covered areas, and some watercourses. The thermophiles indicators are very scarce, which could indicate that the climate could be a lesser temperate than other Upper Pleistocene periods and the present-day climate in the area. \nKeywords: Micromammals; Late Pleistocene; Cantabrian Region; Taphonomy; Paleoecology; Paleoclimatology.\n","internal_url":"https://www.academia.edu/35671362/Los_micromam%C3%ADferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_","translated_internal_url":"","created_at":"2018-01-15T05:36:10.569-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Los_micromamíferos_Eulipotyphla_Chiroptera_Rodentia_y_Lagomorpha_del_yacimiento_del_Pleistoceno_Superior_de_la_cueva_de_El_Castillo_Cantabria_","translated_slug":"","page_count":null,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[{"id":292,"name":"Palaeoclimatology","url":"https://www.academia.edu/Documents/in/Palaeoclimatology"},{"id":17472,"name":"Palaeoecology","url":"https://www.academia.edu/Documents/in/Palaeoecology"},{"id":53800,"name":"Pleistocene mammals","url":"https://www.academia.edu/Documents/in/Pleistocene_mammals"},{"id":87213,"name":"Vertebrate taphonomy","url":"https://www.academia.edu/Documents/in/Vertebrate_taphonomy"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"}],"urls":[{"id":8443634,"url":"http://hdl.handle.net/10261/159027"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="34555405"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A"><img alt="Research paper thumbnail of New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. & Pérez-González, A." class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A">New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. & Pérez-González, A.</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews </span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape <br />and climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher <br />than at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="34555405"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="34555405"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 34555405; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=34555405]").text(description); $(".js-view-count[data-work-id=34555405]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 34555405; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='34555405']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 34555405, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=34555405]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":34555405,"title":"New palaeoenvironmental and palaeoclimatic reconstructions for the Middle Palaeolithic site of Cuesta de la Bajada (Teruel, eastern Spain) inferred from the amphibian and squamate reptile assemblages. Blain, H.-A.; Ruiz Zapata, M. B.; Gil García, M. J.; Sesé, C.; Santonja, M. \u0026 Pérez-González, A.","translated_title":"","metadata":{"volume":"173","abstract":"In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape\r\nand climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher\r\nthan at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.\r\n","page_numbers":"78-91","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Quaternary Science Reviews "},"translated_abstract":"In the eastern Iberian Peninsula, the archaeological site of Cuesta de la Bajada (Teruel, Spain) has produced some of the earliest evidence of Middle Paleolithic stone tool traditions together with evidence of equid and cervid carcasses defleshed by hominins. Based on the numerical age of 317-240 ka derived from OSL, ESR and AAR dating methods for the lower part of the Cuesta de la Bajada sedimentological sequence (level CB3), as well as the biochronological inferences for the small and large mammal associations, the site can be attributed toMarine Isotope Stage (MIS) 8 or the end of MIS 9. As amphibians and reptiles have precise environmental and climatic requirements and do not differ at species level from the extant herpetofauna of the Iberian Peninsula, they can contribute to the reconstruction of the landscape\r\nand climate. In this paper, the fossil amphibians and squamate reptiles from Cuesta de la Bajada are studied for the first time. The mutual ecogeographic range and habitat weighting methods were applied to the herpetofaunal assemblages to estimate quantitative data for the landscape and climate reconstructions. The climate is shown to have been colder and wetter than today in the interior of eastern Spain, with mean annual temperature up to 2.5º C lower and mean annual precipitation slightly higher\r\nthan at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation from late autumn to spring (i.e. from October to May), and more or less similar precipitation to today during the summer months (July and August). This suggests there was stronger rainfall seasonality between winter and summer than currently occurs. The paleoenvironmental reconstruction based on the herpetofaunal assemblage depicts a poorly forested (15-20%) patchy landscape with a large representation of dry meadows and scrubland habitats together with well-evidenced aquatic habitats. These reconstructions are consistent with other proxies recovered at Cuesta de la Bajada (pollen, small and large mammals) as well as other European MIS 8-9 paleoclimatic records.We can thus correlate levels CB2 and CB3 with the later part of MIS 8 (265-257 ka) or with a humid fluctuation within the MIS 9b (303-290 ka). It is also possible to provide a new description of the environmental and climatic conditions that occurred in inner Spain during a cold period of the late Middle Pleistocene.\r\n","internal_url":"https://www.academia.edu/34555405/New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_Garc%C3%ADa_M_J_Ses%C3%A9_C_Santonja_M_and_P%C3%A9rez_Gonz%C3%A1lez_A","translated_internal_url":"","created_at":"2017-09-13T01:04:52.312-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"New_palaeoenvironmental_and_palaeoclimatic_reconstructions_for_the_Middle_Palaeolithic_site_of_Cuesta_de_la_Bajada_Teruel_eastern_Spain_inferred_from_the_amphibian_and_squamate_reptile_assemblages_Blain_H_A_Ruiz_Zapata_M_B_Gil_García_M_J_Sesé_C_Santonja_M_and_Pérez_González_A","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="34015262"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living"><img alt="Research paper thumbnail of The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living." class="work-thumbnail" src="https://attachments.academia-assets.com/53959609/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living">The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living.</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/EduardoGarc%C3%ADaS%C3%A1nchez">Eduardo García Sánchez</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/JFJorda">Jesús F. Jordá</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/Mar%C3%ADadeAndr%C3%A9sHerrero">María de Andrés Herrero</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/MariaJoseIriarteChiapusso">Maria-Jose Iriarte-Chiapusso</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/%C3%93scarFuente">Óscar Fuente Fernández</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/PabloLopezCisneros">Pablo Lopez Cisneros</a></span></div><div class="wp-workCard_item"><span>Conference: Hugo Obermaier-Gesellschaft für Erforschung des Eizeitalters und der Steinzeit e V. 57th Annual Meeting in Heidenheim, 2015, Volume: 57th Annual Meeting in Heidenheim. Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).<br /><br />Coímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.<br />Moreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.<br />This work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44f29afe83ef5308ea9f237dd6b254f1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53959609,"asset_id":34015262,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53959609/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="34015262"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="34015262"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 34015262; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=34015262]").text(description); $(".js-view-count[data-work-id=34015262]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 34015262; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='34015262']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 34015262, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44f29afe83ef5308ea9f237dd6b254f1" } } $('.js-work-strip[data-work-id=34015262]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":34015262,"title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living.","translated_title":"","metadata":{"volume":"57","abstract":"Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).\n\nCoímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.\nMoreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.\nThis work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.\n","page_numbers":"15-16","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Conference: Hugo Obermaier-Gesellschaft für Erforschung des Eizeitalters und der Steinzeit e V. 57th Annual Meeting in Heidenheim, 2015, Volume: 57th Annual Meeting in Heidenheim. Hugo Obermaier Society for Quaternary Research and Archaeology of the Stone Age"},"translated_abstract":"Coímbre cave (135 meters asl) is located on the southwestern slope of Mount Pendendo (532 m), in the small valley of Besnes river, tributary of Cares river, in a medium-higher mountain are in the central-western Cantabria –northern Iberian Peninsula- (Álvarez-Alonso et al., 2009; 2013b). The landscape in the surroundings of the cave –situated in an interior valley but near to the current coast in a low altitude- can be described as a mountainous environment where valleys, small hills and steep mountains with high slopes are integrated, which confer a relative variety of ecosystems to this area. Coímbre contains an important archaeological site divided in two different areas. B Area, is the farthest from the entrance, and is the place where took place the excavations carried out to date, between 2008 and 2012 (Álvarez-Alonso et al., 2009, 2011, 2013a, 2013b).\n\nCoímbre B shows a complete and very interesting Magdalenian sequence (with Lower, Middle and Upper Magdalenian levels), and a gravettian level, that converts this cave in one of the biggest habitat areas in western Cantabria. Its rich set of bone industries, mobiliar art and ornaments, provide key information that shows the connections between this area, the Pyrenees and the south-west of Aquitaine.\nMoreover, Coímbre cave presents an interesting set of Magdalenian engravings, located in different places of the cavity, both in open and accessible areas, and in narrower and inaccessible places, which clearly define two different symbolic spaces. All this artistic expressions belong to the Magdalenian, and it is possible to establish a division between a set of engravings framed in the first stages of this period (the most abundant and remote); and a more limited set of engravings, in which stand out a block with a engraving of a bison with a deep trace of more than one meter long, that belongs to the recent Magdalenian.\nThis work presents the preliminary results of the analysis of Magdalenian occupations in Coímbre, after the end of the excavations in B Area, and the study of its rock art, shaping this site as one of the most important places of Magdalenian human activities in western Cantabria.\n","internal_url":"https://www.academia.edu/34015262/The_Upper_Palaeolithic_record_of_Co%C3%ADmbre_Cave_Asturias_northern_Spain_A_symbolic_place_a_place_for_living","translated_internal_url":"","created_at":"2017-07-24T02:37:45.919-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2497886,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":29838809,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":352134,"co_author_invite_id":null,"email":"d***z@ucm.es","affiliation":"Universidad Complutense de Madrid","display_order":1,"name":"David Álvarez-Alonso","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838811,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":264753,"co_author_invite_id":null,"email":"a***a@ehu.es","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":3,"name":"Alvaro Arrizabalaga","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838812,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":621849,"co_author_invite_id":null,"email":"j***a@geo.uned.es","affiliation":"Universidad Nacional de Educación a Distancia","display_order":4,"name":"Jesús F. Jordá","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838813,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":722671,"co_author_invite_id":null,"email":"e***k@usal.es","affiliation":"University of Salamanca","display_order":5,"name":"Esteban Álvarez-Fernández","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838814,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":426160,"co_author_invite_id":null,"email":"m***s@gmail.com","affiliation":"Universidad Complutense de Madrid","display_order":6,"name":"María de Andrés Herrero","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838815,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":467560,"co_author_invite_id":null,"email":"j***o@terra.es","affiliation":"Universidad Nacional de Educación a Distancia","display_order":7,"name":"Julio Rojo","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838816,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":372428,"co_author_invite_id":null,"email":"m***e@ehu.es","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":8,"name":"Maria-Jose Iriarte-Chiapusso","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838817,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":4287495,"co_author_invite_id":null,"email":"c***e@mncn.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":9,"name":"Carmen Sesé","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838818,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":1256507,"co_author_invite_id":null,"email":"p***o@hotmail.com","display_order":10,"name":"Paloma Uzquiano Ollero","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838819,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":2788011,"co_author_invite_id":null,"email":"m***a@hotmail.com","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":11,"name":"Martin Arriolabengoa","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838820,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":490382,"co_author_invite_id":null,"email":"i***i@hotmail.com","affiliation":"University of the Basque Country, Euskal Herriko Unibertsitatea","display_order":12,"name":"Irantzu Elorrieta-Baigorri","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838821,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":2888704,"co_author_invite_id":null,"email":"h***o@gmail.com","affiliation":"Universidad Nacional de Educación a Distancia","display_order":13,"name":"Óscar Fuente Fernández","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838822,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":383489,"co_author_invite_id":null,"email":"p***8@hotmail.com","affiliation":"Universidad Nacional de Educación a Distancia","display_order":14,"name":"Pablo Lopez Cisneros","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838823,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":36200417,"co_author_invite_id":null,"email":"a***o@cenieh.es","affiliation":"CENIEH","display_order":15,"name":"Andoni Tarriño","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). A symbolic place, a place for living."},{"id":29838824,"work_id":34015262,"tagging_user_id":2497886,"tagged_user_id":33323886,"co_author_invite_id":null,"email":"g***o@bio.ucm.es","display_order":16,"name":"Gonzalo Trancho","title":"The Upper Palaeolithic record of Coímbre Cave (Asturias, northern Spain). 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="33992028"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33992028/Subsistencia_movilidad_y_adaptaci%C3%B3n_al_medio_de_los_cazadores_recolectores_gravetienses_en_el_sector_occidental_de_la_regi%C3%B3n_cant%C3%A1brica_la_cueva_de_Co%C3%ADmbre_Asturias_"><img alt="Research paper thumbnail of Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)" class="work-thumbnail" src="https://attachments.academia-assets.com/53942206/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33992028/Subsistencia_movilidad_y_adaptaci%C3%B3n_al_medio_de_los_cazadores_recolectores_gravetienses_en_el_sector_occidental_de_la_regi%C3%B3n_cant%C3%A1brica_la_cueva_de_Co%C3%ADmbre_Asturias_">Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/David%C3%81lvarezAlonso">David Álvarez-Alonso</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uned.academia.edu/JFJorda">Jesús F. Jordá</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/AlvaroArrizabalaga">Alvaro Arrizabalaga</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PalomaUzquianoOllero">Paloma Uzquiano Ollero</a></span></div><div class="wp-workCard_item"><span>Trabajos de Prehistoria</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Coímbre is one of the few Gravettian sites the middle- western part of Cantabria. It is one of th...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Coímbre is one of the few Gravettian sites the middle-<br />western part of Cantabria. It is one of the most interesting<br />sites for the analysis of the Gravettian close to the boundary of its western expansion in Europe. Zooarchaeological and taphonomical study of the faunal and archaeobotanical remains and the lithic industry and the interpretation of its AMS-dated archaeological and<br />sedimentological sequence make it possible to analyse<br />the Gravettian settlement in Coímbre cave using a territorial<br />perspective. The subsistence strategies developed<br />in Coímbre have been determinant in the interpretation<br />of its occupation patterns. Thus, we can assess the existence<br />of the specific mobility and subsistence patterns<br />developed by these human groups in the framework of<br />Cantabria. This pattern shows an ephemeral logistic and<br />punctual occupation of the cave, probably linked to an<br />eastern-western corridor. This is one of the paper’s most<br />interesting contributions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6ada514d59db5f37f8f7a85fb68cb623" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53942206,"asset_id":33992028,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53942206/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33992028"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33992028"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33992028; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33992028]").text(description); $(".js-view-count[data-work-id=33992028]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33992028; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33992028']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33992028, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "6ada514d59db5f37f8f7a85fb68cb623" } } $('.js-work-strip[data-work-id=33992028]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33992028,"title":"Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)","translated_title":"","metadata":{"issue":"1","volume":"74","abstract":"Coímbre is one of the few Gravettian sites the middle-\nwestern part of Cantabria. It is one of the most interesting\nsites for the analysis of the Gravettian close to the boundary of its western expansion in Europe. Zooarchaeological and taphonomical study of the faunal and archaeobotanical remains and the lithic industry and the interpretation of its AMS-dated archaeological and\nsedimentological sequence make it possible to analyse\nthe Gravettian settlement in Coímbre cave using a territorial\nperspective. The subsistence strategies developed\nin Coímbre have been determinant in the interpretation\nof its occupation patterns. Thus, we can assess the existence\nof the specific mobility and subsistence patterns\ndeveloped by these human groups in the framework of\nCantabria. This pattern shows an ephemeral logistic and\npunctual occupation of the cave, probably linked to an\neastern-western corridor. This is one of the paper’s most\ninteresting contributions.","page_numbers":"47-67","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Trabajos de Prehistoria"},"translated_abstract":"Coímbre is one of the few Gravettian sites the middle-\nwestern part of Cantabria. It is one of the most interesting\nsites for the analysis of the Gravettian close to the boundary of its western expansion in Europe. Zooarchaeological and taphonomical study of the faunal and archaeobotanical remains and the lithic industry and the interpretation of its AMS-dated archaeological and\nsedimentological sequence make it possible to analyse\nthe Gravettian settlement in Coímbre cave using a territorial\nperspective. The subsistence strategies developed\nin Coímbre have been determinant in the interpretation\nof its occupation patterns. Thus, we can assess the existence\nof the specific mobility and subsistence patterns\ndeveloped by these human groups in the framework of\nCantabria. This pattern shows an ephemeral logistic and\npunctual occupation of the cave, probably linked to an\neastern-western corridor. This is one of the paper’s most\ninteresting contributions.","internal_url":"https://www.academia.edu/33992028/Subsistencia_movilidad_y_adaptaci%C3%B3n_al_medio_de_los_cazadores_recolectores_gravetienses_en_el_sector_occidental_de_la_regi%C3%B3n_cant%C3%A1brica_la_cueva_de_Co%C3%ADmbre_Asturias_","translated_internal_url":"","created_at":"2017-07-21T23:16:43.554-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":352134,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":29815537,"work_id":33992028,"tagging_user_id":352134,"tagged_user_id":6396581,"co_author_invite_id":null,"email":"j***a@gmail.com","affiliation":"Universidad Complutense de Madrid","display_order":1,"name":"jose yravedra","title":"Subsistencia, movilidad y adaptación al medio de los cazadores-recolectores gravetienses en el sector occidental de la región cantábrica: la cueva de Coímbre (Asturias)"},{"id":29815538,"work_id":33992028,"tagging_user_id":352134,"tagged_user_id":621849,"co_author_invite_id":null,"email":"j***a@geo.uned.es","affiliation":"Universidad Nacional de Educación a Distancia","display_order":2,"name":"Jesús F. 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class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_"><img alt="Research paper thumbnail of Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/53856315/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_">Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)</a></div><div class="wp-workCard_item"><span>Spanish Journal of Paleontology</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. & Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burg...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. &  Morales, J. (2017).  Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.<br />Abstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.<br />Keywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.<br />Resumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.<br />Palabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7129c09a041b1d9d97c677b57ad914c7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53856315,"asset_id":33880579,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33880579"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33880579"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33880579; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33880579]").text(description); $(".js-view-count[data-work-id=33880579]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33880579; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33880579']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33880579, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "7129c09a041b1d9d97c677b57ad914c7" } } $('.js-work-strip[data-work-id=33880579]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33880579,"title":"Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)","translated_title":"","metadata":{"issue":"1","volume":"32","abstract":"Sesé, C. \u0026 Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.\nAbstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.\nKeywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.\nResumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.\nPalabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.\n\n","page_numbers":"63-78","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Spanish Journal of Paleontology"},"translated_abstract":"Sesé, C. \u0026 Morales, J. (2017). Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain). Spanish Journal of Palaeontology, 32 (1), 63-78.\nAbstract: The Cuesta del Rey mammal sites located on the NE border of the Duero Basin are of great importance with regard to understand the general biostratigraphy of the basin, because Miocene mammal sites are extremely scarce in this area in comparison with the central part of the basin. The mammals identifi ed in Cuesta del Rey-1 are: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. and Democricetodon sp. The Cuesta del Rey-1 rodent assemblage is characteristic of the end of the upper Aragonian (MN 7/8, end of the middle Miocene), equivalent to the local subzone G3 of the G zone. The presence of the genera Heteroxerus and Armantomys, and the predominance of Megacricetodon (with 80% of the total percentage of the minimum number of individuals of the micromammals) suggested an open savannah or steppe palaeoenvironment. The mammals identifi ed in Cuesta del Rey-3 are: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Dorcatherium sp. and Listriodon cf. splendens. Dorcatherium sp. represents the fi rst appearance of the Tragulidae family in the Duero Basin, suggesting the existence of permanent watercourses.\nKeywords: Mammals, middle Miocene, upper Aragonian, Duero Basin, Cuesta del Rey sites.\nResumen: Los yacimientos con mamíferos de Cuesta del Rey, situados en el borde NE de la cuenca del Duero, tienen una gran importancia para el conocimiento general de la biostratigrafía de la cuenca debido a la extrema escasez de yacimientos miocenos con mamíferos en comparación con las partes centrales de la misma. Los mamíferos identificados en Cuesta del Rey-1 son: Eulipotyphla: cf. Miosorex sp.; Rodentia: Heteroxerus sp., Armantomys cf. tricristatus, Megacricetodon ibericus, Megacricetodon minor-Megacricetodon debruijni, Hispanomys sp. y Democricetodon sp. Esta asociación, principalmente por la composición de los roedores, es característica del final del Aragoniense superior (final del Mioceno medio), de la subzona G3 de la zona G, unidades MN 7/8. La presencia de los géneros Heteroxerus, Armantomys, y el predominio de Megacricetodon (que constituye el 80 % del porcentaje total del número mínimo de individuos de los micromamíferos), sugieren un ambiente abierto de tipo sabana o estepa. Los mamíferos identificados en Cuesta del Rey-3 son: Rodentia: Megacricetodon cf. ibericus; Artiodactyla: Listriodon cf. splendens and Dorcatherium sp. El tragúlido Dorcatherium sp. representa la primera aparición de la familia en la cuenca del Duero, y sugiere la existencia de cursos de agua permanentes.\nPalabras clave: Mamíferos, Mioceno medio, Aragoniense superior, Cuenca del Duero, Yacimientos de Cuesta del Rey.\n\n","internal_url":"https://www.academia.edu/33880579/Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_","translated_internal_url":"","created_at":"2017-07-14T02:26:55.903-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":29717169,"work_id":33880579,"tagging_user_id":4287495,"tagged_user_id":2992261,"co_author_invite_id":null,"email":"j***1@gmail.com","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":1,"name":"Jorge Morales","title":"Late Aragonian mammal sites of Cuesta del Rey (Duero Basin, Burgos, Spain)"}],"downloadable_attachments":[{"id":53856315,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53856315/thumbnails/1.jpg","file_name":"Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos.pdf","download_url":"https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Late_Aragonian_mammal_sites_of_Cuesta_de.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53856315/Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos-libre.pdf?1500024541=\u0026response-content-disposition=attachment%3B+filename%3DLate_Aragonian_mammal_sites_of_Cuesta_de.pdf\u0026Expires=1732804965\u0026Signature=Y~S59qtkugkHksSb~~gPgfQpWmkYoXUzbq06S7e-KTG3FNdSMKH98kF8Rd4g1hXKkerYB8cpM9wnYFuD9zW9LWAajx5QSzl8y5YNjrtqNUheCG4inIUq6Eg38ca6OIGP-6TS1kqwpLS5QeIfBHC8Amg8umUwDyCqQPFST~BuTYSSYURyJ8mcKeStVSenLSffelLR~lnIzJUXp~pC0ub14OYmwiyeCSaAasJPLrnDiw2pXAmXVzaHRqaSO9PZnVHNQZ8hK9OPJEUlY~dZqRe5YX0kyGe9xx1zlnaeiLMDR4H1MVmyGfDkXV4pUtw9lY-FUpEBGxsMXxFwJTEmNmeEQA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_Basin_Burgos_Spain_","translated_slug":"","page_count":16,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":53856315,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/53856315/thumbnails/1.jpg","file_name":"Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos.pdf","download_url":"https://www.academia.edu/attachments/53856315/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Late_Aragonian_mammal_sites_of_Cuesta_de.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/53856315/Sese_y_Morales_2017_Late_Aragonian_mammal_sites_of_Cuesta_del_Rey_Duero_basin_Burgos-libre.pdf?1500024541=\u0026response-content-disposition=attachment%3B+filename%3DLate_Aragonian_mammal_sites_of_Cuesta_de.pdf\u0026Expires=1732804965\u0026Signature=Y~S59qtkugkHksSb~~gPgfQpWmkYoXUzbq06S7e-KTG3FNdSMKH98kF8Rd4g1hXKkerYB8cpM9wnYFuD9zW9LWAajx5QSzl8y5YNjrtqNUheCG4inIUq6Eg38ca6OIGP-6TS1kqwpLS5QeIfBHC8Amg8umUwDyCqQPFST~BuTYSSYURyJ8mcKeStVSenLSffelLR~lnIzJUXp~pC0ub14OYmwiyeCSaAasJPLrnDiw2pXAmXVzaHRqaSO9PZnVHNQZ8hK9OPJEUlY~dZqRe5YX0kyGe9xx1zlnaeiLMDR4H1MVmyGfDkXV4pUtw9lY-FUpEBGxsMXxFwJTEmNmeEQA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="33272836"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33272836/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_"><img alt="Research paper thumbnail of Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/53341269/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33272836/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/LydiaZapata">Lydia Zapata</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/M%C3%B3nicaRuizAlonso">Mónica Ruiz-Alonso</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula cur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440e21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770e12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural<br />resources may have been used. The faunal remains represented at this site reflect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality fix the occupation of levels IeIII from the spring to the autumn. Certain types of wood were collected for use as firewood. Other elements found in the record (personal ornaments, mobiliary art and raw materials) provide evidence that the people that occupied the site moved over a more extensive territory.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d74023c6760eecc9d5b89cefe9de4589" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53341269,"asset_id":33272836,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53341269/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33272836"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33272836"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33272836; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33272836]").text(description); $(".js-view-count[data-work-id=33272836]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33272836; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33272836']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33272836, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d74023c6760eecc9d5b89cefe9de4589" } } $('.js-work-strip[data-work-id=33272836]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33272836,"title":"Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)","translated_title":"","metadata":{"abstract":"The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440e21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770e12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural\nresources may have been used. The faunal remains represented at this site reflect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality fix the occupation of levels IeIII from the spring to the autumn. Certain types of wood were collected for use as firewood. Other elements found in the record (personal ornaments, mobiliary art and raw materials) provide evidence that the people that occupied the site moved over a more extensive territory.","more_info":"C. Cacho, J.A. Martos, J. Jordá-Pardo, J. Yravedra, C. Sesé, L. Zapata, B. Avezuela, J. Valdivia, M. Ruiz, L. Marquer, I. Martín-Lerma, J.M. Tejero","journal_name":"Quaternary International, 272-273 (2012), 42-54.","publication_date":{"day":null,"month":null,"year":2012,"errors":{}}},"translated_abstract":"The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440e21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770e12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural\nresources may have been used. The faunal remains represented at this site reflect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality fix the occupation of levels IeIII from the spring to the autumn. 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href="https://www.academia.edu/32637472/El_aprovechamiento_de_lagomorfos_en_el_Paleol%C3%ADtico_superior_cant%C3%A1brico_Nuevas_perspectivas_desde_la_cueva_de_Co%C3%ADmbre_Asturias_"><img alt="Research paper thumbnail of El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias)." class="work-thumbnail" src="https://attachments.academia-assets.com/52807453/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32637472/El_aprovechamiento_de_lagomorfos_en_el_Paleol%C3%ADtico_superior_cant%C3%A1brico_Nuevas_perspectivas_desde_la_cueva_de_Co%C3%ADmbre_Asturias_">El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias).</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. & Sesé, C. 2017: El aprovecha...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. & Sesé, C. 2017: El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias). Arqueobiología durante el Greenland Stadial 2 en la Región Cantábrica (CA. 22000-15000 CAL BP). Salamanca 20-21 de abril 2017. Universidad de Salamanca: p. 5<br /><br />Resumen: En la mayor parte de los yacimientos del norte peninsular, estos animales son escasos o excepcionales y prácticamente sus restos son testimoniales. Sin embargo, en los niveles del Magdaleniense superior de la zona B de la cueva de Coímbre (Peñamellera Alta,<br />Asturias) ha aparecido una importante concentración de restos de conejo que merecen la pena<br />ser analizados en cierto detalle. Con este estudio, presentamos los resultados del análisis tafonómico de los conejos del yacimiento. Desde una perspectiva taxonómica los lagomorfos<br />suponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las<br />especies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,<br />otros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia<br />tafonómica compleja con individuos aportados por el ser humano frente a otros con aportes<br />biológicos no humanos. En todo caso las evidencias registradas en la cueva de Coímbre deben<br />ser consideradas y tenidas en cuenta a la hora de reflexionar por qué en los otros contextos<br />cantábricos son tan escasos estos animales.<br /><br />Palabras clave: Tafonomía, Lagomorfos, Paleolítico superior, Pleistoceno superior, Yacimiento de la cueva de Coímbre, Asturias, Región Cantábrica, Norte de España.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="094c8c6b4f025401437eb78ba683f651" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52807453,"asset_id":32637472,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52807453/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32637472"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32637472"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32637472; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32637472]").text(description); $(".js-view-count[data-work-id=32637472]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32637472; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32637472']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32637472, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "094c8c6b4f025401437eb78ba683f651" } } $('.js-work-strip[data-work-id=32637472]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32637472,"title":"El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. 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Desde una perspectiva taxonómica los lagomorfos\nsuponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las\nespecies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,\notros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia\ntafonómica compleja con individuos aportados por el ser humano frente a otros con aportes\nbiológicos no humanos. En todo caso las evidencias registradas en la cueva de Coímbre deben\nser consideradas y tenidas en cuenta a la hora de reflexionar por qué en los otros contextos\ncantábricos son tan escasos estos animales.\n\nPalabras clave: Tafonomía, Lagomorfos, Paleolítico superior, Pleistoceno superior, Yacimiento de la cueva de Coímbre, Asturias, Región Cantábrica, Norte de España.\n\n\n"},"translated_abstract":"Yravedra Sainz de los Terreros, J.; Herranz, D.; Álvarez-Alonso, D. \u0026 Sesé, C. 2017: El aprovechamiento de lagomorfos en el Paleolítico superior cantábrico. Nuevas perspectivas desde la cueva de Coímbre (Asturias). Arqueobiología durante el Greenland Stadial 2 en la Región Cantábrica (CA. 22000-15000 CAL BP). Salamanca 20-21 de abril 2017. Universidad de Salamanca: p. 5\n\nResumen: En la mayor parte de los yacimientos del norte peninsular, estos animales son escasos o excepcionales y prácticamente sus restos son testimoniales. Sin embargo, en los niveles del Magdaleniense superior de la zona B de la cueva de Coímbre (Peñamellera Alta,\nAsturias) ha aparecido una importante concentración de restos de conejo que merecen la pena\nser analizados en cierto detalle. Con este estudio, presentamos los resultados del análisis tafonómico de los conejos del yacimiento. Desde una perspectiva taxonómica los lagomorfos\nsuponen casi el 10% de la representación faunística de los niveles superiores, siendo una de las\nespecies más frecuentes. Tafonómicamente, hemos podido observar que los conejos estuvieron expuestos a varios fenómenos, así hay huesos con alteraciones generadas por carnívoros, y dientes que presentan alteraciones químicas producidas por aves. Por otra parte,\notros restos tienen alteraciones de carácter antrópico como marcas de corte, las cuales las relacionan con el comportamiento humano. En consecuencia, nos encontramos una historia\ntafonómica compleja con individuos aportados por el ser humano frente a otros con aportes\nbiológicos no humanos. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474865"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662687/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf">Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016.  Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas  (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. <br /><br />Resumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres<br />yacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment<br />and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="90c8ea538ad036e819e08e791ad2c15b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662687,"asset_id":32474865,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474865"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474865"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474865; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474865]").text(description); $(".js-view-count[data-work-id=32474865]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474865; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474865']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474865, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "90c8ea538ad036e819e08e791ad2c15b" } } $('.js-work-strip[data-work-id=32474865]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474865,"title":"Interpretacion paleoambiental de los micromamiferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España) .pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. \n\nResumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres\nyacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.\n\nAbstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment\nand a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Interpretación paleoambiental de los micromamíferos de los yacimientos del final del Pleistoceno superior de la cueva de Cualventi, cueva de El Linar y cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 287-319. \n\nResumen: Se realiza la síntesis de los micromamíferos de los yacimientos de la cueva de Cualventi (con el nivel E datado entre 14.580 y 15.950 BP), cueva de El Linar (con niveles datados entre 14.000 y 19.700 BP) y cueva de Las Aguas (con niveles datados entre 14.440 y 17.630 BP) fundamentalmente desde el punto de vista paleoambiental. Las asociaciones faunísticas de los tres yacimientos tienen la mayoría de los taxones comunes: el género Apodemus (en el yacimiento de la cueva de Cualventi se ha identificado la especie Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determinado como Neomys cf. fodiens en la cueva de El Linar), Talpa europaea, Erinaceus europaeus y cf. Lepus sp., entre los que se encuentran algunos de los que suelen ser los más abundantes. Los taxones que faltan en alguno de los tres yacimientos o solo están en uno de ellos: Glis glis (se registra en la cueva de Cualventi pero sin contexto estratigráfico seguro), Clethrionomys glareolus (en la cueva de El Linar), Sorex minutus (en la cueva de Cualventi y la cueva de El Linar), Crocidura russula (en la cueva de Cualventi y la cueva de Las Aguas) y Miniopterus schreibersii (en la cueva de Las Aguas) son, por el contrario, muy escasos en los niveles de los yacimientos en los que aparecen. La mayoría de los taxones que se registran en los tres yacimientos presentan una gran continuidad en los distintos niveles y sondeos. Es decir que no hay un cambio faunístico apreciable que refleje a su vez ningún cambio paleoambiental significativo entre los distintos niveles de los tres\nyacimientos. Solo dos de los taxones que se registran en estos yacimientos no están actualmente presentes en la fauna de la región cantábrica: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Del estudio de las asociaciones de micromamíferos de los tres yacimientos se deducen unas condiciones paleoambientales de un medio abierto húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Cualventi, yacimiento de cueva de El Linar, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, interpretación paleoambiental, paleoclimatología, Cantabria, norte de España.\n\nAbstract: It is made here a synthesis of the micromammals from the sites of the cave of Cualventi (with the level E dated between 14.580 and 15.950 BP), cave of El Linar (with some levels dated between 14.000 and 19.700 BP) and cave of Las Aguas (with some levels dated between 14.440 and 17.630 BP) mainly from the paleoenvironmental point of view. The faunal assemblages of the three sites have in common the majority of the taxa: the genus Apodemus (in the Cualventi cave site has been identified the species Apodemus cf. flavicollis), Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens (determined as Neomys cf. fodiens in the Linar cave site), Talpa europaea, Erinaceus europaeus and cf. Lepus sp., some of which are also the most abundant. The taxa that are absent in some of the sites or that are only in one of them: Glis glis (registered in the cave of Cualventi but without a secure stratigraphical context), Clethrionomys glareolus (in the cave of El Linar), Sorex minutus (in the cave of Cualventi and the cave of El Linar), Crocidura russula (in the cave of Cualventi and the cave of Las Aguas) and Miniopterus schreibersii (in the cave of Aguas), are, by contrary, very scarce in the levels of the sites in which they appear. The majority of the taxa that are registered in the three sites have a great continuity in the different drillings and levels. It is to say that there is not an appreciable faunal change that shows any significant paleoenvironmental change between the different drillings and levels of the three sites. From all these taxa that are registered in the three sites, only two are not nowadays in the cantabrian region: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. From the study of the micromammal assemblages of the three sites, are deduced a mainly open and humid environment\nand a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Cualventi cave site, El Linar cave site, Las Aguas cave site, late Upper Pleistocene, paleoenvironmental interpretation, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474865/Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:53:51.062-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662687,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662687/thumbnails/1.jpg","file_name":"Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Interpretacion_paleoambiental_de_los_mic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662687/Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria-libre.pdf?1492502142=\u0026response-content-disposition=attachment%3B+filename%3DInterpretacion_paleoambiental_de_los_mic.pdf\u0026Expires=1732591648\u0026Signature=AUxjzxEmfQQ-g4AbhmHYxc5vjUP-g41J~YCCOdPXUSCnefIK5ueLgrfcJK4gRIXxZJUjT7yLJ7TH2vL7m6uto7XNrn45NdiRLvP5VJpebZRMqmiuBb0gemcOpMYp9ilGa1h4SzozDxP-b0aOPFSuTl15mqlKMy16bD9bmo50oSIvWTTD77a9EZtVDKBbURo27UOohNA7ceNR9AzZiwTkOymKtX8oQdpIDHK9I2OC9pZhaxm1LByD6NTwwtQJBat7ncVNo4nnvwYky5SyYvWvfBGm~BH0BZOmdTDtmuoAiTZkn8WCgVt476p-50O1aOt-XCLeMkddr-0zkniN0Ap2sw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Interpretacion_paleoambiental_de_los_micromamiferos_de_los_yacimientos_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_cueva_de_El_Linar_y_cueva_de_Las_Aguas_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":48,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662687,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662687/thumbnails/1.jpg","file_name":"Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662687/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Interpretacion_paleoambiental_de_los_mic.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662687/Sese_2016_Interpretacion_paleoambiental_micromamiferos_Pleistoceno_superior_de_Cualventi_El_Linar_y_Las_Aguas_Cantabria-libre.pdf?1492502142=\u0026response-content-disposition=attachment%3B+filename%3DInterpretacion_paleoambiental_de_los_mic.pdf\u0026Expires=1732591648\u0026Signature=AUxjzxEmfQQ-g4AbhmHYxc5vjUP-g41J~YCCOdPXUSCnefIK5ueLgrfcJK4gRIXxZJUjT7yLJ7TH2vL7m6uto7XNrn45NdiRLvP5VJpebZRMqmiuBb0gemcOpMYp9ilGa1h4SzozDxP-b0aOPFSuTl15mqlKMy16bD9bmo50oSIvWTTD77a9EZtVDKBbURo27UOohNA7ceNR9AzZiwTkOymKtX8oQdpIDHK9I2OC9pZhaxm1LByD6NTwwtQJBat7ncVNo4nnvwYky5SyYvWvfBGm~BH0BZOmdTDtmuoAiTZkn8WCgVt476p-50O1aOt-XCLeMkddr-0zkniN0Ap2sw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":7075,"name":"Paleoenvironment","url":"https://www.academia.edu/Documents/in/Paleoenvironment"},{"id":27230,"name":"Chiroptera","url":"https://www.academia.edu/Documents/in/Chiroptera"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474804"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662596/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final d...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286<br /><br />Resumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa  europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f3e5235844801df9ae1ac01d19239ccd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662596,"asset_id":32474804,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474804"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474804"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474804; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474804]").text(description); $(".js-view-count[data-work-id=32474804]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474804; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474804']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474804, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f3e5235844801df9ae1ac01d19239ccd" } } $('.js-work-strip[data-work-id=32474804]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474804,"title":"Los micromamiferos (Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte España) .pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286\n\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Los micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 264-286\n\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora, Lagomorpha y Chiroptera) del yacimiento del final del Pleistoceno superior de la cueva de Las Aguas (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: vestíbulo, sondeo cuadros G6-G7: niveles A, B (14.440-15.030 BP), C (14.740-17.630 BP) y D; sondeo cuadro N1’: niveles A, B (14.750 BP) y C; y sondeo cuadro M3: nivel B. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. y Miniopterus schreibersii. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en casi todos los niveles del yacimiento es Arvicola terrestris (con porcentajes que varían entre el 48,7 % y el 35,4 %), siguiéndole en abundancia por orden decreciente con porcentajes muy altos y bastante similares Microtus arvalis-Microtus agrestis y Microtus oeconomus. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, quirópteros, yacimiento de la cueva de Las Aguas, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora, Lagomorpha and Chiroptera) from the cave of Las Aguas site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the following drillings and levels: vestibule, drilling squares G6-G7: levels A, B (14.440-15.030 BP), C (14.740-17.630 BP) and D; drilling square N1: levels A, B (14.750 BP) and C, and drilling square M3: level B. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus, cf. Lepus sp. and Miniopterus schreibersii. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in almost all the levels is Arvicola terrestris (between the 48,7 % and the 35,4 %). After Arvicola terrestris, the most abundant taxa in decreasing order with high and very similar percentages are: Microtus arvalis-Microtus agrestis and Microtus oeconomus. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Chiroptera, Las Aguas cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474804/Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:47:14.990-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662596,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662596/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662596/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria-libre.pdf?1492501763=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=AcHtWzpyqNdm0xtfdTBDtsnAsvn2va1WqC4deL-0YojaVQKa1Oz1JfvpsfJ~kL3ZR~TsUTLmJ64gwWy-mMsbko2DE7NHfB-ywWWMB30i-J-~XCnzlJoSrBcT7mwlvzduzEnE21Xgv0wGVkI4~Mq7A1irkAfnGMDfLoGXFcS12dkMeewI-M468yMAS9winfe4hOo0j2kn~5TXoXeSrM5Ka3V4RxgZX~18xOu63eO9zLkHg3v5bAzRrMdBoEh5QEbc9otqd5~bOzk8DP0SKkG5ik~mskYQEt66iCIX3Ts~H3ygK7grq6iW9bK--KV45C3QMTfX7FGjq0ZeQJJxDNcBoA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_Lagomorpha_y_Chiroptera_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Las_Aguas_Cantabria_norte_España_pdf","translated_slug":"","page_count":38,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662596,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662596/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662596/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662596/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Las_Aguas_Cantabria-libre.pdf?1492501763=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=AcHtWzpyqNdm0xtfdTBDtsnAsvn2va1WqC4deL-0YojaVQKa1Oz1JfvpsfJ~kL3ZR~TsUTLmJ64gwWy-mMsbko2DE7NHfB-ywWWMB30i-J-~XCnzlJoSrBcT7mwlvzduzEnE21Xgv0wGVkI4~Mq7A1irkAfnGMDfLoGXFcS12dkMeewI-M468yMAS9winfe4hOo0j2kn~5TXoXeSrM5Ka3V4RxgZX~18xOu63eO9zLkHg3v5bAzRrMdBoEh5QEbc9otqd5~bOzk8DP0SKkG5ik~mskYQEt66iCIX3Ts~H3ygK7grq6iW9bK--KV45C3QMTfX7FGjq0ZeQJJxDNcBoA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":27230,"name":"Chiroptera","url":"https://www.academia.edu/Documents/in/Chiroptera"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474592"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662423/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated"> Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.<br /><br />Resumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,<br />Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus<br />agrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. <br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly<br />open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2888c2d016868011a23be981c8863030" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662423,"asset_id":32474592,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474592"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474592"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474592; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474592]").text(description); $(".js-view-count[data-work-id=32474592]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474592; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474592']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474592, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2888c2d016868011a23be981c8863030" } } $('.js-work-strip[data-work-id=32474592]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474592,"title":"Los micromamiferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España) .pdf","translated_title":"","metadata":{"abstract":"\nSesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.\n\nResumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,\nMicrotus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus\nagrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. \n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly\nopen and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n\n"},"translated_abstract":"\nSesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 242-263.\n\nResumen: En este trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de El Linar (Cantabria, norte de España). La fauna procede de los siguientes sondeos y niveles: sondeo A: niveles 3 (15.250 BP) y 4; sondeo B: nivel 3 (19.700 BP) y sondeo C: niveles 2, 3 (14.000-15.900 BP) y 4. La relación de micromamíferos del yacimiento es la siguiente: Apodemus sp., Arvicola terrestris,\nMicrotus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus que no está en España sino en regiones más septentrionales de Eurasia. Los taxones más abundantes en la mayor parte de los sondeos y niveles son: Microtus arvalis-Microtus\nagrestis y Microtus oeconomus, con porcentajes muy parecidos del 30,6 % y 30,3 % respectivamente de media para todo el yacimiento, siguiéndole en abundancia Arvicola terrestris que constituye el 19,8 % de media para todo el yacimiento. El estudio paleoambiental de la asociación de micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío. \n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de El Linar, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Linar site of the end of the upper Pleistocene are here studied for the first time. The fauna comesfrom the following drillings and levels: Drilling A: Levels 3 (15.250 BP) and 4; Drilling B: Level 3 (19.700 BP) and Drilling C: Levels 2, 3 (14.000-15.900 BP) and 4. The list of micromammals of the site is the following: Apodemus sp., Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Clethrionomys glareolus, Sorex araneus, Sorex minutus, Neomys cf. fodiens, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. All these taxa live nowadays in the Cantabrian Region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant taxa in almost all the drillings and levels are: Microtus arvalis-Microtus agrestis and Microtus oeconomus, with a mean of percentage very similar of 30,6 % and 30,3 % respectively for all the site. After these taxa, the most abundant species in decreasing order is Arvicola terrestris with a mean of percentage of 19,8 % for all the site. The paleoenvironmental study of the faunal assemblage suggests a mainly\nopen and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Linar cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n\n","internal_url":"https://www.academia.edu/32474592/Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:38:49.798-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662423,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662423/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662423/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria-libre.pdf?1492501251=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=YwlrsaXVlaMUGNlpYtw6giS3hbWkqplEHdZawpMttMCZepIey5CsHNmyN1R2T2paTFOKTI8RjrLukkjjr8bBS9fTzU0sJJAQjlegDS2m1~OU7NmBes8Mv~gkL64gKjEmyvV5PpMfsw31X2Z-gRVQJkSgQJ485XEtm0509F6AAItfrmf~Q0VQWXShslnMxGqnWvWWtZJwc2yUgn3dEYhK5w1Z00INTDg78iGLA~yIXSKUoo43~IMiZjNfOwY76Ag6ZrgSE4QajsX2wLb6WYfl-H8TC4T52cCMnMHyJ6K-ZfHAHsMIqJaItSdmr4rtEeMxO4CofZQl7nWln6lhzkiExg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_y_Lagomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_El_Linar_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":37,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662423,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662423/thumbnails/1.jpg","file_name":"Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria.pdf","download_url":"https://www.academia.edu/attachments/52662423/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662423/Sese_2016_Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_El_Linar_Cantabria-libre.pdf?1492501251=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=YwlrsaXVlaMUGNlpYtw6giS3hbWkqplEHdZawpMttMCZepIey5CsHNmyN1R2T2paTFOKTI8RjrLukkjjr8bBS9fTzU0sJJAQjlegDS2m1~OU7NmBes8Mv~gkL64gKjEmyvV5PpMfsw31X2Z-gRVQJkSgQJ485XEtm0509F6AAItfrmf~Q0VQWXShslnMxGqnWvWWtZJwc2yUgn3dEYhK5w1Z00INTDg78iGLA~yIXSKUoo43~IMiZjNfOwY76Ag6ZrgSE4QajsX2wLb6WYfl-H8TC4T52cCMnMHyJ6K-ZfHAHsMIqJaItSdmr4rtEeMxO4CofZQl7nWln6lhzkiExg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="32474411"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf"><img alt="Research paper thumbnail of Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf" class="work-thumbnail" src="https://attachments.academia-assets.com/52662276/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf">Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, C. 2016.  Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A.  (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.<br />Resumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden  decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de<br />micromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.<br /><br />Palabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.<br /><br />Abstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.<br /><br />Keywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d73e1ce7866d2c915c22d59cc88074a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52662276,"asset_id":32474411,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="32474411"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="32474411"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32474411; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32474411]").text(description); $(".js-view-count[data-work-id=32474411]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32474411; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='32474411']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 32474411, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9d73e1ce7866d2c915c22d59cc88074a" } } $('.js-work-strip[data-work-id=32474411]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":32474411,"title":"Los micromamiferos (Rodentia, Insectivora y Lalomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España).pdf","translated_title":"","metadata":{"abstract":"Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de\nmicromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n"},"translated_abstract":"Sesé, C. 2016. Los Micromamíferos (Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). En: Lasheras Corruchaga, J. A. (Dir.): Proyecto de investigación Los tiempos de Altamira. Actuaciones arqueológicas en las cuevas de Cualventi, El Linar y Las Aguas (Alfoz de Lloredo. Cantabria). Monografías del Museo Nacional y Centro de Investigación de Altamira, nº 26, Ministerio de Educación, Cultura y Deporte: 219-241.\nResumen: En ese trabajo se estudian por primera vez los micromamíferos (órdenes Rodentia, Insectivora y Lagomorpha) del yacimiento del final del Pleistoceno superior de la cueva de Cualventi (Cantabria, norte de España). La fauna procede de los niveles D, E (datado en 14.580-15.950 BP) y F, de los cuales el más rico es el E con un NMI de 1489 sobre un NMI total del yacimiento de 1640. La relación de micromamíferos del yacimiento es la siguiente: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus y cf. Lepus sp. Además de estas especies se registra también Glis glis, pero sin contexto estratigráfico seguro. Todos estos taxones viven actualmente en la región cantábrica excepto: Sorex araneus, cuya distribución se ha reducido en la península ibérica al norte de Cataluña y Microtus oeconomus, que no está en España sino en regiones más septentrionales de Eurasia. La especie más abundante en todos los niveles del yacimiento, con diferencia respecto a las demás, es Talpa europaea (entre el 41,8 % y el 30,2 %), siguiéndole en abundancia por orden decreciente y con porcentajes muy altos: Microtus oeconomus, Arvicola terrestris y Microtus arvalis-Microtus agrestis. El estudio paleoambiental de la asociación de\nmicromamíferos del yacimiento sugiere un medio fundamentalmente abierto y húmedo, y un clima frío.\n\nPalabras clave: micromamíferos, roedores, insectívoros, lagomorfos, yacimiento de la cueva de Cualventi, final del Pleistoceno superior, paleoclimatología, Cantabria, norte de España.\n\nAbstract: The micromammals (orders Rodentia, Insectivora and Lagomorpha) from the cave of Cualventi site of the end of the upper Pleistocene are here studied for the first time. The fauna comes from the levels D, E (dated in 14.580-15.950 BP) and F, from which the E level is the richest with a MNI of 1489 out of a total MNI of the site of 1640. The list of micromammals of the site is the following: Apodemus cf. flavicollis, Arvicola terrestris, Microtus arvalis-Microtus agrestis, Microtus oeconomus, Microtus lusitanicus, Chionomys nivalis, Sorex araneus, Sorex minutus, Neomys fodiens, Crocidura russula, Talpa europaea, Erinaceus europaeus and cf. Lepus sp. It has been also registered Glis glis but without a secure stratigraphical context. All these taxa live nowadays in the cantabrian region except: Sorex araneus which distribution in the Iberian Peninsula has reduced to the north of Catalonia and Microtus oeconomus that is not in Spain but in northern Euroasiatic regions. The most abundant species in all the levels is Talpa europaea (between the 41,8 % and the 30,2 %) with difference as regards to the rest of the taxa. After Talpa europaea, the most abundant taxa with high percentages in decreasing order are: Microtus oeconomus, Arvicola terrestris and Microtus arvalis-Microtus agrestis. The paleoenvironmental study of the faunal assemblage suggests a mainly open and humid environment and a cold climate.\n\nKeywords: Micromammals, Rodentia, Insectivora, Lagomorpha, Cualventi cave site, late Upper Pleistocene, paleoclimatology, Cantabria, North of Spain.\n","internal_url":"https://www.academia.edu/32474411/Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_Espa%C3%B1a_pdf","translated_internal_url":"","created_at":"2017-04-18T00:31:31.429-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":52662276,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662276/thumbnails/1.jpg","file_name":"Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana.pdf","download_url":"https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662276/Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana-libre.pdf?1492500765=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=VLBzKBTh4ivZV4tfM-DtAgGHF3EPxXyFM0kdh9YfQytBhL8rfHGqdr7wi-nXd1WhfD6FcV-Cx~9QvDENqX91PVcagQntb4Hu4L67vpscAZguLYC-0F3nkWLsekQNmTucFVFAiK4BQND8LTjdcwvtx3zaRIetO1gZ61BhpIuwYNVvVju56KsRN7q7qYW3RrtwUfxbsyRWqlFzYC-QgbWe0rkTlH3yehhgss~tyNCxCTGr7dPB6VQR99i37rd26Ky8LqwYwOaQXDw06t74gm1DWsau-tkoQ7YDyTcbpZomZghkZUNHhuloWX8hqg0H5ToEXMV0dn6UXa2lTBYH6OwnsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Los_micromamiferos_Rodentia_Insectivora_y_Lalomorpha_del_yacimiento_del_final_del_Pleistoceno_superior_de_la_cueva_de_Cualventi_Cantabria_norte_de_España_pdf","translated_slug":"","page_count":38,"language":"es","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52662276,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52662276/thumbnails/1.jpg","file_name":"Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana.pdf","download_url":"https://www.academia.edu/attachments/52662276/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Los_micromamiferos_Rodentia_Insectivora.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52662276/Los_micromamiferos_del_yacimiento_del_final_del_Pleistoceno_superior_de_Cualventi_Cantabria__norte_de_Espana-libre.pdf?1492500765=\u0026response-content-disposition=attachment%3B+filename%3DLos_micromamiferos_Rodentia_Insectivora.pdf\u0026Expires=1732591648\u0026Signature=VLBzKBTh4ivZV4tfM-DtAgGHF3EPxXyFM0kdh9YfQytBhL8rfHGqdr7wi-nXd1WhfD6FcV-Cx~9QvDENqX91PVcagQntb4Hu4L67vpscAZguLYC-0F3nkWLsekQNmTucFVFAiK4BQND8LTjdcwvtx3zaRIetO1gZ61BhpIuwYNVvVju56KsRN7q7qYW3RrtwUfxbsyRWqlFzYC-QgbWe0rkTlH3yehhgss~tyNCxCTGr7dPB6VQR99i37rd26Ky8LqwYwOaQXDw06t74gm1DWsau-tkoQ7YDyTcbpZomZghkZUNHhuloWX8hqg0H5ToEXMV0dn6UXa2lTBYH6OwnsQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":2258,"name":"Paleoclimatology","url":"https://www.academia.edu/Documents/in/Paleoclimatology"},{"id":35390,"name":"Rodentia","url":"https://www.academia.edu/Documents/in/Rodentia"},{"id":146812,"name":"Insectivora","url":"https://www.academia.edu/Documents/in/Insectivora"},{"id":214386,"name":"Upper Pleistocene","url":"https://www.academia.edu/Documents/in/Upper_Pleistocene"},{"id":299591,"name":"Micromammals","url":"https://www.academia.edu/Documents/in/Micromammals"},{"id":538109,"name":"Lagomorpha","url":"https://www.academia.edu/Documents/in/Lagomorpha"}],"urls":[]}, dispatcherData: dispatcherData }); 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Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)" class="work-thumbnail" src="https://attachments.academia-assets.com/51731379/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/31349018/Patrimonio_geopaleontol%C3%B3gico_de_los_dep%C3%B3sitos_aluviales_situados_sobre_la_terraza_28_m_del_Jarama_Nuevos_datos_micropaleontol%C3%B3gicos_y_cronol%C3%B3gicos_Solar_de_la_Real_F%C3%A1brica_de_Pa%C3%B1os_de_San_Fernando_de_Henares_">Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://audema.academia.edu/JorgeMorindePablosLateAntiquityVisigothicKingdomandAlAndalusArchaeology">Jorge Morin de Pablos</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://uam.academia.edu/MarioLopezRecio">Mario Lopez Recio</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí,...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.;  Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. & Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. <br /><br /> Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). <br />Palabras clave: Micromamíferos, Jarama, Madrid, España. <br />Abstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). <br />Key words: Micromammals, Jarama, Madrid, Spain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="937dae8696ed6afd2aabb380b5decd27" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":51731379,"asset_id":31349018,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/51731379/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="31349018"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="31349018"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 31349018; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=31349018]").text(description); $(".js-view-count[data-work-id=31349018]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 31349018; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='31349018']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 31349018, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "937dae8696ed6afd2aabb380b5decd27" } } $('.js-work-strip[data-work-id=31349018]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":31349018,"title":"Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. Nuevos datos micropaleontológicos y cronológicos (Solar de la Real Fábrica de Paños de San Fernando de Henares)","translated_title":"","metadata":{"abstract":"Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. \u0026 Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. \n\n Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). \nPalabras clave: Micromamíferos, Jarama, Madrid, España. \nAbstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). \nKey words: Micromammals, Jarama, Madrid, Spain."},"translated_abstract":"Tapias, F.; Sesé, C.; Yravedra, J.; Alarcón, A.; Arango, C.; López-Recio, M.; Dones, V.; Agustí, E.; Morín, J.; Ortiz, J. E. \u0026 Torres, T. de (2016). Actas de la Reunión de Arqueología Madrileña, Museo Arqueológico Regional, Alcalá de Henares, Madrid, 2014: 49-58. \n\n Resumen: Durante los trabajos de vigilancia de los movimientos de tierras asociados a la obra de la construcción de viviendas en el solar de la Real Fábrica de Paños (en adelante RFP) de San Fernando de Henares se documentaron materiales geológicos de edad miocena y cuaternaria con un contacto lateral dinámico entre ellos, constituido por una falla extensional de dirección norte-sur. En los niveles cuaternarios se registraron numerosos restos paleontológicos y algunas piezas de industria lítica. Según los estudios preliminares geomorfológicos y de macromamíferos (Tapias y Arango 2008; Yravedra et al. 2008; Dones et al. 2011) se asignó una cronología genérica de Pleistoceno Medio, confirmada por la datación obtenida por racemización de aminoácidos de un molar de Equus caballus (304 ka). En este trabajo se aportan nuevos datos a partir de la revisión y estudio de los restos de micromamíferos recuperados en la unidad 3. La presencia de Microtus brecciensis y M. arvalis en la base de los depósitos aluviales posibilita su adscripción cronológica al Pleistoceno Medio avanzado (MIS 8 o MIS 6). \nPalabras clave: Micromamíferos, Jarama, Madrid, España. \nAbstract: During the monitoring of the movements of land associated with the work of the construction of homes in the Solar of the Royal Factory of Cloths of San Fernando de Henares, some geological materials of Miocene and Quaternary age were documented. Numerous paleontological remains and some stone tools have been registered in these qua¬ternary levels. According to geomorphological preliminary studies and macromammals (Tapias y Arango 2008; Yra¬vedra et al. 2008; Dones et al. 2011) a generic Middle Pleistocene chronology was assigned. This was confirmed by the aminoacids racemization dating of Equus caballus molar (304 ka) This paper provides new data of the remains of micromammals recovered. The faunal assemblage, with Microtus brecciensis and M arvalis found at the base of the alluvial deposits, has allowed reviewing previous studies. It could be more specific on the geochronological and paleoenviromental contextualization of remains and materials that could be assigned to advanced Middle Pleisto¬cene (MIS 8 or MIS 6). \nKey words: Micromammals, Jarama, Madrid, Spain.","internal_url":"https://www.academia.edu/31349018/Patrimonio_geopaleontol%C3%B3gico_de_los_dep%C3%B3sitos_aluviales_situados_sobre_la_terraza_28_m_del_Jarama_Nuevos_datos_micropaleontol%C3%B3gicos_y_cronol%C3%B3gicos_Solar_de_la_Real_F%C3%A1brica_de_Pa%C3%B1os_de_San_Fernando_de_Henares_","translated_internal_url":"","created_at":"2017-02-10T04:34:03.039-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":27519999,"work_id":31349018,"tagging_user_id":4287495,"tagged_user_id":687105,"co_author_invite_id":null,"email":"j***n@audema.com","affiliation":"AUDEMA","display_order":1,"name":"Jorge Morin de Pablos","title":"Patrimonio geopaleontológico de los depósitos aluviales situados sobre la terraza +28 m del Jarama. 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(2016). Los micromam...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. & Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. <a href="http://dx.doi.org/10.3989/egeol.42424.405" rel="nofollow">http://dx.doi.org/10.3989/egeol.42424.405</a>.<br />Resumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.<br />Abstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. The climate would be of Mediterranean type, similar to the actual or perhaps a little milder and more humid.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b90c2989e9453261f9b3f44253fb42ac" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50798832,"asset_id":30346107,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50798832/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="30346107"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="30346107"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 30346107; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=30346107]").text(description); $(".js-view-count[data-work-id=30346107]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 30346107; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='30346107']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 30346107, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b90c2989e9453261f9b3f44253fb42ac" } } $('.js-work-strip[data-work-id=30346107]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":30346107,"title":"Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales","translated_title":"","metadata":{"abstract":"Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. \u0026 Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. http://dx.doi.org/10.3989/egeol.42424.405.\nResumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.\nAbstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. The climate would be of Mediterranean type, similar to the actual or perhaps a little milder and more humid."},"translated_abstract":"Sesé, c.; Soto, E.; Santonja, M.; Pérez-González, A. \u0026 Domínguez-Rodrigo, M. (2016). Los micromamíferos (Lagomorpha, Eulipotyphla y Rodentia) del yacimiento del Pleistoceno Medio de Cuesta de la Bajada (Teruel, España): Estudio sistemático y consideraciones paleoambientales. Estudios Geológicos 72 (2): e057. http://dx.doi.org/10.3989/egeol.42424.405.\nResumen: La asociación de micromamíferos determinada en este trabajo es la siguiente: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. y Talpa sp.; y Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis y Microtus (Terricola) duodecimcostatus. Es una asociación característica del Pleistoceno Medio. El estadio evolutivo de Cricetulus (A.) bur¬sae, Arvicola aff. sapidus y Microtus (I.) brecciensis le aproximan a las poblaciones de dichas especies de algunos yacimientos de la Península Ibérica del Pleistoceno Medio avanzado, pero no final, lo que es acorde con las dataciones numéricas obtenidas en el yacimiento (243-337 ka) que le sitúan en el MIS 8 o 9. Los micromamíferos indican la predominancia de los espacios abiertos con abundante vegetación herbácea y arbustiva, en los que podría haber también alguna zona arbolada. El clima que indican es de tipo mediterráneo, similar al actual en la zona o quizás algo más benigno y más húmedo.\nAbstract: The micromammal association established in this work is the following: Lagomorpha: Oryctolagus cuniculus; Eulipotyphla: Crocidura cf. russula, cf. Sorex sp., Neomys sp., Soricidae indet. and Talpa sp.; and Rodentia: Eliomys quercinus, Apodemus cf. sylvaticus, Cricetulus (Allocricetus) bursae, Arvicola aff. sapidus, Microtus (Iberomys) brecciensis and Microtus (Terricola) duodecimcostatus. This association is characteristic of the Middle Pleistocene. The morphological state of Cricetulus (A.) bur¬sae, Arvicola aff. sapidus and Microtus (I.) brecciensis allows to place it in the advanced, but not final, Middle Pleistocene, which agrees with the numerical data of the site (243–337 ka) that places it in the MIS 8 or 9. The micromammals indicate the predomi¬nance of the open spaces with abundant vegetation mainly of herbaceous and bushes but also with some areas with trees. 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Rosas, A.; Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánche...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Rasilla, M. de la;  Rosas, A.;  Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.;  Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. 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Cartafueyos Asturianos de Ciencia y Teunoloxía, 6: 62-79.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7aad22faa7ebb7b2bd45827c30cf9482" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":50247894,"asset_id":29791626,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/50247894/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="29791626"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="29791626"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 29791626; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=29791626]").text(description); $(".js-view-count[data-work-id=29791626]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 29791626; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='29791626']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 29791626, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "7aad22faa7ebb7b2bd45827c30cf9482" } } $('.js-work-strip[data-work-id=29791626]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":29791626,"title":"El grupu neandertal de la Cueva d´El Sidron (Borines Piloña)","translated_title":"","metadata":{"abstract":"Rasilla, M. de la; Rosas, A.; Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.; Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. E.; Valladas, H.; Mercier, N.; Tisnèrat-Laborde, N.; Grün, R.; Eggins, S.; Higham, T.; Wood, R. E.; Julià, R.; Soler, V.; Badal, E.; Tarriño, A. \u0026 Alonso, J. (2016). El grupu neandertal de la Cueva d' El Sidrón (Borines, Piloña). Ciencies. Cartafueyos Asturianos de Ciencia y Teunoloxía, 6: 62-79."},"translated_abstract":"Rasilla, M. de la; Rosas, A.; Cañaveras, J. C.; Lalueza, C.; Santamaría, D.; Duarte, E.; Sánchez Moral, S.; Estalrrich, A.; García Tabernero, A.; Silva, P. G.; Santos, G.; Huguet, R.; Bastir, M.; Martínez, L.; Suárez, P.; Díez, A. B.; López Tascón, C.; Fernández Cascón, B.; Cuezva, S.; Fernández Cortés, A.; Muñoz, C.; Lario, J.; García Antón, E.; Ríos, L.; Pérez-Criado, L.; García-Martínez, D.; Rodríguez Pérez, F. J.; Ferrando, A.; Standing, M.; Carrasco, P.; Huerta, P.; Ayarza, P.; Álvarez Lobato, F.; Rodríguez, L.; Picón, I.; Fernández, B.; Sesé, C.; Torres, T. de; Ortiz, J. E.; Valladas, H.; Mercier, N.; Tisnèrat-Laborde, N.; Grün, R.; Eggins, S.; Higham, T.; Wood, R. E.; Julià, R.; Soler, V.; Badal, E.; Tarriño, A. \u0026 Alonso, J. (2016). El grupu neandertal de la Cueva d' El Sidrón (Borines, Piloña). Ciencies. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="28945890"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/28945890/New_data_from_Ambrona_Closing_the_hunting_versus_scavenging_debate"><img alt="Research paper thumbnail of New data from Ambrona Closing the hunting versus scavenging debate" class="work-thumbnail" src="https://attachments.academia-assets.com/49383844/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/28945890/New_data_from_Ambrona_Closing_the_hunting_versus_scavenging_debate">New data from Ambrona Closing the hunting versus scavenging debate</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/VillaPaola">Paola Villa</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uab.academia.edu/RMora">Rafael Mora</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavation...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavations at Ambrona (Spain), directed by Santonja and Pe´rez-Gonzaíez. The purpose of the new excavations was to achieve a better understanding of the stratigraphic sequence, general geology, sedimentary context and processes of accumulation of materials. Our objectives are to evaluate the opposing interpretations of the hominid subsistence activities at the site proposed by Freeman and Binford. The faunal and lithic remains are found in different sedimentary contexts: an alluvial fan, lacustrine muds, fluviatile clay–sands and channel deposits. Faunal remains in the lacustrine muds are often, but not always, in primary context. Remains of elephant and deer carcasses may be found in partial articulation or proximity and represent natural occurrences without any clear evidence of hominid intervention. In other contexts the faunal remains are occurrences of single anatomical elements either displaced by water or left isolated in situ. There are no carnivore marks; bones and stone artifacts show varying degrees of mechanical abrasion due to water transport. Limited evidence of human action on bones is provided by a few SEM verified cutmarks and some anthropic fractures. They document butchery of various animals, including elephants. We cannot prove hunting but we can definitely reject Binford's idea of marginal scavenging of medium-size ungulates from carnivore kills. Ambrona is a complex mix of natural and human components, the remnant of a natural landscape regularly visited by hominids, who transported some artifacts from nonlocal raw material sources and had an organized approach to meat acquisition. However, strong evidence of elephant hunting is provided only by sites younger than Ambrona.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="aaefd330ab10a81cf6e76a55f8052493" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49383844,"asset_id":28945890,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49383844/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="28945890"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="28945890"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 28945890; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=28945890]").text(description); $(".js-view-count[data-work-id=28945890]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 28945890; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='28945890']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 28945890, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "aaefd330ab10a81cf6e76a55f8052493" } } $('.js-work-strip[data-work-id=28945890]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":28945890,"title":"New data from Ambrona Closing the hunting versus scavenging debate","translated_title":"","metadata":{"abstract":"This paper presents a taphonomic analysis of the faunal assemblages from the 1993–1999 excavations at Ambrona (Spain), directed by Santonja and Pe´rez-Gonzaíez. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="4712699" id="other"><div class="js-work-strip profile--work_container" data-work-id="22593001"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/22593001/New_evidence_of_bones_used_as_fuel_in_the_Gravettian_level_at_Co%C3%ADmbre_cave_northern_Iberian_Peninsula"><img alt="Research paper thumbnail of New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula." class="work-thumbnail" src="https://attachments.academia-assets.com/52666741/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/22593001/New_evidence_of_bones_used_as_fuel_in_the_Gravettian_level_at_Co%C3%ADmbre_cave_northern_Iberian_Peninsula">New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula.</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Yravedra, J.; Álvarez-Alonso, D.; Estaca-Gómez, V.; López-Cisneros, P.; Arrizabalaga, A.; Elorza,...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Yravedra, J.; Álvarez-Alonso, D.; Estaca-Gómez, V.; López-Cisneros, P.; Arrizabalaga, A.; Elorza, M.; Iriarte, M. J.; Jordá Pardo, J. F.; Sesé, C. & Uzquiano, P. 2016. New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula. <br />Archaeological and Anthropological Sciences.  <br />DOI 10.1007/s12520-016-0317-0</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="65d79e2604aa1bd26b8498b031fc43be" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":52666741,"asset_id":22593001,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/52666741/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="22593001"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="22593001"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 22593001; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=22593001]").text(description); $(".js-view-count[data-work-id=22593001]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 22593001; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='22593001']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 22593001, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "65d79e2604aa1bd26b8498b031fc43be" } } $('.js-work-strip[data-work-id=22593001]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":22593001,"title":"New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula.","translated_title":"","metadata":{"abstract":"Yravedra, J.; Álvarez-Alonso, D.; Estaca-Gómez, V.; López-Cisneros, P.; Arrizabalaga, A.; Elorza, M.; Iriarte, M. J.; Jordá Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. 2016. New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula. \nArchaeological and Anthropological Sciences. \nDOI 10.1007/s12520-016-0317-0"},"translated_abstract":"Yravedra, J.; Álvarez-Alonso, D.; Estaca-Gómez, V.; López-Cisneros, P.; Arrizabalaga, A.; Elorza, M.; Iriarte, M. J.; Jordá Pardo, J. F.; Sesé, C. \u0026 Uzquiano, P. 2016. New evidence of bones used as fuel in the Gravettian level at Coímbre cave, northern Iberian Peninsula. \nArchaeological and Anthropological Sciences. \nDOI 10.1007/s12520-016-0317-0","internal_url":"https://www.academia.edu/22593001/New_evidence_of_bones_used_as_fuel_in_the_Gravettian_level_at_Co%C3%ADmbre_cave_northern_Iberian_Peninsula","translated_internal_url":"","created_at":"2016-02-29T05:11:40.827-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":4287495,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[],"downloadable_attachments":[{"id":52666741,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52666741/thumbnails/1.jpg","file_name":"123_Yravedra_et_al_coimbre_hogares.pdf","download_url":"https://www.academia.edu/attachments/52666741/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"New_evidence_of_bones_used_as_fuel_in_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52666741/123_Yravedra_et_al_coimbre_hogares-libre.pdf?1492518241=\u0026response-content-disposition=attachment%3B+filename%3DNew_evidence_of_bones_used_as_fuel_in_th.pdf\u0026Expires=1732804965\u0026Signature=LfnYYP95pG7daLw9sYoAU-m~2XYivc~Uo8dNuHwhVG8yMY8BhY5CEaDDcI7QJg5KQZ0AZni4UfUGFJMKE~xkogUn0X2Je~q-uod-hEfrQujD3PvylL3se9K5aVCz5RJdTLF-EPyMb3QevhPKITRqplyZknOjbp5iPJaCzpBepP~CHjueE3The6IYvmaCeENEp7r4j-ICb3aTtXJQj9q3sHT0fJHGetw7vpCd33IQk7bpkQBOzrColkTWMQvhTXjpvLDTJikloITNnf2My3EPel925x9ZHh9Nv0JJwPoUBiNaxlBlDH2r-xfLzWDGB8fOyufi5DxLf~mMD38XSqCtkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"New_evidence_of_bones_used_as_fuel_in_the_Gravettian_level_at_Coímbre_cave_northern_Iberian_Peninsula","translated_slug":"","page_count":19,"language":"en","content_type":"Work","owner":{"id":4287495,"first_name":"Carmen","middle_initials":null,"last_name":"Sesé","page_name":"CarmenSesé","domain_name":"csic","created_at":"2013-05-22T21:35:33.672-07:00","display_name":"Carmen Sesé","url":"https://csic.academia.edu/CarmenSes%C3%A9"},"attachments":[{"id":52666741,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/52666741/thumbnails/1.jpg","file_name":"123_Yravedra_et_al_coimbre_hogares.pdf","download_url":"https://www.academia.edu/attachments/52666741/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"New_evidence_of_bones_used_as_fuel_in_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/52666741/123_Yravedra_et_al_coimbre_hogares-libre.pdf?1492518241=\u0026response-content-disposition=attachment%3B+filename%3DNew_evidence_of_bones_used_as_fuel_in_th.pdf\u0026Expires=1732804965\u0026Signature=LfnYYP95pG7daLw9sYoAU-m~2XYivc~Uo8dNuHwhVG8yMY8BhY5CEaDDcI7QJg5KQZ0AZni4UfUGFJMKE~xkogUn0X2Je~q-uod-hEfrQujD3PvylL3se9K5aVCz5RJdTLF-EPyMb3QevhPKITRqplyZknOjbp5iPJaCzpBepP~CHjueE3The6IYvmaCeENEp7r4j-ICb3aTtXJQj9q3sHT0fJHGetw7vpCd33IQk7bpkQBOzrColkTWMQvhTXjpvLDTJikloITNnf2My3EPel925x9ZHh9Nv0JJwPoUBiNaxlBlDH2r-xfLzWDGB8fOyufi5DxLf~mMD38XSqCtkw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="4931107" id="2012"><div class="js-work-strip profile--work_container" data-work-id="4902141"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/4902141/Human_behaviour_and_adaptations_to_MIS_3_environmental_trends_53_30_ka_BP_at_Esquilleu_cave_Cantabria_northern_Spain_"><img alt="Research paper thumbnail of Human behaviour and adaptations to MIS 3 environmental trends (>53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) " class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/4902141/Human_behaviour_and_adaptations_to_MIS_3_environmental_trends_53_30_ka_BP_at_Esquilleu_cave_Cantabria_northern_Spain_">Human behaviour and adaptations to MIS 3 environmental trends (>53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) </a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/joseyravedra">jose yravedra</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://uam.academia.edu/httpswwwuamesssSatelliteFilosofiayLetrases12426588850991242658428163personadetallePDIBaena_Preysler_Javierhtm">javier J baena</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span>quaternary intrrnational Volume 252, 27 February 2012, Pages 82–89</span><span>, 2012</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Esquilleu cave (Cantabria, northern Spain) presents 30 Mousterian archaeological layers covering ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Esquilleu cave (Cantabria, northern Spain) presents 30 Mousterian archaeological layers covering virtually the complete MIS 3 both in chronology and environmental. A number of environmental analyses (faunal, pollen, charcoal) allow the study of the different strategies for the procurement and management of resources available near the site and indicate the Neanderthals’ wide adaptability to the changing environment typical of this period. This paper also discusses the possibility of using bones as fuel either as a palliative for a presumed lack of wood resources in the environment or as a mere pattern of human behaviour.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4902141"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4902141"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4902141; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4902141]").text(description); $(".js-view-count[data-work-id=4902141]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4902141; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4902141']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4902141, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4902141]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4902141,"title":"Human behaviour and adaptations to MIS 3 environmental trends (\u003e53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) ","translated_title":"","metadata":{"abstract":"Esquilleu cave (Cantabria, northern Spain) presents 30 Mousterian archaeological layers covering virtually the complete MIS 3 both in chronology and environmental. A number of environmental analyses (faunal, pollen, charcoal) allow the study of the different strategies for the procurement and management of resources available near the site and indicate the Neanderthals’ wide adaptability to the changing environment typical of this period. This paper also discusses the possibility of using bones as fuel either as a palliative for a presumed lack of wood resources in the environment or as a mere pattern of human behaviour.","more_info":"http://www.sciencedirect.com/science/article/pii/S1040618211004046","publication_date":{"day":null,"month":null,"year":2012,"errors":{}},"publication_name":"quaternary intrrnational Volume 252, 27 February 2012, Pages 82–89"},"translated_abstract":"Esquilleu cave (Cantabria, northern Spain) presents 30 Mousterian archaeological layers covering virtually the complete MIS 3 both in chronology and environmental. A number of environmental analyses (faunal, pollen, charcoal) allow the study of the different strategies for the procurement and management of resources available near the site and indicate the Neanderthals’ wide adaptability to the changing environment typical of this period. This paper also discusses the possibility of using bones as fuel either as a palliative for a presumed lack of wood resources in the environment or as a mere pattern of human behaviour.","internal_url":"https://www.academia.edu/4902141/Human_behaviour_and_adaptations_to_MIS_3_environmental_trends_53_30_ka_BP_at_Esquilleu_cave_Cantabria_northern_Spain_","translated_internal_url":"","created_at":"2013-10-27T01:26:01.473-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6396581,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":18064351,"work_id":4902141,"tagging_user_id":6396581,"tagged_user_id":905235,"co_author_invite_id":null,"email":"m***o@cchs.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":0,"name":"Marta Moreno-García","title":"Human behaviour and adaptations to MIS 3 environmental trends (\u003e53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) "},{"id":18064352,"work_id":4902141,"tagging_user_id":6396581,"tagged_user_id":null,"co_author_invite_id":4129560,"email":"c***3@yahoo.es","display_order":4194304,"name":"M. José","title":"Human behaviour and adaptations to MIS 3 environmental trends (\u003e53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) "},{"id":18064416,"work_id":4902141,"tagging_user_id":6396581,"tagged_user_id":1123750,"co_author_invite_id":null,"email":"j***a@uam.es","affiliation":"Universidad Autónoma de Madrid","display_order":6291456,"name":"javier J baena","title":"Human behaviour and adaptations to MIS 3 environmental trends (\u003e53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) "},{"id":18064441,"work_id":4902141,"tagging_user_id":6396581,"tagged_user_id":4287495,"co_author_invite_id":null,"email":"c***e@mncn.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":7340032,"name":"Carmen Sesé","title":"Human behaviour and adaptations to MIS 3 environmental trends (\u003e53–30 ka BP) at Esquilleu cave (Cantabria, northern Spain) "}],"downloadable_attachments":[],"slug":"Human_behaviour_and_adaptations_to_MIS_3_environmental_trends_53_30_ka_BP_at_Esquilleu_cave_Cantabria_northern_Spain_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":6396581,"first_name":"jose","middle_initials":null,"last_name":"yravedra","page_name":"joseyravedra","domain_name":"ucm","created_at":"2013-10-26T21:59:58.395-07:00","display_name":"jose yravedra","url":"https://ucm.academia.edu/joseyravedra"},"attachments":[],"research_interests":[{"id":28126,"name":"Neanderthals (Palaeolithic Archaeology)","url":"https://www.academia.edu/Documents/in/Neanderthals_Palaeolithic_Archaeology_"},{"id":41112,"name":"Middle Palaeolithic","url":"https://www.academia.edu/Documents/in/Middle_Palaeolithic"},{"id":52468,"name":"Alternative Fuels","url":"https://www.academia.edu/Documents/in/Alternative_Fuels"},{"id":185181,"name":"Middle to Upper Palaeolithic Transition","url":"https://www.academia.edu/Documents/in/Middle_to_Upper_Palaeolithic_Transition"},{"id":1164067,"name":"Bone As Fuel","url":"https://www.academia.edu/Documents/in/Bone_As_Fuel"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4902123"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4902123/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_"><img alt="Research paper thumbnail of Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain) " class="work-thumbnail" src="https://attachments.academia-assets.com/37637392/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4902123/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain) </a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/joseyravedra">jose yravedra</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BSalvador1">B. Salvador</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span>Quaternary International Volumes 272–273, 12 September 2012, Pages 42–54</span><span>, 2012</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula cur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440–21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770–12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural resources may have been used. The faunal remains represented at this site reflect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality fix the occupation of levels I–III from the spring to the autumn. Certain types of wood were collected for use as firewood. Other elements found in the record (personal ornaments, mobiliary art and raw materials) provide evidence that the people that occupied the site moved over a more extensive territory.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44794f82f30649b1f142b25f27e0c481" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":37637392,"asset_id":4902123,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/37637392/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4902123"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4902123"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4902123; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4902123]").text(description); $(".js-view-count[data-work-id=4902123]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4902123; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4902123']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4902123, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44794f82f30649b1f142b25f27e0c481" } } $('.js-work-strip[data-work-id=4902123]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4902123,"title":"Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain) ","translated_title":"","metadata":{"abstract":"The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440–21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770–12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="4931115" id="2013"><div class="js-work-strip profile--work_container" data-work-id="4903397"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4903397/A_modo_de_conclusi%C3%B3n_ocupaciones_magdalenienses_en_la_Pe%C3%B1a_de_Estebanvela"><img alt="Research paper thumbnail of A modo de conclusión, ocupaciones magdalenienses en la Peña de Estebanvela" class="work-thumbnail" src="https://attachments.academia-assets.com/32169200/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4903397/A_modo_de_conclusi%C3%B3n_ocupaciones_magdalenienses_en_la_Pe%C3%B1a_de_Estebanvela">A modo de conclusión, ocupaciones magdalenienses en la Peña de Estebanvela</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/joseyravedra">jose yravedra</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JuanAntonioMartosRomero">Juan Antonio Martos Romero</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span>Cacho C. (Coord). Ocupaciones magdaleniense en el interior de la Península Ibérica. La Peña de Estebanvela, Ayllón, Segovia. ISBN: 978-84-616-5992-0. 536-544.</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">his last chapter provides an overall interpretation of the La Peña de Estebanvela site, the resul...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">his last chapter provides an overall interpretation of the La Peña de Estebanvela site, the result of multidisciplinary research. Studies of the geoarchaeological, chronostratigraphic, taxonomic, zooarchaeological, taphonomic, anthracological and phytological records allow the chronology of the site’s occupations to be determined. Sometimes even the seasonality of occupation can be established, and patterns of territory exploitation discerned. The results of technotypological, traceological and spatial analyses show a marked internal structuring of the site’s space, and provide clues on the possible functions of the site. Finally, the detailed examination of the site’s ornamental pieces and decorated stones shows the groups that used the rock shelter sometimes travelled great distances.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ce40e3abf62994a75242644df467950c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":32169200,"asset_id":4903397,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/32169200/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4903397"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4903397"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4903397; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4903397]").text(description); $(".js-view-count[data-work-id=4903397]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4903397; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4903397']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4903397, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ce40e3abf62994a75242644df467950c" } } $('.js-work-strip[data-work-id=4903397]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4903397,"title":"A modo de conclusión, ocupaciones magdalenienses en la Peña de Estebanvela","translated_title":"","metadata":{"abstract":"his last chapter provides an overall interpretation of the La Peña de Estebanvela site, the result of multidisciplinary research. 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Jordá","title":"A modo de conclusión, ocupaciones magdalenienses en la Peña de Estebanvela"},{"id":18064442,"work_id":4903397,"tagging_user_id":6396581,"tagged_user_id":4287495,"co_author_invite_id":null,"email":"c***e@mncn.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":7340032,"name":"Carmen Sesé","title":"A modo de conclusión, ocupaciones magdalenienses en la Peña de Estebanvela"}],"downloadable_attachments":[{"id":32169200,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/32169200/thumbnails/1.jpg","file_name":"Cacho_et_al_2013_conclusion.pdf","download_url":"https://www.academia.edu/attachments/32169200/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_modo_de_conclusion_ocupaciones_magdale.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/32169200/Cacho_et_al_2013_conclusion-libre.pdf?1391496936=\u0026response-content-disposition=attachment%3B+filename%3DA_modo_de_conclusion_ocupaciones_magdale.pdf\u0026Expires=1732722057\u0026Signature=S5edaw4CcejTebaChVTlI3FooahZ~rJxeNZU4WXbLYQmWV79EDa9-62Gc7VPixEHWJxduGwWw40ZOCOzaev88baLEzCVE3bS3o6Rwb54dkJG7lpMcgcYc6WrVd6zrfjWBwF6Jsei-peMS3MQoClwydsPlo5GLGfIx-KpWz52SYEMpBWe68J8fLpJRiFJXEa23FNsznvXOkRJHfexktmPzFgr-ROqbhImjyLvrQCHYLtrhCxv5Ca0O0ly79FkXPvcbLDwteXSc3RwSt1dvSFzof2j~1bU7y9LoQKbusine5wRpVqg50~9Rdw9i9HasT8q3A2RbNdDbU1GWdpuChSmHw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"A_modo_de_conclusión_ocupaciones_magdalenienses_en_la_Peña_de_Estebanvela","translated_slug":"","page_count":10,"language":"es","content_type":"Work","owner":{"id":6396581,"first_name":"jose","middle_initials":null,"last_name":"yravedra","page_name":"joseyravedra","domain_name":"ucm","created_at":"2013-10-26T21:59:58.395-07:00","display_name":"jose yravedra","url":"https://ucm.academia.edu/joseyravedra"},"attachments":[{"id":32169200,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/32169200/thumbnails/1.jpg","file_name":"Cacho_et_al_2013_conclusion.pdf","download_url":"https://www.academia.edu/attachments/32169200/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"A_modo_de_conclusion_ocupaciones_magdale.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/32169200/Cacho_et_al_2013_conclusion-libre.pdf?1391496936=\u0026response-content-disposition=attachment%3B+filename%3DA_modo_de_conclusion_ocupaciones_magdale.pdf\u0026Expires=1732722057\u0026Signature=S5edaw4CcejTebaChVTlI3FooahZ~rJxeNZU4WXbLYQmWV79EDa9-62Gc7VPixEHWJxduGwWw40ZOCOzaev88baLEzCVE3bS3o6Rwb54dkJG7lpMcgcYc6WrVd6zrfjWBwF6Jsei-peMS3MQoClwydsPlo5GLGfIx-KpWz52SYEMpBWe68J8fLpJRiFJXEa23FNsznvXOkRJHfexktmPzFgr-ROqbhImjyLvrQCHYLtrhCxv5Ca0O0ly79FkXPvcbLDwteXSc3RwSt1dvSFzof2j~1bU7y9LoQKbusine5wRpVqg50~9Rdw9i9HasT8q3A2RbNdDbU1GWdpuChSmHw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":101687,"name":"Upper Palaeolithic","url":"https://www.academia.edu/Documents/in/Upper_Palaeolithic"},{"id":1164176,"name":"Magdallenian","url":"https://www.academia.edu/Documents/in/Magdallenian"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="4901973"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/4901973/Manzanares_Valley_Madrid_Spain_A_good_country_for_Proboscideans_and_Neanderthals"><img alt="Research paper thumbnail of Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/4901973/Manzanares_Valley_Madrid_Spain_A_good_country_for_Proboscideans_and_Neanderthals">Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/joseyravedra">jose yravedra</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/HuguesAlexandreBlain">Hugues-Alexandre Blain</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents the findings from four sites with proboscidean remains associated with Middle...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">This paper presents the findings from four sites with proboscidean remains associated with Middle Palaeolithic stone tools from the Manzanares Valley Complex Terrace of Butarque (CTB), which has been dated to between the final Middle Pleistocene (MIS 6, 190–130 ka) and the early Late Pleistocene (MIS 5, 130-74-71 ka). We review the direct and indirect evidence of proboscidean exploitation in the Middle Paleolithic sites of Europe, and provide information on Lower Paleolithic European sites with proboscidean remains and stone tools. Geological, chronological, bio-stratigraphic and climatic data of the CTB are provided, and the sites with proboscidean remains and Middle Palaeolithic stone tools are described in detail. <br /> <br />Systematic exploitation of large mammals during the Middle Palaeolithic, and even their regular hunting, is widely accepted. However, the exploitation of proboscideans is not as evident in the archaeological record of this period. The exploitation of proboscideans cannot be considered as merely occasional before the Upper Palaeolithic, and although there is more evidence of the exploitation of these mega-herbivores during the Lower than during the Middle Palaeolithic, the discoveries from the Manzanares Valley state that, at least in this area, proboscideans continued to play an important role with regards to the exploitation of the environmental resources.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="4901973"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4901973"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4901973; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4901973]").text(description); $(".js-view-count[data-work-id=4901973]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4901973; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4901973']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4901973, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=4901973]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4901973,"title":"Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals","translated_title":"","metadata":{"abstract":"This paper presents the findings from four sites with proboscidean remains associated with Middle Palaeolithic stone tools from the Manzanares Valley Complex Terrace of Butarque (CTB), which has been dated to between the final Middle Pleistocene (MIS 6, 190–130 ka) and the early Late Pleistocene (MIS 5, 130-74-71 ka). We review the direct and indirect evidence of proboscidean exploitation in the Middle Paleolithic sites of Europe, and provide information on Lower Paleolithic European sites with proboscidean remains and stone tools. Geological, chronological, bio-stratigraphic and climatic data of the CTB are provided, and the sites with proboscidean remains and Middle Palaeolithic stone tools are described in detail.\r\n\r\nSystematic exploitation of large mammals during the Middle Palaeolithic, and even their regular hunting, is widely accepted. However, the exploitation of proboscideans is not as evident in the archaeological record of this period. The exploitation of proboscideans cannot be considered as merely occasional before the Upper Palaeolithic, and although there is more evidence of the exploitation of these mega-herbivores during the Lower than during the Middle Palaeolithic, the discoveries from the Manzanares Valley state that, at least in this area, proboscideans continued to play an important role with regards to the exploitation of the environmental resources.\r\n","more_info":"http://www.sciencedirect.com/science/article/pii/S104061821300709X","publication_date":{"day":null,"month":null,"year":2013,"errors":{}},"publication_name":"Quaternary International"},"translated_abstract":"This paper presents the findings from four sites with proboscidean remains associated with Middle Palaeolithic stone tools from the Manzanares Valley Complex Terrace of Butarque (CTB), which has been dated to between the final Middle Pleistocene (MIS 6, 190–130 ka) and the early Late Pleistocene (MIS 5, 130-74-71 ka). We review the direct and indirect evidence of proboscidean exploitation in the Middle Paleolithic sites of Europe, and provide information on Lower Paleolithic European sites with proboscidean remains and stone tools. Geological, chronological, bio-stratigraphic and climatic data of the CTB are provided, and the sites with proboscidean remains and Middle Palaeolithic stone tools are described in detail.\r\n\r\nSystematic exploitation of large mammals during the Middle Palaeolithic, and even their regular hunting, is widely accepted. However, the exploitation of proboscideans is not as evident in the archaeological record of this period. The exploitation of proboscideans cannot be considered as merely occasional before the Upper Palaeolithic, and although there is more evidence of the exploitation of these mega-herbivores during the Lower than during the Middle Palaeolithic, the discoveries from the Manzanares Valley state that, at least in this area, proboscideans continued to play an important role with regards to the exploitation of the environmental resources.\r\n","internal_url":"https://www.academia.edu/4901973/Manzanares_Valley_Madrid_Spain_A_good_country_for_Proboscideans_and_Neanderthals","translated_internal_url":"","created_at":"2013-10-27T01:01:58.948-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6396581,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":18064343,"work_id":4901973,"tagging_user_id":6396581,"tagged_user_id":45768498,"co_author_invite_id":null,"email":"h***n@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":0,"name":"Hugues-Alexandre Blain","title":"Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals"},{"id":18064420,"work_id":4901973,"tagging_user_id":6396581,"tagged_user_id":431842,"co_author_invite_id":null,"email":"j***a@gmail.com","display_order":4194304,"name":"Joaquín Panera","title":"Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals"},{"id":18064439,"work_id":4901973,"tagging_user_id":6396581,"tagged_user_id":4287495,"co_author_invite_id":null,"email":"c***e@mncn.csic.es","affiliation":"CSIC (Consejo Superior de Investigaciones Científicas-Spanish National Research Council)","display_order":6291456,"name":"Carmen Sesé","title":"Manzanares Valley (Madrid, Spain): A good country for Proboscideans and Neanderthals"}],"downloadable_attachments":[],"slug":"Manzanares_Valley_Madrid_Spain_A_good_country_for_Proboscideans_and_Neanderthals","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":6396581,"first_name":"jose","middle_initials":null,"last_name":"yravedra","page_name":"joseyravedra","domain_name":"ucm","created_at":"2013-10-26T21:59:58.395-07:00","display_name":"jose yravedra","url":"https://ucm.academia.edu/joseyravedra"},"attachments":[],"research_interests":[{"id":28126,"name":"Neanderthals (Palaeolithic Archaeology)","url":"https://www.academia.edu/Documents/in/Neanderthals_Palaeolithic_Archaeology_"},{"id":41112,"name":"Middle Palaeolithic","url":"https://www.academia.edu/Documents/in/Middle_Palaeolithic"},{"id":183314,"name":"Neanderthal subsistence","url":"https://www.academia.edu/Documents/in/Neanderthal_subsistence"},{"id":633101,"name":"Proboscidians, Elephant Mamut Paleoxodon Antiqus","url":"https://www.academia.edu/Documents/in/Proboscidians_Elephant_Mamut_Paleoxodon_Antiqus"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="6735220" id="2015"><div class="js-work-strip profile--work_container" data-work-id="12387946"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/12387946/haploidoceros_mediterraneus_una_nueva_especie_de_ciervo_en_el_pleistoceno_ib%C3%A9rico"><img alt="Research paper thumbnail of haploidoceros mediterraneus una nueva especie de ciervo en el pleistoceno ibérico" class="work-thumbnail" src="https://attachments.academia-assets.com/37637123/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/12387946/haploidoceros_mediterraneus_una_nueva_especie_de_ciervo_en_el_pleistoceno_ib%C3%A9rico">haploidoceros mediterraneus una nueva especie de ciervo en el pleistoceno ibérico</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://ucm.academia.edu/joseyravedra">jose yravedra</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="15e00e48a645ea43e861036c26d5d0b1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":37637123,"asset_id":12387946,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/37637123/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="12387946"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="12387946"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 12387946; 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</div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="7046039" id="drafts"><div class="js-work-strip profile--work_container" data-work-id="33230885"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/33230885/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_"><img alt="Research paper thumbnail of Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/53306186/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/33230885/Human_landscapes_of_the_Late_Glacial_Period_in_the_interior_of_the_Iberian_Peninsula_La_Pe%C3%B1a_de_Estebanvela_Segovia_Spain_">Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://ehu.academia.edu/LydiaZapata">Lydia Zapata</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://csic.academia.edu/CarmenSes%C3%A9">Carmen Sesé</a></span></div><div class="wp-workCard_item"><span>Poster presented at the XVIII INQUA Congress: The Magdalenian: Human Adaptations to the Late Last Glacial in Western and Central Europe, Berna, 2011.</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula cur...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440-21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770-12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). These dates embrace times of strong climatic oscillation, beginning with very rigorous environmental conditions (stage GS2) and ending with a temperate climate (Alleröd); over this period, extreme events such as Heinrich event 1 occurred. However, little information is available that would allow the environments through which human groups moved during the Late Last Glacial of the Iberian interior to be characterised. The La Peña de Estebanvela site is something of an exception in that its archaeological features allow the reconstruction of the surrounding environment, and provide information on how natural resources may have been used. The faunal remains represented at this site reﬂect changes in palaeoecology over time. Taphonomic analysis of recovered macromammals and lagomorphs shows that these animals were brought to the site, butchered and consumed. The available data on seasonality ﬁx the occupation of levels I-III from the spring to the autumn. Certain types of wood were collected for use as ﬁrewood. Other elements found in the record (personal ornaments, mobiliary art and raw materials) provide evidence that the people that occupied the site moved over a more extensive territory.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5034c252413e4cfcef51ee202231fd23" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53306186,"asset_id":33230885,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53306186/download_file?st=MTczMjgwMTM2NSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33230885"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33230885"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33230885; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=33230885]").text(description); $(".js-view-count[data-work-id=33230885]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 33230885; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='33230885']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 33230885, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "5034c252413e4cfcef51ee202231fd23" } } $('.js-work-strip[data-work-id=33230885]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":33230885,"title":"Human landscapes of the Late Glacial Period in the interior of the Iberian Peninsula: La Peña de Estebanvela (Segovia, Spain)","translated_title":"","metadata":{"abstract":"The chronostratigraphic framework of the Magdalenian in the interior of the Iberian Peninsula currently covers the period 21,440-21,040 cal BP (level 2 of the Cueva del Gato site at Epila, Province of Zaragoza) to 12,770-12,570 cal BP (level I of the La Peña de Estebanvela site, Ayllón, Province of Segovia). 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