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data-click-track="profile-works-tab" data-section-name="Call-for-papers" data-toggle="tab" href="#callforpapers" role="tab" style="border: none;"><span>1</span> Call for papers</a></li><li role="presentation"><a data-click-track="profile-works-tab" data-section-name="Conference-Presentations" data-toggle="tab" href="#conferencepresentations" role="tab" style="border: none;"><span>7</span> Conference Presentations</a></li></ul></li></ul></div><div class="divider ds-divider-16" style="margin: 0px;"></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Journal Papers" id="Journal Papers"><h3 class="profile--tab_heading_container">Journal Papers by Andreu Ollé</h3></div><div class="js-work-strip profile--work_container" data-work-id="8466609"><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/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_"><img alt="Research paper thumbnail of Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, 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/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_">Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ubu.academia.edu/%C3%81ngelCarrancho">Ángel Carrancho</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MontserratEstebannadal">Montserrat Esteban-nadal</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://univ-amu.academia.edu/DBourl%C3%A8s">D. Bourlès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/JosepMariaVerg%C3%A8s">Josep Maria Vergès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/RosaHuguet">Rosa Huguet</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/Luc%C3%ADaL%C3%B3pezPol%C3%ADn">Lucía López-Polín</a></span></div><div class="wp-workCard_item"><span>Vallverdú, J. et al. 2014. PLoS ONE 9, e103634</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The first arrivals of hominin populations into Eurasia during the Early Pleistocene are currently...</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 first arrivals of hominin populations into Eurasia during the Early Pleistocene are currently considered to have occurred as short and poorly dated biological dispersions. Questions as to the tempo and mode of these early prehistoric settlements have given rise to debates concerning the taxonomic significance of the lithic assemblages, as trace fossils, and the geographical distribution of the technological traditions found in the Lower Palaeolithic record. Here, we report on the Barranc de la Boella site which has yielded a lithic assemblage dating to ,1 million years ago that includes large cutting tools (LCT). We argue that distinct technological traditions coexisted in the Iberian archaeological repertoires of the late Early Pleistocene age in a similar way to the earliest sub-Saharan African artefact assemblages. These differences between stone tool assemblages may be attributed to the different chronologies of hominin dispersal events. The archaeological <br />record of Barranc de la Boella completes the geographical distribution of LCT assemblages across southern Eurasia during the EMPT (Early-Middle Pleistocene Transition, circa 942 to 641 kyr). Up to now, chronology of the earliest European LCT assemblages is based on the abundant Palaeolithic record found in terrace river sequences which have been dated to the end of the EMPT and later. However, the findings at Barranc de la Boella suggest that early LCT lithic assemblages appeared in the SW of Europe during earlier hominin dispersal episodes before the definitive colonization of temperate Eurasia took place.</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="8466609"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="8466609"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8466609; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=8466609]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8466609,"title":"Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, Spain)","internal_url":"https://www.academia.edu/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="7186887"><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/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_"><img alt="Research paper thumbnail of The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)" 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/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_">The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)</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://iphes.academia.edu/PaulaGarc%C3%ADaMedrano">Paula García-Medrano</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelC%C3%A1ceres">Isabel Cáceres</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span>Quaternary International</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, spec...</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 work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size <br />of the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.</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="7186887"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186887"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186887; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186887]").text(description); $(".js-view-count[data-work-id=7186887]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186887; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186887']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=7186887]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186887,"title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)","translated_title":"","metadata":{"abstract":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","more_info":"García-Medrano, P., Ollé, A., Mosquera, M., Cáceres, I., Díez, C., Carbonell, E., 2014. Quaternary International, 353-170-194","publication_name":"Quaternary International"},"translated_abstract":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","internal_url":"https://www.academia.edu/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_","translated_internal_url":"","created_at":"2014-05-28T07:20:39.548-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":31418960,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":8555584,"co_author_invite_id":6677090,"email":"p***o@gmail.com","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":-2,"name":"Paula García-Medrano","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920268,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":2877449,"co_author_invite_id":null,"email":"i***s@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":-1,"name":"Isabel Cáceres","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920270,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":2354763,"email":"i***s@prehistoria.urv.cat","display_order":1,"name":"Isabel Cáceres","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920271,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":201961,"email":"e***l@urv.cat","display_order":2,"name":"Eudald Carbonell","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920286,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":6034595,"co_author_invite_id":null,"email":"m***a@urv.cat","display_order":3,"name":"Marina Mosquera","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920287,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":32097084,"co_author_invite_id":null,"email":"e***l@iphes.cat","display_order":4,"name":"Eudald Carbonell","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":21192374,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":988520,"co_author_invite_id":null,"email":"c***a@ubu.es","display_order":5,"name":"carlos diez","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":31888545,"work_id":7186887,"tagging_user_id":8555584,"tagged_user_id":50384099,"co_author_invite_id":null,"email":"a***e@urv.cat","display_order":6,"name":"Andreu Cañellas","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"}],"downloadable_attachments":[],"slug":"The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galería_site_GII_Unit_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":2964767,"url":"http://dx.doi.org/10.1016/j.quaint.2014.03.053"}]}, 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="7186871"><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/7186871/Test_excavations_and_initial_results_at_the_Middle_and_Upper_Paleolithic_sites_of_Gilvaran_Kaldar_Ghamari_Caves_and_Gar_Arjene_Rockshelter_Khorramabad_Valley_western_Iran"><img alt="Research paper thumbnail of Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran, Kaldar, Ghamari Caves and Gar Arjene Rockshelter, Khorramabad Valley, western Iran" 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/7186871/Test_excavations_and_initial_results_at_the_Middle_and_Upper_Paleolithic_sites_of_Gilvaran_Kaldar_Ghamari_Caves_and_Gar_Arjene_Rockshelter_Khorramabad_Valley_western_Iran">Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran, Kaldar, Ghamari Caves and Gar Arjene Rockshelter, Khorramabad Valley, western Iran</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://deccancollege.academia.edu/SushamaDeo">Sushama Deo</a></span></div><div class="wp-workCard_item"><span>C.R. Palevol</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper introduces the excavations in several Paleolithic sites in the Khorramabad Val-ley, We...</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 introduces the excavations in several Paleolithic sites in the Khorramabad Val-ley, Western Iran. Apart from the two well-known sites of Ghamari Cave and Gar Arjenerock shelter, first excavated by Frank Hole and Kent Flannery in the 1960s, the Gilvaran and Kaldar caves were excavated for the first time. Here we present the stratigraphy of these sites, general data from the lithic assemblages, and the identifications of a small part of thefaunal remains. Preliminary results are showing that all of the sites were occupied from the Middle and Upper Paleolithic onward, and therefore provide great potential for the study of the transition between these cultural periods. Our preliminary techno-typological obser-vations show that the lower levels of the Gilvaran and Ghamari sequences may represent an early phase of the Middle Paleolithic.</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="7186871"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186871"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186871; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=7186871]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186871,"title":"Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran, Kaldar, Ghamari Caves and Gar Arjene Rockshelter, Khorramabad Valley, western Iran","internal_url":"https://www.academia.edu/7186871/Test_excavations_and_initial_results_at_the_Middle_and_Upper_Paleolithic_sites_of_Gilvaran_Kaldar_Ghamari_Caves_and_Gar_Arjene_Rockshelter_Khorramabad_Valley_western_Iran","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="7186862"><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/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context"><img alt="Research paper thumbnail of Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context" 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/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context">Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LenaAsryan">Lena Asryan</a></span></div><div class="wp-workCard_item"><span>Journal of Lithic Studies</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus)...</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">Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals. <br />The lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex. <br />Different local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.</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="7186862"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186862"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186862; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186862]").text(description); $(".js-view-count[data-work-id=7186862]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186862; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186862']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=7186862]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186862,"title":"Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context","translated_title":"","metadata":{"abstract":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","more_info":"Asryan, L., Ollé, A., Moloney, N., King, T., 2014. , Journal of Lithic Studies 1, 33-54.","publication_name":"Journal of Lithic Studies"},"translated_abstract":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","internal_url":"https://www.academia.edu/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context","translated_internal_url":"","created_at":"2014-05-28T07:17:31.750-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":19905148,"work_id":7186862,"tagging_user_id":2858486,"tagged_user_id":48557794,"co_author_invite_id":1791325,"email":"l***n@iphes.cat","display_order":0,"name":"Lena Asryan","title":"Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context"}],"downloadable_attachments":[],"slug":"Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":2966158,"url":"http://journals.ed.ac.uk/lithicstudies/article/view/775"}]}, 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="7186829"><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/7186829/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools"><img alt="Research paper thumbnail of Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools" 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/7186829/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools">Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools</a></div><div class="wp-workCard_item"><span>Journal of Lithic Studies</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">While many experimental studies have been done on siliceous and metamorphic rocks for both use-we...</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">While many experimental studies have been done on siliceous and metamorphic rocks for both use-wear and post depositional surface modification (PDSM) events, little is known about such experiments on volcanic materials (other than obsidian), and on basalt in particular. Here we present the preliminary results of several experiments related to: a) evidence for basalt use (e.g., butchery and fresh hide scraping) and the subsequent characteristic use-wear patterns that can be seen; and b) post-depositional surface modifications caused by bear (Ursidae) trampling on experimental basalt flakes and subsequent use of these flakes for a tumbling experiment in a special tumbling machine. <br />The results of these experiments were compared to better understand some surface modifications noted on the Middle to Upper Pleistocene lithic assemblages of the Azokh Cave site (Nagorno Karabagh, Lesser Caucasus). <br />Although some aspects of both events (use-wear and PDSM) remain to be studied in depth, the experiments have improved our understanding of the effects of use-wear and post-depositional trampling and tumbling on basalt lithic artefacts. In particular, it has allowed us to recognise mechanical alterations (e.g., cracks, striations, fractures, edge damage) caused by trampling and tumbling and to note differences between these modifications and those caused by use. In particular, the experiments have shown that macroscopic modifications are rarely diagnostic, especially those observed after use. Microscopic wear features such as edge rounding, polish, abrasion and striations were the most evident types of alteration on basalt flakes, although occurring at different times and from different types of use. Distribution and orientation of alterations may be key in distinguishing use-wear from post-depositional alterations on basalt artefacts.</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="7186829"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186829"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186829; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186829]").text(description); 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</script> <div class="js-work-strip profile--work_container" data-work-id="7186820"><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/7186820/La_Cova_de_Dalt_del_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3n_conclusiones_preliminares_de_las_intervenciones_arqueol%C3%B3gicas_1982_1987_2004_2012_"><img alt="Research paper thumbnail of La Cova de Dalt del Tossal de la Font (Vilafamés, Castellón): conclusiones preliminares de las intervenciones arqueológicas (1982-1987 / 2004-2012)" 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/7186820/La_Cova_de_Dalt_del_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3n_conclusiones_preliminares_de_las_intervenciones_arqueol%C3%B3gicas_1982_1987_2004_2012_">La Cova de Dalt del Tossal de la Font (Vilafamés, Castellón): conclusiones preliminares de las intervenciones arqueológicas (1982-1987 / 2004-2012)</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/Luc%C3%ADaL%C3%B3pezPol%C3%ADn">Lucía López-Polín</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelExp%C3%B3sitoBarea">Isabel Expósito Barea</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the 1980’s, archaeological excavations at the site of Cova de Dalt del Tossal de la Font 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">During the 1980’s, archaeological excavations at the site of Cova de Dalt del Tossal de la Font discovered an <br />important Upper Pleistocene karstic infilling. Three human fossils, ascribed generally to Neanderthals, stand out. Besides, <br />several herbivore and carnivore species and a small lithic assemblage were recovered. From 2004 to 2012 a second <br />campaign of excavations was carried out in the framework of a research agreement between the Jaume I University of <br />Castelló (UJI), the Archaeological and Prehistorical Research Service (SIAP) of the Diputació de Castelló, and the Catalan <br />Institute of Human Paleoecology and Social Evolution (IPHES). In this paper we present the currently available information <br />on the site, paying special attention to the taphonomical issues and the site formation processes.</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="7186820"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186820"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186820; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="6997272"><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/6997272/Usewear_sessions_at_the_XVII_UISPP_Congress_Burgos_Spain_September_2014_"><img alt="Research paper thumbnail of Usewear sessions at the XVII UISPP Congress (Burgos, Spain, September 2014)" class="work-thumbnail" src="https://attachments.academia-assets.com/33660856/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/6997272/Usewear_sessions_at_the_XVII_UISPP_Congress_Burgos_Spain_September_2014_">Usewear sessions at the XVII UISPP Congress (Burgos, Spain, September 2014)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="90b594bb23c2263855e30f40456293c0" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":33660856,"asset_id":6997272,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/33660856/download_file?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="6997272"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="6997272"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 6997272; 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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="5076930"><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/5076930/The_use_of_sequential_experiments_and_SEM_in_documenting_stone_tool_microwear"><img alt="Research paper thumbnail of The use of sequential experiments and SEM in documenting stone tool microwear" class="work-thumbnail" src="https://attachments.academia-assets.com/40531616/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/5076930/The_use_of_sequential_experiments_and_SEM_in_documenting_stone_tool_microwear">The use of sequential experiments and SEM in documenting stone tool microwear</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">""This paper focuses on a methodological proposal for documenting and describing the wear process...</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 focuses on a methodological proposal for documenting and describing the wear processes on lithic artefacts based on two main aspects: sequential experiments and systematic SEM (scanning electron microscope) analysis. <br />The procedures followed during experimentation, sample preparation and microscopic observation are presented, and a selection of our experimental results is described in detail and discussed. <br />We argue that sequential experiments allow stone tool wear to be closely monitored during use, and that this information is crucial in understanding microwear formation processes as well as in interpreting the traces observed on archaeological materials.""</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c4b634b0534b76e164d82c5ace40ed49" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":40531616,"asset_id":5076930,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/40531616/download_file?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="5076930"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="5076930"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 5076930; 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</script> <div class="js-work-strip profile--work_container" data-work-id="4404357"><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/4404357/Scanning_Electron_and_Optical_Light_Microscopy_two_complementary_approaches_for_the_understanding_and_interpretation_of_usewear_and_residues_on_stone_tools"><img alt="Research paper thumbnail of Scanning Electron and Optical Light Microscopy: two complementary approaches for the understanding and interpretation of usewear and residues on stone tools" 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/4404357/Scanning_Electron_and_Optical_Light_Microscopy_two_complementary_approaches_for_the_understanding_and_interpretation_of_usewear_and_residues_on_stone_tools">Scanning Electron and Optical Light Microscopy: two complementary approaches for the understanding and interpretation of usewear and residues on stone tools</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalaRobert">Robert Sala</a></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="4404357"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4404357"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4404357; 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="2281462"><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/2281462/From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe"><img alt="Research paper thumbnail of From Atapuerca to Europe: tracing back the earliest peopling of Europe" 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/2281462/From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe">From Atapuerca to Europe: tracing back the earliest peopling of Europe</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest ...</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 Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.</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="2281462"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281462"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281462; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2281462]").text(description); $(".js-view-count[data-work-id=2281462]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2281462; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2281462']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2281462]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281462,"title":"From Atapuerca to Europe: tracing back the earliest peopling of Europe","translated_title":"","metadata":{"abstract":"The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.","more_info":"Mosquera, M., Ollé, A. \u0026 Rodríguez, X. P. (2013). From Atapuerca to Europe: tracing back the earliest peopling of Europe. Quaternary International, 295: 130-137","publication_date":{"day":18,"month":4,"year":2013,"errors":{}}},"translated_abstract":"The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.","internal_url":"https://www.academia.edu/2281462/From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe","translated_internal_url":"","created_at":"2012-12-12T02:45:00.266-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":20435697,"work_id":2281462,"tagging_user_id":2858486,"tagged_user_id":6034595,"co_author_invite_id":null,"email":"m***a@urv.cat","display_order":0,"name":"Marina Mosquera","title":"From Atapuerca to Europe: tracing back the earliest peopling of Europe"},{"id":20435703,"work_id":2281462,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":201960,"email":"x***z@iphes.cat","display_order":4194304,"name":"Xose-pedro Rodriguez","title":"From Atapuerca to Europe: tracing back the earliest peopling of Europe"}],"downloadable_attachments":[],"slug":"From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":415280,"url":"http://www.sciencedirect.com/science/article/pii/S1040618212000468"}]}, 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="2281455"><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/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_"><img alt="Research paper thumbnail of The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_">The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/ameliabargallo">amelia bargallo</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://todofp.academia.edu/BelenMarquez">Belen Marquez</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MarinaMosquera">Marina Mosquera</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technol...</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 Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).</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="2281455"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281455"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281455; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2281455]").text(description); $(".js-view-count[data-work-id=2281455]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2281455; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2281455']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2281455]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281455,"title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)","translated_title":"","metadata":{"abstract":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","more_info":"Ollé, A., Mosquera, M., Rodríguez, X. P., de Lombera-Hermida, A., García-Antón, M. D., García-Medrano, P., Peña, L., Menéndez, L., Navazo, M., Terradillos, M., Bargalló, A., Márquez, B., Sala, R. \u0026 Carbonell, E. (ip). Quaternary International, 295: 138-167","publication_date":{"day":18,"month":4,"year":2013,"errors":{}}},"translated_abstract":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","internal_url":"https://www.academia.edu/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_","translated_internal_url":"","created_at":"2012-12-12T02:42:35.081-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":8019056,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":322629,"email":"a***a@prehistoria.urv.cat","display_order":0,"name":"Arturo Lombera","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8019058,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":492560,"email":"l***g@prehistoria.urv.cat","display_order":6291456,"name":"Leticia Menéndez","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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Atapuerca (Burgos, Spain)"},{"id":8485058,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":7499599,"co_author_invite_id":null,"email":"m***o@ubu.es","display_order":8380416,"name":"Marta Navazo","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485059,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":null,"co_author_invite_id":316980,"email":"r***a@urv.net","display_order":8384512,"name":"Robert Sala","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485060,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":7915440,"co_author_invite_id":null,"email":"r***a@urv.cat","affiliation":"Universitat Rovira i Virgili","display_order":8386560,"name":"Robert Sala Ramos","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485082,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":null,"co_author_invite_id":201960,"email":"x***z@iphes.cat","display_order":8387584,"name":"Xosé-Pedro Rodríguez-Álvarez","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485084,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":null,"co_author_invite_id":201961,"email":"e***l@urv.cat","display_order":8388096,"name":"Eudald Carbonell","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485086,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":32097084,"co_author_invite_id":null,"email":"e***l@iphes.cat","display_order":8388352,"name":"Eudald Carbonell","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485088,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":null,"co_author_invite_id":1696108,"email":"a***e@prehistoria.urv.net","display_order":8388480,"name":"Andreu OllÉ","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485090,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":null,"co_author_invite_id":1244716,"email":"r***u@math.ncsu.edu","display_order":8388544,"name":"Xose RodrÍguez","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8485109,"work_id":2281455,"tagging_user_id":287391,"tagged_user_id":6034595,"co_author_invite_id":null,"email":"m***a@urv.cat","display_order":8388576,"name":"Marina Mosquera","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":19905209,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":1135489,"co_author_invite_id":null,"email":"m***s@hotmail.com","affiliation":"Universidad Internacional Isabel I de Castilla","display_order":8388592,"name":"Marcos Terradillos-Bernal","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"}],"downloadable_attachments":[],"slug":"The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":415278,"url":"http://www.sciencedirect.com/science/article/pii/S1040618211006483"}]}, 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="2898699"><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/2898699/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_"><img alt="Research paper thumbnail of New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)" 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/2898699/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_">New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/GiovanniSimone">Giovanni Di Simone</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://uib-es.academia.edu/Lloren%C3%A7PicornellGelabert">Llorenç Picornell-Gelabert</a></span></div><div class="wp-workCard_item"><span>C.R. Palevol doi:10.1016/j.crpv.2012.11.002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in S...</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">Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.</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="2898699"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2898699"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2898699; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2898699]").text(description); $(".js-view-count[data-work-id=2898699]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2898699; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2898699']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2898699]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2898699,"title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)","translated_title":"","metadata":{"abstract":"Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.","more_info":"Forgia,V., Martín,P., López-García,J.M., Ollé,A., Vergès,J.M., Allué,E., Angelucci,D.E., Arnone,M., Blain,H.-A., Burjachs,F., Expósito,I., Messina,A., Picornell,L., Rodríguez,A., Scopelliti,G., Sieno,L., Virruso,G., Alessi,E., Di Simone,G., Morales,J.I., Pagano,E. \u0026 Belvedere,O. (2013)","publication_name":"C.R. Palevol doi:10.1016/j.crpv.2012.11.002"},"translated_abstract":"Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.","internal_url":"https://www.academia.edu/2898699/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_","translated_internal_url":"","created_at":"2013-03-04T00:20:34.657-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":8018947,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2787872,"co_author_invite_id":null,"email":"m***e@tin.it","display_order":0,"name":"Massimo Arnone","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018948,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":34945932,"co_author_invite_id":null,"email":"v***a@gmail.com","affiliation":"Università degli Studi di Palermo","display_order":4194304,"name":"Vincenza Forgia","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018949,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":9912093,"co_author_invite_id":null,"email":"c***5@hotmail.it","display_order":6291456,"name":"Giovanni Di Simone","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018950,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2836831,"co_author_invite_id":null,"email":"a***z@gmail.com","display_order":7340032,"name":"Ana Rodriguez Cruz","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018951,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2895203,"co_author_invite_id":null,"email":"p***9@hotmail.com","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":7864320,"name":"Patricia Martín","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018952,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2710684,"co_author_invite_id":null,"email":"p***9@gmail.com","affiliation":"Universidad de Barcelona","display_order":8126464,"name":"Patricia Martín","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018953,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":380538,"co_author_invite_id":null,"email":"j***s@gmail.com","affiliation":"University of Barcelona","display_order":8257536,"name":"Juan I. Morales","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":8018954,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2819990,"co_author_invite_id":null,"email":"g***o@gmail.com","display_order":8323072,"name":"Giovanni Virruso","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":15062711,"work_id":2898699,"tagging_user_id":380538,"tagged_user_id":45768498,"co_author_invite_id":203111,"email":"h***n@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":8355840,"name":"Hugues-Alexandre Blain","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":15062714,"work_id":2898699,"tagging_user_id":380538,"tagged_user_id":3017074,"co_author_invite_id":null,"email":"j***s@gmail.com","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":8372224,"name":"Francesc Burjachs","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":15062726,"work_id":2898699,"tagging_user_id":380538,"tagged_user_id":1083046,"co_author_invite_id":null,"email":"e***e@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":8384512,"name":"Ethel Allue","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":15062729,"work_id":2898699,"tagging_user_id":380538,"tagged_user_id":10574694,"co_author_invite_id":null,"email":"j***s@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":8386560,"name":"Josep Maria Vergès","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":15062735,"work_id":2898699,"tagging_user_id":380538,"tagged_user_id":null,"co_author_invite_id":2232136,"email":"p***n@sydney.edu.au","display_order":8387584,"name":"Patricia Martin","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":19905205,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":2288451,"email":"i***a@prehistoria.urv.cat","display_order":8388096,"name":"Isabel Expósito","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"},{"id":19905206,"work_id":2898699,"tagging_user_id":2858486,"tagged_user_id":2530541,"co_author_invite_id":null,"email":"t***4@gmail.com","affiliation":"Universitat de les Illes Balears","display_order":8388352,"name":"Llorenç Picornell-Gelabert","title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)"}],"downloadable_attachments":[],"slug":"New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":777875,"url":"http://www.sciencedirect.com/science/article/pii/S1631068312001959"}]}, 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="2898539"><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/2898539/The_first_evidence_of_cut_marks_and_usewear_traces_from_the_Plio_Pleistocene_locality_of_El_Kherba_Ain_Hanech_Algeria_implications_for_early_hominin_subsistence_activities_circa_1_8_Ma"><img alt="Research paper thumbnail of The first evidence of cut marks and usewear traces from the Plio-Pleistocene locality of El-Kherba (Ain Hanech), Algeria : implications for early hominin subsistence activities circa 1.8 Ma" 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/2898539/The_first_evidence_of_cut_marks_and_usewear_traces_from_the_Plio_Pleistocene_locality_of_El_Kherba_Ain_Hanech_Algeria_implications_for_early_hominin_subsistence_activities_circa_1_8_Ma">The first evidence of cut marks and usewear traces from the Plio-Pleistocene locality of El-Kherba (Ain Hanech), Algeria : implications for early hominin subsistence activities circa 1.8 Ma</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/JanVanDerMade">Jan Van Der Made</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The current archaeological data on early hominin subsistence activities in Africa are derived chi...</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 current archaeological data on early hominin subsistence activities in Africa are derived chiefly from Sub-Saharan Plio-Pleistocene sites. The recent studies at El-Kherba (Ain Hanech) in northeastern Algeria expand the geographic range of evidence of hominin subsistence patterns to include the earliest known archaeological sites documented in North Africa. Dated to 1.78 million years ago (Ma), excavations from El-Kherba yielded an Oldowan industry associated with a savanna-like fauna contained in floodplain deposits. The faunal assemblage is dominated by large and medium-sized animals (mainly adults), especially equids, which are represented by at least 11 individuals. The mammalian archaeofauna preserves numerous cut-marked and hammerstone-percussed bones. Made of primarily limestone and flint, the stone assemblage consists of core forms, débitage, and retouched pieces. Evidence of usewear traces is found on several of the flint artifacts, indicating meat processing by early hominins. Overall, our subsistence analysis indicates that early hominins were largely responsible for bone modification at the site, which is also corroborated by other relevant taphonomic evidence. Moreover, at 1.78 Ma, the cutmarked bones recovered from El-Kherba represent the earliest known evidence for ancestral hominin butchery activities and large animal foraging capabilities in northern Africa.</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="2898539"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2898539"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2898539; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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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="2281433"><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/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence"><img alt="Research paper thumbnail of Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence" 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/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence">Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/HuguesAlexandreBlain">Hugues-Alexandre Blain</a></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="2281433"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281433"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281433; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2281433]").text(description); $(".js-view-count[data-work-id=2281433]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2281433; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2281433']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2281433]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281433,"title":"Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence","internal_url":"https://www.academia.edu/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2276611"><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/2276611/One_million_years_of_cultural_evolution_in_a_stable_environment_at_Atapuerca_Burgos_Spain_"><img alt="Research paper thumbnail of One million years of cultural evolution in a stable environment at Atapuerca (Burgos, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/36401884/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/2276611/One_million_years_of_cultural_evolution_in_a_stable_environment_at_Atapuerca_Burgos_Spain_">One million years of cultural evolution in a stable environment at Atapuerca (Burgos, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelExp%C3%B3sitoBarea">Isabel Expósito Barea</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://urv.academia.edu/MariaBennasar">Maria Bennàsar</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/HuguesAlexandreBlain">Hugues-Alexandre Blain</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present paper analyses the evidence provided by three sites (Sima del Elefante, Gran Dolina, ...</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 present paper analyses the evidence provided by three sites (Sima del Elefante, Gran Dolina, and Galería) located in the Trinchera del Ferrocarril of the Sierra de Atapuerca. These three sites are cave infillings that contain sediments deposited from approximately 1.2 Ma to 200 kyr. Pollen, herpetofauna, and small and large mammal remains are used as proxies to obtain a general picture of the environmental changes that occurred at the Sierra de Atapuerca throughout the one million-year period represented at these sites. Similarly, cultural changes are tracked analyzing the evidence of human behavior obtained from the study of several bone and lithic assemblages from these three sites. At least three periods with different cultural features, involving technology, subsistence and behavior, are determined from the available evidence. The first two periods correspond to the Mode 1 technology and Homo antecessor: the first is dated around 1.2 to 1.0 Ma and reflects opportunistic behavior both in technology and subsistence. The second period is around 800 kyr BP. Mode 1 technology is still maintained, but subsistence strategies include systematic hunting and the use of base camps. The third period is dated between 500 ka and 200 ka and corresponds to the Mode 2 technology and the acquisition of directional hunting and other organizational strategies by Homo heidelbergensis. A transition from Mode 2 to Mode 3 seems to appear at the end of this time-range, and may reflect the early phases of a fourth cultural change. With regard to the environment, our main conclusion is that there was an absence of extremely harsh conditions at Atapuerca throughout this time period. The presence of Mediterranean taxa was constant and the dominant landscape was a savannah-like open environment, probably with small forest patches. An alternation of Mediterranean and mesic species Quaternary Science Reviews 30 as the dominant component of the tree storey was induced by the climatic cycles, and steppes spread across the landscape during the drier periods. In any case, it is not possible to establish clear cut-off points separating entirely different environmental episodes. Our results show no evidence of any relationship between environmental change and cultural change at the Sierra de Atapuerca.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1e3b4206d052173aa132d50ccc797f81" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":36401884,"asset_id":2276611,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/36401884/download_file?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="2276611"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2276611"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2276611; 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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="2276566"><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/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data"><img alt="Research paper thumbnail of Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data" 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/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data">Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The functional study of the stone tool artefacts from the Middle Pleistocene site of Isernia la P...</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 functional study of the stone tool artefacts from the Middle Pleistocene site of Isernia la Pineta (Molise, central Italy) revealed microtraces that display certain features that did not fit in with what we know as use-wear traces. The suspicion that these microtraces may be technical traces derived from bipolar flaking, which is prevalent at this site, led us to initiate an experimental programme to check our hypothesis. The experiments conducted allowed us to identify residues associated with bipolar flaking on an anvil and to characterise the microscopic traces derived from this production technique. Our results proved very useful in identifying the artefacts produced by bipolar flaking, as well as in determining the basic lithological features of the anvil. Moreover, these experiments allowed us to assess the possible interferences that these kinds of technical traces can cause when performing the functional analyses of lithic assemblages produced by the bipolar technique.► We present the results of an experimental programme on bipolar knapping on an anvil. ► First we study the mechanics of bipolar flaking and the variants of the technique. ► We describe under SEM the resulting technical deposits of residues and microtraces. ► These traces can easily mimic usewear traces and, so, interfere functional studies.</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="2276566"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2276566"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2276566; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2276566]").text(description); $(".js-view-count[data-work-id=2276566]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2276566; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2276566']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2276566]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2276566,"title":"Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data","internal_url":"https://www.academia.edu/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2298642"><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/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_"><img alt="Research paper thumbnail of Early hominid dispersals: a technological hypothesis for “out of Africa”" 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/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_">Early hominid dispersals: a technological hypothesis for “out of Africa”</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BienvenidoMart%C3%ADnezNavarro">Bienvenido Martínez-Navarro</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Homo is the only genus that responds to environmental pressures by adopting such strategies as no...</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">Homo is the only genus that responds to environmental pressures by adopting such strategies as non-standardized behaviour, a general diet, and technology. Considering that basic idea, this paper introduces the general hypothesis that the Pliocene and Early Pleistocene Homo dispersals within and out of Africa were consequences of that human characteristic behaviour. In particular, they were driven by a process starting with the emergence of technology, followed in a second phase by its socialization. From this point, social reorganization within communities (changing behaviours and social, cultural and economic strategies) occurred, driving demographic growth, and frequently geographic expansion.</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="2298642"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298642"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298642; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2298642]").text(description); $(".js-view-count[data-work-id=2298642]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2298642; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2298642']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2298642]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2298642,"title":"Early hominid dispersals: a technological hypothesis for “out of Africa”","internal_url":"https://www.academia.edu/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2298560"><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/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas"><img alt="Research paper thumbnail of Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas" 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/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas">Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalaRobert">Robert Sala</a></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="2298560"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298560"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298560; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2298560]").text(description); $(".js-view-count[data-work-id=2298560]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2298560; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2298560']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2298560]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2298560,"title":"Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas","internal_url":"https://www.academia.edu/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="329507" id="journalpapers"><div class="js-work-strip profile--work_container" data-work-id="8466609"><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/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_"><img alt="Research paper thumbnail of Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, 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/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_">Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://ubu.academia.edu/%C3%81ngelCarrancho">Ángel Carrancho</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MontserratEstebannadal">Montserrat Esteban-nadal</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://univ-amu.academia.edu/DBourl%C3%A8s">D. Bourlès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/JosepMariaVerg%C3%A8s">Josep Maria Vergès</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/RosaHuguet">Rosa Huguet</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/Luc%C3%ADaL%C3%B3pezPol%C3%ADn">Lucía López-Polín</a></span></div><div class="wp-workCard_item"><span>Vallverdú, J. et al. 2014. PLoS ONE 9, e103634</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The first arrivals of hominin populations into Eurasia during the Early Pleistocene are currently...</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 first arrivals of hominin populations into Eurasia during the Early Pleistocene are currently considered to have occurred as short and poorly dated biological dispersions. Questions as to the tempo and mode of these early prehistoric settlements have given rise to debates concerning the taxonomic significance of the lithic assemblages, as trace fossils, and the geographical distribution of the technological traditions found in the Lower Palaeolithic record. Here, we report on the Barranc de la Boella site which has yielded a lithic assemblage dating to ,1 million years ago that includes large cutting tools (LCT). We argue that distinct technological traditions coexisted in the Iberian archaeological repertoires of the late Early Pleistocene age in a similar way to the earliest sub-Saharan African artefact assemblages. These differences between stone tool assemblages may be attributed to the different chronologies of hominin dispersal events. The archaeological <br />record of Barranc de la Boella completes the geographical distribution of LCT assemblages across southern Eurasia during the EMPT (Early-Middle Pleistocene Transition, circa 942 to 641 kyr). Up to now, chronology of the earliest European LCT assemblages is based on the abundant Palaeolithic record found in terrace river sequences which have been dated to the end of the EMPT and later. However, the findings at Barranc de la Boella suggest that early LCT lithic assemblages appeared in the SW of Europe during earlier hominin dispersal episodes before the definitive colonization of temperate Eurasia took place.</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="8466609"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="8466609"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8466609; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=8466609]").text(description); $(".js-view-count[data-work-id=8466609]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 8466609; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='8466609']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=8466609]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":8466609,"title":"Age and Date for Early Arrival of the Acheulian in Europe (Barranc de la Boella, la Canonja, Spain)","internal_url":"https://www.academia.edu/8466609/Age_and_Date_for_Early_Arrival_of_the_Acheulian_in_Europe_Barranc_de_la_Boella_la_Canonja_Spain_","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="7186887"><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/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_"><img alt="Research paper thumbnail of The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)" 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/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_">The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)</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://iphes.academia.edu/PaulaGarc%C3%ADaMedrano">Paula García-Medrano</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelC%C3%A1ceres">Isabel Cáceres</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span>Quaternary International</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, spec...</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 work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size <br />of the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.</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="7186887"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186887"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186887; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186887]").text(description); $(".js-view-count[data-work-id=7186887]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186887; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186887']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=7186887]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186887,"title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)","translated_title":"","metadata":{"abstract":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","more_info":"García-Medrano, P., Ollé, A., Mosquera, M., Cáceres, I., Díez, C., Carbonell, E., 2014. Quaternary International, 353-170-194","publication_name":"Quaternary International"},"translated_abstract":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","internal_url":"https://www.academia.edu/7186887/The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galer%C3%ADa_site_GII_Unit_","translated_internal_url":"","created_at":"2014-05-28T07:20:39.548-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":31418960,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":8555584,"co_author_invite_id":6677090,"email":"p***o@gmail.com","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":-2,"name":"Paula García-Medrano","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920268,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":2877449,"co_author_invite_id":null,"email":"i***s@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":-1,"name":"Isabel Cáceres","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920270,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":2354763,"email":"i***s@prehistoria.urv.cat","display_order":1,"name":"Isabel Cáceres","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920271,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":201961,"email":"e***l@urv.cat","display_order":2,"name":"Eudald Carbonell","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920286,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":6034595,"co_author_invite_id":null,"email":"m***a@urv.cat","display_order":3,"name":"Marina Mosquera","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":11920287,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":32097084,"co_author_invite_id":null,"email":"e***l@iphes.cat","display_order":4,"name":"Eudald Carbonell","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":21192374,"work_id":7186887,"tagging_user_id":2858486,"tagged_user_id":988520,"co_author_invite_id":null,"email":"c***a@ubu.es","display_order":5,"name":"carlos diez","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"},{"id":31888545,"work_id":7186887,"tagging_user_id":8555584,"tagged_user_id":50384099,"co_author_invite_id":null,"email":"a***e@urv.cat","display_order":6,"name":"Andreu Cañellas","title":"The earliest Acheulean technology at Atapuerca (Burgos, Spain): Oldest levels of the Galería site (GII Unit)"}],"downloadable_attachments":[],"slug":"The_earliest_Acheulean_technology_at_Atapuerca_Burgos_Spain_Oldest_levels_of_the_Galería_site_GII_Unit_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"This work presents a study of the oldest Acheulean lithic assemblages from the Galería site, specifically the GIIa subunit, which has been dated to c. 503 \u0002 95 ka, and compares them with the subsequent subunit in the sequence, GIIb, dated to around 237e269 ka. The main goals of this study are to offer a detailed technological characterization of the earliest Acheulean presence in Atapuerca and to assess the elements determining the technological variability in a given site by studying the sequence, evaluating the concept of variability and defining the aspects which determine it. The Galería site does not display the features of a living space. It is a cave which was accessed by both humans and carnivores in order to obtain the animal biomass of the herbivores that had fallen down into the cave through a natural shaft. The archaeological record is therefore incomplete and fragmented, since it is the product of highly changeable occupational dynamics. In the lower Galería levels, we identified the development from an almost exclusive use of cobbles as blanks for knapping activities in the earliest periods to an increasing use of flakes. In terms of raw materials, the initially predominant use of Neogene chert and quartzite evolved towards a more balanced use of six raw materials. Furthermore, there was an increase in the size \r\nof the large tools. After comparing these two Acheulean assemblages, it is important to put them into context by taking into account a) the significance of cobbles and flakes as blanks; b) the significance of cleavers; and c) the use of raw materials such as quartzite, sandstone or chert. These aspects have traditionally been used to facilitate comparisons of the technologies used within the Iberian Peninsula, and comparisons between the Acheulean technology of the Iberian Peninsula and North Africa and the European (i.e. trans-Pyrenean) Acheulean technology.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":2964767,"url":"http://dx.doi.org/10.1016/j.quaint.2014.03.053"}]}, 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="7186871"><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/7186871/Test_excavations_and_initial_results_at_the_Middle_and_Upper_Paleolithic_sites_of_Gilvaran_Kaldar_Ghamari_Caves_and_Gar_Arjene_Rockshelter_Khorramabad_Valley_western_Iran"><img alt="Research paper thumbnail of Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran, Kaldar, Ghamari Caves and Gar Arjene Rockshelter, Khorramabad Valley, western Iran" 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/7186871/Test_excavations_and_initial_results_at_the_Middle_and_Upper_Paleolithic_sites_of_Gilvaran_Kaldar_Ghamari_Caves_and_Gar_Arjene_Rockshelter_Khorramabad_Valley_western_Iran">Test excavations and initial results at the Middle and Upper Paleolithic sites of Gilvaran, Kaldar, Ghamari Caves and Gar Arjene Rockshelter, Khorramabad Valley, western Iran</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://deccancollege.academia.edu/SushamaDeo">Sushama Deo</a></span></div><div class="wp-workCard_item"><span>C.R. Palevol</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper introduces the excavations in several Paleolithic sites in the Khorramabad Val-ley, We...</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 introduces the excavations in several Paleolithic sites in the Khorramabad Val-ley, Western Iran. Apart from the two well-known sites of Ghamari Cave and Gar Arjenerock shelter, first excavated by Frank Hole and Kent Flannery in the 1960s, the Gilvaran and Kaldar caves were excavated for the first time. Here we present the stratigraphy of these sites, general data from the lithic assemblages, and the identifications of a small part of thefaunal remains. Preliminary results are showing that all of the sites were occupied from the Middle and Upper Paleolithic onward, and therefore provide great potential for the study of the transition between these cultural periods. Our preliminary techno-typological obser-vations show that the lower levels of the Gilvaran and Ghamari sequences may represent an early phase of the Middle Paleolithic.</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="7186871"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186871"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186871; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186871]").text(description); $(".js-view-count[data-work-id=7186871]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186871; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186871']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(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="7186862"><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/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context"><img alt="Research paper thumbnail of Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context" 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/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context">Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LenaAsryan">Lena Asryan</a></span></div><div class="wp-workCard_item"><span>Journal of Lithic Studies</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus)...</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">Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals. <br />The lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex. <br />Different local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.</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="7186862"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186862"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186862; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186862]").text(description); $(".js-view-count[data-work-id=7186862]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186862; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186862']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=7186862]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186862,"title":"Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context","translated_title":"","metadata":{"abstract":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","more_info":"Asryan, L., Ollé, A., Moloney, N., King, T., 2014. , Journal of Lithic Studies 1, 33-54.","publication_name":"Journal of Lithic Studies"},"translated_abstract":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","internal_url":"https://www.academia.edu/7186862/Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context","translated_internal_url":"","created_at":"2014-05-28T07:17:31.750-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":19905148,"work_id":7186862,"tagging_user_id":2858486,"tagged_user_id":48557794,"co_author_invite_id":1791325,"email":"l***n@iphes.cat","display_order":0,"name":"Lena Asryan","title":"Lithic assemblages of Azokh Cave (Nagorno Karabagh, Lesser Caucasus): raw materials, technology and regional context"}],"downloadable_attachments":[],"slug":"Lithic_assemblages_of_Azokh_Cave_Nagorno_Karabagh_Lesser_Caucasus_raw_materials_technology_and_regional_context","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Azokh Cave is a Middle Pleistocene to Holocene site located in Nagorno Karabagh (Lesser Caucasus). The main entrance, Azokh 1, is a large cave that has two geological sequences (lower and upper) with nine geo-archaeological units of which only the upper ones (Units I to V) have a significant archaeological record. The faunal remains and lithic artefacts in these units indicate aspects of human occupation, and exploitation of, and association with animals.\r\nThe lithic artefacts presented here were recovered from Units V, III and II during the 2002 – 2009 excavation seasons. The available chronological data indicates an age between 293 – 100 Ka for these units. The operational chain is incomplete and artefacts found in the cave are primarily end-products dominated by flake-tools. The assemblage of Unit V is composed primarily of simple, unretouched flakes with a minimal presence of retouched flakes and cores. The Unit II lithic assemblage includes a substantial Levallois component, although with fewer cores and retouched flakes. There are very few flake tools in Unit III. While it is still difficult to assign the Unit V assemblage to a techno-typological group or complex (i.e. Acheulean, Mousterian or other local techno-complexes such as the Kudarian), the Unit II assemblage is clearly associated with Mode 3 or the Mousterian techno-complex.\r\nDifferent local and non-local raw materials were exploited in all units for the production of lithic artefacts, although the range of raw materials is more varied in Unit II. Local chert, flint and basalt were used most commonly, probably due to their easy accessibility. Limestone, jasper and sandstone, from local and non-local sources, are present in small quantities in Units V and II. Obsidian is the only raw material that possibly originates from more distant sources. Flint and chert appear to have been preferentially exploited for flake tool production in all units, but the toolmakers show a preference for better quality raw material (flint, basalt, obsidian) for retouched pieces in Units V and II, and for Levallois production in Unit II.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":2966158,"url":"http://journals.ed.ac.uk/lithicstudies/article/view/775"}]}, 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="7186829"><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/7186829/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools"><img alt="Research paper thumbnail of Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools" 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/7186829/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools">Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools</a></div><div class="wp-workCard_item"><span>Journal of Lithic Studies</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">While many experimental studies have been done on siliceous and metamorphic rocks for both use-we...</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">While many experimental studies have been done on siliceous and metamorphic rocks for both use-wear and post depositional surface modification (PDSM) events, little is known about such experiments on volcanic materials (other than obsidian), and on basalt in particular. Here we present the preliminary results of several experiments related to: a) evidence for basalt use (e.g., butchery and fresh hide scraping) and the subsequent characteristic use-wear patterns that can be seen; and b) post-depositional surface modifications caused by bear (Ursidae) trampling on experimental basalt flakes and subsequent use of these flakes for a tumbling experiment in a special tumbling machine. <br />The results of these experiments were compared to better understand some surface modifications noted on the Middle to Upper Pleistocene lithic assemblages of the Azokh Cave site (Nagorno Karabagh, Lesser Caucasus). <br />Although some aspects of both events (use-wear and PDSM) remain to be studied in depth, the experiments have improved our understanding of the effects of use-wear and post-depositional trampling and tumbling on basalt lithic artefacts. In particular, it has allowed us to recognise mechanical alterations (e.g., cracks, striations, fractures, edge damage) caused by trampling and tumbling and to note differences between these modifications and those caused by use. In particular, the experiments have shown that macroscopic modifications are rarely diagnostic, especially those observed after use. Microscopic wear features such as edge rounding, polish, abrasion and striations were the most evident types of alteration on basalt flakes, although occurring at different times and from different types of use. Distribution and orientation of alterations may be key in distinguishing use-wear from post-depositional alterations on basalt artefacts.</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="7186829"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186829"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186829; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=7186829]").text(description); $(".js-view-count[data-work-id=7186829]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 7186829; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='7186829']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=7186829]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":7186829,"title":"Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools","internal_url":"https://www.academia.edu/7186829/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="7186820"><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/7186820/La_Cova_de_Dalt_del_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3n_conclusiones_preliminares_de_las_intervenciones_arqueol%C3%B3gicas_1982_1987_2004_2012_"><img alt="Research paper thumbnail of La Cova de Dalt del Tossal de la Font (Vilafamés, Castellón): conclusiones preliminares de las intervenciones arqueológicas (1982-1987 / 2004-2012)" 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/7186820/La_Cova_de_Dalt_del_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3n_conclusiones_preliminares_de_las_intervenciones_arqueol%C3%B3gicas_1982_1987_2004_2012_">La Cova de Dalt del Tossal de la Font (Vilafamés, Castellón): conclusiones preliminares de las intervenciones arqueológicas (1982-1987 / 2004-2012)</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/Luc%C3%ADaL%C3%B3pezPol%C3%ADn">Lucía López-Polín</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelExp%C3%B3sitoBarea">Isabel Expósito Barea</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">During the 1980’s, archaeological excavations at the site of Cova de Dalt del Tossal de la Font 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">During the 1980’s, archaeological excavations at the site of Cova de Dalt del Tossal de la Font discovered an <br />important Upper Pleistocene karstic infilling. Three human fossils, ascribed generally to Neanderthals, stand out. Besides, <br />several herbivore and carnivore species and a small lithic assemblage were recovered. From 2004 to 2012 a second <br />campaign of excavations was carried out in the framework of a research agreement between the Jaume I University of <br />Castelló (UJI), the Archaeological and Prehistorical Research Service (SIAP) of the Diputació de Castelló, and the Catalan <br />Institute of Human Paleoecology and Social Evolution (IPHES). In this paper we present the currently available information <br />on the site, paying special attention to the taphonomical issues and the site formation processes.</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="7186820"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="7186820"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 7186820; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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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="5076930"><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/5076930/The_use_of_sequential_experiments_and_SEM_in_documenting_stone_tool_microwear"><img alt="Research paper thumbnail of The use of sequential experiments and SEM in documenting stone tool microwear" class="work-thumbnail" src="https://attachments.academia-assets.com/40531616/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/5076930/The_use_of_sequential_experiments_and_SEM_in_documenting_stone_tool_microwear">The use of sequential experiments and SEM in documenting stone tool microwear</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">""This paper focuses on a methodological proposal for documenting and describing the wear process...</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 focuses on a methodological proposal for documenting and describing the wear processes on lithic artefacts based on two main aspects: sequential experiments and systematic SEM (scanning electron microscope) analysis. <br />The procedures followed during experimentation, sample preparation and microscopic observation are presented, and a selection of our experimental results is described in detail and discussed. <br />We argue that sequential experiments allow stone tool wear to be closely monitored during use, and that this information is crucial in understanding microwear formation processes as well as in interpreting the traces observed on archaeological materials.""</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c4b634b0534b76e164d82c5ace40ed49" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":40531616,"asset_id":5076930,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/40531616/download_file?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="5076930"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="5076930"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 5076930; 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</script> <div class="js-work-strip profile--work_container" data-work-id="4404357"><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/4404357/Scanning_Electron_and_Optical_Light_Microscopy_two_complementary_approaches_for_the_understanding_and_interpretation_of_usewear_and_residues_on_stone_tools"><img alt="Research paper thumbnail of Scanning Electron and Optical Light Microscopy: two complementary approaches for the understanding and interpretation of usewear and residues on stone tools" 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/4404357/Scanning_Electron_and_Optical_Light_Microscopy_two_complementary_approaches_for_the_understanding_and_interpretation_of_usewear_and_residues_on_stone_tools">Scanning Electron and Optical Light Microscopy: two complementary approaches for the understanding and interpretation of usewear and residues on stone tools</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalaRobert">Robert Sala</a></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="4404357"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="4404357"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4404357; 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} }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="2281462"><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/2281462/From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe"><img alt="Research paper thumbnail of From Atapuerca to Europe: tracing back the earliest peopling of Europe" 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/2281462/From_Atapuerca_to_Europe_tracing_back_the_earliest_peopling_of_Europe">From Atapuerca to Europe: tracing back the earliest peopling of Europe</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest ...</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 Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.</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="2281462"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281462"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281462; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2281462]").text(description); $(".js-view-count[data-work-id=2281462]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2281462; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2281462']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2281462]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281462,"title":"From Atapuerca to Europe: tracing back the earliest peopling of Europe","translated_title":"","metadata":{"abstract":"The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.","more_info":"Mosquera, M., Ollé, A. \u0026 Rodríguez, X. P. (2013). From Atapuerca to Europe: tracing back the earliest peopling of Europe. Quaternary International, 295: 130-137","publication_date":{"day":18,"month":4,"year":2013,"errors":{}}},"translated_abstract":"The Sierra de Atapuerca sites (Spain) have yielded excellent data and they represent the longest chronological sequence discovered in Europe to date, covering the late Early Pleistocene to the late Middle Pleistocene. In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. 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These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. 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In view of these exceptional characteristics, this work aims to meet three objectives: to characterise the technological features of various key European sites in relation to the significant factors observed through the Atapuerca sequence; to evaluate whether technological evolution in Europe during the Early and the Middle Pleistocene is consistent with that of Atapuerca; and finally, to consider the possibility of extrapolating population inferences from Atapuerca to the rest of the continent.The conclusions suggest that the earliest peopling of western Europe occurred not long before 1 Ma and was accompanied by a relatively homogeneous Mode 1 technology. Between 800 and 600 ka, the European framework is limited to a few assemblages, most of them derived from European Mode 1, and even probably belonging to the earliest European Acheulean. Interestingly, at Atapuerca there is a gap between c. 900 ka and c. 500 ka with no hominin presence; in other words, approximately 400,000 years passed between the late Mode 1 of Homo antecessor and the first Mode 2 represented there with Homo heidelbergensis. Significantly, this hominin gap has been observed in three consecutive levels of the Gran Dolina site (about 4 m thickness), all of them extremely rich in faunal remains.This paper poses the hypothesis that this gap at Atapuerca represents a non-local, continental phenomenon, leading to consideration of several different points. Firstly, H. antecessor and its possible ascendants, who had formerly peopled Europe, might have been in the process of extinction around 800 ka. Secondly, before 650 ka new but light waves of hominins may have arrived in Europe carrying the new Acheulean technology. These waves did not reach most of the continent, and surely they were not successful in demographic terms until (thirdly) the arrival of the full Acheulean groups at 500 ka. Between 500 ka and 300 ka this full Acheulean appeared at several European sites, and H. heidelbergensis, whatever its origin, is strongly associated with this technology on this subcontinent. Fourthly, if the Mode 1 populations eventually disappeared before 650 ka then the later Clactonian/Tayacian sites of northern Europe cannot be derived from this legacy, but must come from the Acheulean line, and are therefore a variant. Finally, the data suggest that the Acheulean may have technically developed into the European Middle Palaeolithic, as H. heidelbergensis evolved into Neanderthals.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":415280,"url":"http://www.sciencedirect.com/science/article/pii/S1040618212000468"}]}, 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="2281455"><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/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_"><img alt="Research paper thumbnail of The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_">The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/ameliabargallo">amelia bargallo</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://todofp.academia.edu/BelenMarquez">Belen Marquez</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MarinaMosquera">Marina Mosquera</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technol...</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 Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).</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="2281455"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281455"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281455; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2281455]").text(description); $(".js-view-count[data-work-id=2281455]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2281455; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2281455']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2281455]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281455,"title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)","translated_title":"","metadata":{"abstract":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","more_info":"Ollé, A., Mosquera, M., Rodríguez, X. P., de Lombera-Hermida, A., García-Antón, M. D., García-Medrano, P., Peña, L., Menéndez, L., Navazo, M., Terradillos, M., Bargalló, A., Márquez, B., Sala, R. \u0026 Carbonell, E. (ip). Quaternary International, 295: 138-167","publication_date":{"day":18,"month":4,"year":2013,"errors":{}}},"translated_abstract":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","internal_url":"https://www.academia.edu/2281455/The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_","translated_internal_url":"","created_at":"2012-12-12T02:42:35.081-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"other","co_author_tags":[{"id":8019056,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":322629,"email":"a***a@prehistoria.urv.cat","display_order":0,"name":"Arturo Lombera","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"},{"id":8019058,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":null,"co_author_invite_id":492560,"email":"l***g@prehistoria.urv.cat","display_order":6291456,"name":"Leticia Menéndez","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, 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Spain)"},{"id":19905209,"work_id":2281455,"tagging_user_id":2858486,"tagged_user_id":1135489,"co_author_invite_id":null,"email":"m***s@hotmail.com","affiliation":"Universidad Internacional Isabel I de Castilla","display_order":8388592,"name":"Marcos Terradillos-Bernal","title":"The Early and Middle Pleistocene technological record from Sierra de Atapuerca (Burgos, Spain)"}],"downloadable_attachments":[],"slug":"The_Early_and_Middle_Pleistocene_technological_record_from_Sierra_de_Atapuerca_Burgos_Spain_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"The Sierra de Atapuerca sites offer a chronological sequence that allows the evolution of technology at a local scale during the Early and Middle Pleistocene to be reconstructed. This paper presents updated information on the main lithic assemblages recovered from the various levels of the Sima del Elefante, Gran Dolina, Galería, and Sima de los Huesos sites. The ultimate goal is to look for technological features on the pieces that make up these assemblages that carry evolutionary significance. Other archaeological data will be cross- referenced with the technical features documented in these artefacts in order to better understand the peopling that took place at Atapuerca during the Pleistocene.The first peopling of Atapuerca occurred at 1.2 Ma, and is represented in level TE9 and probably at the top of level TD3-TD4 by Homo sp. and a Mode 1 technology, which is very poor in terms of diversity and energy invested in tool production. This technology is related to opportunistic subsistence strategies that focused on taking advantage of carcasses that had fallen into the cavities. A second cultural phase has been revealed in level TD6, dating to before 800 ka: a phase characterised by new subsistence and technological strategies, although still belonging to Mode 1 and carried out by Homo antecessor. In TD6, the lithic assemblage is rich and diversified. Intensive occupations with well organised subsistence strategies have been documented, including hunting activities and the earliest trace of cannibalism in prehistory. After a hiatus of approximately 300 ky without evidence of hominin presence, the occupations of Galería and TD10 correspond to a third cultural phase, ranging from between 500 ka and 300 ka. They are represented by a Mode 2 technology associated with systematic and directional carcass processing, including hunting events in TD10. Homo heidelbergensis appears instead of H. antecessor, and is extraordinarily represented at the Sima de los Huesos site in the form of an intentional accumulation of numerous individuals. Finally, TD10.1 may represent the local evolution from Mode 2 to Mode 3 assemblages.After comparing these assemblages, it is clear that several technological features have either been retained or changed over the span of the Atapuerca sequence. The following are considered to have evolutionary significance due to the technological trends described: a) raw material selection (use of local varieties of rock, with the progressive increasing selection of the most workable materials through the Middle Pleistocene); b) production sequences (coexistence of several knapping methods, with a clear increase in centripetal strategies and techniques for flake predetermination, which ultimately lead to Levallois-like methods); c) scarce and insignificant presence of choppers and chopping tools; d) tools on flakes (recorded only from the end of the Early Pleistocene, increasing in number, complexity and standardisation throughout the Middle Pleistocene); and e) large cutting tools (which appear ca 500 ka, and progressively decrease in number, standardisation and intensity of shaping throughout Gran Dolina TD10).","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[],"research_interests":[],"urls":[{"id":415278,"url":"http://www.sciencedirect.com/science/article/pii/S1040618211006483"}]}, 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="2898699"><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/2898699/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_"><img alt="Research paper thumbnail of New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)" 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/2898699/New_data_on_Sicilian_prehistoric_and_historic_evolution_in_a_mountain_context_Vallone_Inferno_Scillato_Italy_">New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/GiovanniSimone">Giovanni Di Simone</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://uib-es.academia.edu/Lloren%C3%A7PicornellGelabert">Llorenç Picornell-Gelabert</a></span></div><div class="wp-workCard_item"><span>C.R. Palevol doi:10.1016/j.crpv.2012.11.002</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in S...</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">Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.</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="2898699"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2898699"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2898699; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2898699]").text(description); $(".js-view-count[data-work-id=2898699]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2898699; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2898699']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2898699]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2898699,"title":"New data on Sicilian prehistoric and historic evolution in a mountain context, Vallone Inferno (Scillato, Italy)","translated_title":"","metadata":{"abstract":"Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. 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Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. 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The recent studies at El-Kherba (Ain Hanech) in northeastern Algeria expand the geographic range of evidence of hominin subsistence patterns to include the earliest known archaeological sites documented in North Africa. Dated to 1.78 million years ago (Ma), excavations from El-Kherba yielded an Oldowan industry associated with a savanna-like fauna contained in floodplain deposits. The faunal assemblage is dominated by large and medium-sized animals (mainly adults), especially equids, which are represented by at least 11 individuals. The mammalian archaeofauna preserves numerous cut-marked and hammerstone-percussed bones. Made of primarily limestone and flint, the stone assemblage consists of core forms, débitage, and retouched pieces. Evidence of usewear traces is found on several of the flint artifacts, indicating meat processing by early hominins. Overall, our subsistence analysis indicates that early hominins were largely responsible for bone modification at the site, which is also corroborated by other relevant taphonomic evidence. Moreover, at 1.78 Ma, the cutmarked bones recovered from El-Kherba represent the earliest known evidence for ancestral hominin butchery activities and large animal foraging capabilities in northern Africa.</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="2898539"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2898539"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2898539; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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$(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="2281433"><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/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence"><img alt="Research paper thumbnail of Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence" 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/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence">Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/HuguesAlexandreBlain">Hugues-Alexandre Blain</a></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="2281433"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2281433"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2281433; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=2281433]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2281433,"title":"Investigating the Mid-Brunhes Event in the Spanish terrestrial sequence","internal_url":"https://www.academia.edu/2281433/Investigating_the_Mid_Brunhes_Event_in_the_Spanish_terrestrial_sequence","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2276611"><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/2276611/One_million_years_of_cultural_evolution_in_a_stable_environment_at_Atapuerca_Burgos_Spain_"><img alt="Research paper thumbnail of One million years of cultural evolution in a stable environment at Atapuerca (Burgos, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/36401884/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/2276611/One_million_years_of_cultural_evolution_in_a_stable_environment_at_Atapuerca_Burgos_Spain_">One million years of cultural evolution in a stable environment at Atapuerca (Burgos, 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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/IsabelExp%C3%B3sitoBarea">Isabel Expósito Barea</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://urv.academia.edu/MariaBennasar">Maria Bennàsar</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/HuguesAlexandreBlain">Hugues-Alexandre Blain</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The present paper analyses the evidence provided by three sites (Sima del Elefante, Gran Dolina, ...</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 present paper analyses the evidence provided by three sites (Sima del Elefante, Gran Dolina, and Galería) located in the Trinchera del Ferrocarril of the Sierra de Atapuerca. These three sites are cave infillings that contain sediments deposited from approximately 1.2 Ma to 200 kyr. Pollen, herpetofauna, and small and large mammal remains are used as proxies to obtain a general picture of the environmental changes that occurred at the Sierra de Atapuerca throughout the one million-year period represented at these sites. Similarly, cultural changes are tracked analyzing the evidence of human behavior obtained from the study of several bone and lithic assemblages from these three sites. At least three periods with different cultural features, involving technology, subsistence and behavior, are determined from the available evidence. The first two periods correspond to the Mode 1 technology and Homo antecessor: the first is dated around 1.2 to 1.0 Ma and reflects opportunistic behavior both in technology and subsistence. The second period is around 800 kyr BP. Mode 1 technology is still maintained, but subsistence strategies include systematic hunting and the use of base camps. The third period is dated between 500 ka and 200 ka and corresponds to the Mode 2 technology and the acquisition of directional hunting and other organizational strategies by Homo heidelbergensis. A transition from Mode 2 to Mode 3 seems to appear at the end of this time-range, and may reflect the early phases of a fourth cultural change. With regard to the environment, our main conclusion is that there was an absence of extremely harsh conditions at Atapuerca throughout this time period. The presence of Mediterranean taxa was constant and the dominant landscape was a savannah-like open environment, probably with small forest patches. An alternation of Mediterranean and mesic species Quaternary Science Reviews 30 as the dominant component of the tree storey was induced by the climatic cycles, and steppes spread across the landscape during the drier periods. In any case, it is not possible to establish clear cut-off points separating entirely different environmental episodes. Our results show no evidence of any relationship between environmental change and cultural change at the Sierra de Atapuerca.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1e3b4206d052173aa132d50ccc797f81" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":36401884,"asset_id":2276611,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/36401884/download_file?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="2276611"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2276611"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2276611; 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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="2276566"><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/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data"><img alt="Research paper thumbnail of Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data" 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/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data">Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The functional study of the stone tool artefacts from the Middle Pleistocene site of Isernia la P...</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 functional study of the stone tool artefacts from the Middle Pleistocene site of Isernia la Pineta (Molise, central Italy) revealed microtraces that display certain features that did not fit in with what we know as use-wear traces. The suspicion that these microtraces may be technical traces derived from bipolar flaking, which is prevalent at this site, led us to initiate an experimental programme to check our hypothesis. The experiments conducted allowed us to identify residues associated with bipolar flaking on an anvil and to characterise the microscopic traces derived from this production technique. Our results proved very useful in identifying the artefacts produced by bipolar flaking, as well as in determining the basic lithological features of the anvil. Moreover, these experiments allowed us to assess the possible interferences that these kinds of technical traces can cause when performing the functional analyses of lithic assemblages produced by the bipolar technique.► We present the results of an experimental programme on bipolar knapping on an anvil. ► First we study the mechanics of bipolar flaking and the variants of the technique. ► We describe under SEM the resulting technical deposits of residues and microtraces. ► These traces can easily mimic usewear traces and, so, interfere functional studies.</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="2276566"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2276566"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2276566; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=2276566]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2276566,"title":"Technical microwear and residues in identifying bipolar knapping on an anvil: experimental data","internal_url":"https://www.academia.edu/2276566/Technical_microwear_and_residues_in_identifying_bipolar_knapping_on_an_anvil_experimental_data","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2298642"><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/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_"><img alt="Research paper thumbnail of Early hominid dispersals: a technological hypothesis for “out of Africa”" 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/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_">Early hominid dispersals: a technological hypothesis for “out of Africa”</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BienvenidoMart%C3%ADnezNavarro">Bienvenido Martínez-Navarro</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Homo is the only genus that responds to environmental pressures by adopting such strategies as no...</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">Homo is the only genus that responds to environmental pressures by adopting such strategies as non-standardized behaviour, a general diet, and technology. Considering that basic idea, this paper introduces the general hypothesis that the Pliocene and Early Pleistocene Homo dispersals within and out of Africa were consequences of that human characteristic behaviour. In particular, they were driven by a process starting with the emergence of technology, followed in a second phase by its socialization. From this point, social reorganization within communities (changing behaviours and social, cultural and economic strategies) occurred, driving demographic growth, and frequently geographic expansion.</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="2298642"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298642"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298642; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2298642]").text(description); $(".js-view-count[data-work-id=2298642]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2298642; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2298642']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2298642]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2298642,"title":"Early hominid dispersals: a technological hypothesis for “out of Africa”","internal_url":"https://www.academia.edu/2298642/Early_hominid_dispersals_a_technological_hypothesis_for_out_of_Africa_","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="2298560"><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/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas"><img alt="Research paper thumbnail of Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas" 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/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas">Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas</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://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalaRobert">Robert Sala</a></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="2298560"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298560"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298560; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2298560]").text(description); $(".js-view-count[data-work-id=2298560]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2298560; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2298560']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2298560]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2298560,"title":"Sleeping activity area within the site structure of archaic human groups. Evidence from Abric Romaní level N combustion activity areas","internal_url":"https://www.academia.edu/2298560/Sleeping_activity_area_within_the_site_structure_of_archaic_human_groups_Evidence_from_Abric_Roman%C3%AD_level_N_combustion_activity_areas","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="335177" id="bookchapters"><div class="js-work-strip profile--work_container" data-work-id="2298635"><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/2298635/Preparation_and_conservation_treatments_of_the_Pleistocene_fossil_vertebrate_remains_from_the_cave_site_of_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3_Spain_"><img alt="Research paper thumbnail of Preparation and conservation treatments of the Pleistocene fossil vertebrate remains from the cave site of Tossal de la Font (Vilafamés, Castelló, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/30345037/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/2298635/Preparation_and_conservation_treatments_of_the_Pleistocene_fossil_vertebrate_remains_from_the_cave_site_of_Tossal_de_la_Font_Vilafam%C3%A9s_Castell%C3%B3_Spain_">Preparation and conservation treatments of the Pleistocene fossil vertebrate remains from the cave site of Tossal de la Font (Vilafamés, Castelló, Spain)</a></div><div class="wp-workCard_item"><span>In (C. Cancelo, S. Val, J. Marigó & L. Celià, Ed) I Consevation Workshop: Finding Global Solutions for Natural History Collections. From the Site to the Storage., pp. 225-231; 238-239. (Paleontologia i Evolució. Memòria especial, 4). Sabadell: ICP - Servei de Publicacions UAB</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this paper we present the preparation of some fossils from the Pleistocene levels of the cave ...</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 this paper we present the preparation of some fossils from the Pleistocene levels of the cave site of Tossal de la Font. The presence of carbonated concretions, which is the main feature of these specimens, is a problem common to many remains from some calcareous caves. Treatments are based on mechanical cleaning, and intervention criteria are directed at recovering the palaeontological and archaeological information.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="68c4451c527742cf7737346a521ca238" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30345037,"asset_id":2298635,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30345037/download_file?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="2298635"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298635"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298635; 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A. Vasil'ev & V. E. Schelinsky, Ed) The Earliest Inhabitants of the Caucasus and Hominid dispersals at Eurasia, pp. 225-242. (Archaeologica Petropolitana) St. Petersburg: Peterburgskoe vostokovedenie Sankt-Petersburg Centre for Oriental Studies Publishers</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1e881458077d016bf61314b608aba851" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30345008,"asset_id":2298598,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30345008/download_file?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="2298598"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298598"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298598; 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$(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="2259592"><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/2259592/SEM_functional_analysis_and_the_mechanism_of_microwear_formation"><img alt="Research paper thumbnail of SEM functional analysis and the mechanism of microwear formation" class="work-thumbnail" src="https://attachments.academia-assets.com/30311336/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/2259592/SEM_functional_analysis_and_the_mechanism_of_microwear_formation">SEM functional analysis and the mechanism of microwear formation</a></div><div class="wp-workCard_item"><span>In (L. Longo & N. Skakun, Ed) 'Prehistoric Technology' 40 years later: Functional Studies and the Russian Legacy. Proceedings of the International Congress Verona (Italy), 20-23 April 2005, pp. 39-49. (B.A.R. International Series, 1783). Oxford: Archaeopress.</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper focuses on wear processes on lithic artefacts. It is based on results from a wide-rang...</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 focuses on wear processes on lithic artefacts. It is based on results from a wide-ranging experimental programme and systematic SEM (Scanning Electron Microscope) analysis. Sequential experiments provided evidence on the processes involved in the deformation of lithic surfaces in function of the raw materials, the worked matters and the actions performed. Study of these processes, based on a theoretical framework from Materials Sciences, led us to support an interpretive model in which use-wear is basically explained in terms of attritional phenomena, including the plastic deformation of lithic materials.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="72f59d2ec93bc6415965ae3e215f6ddb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30311336,"asset_id":2259592,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30311336/download_file?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="2259592"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2259592"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2259592; 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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="2298655"><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/2298655/Human_occupations_at_Galeria_site_Sierra_de_Atapuerca_Burgos_Spain_after_the_technological_and_taphonomical_data"><img alt="Research paper thumbnail of Human occupations at Galeria site (Sierra de Atapuerca, Burgos, Spain) after the technological and taphonomical data" class="work-thumbnail" src="https://attachments.academia-assets.com/30345073/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/2298655/Human_occupations_at_Galeria_site_Sierra_de_Atapuerca_Burgos_Spain_after_the_technological_and_taphonomical_data">Human occupations at Galeria site (Sierra de Atapuerca, Burgos, Spain) after the technological and taphonomical data</a></div><div class="wp-workCard_item"><span>In (N. Molines, M.-H. Moncel & J.-L. Monnier, Ed) Les premiers peuplements en Europe. Colloque international: Données récentes sur les modalités de peuplement et sur le cadre chronostratigraphique, géologique et paléogéographique des industries du Paléolithique ancien et moyen en Europe </span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper presents, in a synthetic and integrated form, a revision of the results obtained after...</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, in a synthetic and integrated form, a revision of the results obtained after the study of the archaeological record of Galería site (Sierra de Atapuerca, Burgos). Based on taphonomic, zooarcheological, and technical data (representation of lithic reduction sequences and usewear), we reconstruct the natural and anthropical processes which generated and modified the accumulation. We propose a model of human intervention, based on a planned strategy to access naturally accumulated herbivore carcasses, in competition with carnivores.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b8c3b47d881e56b9d71af017efa1d043" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30345073,"asset_id":2298655,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30345073/download_file?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="2298655"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2298655"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2298655; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2298655]").text(description); $(".js-view-count[data-work-id=2298655]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2298655; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2298655']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "b8c3b47d881e56b9d71af017efa1d043" } } $('.js-work-strip[data-work-id=2298655]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2298655,"title":"Human occupations at Galeria site (Sierra de Atapuerca, Burgos, Spain) after the technological and taphonomical data","translated_title":"","metadata":{"more_info":"Ollé, A., Cáceres, I. \u0026 Vergès, J. 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Allué, J. Martín, A. Canals & E. Carbonell, Ed) Actas del 1er Congreso de Estudiantes de Prehistoria, pp. 220-224. Tarragona: Universitat Rovira i Virgili</span><span>, 2004</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Información del artículo Evolución Paleoambiental y Poblamiento Prehistórico en las Cuencas de lo...</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">Información del artículo Evolución Paleoambiental y Poblamiento Prehistórico en las Cuencas de los Ríos Francolí y Gaià.</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="2259508"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="2259508"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 2259508; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=2259508]").text(description); $(".js-view-count[data-work-id=2259508]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 2259508; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='2259508']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=2259508]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":2259508,"title":"Evolución Paleoambiental y Poblamiento Prehistórico en las Cuencas de los Ríos Francolí y Gaià","internal_url":"https://www.academia.edu/2259508/Evoluci%C3%B3n_Paleoambiental_y_Poblamiento_Prehist%C3%B3rico_en_las_Cuencas_de_los_R%C3%ADos_Francol%C3%AD_y_Gai%C3%A0","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="335181" id="doctoralthesis"><div class="js-work-strip profile--work_container" data-work-id="2259507"><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/2259507/Variabilitat_i_patrons_funcionals_en_els_sistemes_t%C3%A8cnics_de_Mode_2_An%C3%A0lisi_de_les_deformacions_d%C3%BAs_en_els_conjunts_l%C3%ADtics_del_Riparo_Esterno_de_Grotta_Paglicci_Rignano_Garganico_Foggia_%C3%81ridos_Arganda_Madrid_i_Galer%C3%ADa_TN_Sierra_de_Atapuerca_Burgos_"><img alt="Research paper thumbnail of Variabilitat i patrons funcionals en els sistemes tècnics de Mode 2. Anàlisi de les deformacions d'ús en els conjunts lítics del Riparo Esterno de Grotta Paglicci (Rignano Garganico, Foggia), Áridos (Arganda, Madrid) i Galería-TN (Sierra de Atapuerca, Burgos)" 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/2259507/Variabilitat_i_patrons_funcionals_en_els_sistemes_t%C3%A8cnics_de_Mode_2_An%C3%A0lisi_de_les_deformacions_d%C3%BAs_en_els_conjunts_l%C3%ADtics_del_Riparo_Esterno_de_Grotta_Paglicci_Rignano_Garganico_Foggia_%C3%81ridos_Arganda_Madrid_i_Galer%C3%ADa_TN_Sierra_de_Atapuerca_Burgos_">Variabilitat i patrons funcionals en els sistemes tècnics de Mode 2. Anàlisi de les deformacions d'ús en els conjunts lítics del Riparo Esterno de Grotta Paglicci (Rignano Garganico, Foggia), Áridos (Arganda, Madrid) i Galería-TN (Sierra de Atapuerca, Burgos)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">La tesi que porta per títol Variabilitat i patrons funcionals en els sistemes tècnics de mode 2. ...</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">La tesi que porta per títol Variabilitat i patrons funcionals en els sistemes tècnics de mode 2. 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Archaeological approach for characterizing and distinghuishing wear traces on flint tools with "gloss" 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/94444838/The_proces_of_wear_formation_Archaeological_approach_for_characterizing_and_distinghuishing_wear_traces_on_flint_tools_with_gloss">The proces of wear formation. Archaeological approach for characterizing and distinghuishing wear traces on flint tools with "gloss</a></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="94444838"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444838"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444838; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444838]").text(description); $(".js-view-count[data-work-id=94444838]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444838; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444838']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=94444838]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444838,"title":"The proces of wear formation. Archaeological approach for characterizing and distinghuishing wear traces on flint tools with \"gloss","internal_url":"https://www.academia.edu/94444838/The_proces_of_wear_formation_Archaeological_approach_for_characterizing_and_distinghuishing_wear_traces_on_flint_tools_with_gloss","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="94444837"><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/94444837/The_technological_behaviours_of_Homo_antecessor_core_management_and_reduction_intensity_at_Gran_Dolina_TD6_2_Atapuerca_Spain_"><img alt="Research paper thumbnail of The technological behaviours of Homo antecessor: core management and reduction intensity at Gran Dolina-TD6.2 (Atapuerca, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899213/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/94444837/The_technological_behaviours_of_Homo_antecessor_core_management_and_reduction_intensity_at_Gran_Dolina_TD6_2_Atapuerca_Spain_">The technological behaviours of Homo antecessor: core management and reduction intensity at Gran Dolina-TD6.2 (Atapuerca, Spain)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Approaching the life history of artefacts is fundamental for understanding both the formation pro...</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">Approaching the life history of artefacts is fundamental for understanding both the formation processes of archaeological assemblages and their technological variability. In this paper, we explore the variability of technological behaviours exhibited by the hominins from subunit TD6.2 at the Gran Dolina site (Atapuerca, Burgos), by combining both technological and reduction intensity analyses of the cores recovered. We used the Volumetric Reconstruction Method (VRM) to estimate the original volume of the blanks and quantify the reduction intensity of each core individually, after which we characterised the reduction distribution patterns using Weibull probability distribution functions. Our results suggest differential raw material management in terms of reduction intensity, according to the characteristics of each lithology. This could reflect a solid understanding of raw material qualities and a certain degree of planning. From a technological perspective, our results suggest cont...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="dd47f0d83e7811c658f2073a70b86dcf" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899213,"asset_id":94444837,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899213/download_file?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="94444837"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444837"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444837; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "dd47f0d83e7811c658f2073a70b86dcf" } } $('.js-work-strip[data-work-id=94444837]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444837,"title":"The technological behaviours of Homo antecessor: core management and reduction intensity at Gran Dolina-TD6.2 (Atapuerca, Spain)","internal_url":"https://www.academia.edu/94444837/The_technological_behaviours_of_Homo_antecessor_core_management_and_reduction_intensity_at_Gran_Dolina_TD6_2_Atapuerca_Spain_","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[{"id":96899213,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899213/thumbnails/1.jpg","file_name":"60746006f2ad330536a7638d.pdf","download_url":"https://www.academia.edu/attachments/96899213/download_file","bulk_download_file_name":"The_technological_behaviours_of_Homo_ant.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899213/60746006f2ad330536a7638d-libre.pdf?1673003255=\u0026response-content-disposition=attachment%3B+filename%3DThe_technological_behaviours_of_Homo_ant.pdf\u0026Expires=1739822540\u0026Signature=DrUngWwejUqgiqY~YpDgJxFNQcU4SBzZYNqK21bEjfp1LeXyQgyQ6omIdBlbViLYl0~yZ0QH7MItDDd0eDeT-DwNB0L~-yVrFjByPYveu-l6j10QiG0a6DcgbF1Yzy8MqrA6VMqOQ95G2~bvs1aUd6fezD10DbjeomKy8OTb2aXVysvloXrs7xl58iKArObd7F09iNZdD1i5xzaSa7ukaZSvzQJbLCk388pAVEd13NIw9m0YQ9cwT7mvcmsJopcUMVCPMGLhYYAZ5JGdRD3vVcQ3vQdBAKRt3AR9wcSHyvSjz7hEZEKadAEeW8qumSn4L4VGv6c3d9IcKhu~TaggLQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="94444836"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/94444836/Not_only_use"><img alt="Research paper thumbnail of Not only use" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/94444836/Not_only_use">Not only use</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2020</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="94444836"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444836"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444836; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444836]").text(description); $(".js-view-count[data-work-id=94444836]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444836; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444836']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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" } } $('.js-work-strip[data-work-id=94444836]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444836,"title":"Not only use","internal_url":"https://www.academia.edu/94444836/Not_only_use","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="94444835"><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/94444835/Characterization_of_the_use_wear_and_residues_resulting_from_limestone_working_Experimental_approach_to_the_parietal_art_of_La_Vi%C3%B1a_rock_shelter_La_Manzaneda_Asturias_Spain_"><img alt="Research paper thumbnail of Characterization of the use-wear and residues resulting from limestone working. Experimental approach to the parietal art of La Viña rock shelter (La Manzaneda, Asturias, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899217/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/94444835/Characterization_of_the_use_wear_and_residues_resulting_from_limestone_working_Experimental_approach_to_the_parietal_art_of_La_Vi%C3%B1a_rock_shelter_La_Manzaneda_Asturias_Spain_">Characterization of the use-wear and residues resulting from limestone working. Experimental approach to the parietal art of La Viña rock shelter (La Manzaneda, Asturias, Spain)</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Palaeolithic rock engravings that are located along the Nalón river basin in Northern 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">The Palaeolithic rock engravings that are located along the Nalón river basin in Northern Spain (central area of Asturias) have been studied from various perspectives (morphology, depth, style, manual range), but no use-wear studies on the stone tools used to produce such engravings have ever been undertaken. This paper aims to explore a new approach to this type of incisions based on use-wear analysis of experimental lithic tools used to engrave limestone blocks and slabs. Our results show that the use-wear traces generated by engraving limestone are welldeveloped and can be defined with specific criteria. The principal objective of this study was to provide the first experimental reference collection of use-wear resulting from engraving limestone using flint and quartzite experimental tools to compare with the traces that appear on tools in the archaeological record in contexts with parietal and portable art and, more specifically, to add a new approach to the multidisciplinary study of the La Viña rock shelter.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6d9c35a08de6671f8b8911bcb20afdeb" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899217,"asset_id":94444835,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899217/download_file?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="94444835"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444835"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444835; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444835]").text(description); $(".js-view-count[data-work-id=94444835]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444835; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444835']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "6d9c35a08de6671f8b8911bcb20afdeb" } } $('.js-work-strip[data-work-id=94444835]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444835,"title":"Characterization of the use-wear and residues resulting from limestone working. 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This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9c83bdf5c46e3aa733ed4cad589a26e7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899218,"asset_id":94444834,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899218/download_file?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="94444834"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444834"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444834; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444834]").text(description); $(".js-view-count[data-work-id=94444834]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444834; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444834']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "9c83bdf5c46e3aa733ed4cad589a26e7" } } $('.js-work-strip[data-work-id=94444834]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444834,"title":"Use-wear analysis of the late Middle Pleistocene quartzite assemblage from the Gran Dolina site, TD10.1 subunit (Sierra de Atapuerca, Spain)","translated_title":"","metadata":{"publisher":"Elsevier BV","ai_title_tag":"Use-wear Analysis of Quartzite from Gran Dolina, Spain","grobid_abstract":"This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. 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Boxgrovec.500kais one of the most informative sites at which to analyze shaping strategies and handaxe morphological variability in the European Middle Pleistocene, because of the large number of finished handaxes, and the presence of complete operational chains. We focused on the entire handaxe and rough-out sample from Boxgrove-Q1/B with the aim of assessing the role of raw material characteristicssize, form, and homogeneity of nodulesin the shaping process, and to ascertain if they represent real constraints in the production of handaxes. Additionally, given the large number of handaxes and the intensity of the thinning work at Boxgrove, we also aimed to determine if reduction intensity affected the final shape to the degree that some authors have previously postulated. The methodology combines traditional technological descriptions, metrical analysis, and experimental reproduction of shaping processes together with geometric morphometry and PCA. The conclusions we draw are that the Q1/B handaxe knapping strategies were flexible and adapted to the characteristics of the blanks. These characteristics affected the reduction strategy but there is no clear relationship between initial nodule or blank morphology and final handaxe shape. Throughout the experiments, we explored the capacity to solve problems arising from reduction accidents, which led to re-configuring the knapping strategy to achieve the predetermined "mental template". Furthermore, no substantial morphological differences related to reduction intensity were noticed with the Q1/B handaxes. Systematic re-sharpening as the cause of shape variation seems highly unlikely, perhaps related to the short use-life of the Boxgrove-Q1/B handaxes. Preferred forms constitute part of a broader pattern emerging for specific handaxe types at different times during the British Acheulean. The patterns have tentatively been interpreted as the result of changing environments and the movement of hominin populations.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1ee8b16dbf6cc5b793f4006de36f978f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899216,"asset_id":94444833,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899216/download_file?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="94444833"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444833"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444833; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444833]").text(description); $(".js-view-count[data-work-id=94444833]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444833; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444833']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "1ee8b16dbf6cc5b793f4006de36f978f" } } $('.js-work-strip[data-work-id=94444833]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444833,"title":"The Mental Template in Handaxe Manufacture: New Insights into Acheulean Lithic Technological Behavior at Boxgrove, Sussex, UK","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","grobid_abstract":"The morphological variability of Large Cutting Tools (LCT) during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. Boxgrovec.500kais one of the most informative sites at which to analyze shaping strategies and handaxe morphological variability in the European Middle Pleistocene, because of the large number of finished handaxes, and the presence of complete operational chains. We focused on the entire handaxe and rough-out sample from Boxgrove-Q1/B with the aim of assessing the role of raw material characteristicssize, form, and homogeneity of nodulesin the shaping process, and to ascertain if they represent real constraints in the production of handaxes. Additionally, given the large number of handaxes and the intensity of the thinning work at Boxgrove, we also aimed to determine if reduction intensity affected the final shape to the degree that some authors have previously postulated. The methodology combines traditional technological descriptions, metrical analysis, and experimental reproduction of shaping processes together with geometric morphometry and PCA. The conclusions we draw are that the Q1/B handaxe knapping strategies were flexible and adapted to the characteristics of the blanks. These characteristics affected the reduction strategy but there is no clear relationship between initial nodule or blank morphology and final handaxe shape. Throughout the experiments, we explored the capacity to solve problems arising from reduction accidents, which led to re-configuring the knapping strategy to achieve the predetermined \"mental template\". Furthermore, no substantial morphological differences related to reduction intensity were noticed with the Q1/B handaxes. Systematic re-sharpening as the cause of shape variation seems highly unlikely, perhaps related to the short use-life of the Boxgrove-Q1/B handaxes. Preferred forms constitute part of a broader pattern emerging for specific handaxe types at different times during the British Acheulean. The patterns have tentatively been interpreted as the result of changing environments and the movement of hominin populations.","publication_date":{"day":null,"month":null,"year":2018,"errors":{}},"publication_name":"Journal of Archaeological Method and Theory","grobid_abstract_attachment_id":96899216},"translated_abstract":null,"internal_url":"https://www.academia.edu/94444833/The_Mental_Template_in_Handaxe_Manufacture_New_Insights_into_Acheulean_Lithic_Technological_Behavior_at_Boxgrove_Sussex_UK","translated_internal_url":"","created_at":"2023-01-06T02:34:56.542-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":96899216,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899216/thumbnails/1.jpg","file_name":"JARM-D-17-00047_R2_201.pdf","download_url":"https://www.academia.edu/attachments/96899216/download_file","bulk_download_file_name":"The_Mental_Template_in_Handaxe_Manufactu.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899216/JARM-D-17-00047_R2_201-libre.pdf?1673003262=\u0026response-content-disposition=attachment%3B+filename%3DThe_Mental_Template_in_Handaxe_Manufactu.pdf\u0026Expires=1738797871\u0026Signature=TrUm9h-QICY3xiLp1xpFt36IE7jdc-nPHapWtF1i~n9vx6qZxvRGGh3zQPo7GGu2Ptki-fPLVwlffU6sygEG5Lr2pLTulzVmGhal5wgHgVio0nGY-ykMoleZdBsvHEVwHNJ1Cutm6SzrTGW1KsSIvpqbqAsunfFdOx1Drj1Rb2TaIvOneP3J50R~EyJ-DSG2Lmltd3JPq93f68M0dCQE-2bGxlFUB2lbuI3~t2huGT7L2j3uj7cT55J4aKqAPPB0zaY896WpbsfE~CtkbjCRVl2bWO5rCrT8hsP20XxCdq1DdfubwwOdqBH1URPfgJCLcGhRAKCCbLOLM5nthqhPBg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_Mental_Template_in_Handaxe_Manufacture_New_Insights_into_Acheulean_Lithic_Technological_Behavior_at_Boxgrove_Sussex_UK","translated_slug":"","page_count":39,"language":"en","content_type":"Work","summary":"The morphological variability of Large Cutting Tools (LCT) during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. Boxgrovec.500kais one of the most informative sites at which to analyze shaping strategies and handaxe morphological variability in the European Middle Pleistocene, because of the large number of finished handaxes, and the presence of complete operational chains. We focused on the entire handaxe and rough-out sample from Boxgrove-Q1/B with the aim of assessing the role of raw material characteristicssize, form, and homogeneity of nodulesin the shaping process, and to ascertain if they represent real constraints in the production of handaxes. Additionally, given the large number of handaxes and the intensity of the thinning work at Boxgrove, we also aimed to determine if reduction intensity affected the final shape to the degree that some authors have previously postulated. The methodology combines traditional technological descriptions, metrical analysis, and experimental reproduction of shaping processes together with geometric morphometry and PCA. The conclusions we draw are that the Q1/B handaxe knapping strategies were flexible and adapted to the characteristics of the blanks. These characteristics affected the reduction strategy but there is no clear relationship between initial nodule or blank morphology and final handaxe shape. Throughout the experiments, we explored the capacity to solve problems arising from reduction accidents, which led to re-configuring the knapping strategy to achieve the predetermined \"mental template\". Furthermore, no substantial morphological differences related to reduction intensity were noticed with the Q1/B handaxes. Systematic re-sharpening as the cause of shape variation seems highly unlikely, perhaps related to the short use-life of the Boxgrove-Q1/B handaxes. Preferred forms constitute part of a broader pattern emerging for specific handaxe types at different times during the British Acheulean. The patterns have tentatively been interpreted as the result of changing environments and the movement of hominin populations.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[{"id":96899216,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899216/thumbnails/1.jpg","file_name":"JARM-D-17-00047_R2_201.pdf","download_url":"https://www.academia.edu/attachments/96899216/download_file","bulk_download_file_name":"The_Mental_Template_in_Handaxe_Manufactu.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899216/JARM-D-17-00047_R2_201-libre.pdf?1673003262=\u0026response-content-disposition=attachment%3B+filename%3DThe_Mental_Template_in_Handaxe_Manufactu.pdf\u0026Expires=1738797871\u0026Signature=TrUm9h-QICY3xiLp1xpFt36IE7jdc-nPHapWtF1i~n9vx6qZxvRGGh3zQPo7GGu2Ptki-fPLVwlffU6sygEG5Lr2pLTulzVmGhal5wgHgVio0nGY-ykMoleZdBsvHEVwHNJ1Cutm6SzrTGW1KsSIvpqbqAsunfFdOx1Drj1Rb2TaIvOneP3J50R~EyJ-DSG2Lmltd3JPq93f68M0dCQE-2bGxlFUB2lbuI3~t2huGT7L2j3uj7cT55J4aKqAPPB0zaY896WpbsfE~CtkbjCRVl2bWO5rCrT8hsP20XxCdq1DdfubwwOdqBH1URPfgJCLcGhRAKCCbLOLM5nthqhPBg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":5346,"name":"Archaeological Method \u0026 Theory","url":"https://www.academia.edu/Documents/in/Archaeological_Method_and_Theory"},{"id":19536,"name":"Morphometry","url":"https://www.academia.edu/Documents/in/Morphometry"},{"id":138930,"name":"Acheulean","url":"https://www.academia.edu/Documents/in/Acheulean"},{"id":338207,"name":"Handaxes","url":"https://www.academia.edu/Documents/in/Handaxes"}],"urls":[{"id":27796550,"url":"http://link.springer.com/content/pdf/10.1007/s10816-018-9376-0.pdf"}]}, 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="94444832"><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/94444832/Chemical_Alteration_of_Lithic_Artefacts_an_Experimental_Case_Study_on_the_effect_of_Guano_on_Stone_Flakes_and_Its_Contextualization_in_the_Archaeological_Assemblage_of_Azokh_Cave_Southern_Caucasus_"><img alt="Research paper thumbnail of Chemical Alteration of Lithic Artefacts: an Experimental Case Study on the effect of Guano on Stone Flakes and Its Contextualization in the Archaeological Assemblage of Azokh Cave (Southern Caucasus)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899214/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/94444832/Chemical_Alteration_of_Lithic_Artefacts_an_Experimental_Case_Study_on_the_effect_of_Guano_on_Stone_Flakes_and_Its_Contextualization_in_the_Archaeological_Assemblage_of_Azokh_Cave_Southern_Caucasus_">Chemical Alteration of Lithic Artefacts: an Experimental Case Study on the effect of Guano on Stone Flakes and Its Contextualization in the Archaeological Assemblage of Azokh Cave (Southern Caucasus)</a></div><div class="wp-workCard_item"><span>Archaeometry</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Chemical weathering of archaeological material is well known; however, while there have been a nu...</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">Chemical weathering of archaeological material is well known; however, while there have been a number of experimental studies demonstrating different types and degrees of chemical alteration on faunal remains, little attention has been paid to stone tools, and the few studies that exist relate mainly to siliceous materials and water-induced chemical alteration. Azokh Cave, located in the South Caucasus, contains a Middle Pleistocene to Holocene infill, and detailed macro-and microscopic examination of the lithic assemblages recovered there indicates potential chemical weathering of the stone artefacts. The cave is also currently home to one of the largest bat colonies in the region, and their guano forms a significant component of the infill of the inner galleries. Based on these two factors, an experimental pilot study was set up to artificially chemically alter a range of stone flakes produced specifically for the task, in order to determine the nature and likely cause of weathering. The experimental flakes, produced from different raw materials, were buried in fresh bat guano for up to two years. The results reported herein demonstrate that in a relatively short time, the highly acidic composition of bat guano strongly affects calcium-bearing rocks (e.g., limestone, basalt) altering their entire surface. Similar comparisons may be made with chemical alteration evident on archaeological lithics from Azokh Cave, suggesting that bat guano has played a significant role in diagenetic alteration.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7f4e26d5cb89b065d86a4226b5384c77" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899214,"asset_id":94444832,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899214/download_file?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="94444832"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444832"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444832; 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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="94444831"><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/94444831/New_contributions_to_the_functional_analysis_of_prehistoric_tools"><img alt="Research paper thumbnail of New contributions to the functional analysis of prehistoric tools" class="work-thumbnail" src="https://attachments.academia-assets.com/96899215/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/94444831/New_contributions_to_the_functional_analysis_of_prehistoric_tools">New contributions to the functional analysis of prehistoric tools</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2017</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ce5d59efe7b3dd64f4029d62188bdf8f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899215,"asset_id":94444831,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899215/download_file?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="94444831"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444831"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444831; 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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="94444830"><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/94444830/Human_predatory_behavior_and_the_social_implications_of_communal_hunting_based_on_evidence_from_the_TD10_2_bison_bone_bed_at_Gran_Dolina_Atapuerca_Spain_"><img alt="Research paper thumbnail of Human predatory behavior and the social implications of communal hunting based on evidence from the TD10.2 bison bone bed at Gran Dolina (Atapuerca, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899236/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/94444830/Human_predatory_behavior_and_the_social_implications_of_communal_hunting_based_on_evidence_from_the_TD10_2_bison_bone_bed_at_Gran_Dolina_Atapuerca_Spain_">Human predatory behavior and the social implications of communal hunting based on evidence from the TD10.2 bison bone bed at Gran Dolina (Atapuerca, Spain)</a></div><div class="wp-workCard_item"><span>Journal of human evolution</span><span>, Apr 1, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Zooarcheological research is an important tool in reconstructing subsistence, as well as for infe...</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">Zooarcheological research is an important tool in reconstructing subsistence, as well as for inferring relevant aspects regarding social behavior in the past. The organization of hunting parties, forms of predation (number and rate of animals slaughtered), and the technology used (tactics and tools) must be taken into account in the identification and classification of hunting methods in prehistory. The archeological recognition of communal hunting reflects an interest in evolutionary terms and their inherent implications for anticipatory capacities, social complexity, and the development of cognitive tools, such as articulated language. Late and Middle Paleolithic faunal assemblages in Europe have produced convincing evidence of communal hunting of large ungulates allowing for the formation of hypotheses concerning the skills of Neanderthals anatomically modern humans as social predators. However, the emergence of this cooperative behavior is not currently understood. Here, faunal ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2591cefc2b80ce72ec3a0cca011cd291" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899236,"asset_id":94444830,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899236/download_file?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="94444830"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444830"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444830; 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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="94444829"><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/94444829/Microwear_study_of_quartzite_artefacts_preliminary_results_from_the_Middle_Pleistocene_site_of_Payre_South_eastern_France_"><img alt="Research paper thumbnail of Microwear study of quartzite artefacts: preliminary results from the Middle Pleistocene site of Payre (South-eastern France)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899219/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/94444829/Microwear_study_of_quartzite_artefacts_preliminary_results_from_the_Middle_Pleistocene_site_of_Payre_South_eastern_France_">Microwear study of quartzite artefacts: preliminary results from the Middle Pleistocene site of Payre (South-eastern France)</a></div><div class="wp-workCard_item"><span>Archaeological and Anthropological Sciences</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Preliminary functional results obtained from the quartzite assemblage of the Early Middle Palaeol...</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">Preliminary functional results obtained from the quartzite assemblage of the Early Middle Palaeolithic site of Payre (South-eastern France) are presented. In an area rich in flint, hominins at Payre also collected quartzite in their local environment, specifically along the Rhône River banks. Although the Payre lithic assemblage is largely composed of flint, quartzite was introduced in the site mainly as large cutting tools knapped outside. This fact pointed out an apparently highly differential treatment of the raw material types available in the region. A major concern is to understand the reason why. Is there any functional reason for the introduction of those artefacts, perhaps to perform specific activities related to the toughness of quartzite? Or is there any functional differentiation among the various raw materials? Use-wear analysis is a useful tool for better understanding human technological choices and strategies of lithic raw material management. Before attempting to extensively apply use-wear analysis on the quartzite assemblage, we analysed a limited sample to evaluate the general surface preservation. A specific experimental programme with the same local quartzite was carried out in order to provide a reliable comparative reference for interpreting use-wear evidence on archaeological implements. Methodological difficulties related to use-wear analysis applied to quartzite artefacts are also discussed. Both Optical light microscopy (OLM) and Scanning Electron Microscopy (SEM) were employed in this study; however, interpretations were elaborated considering principally SEM micro-graphs. The analysis of the archaeological material showed a good state of preservation of the surfaces with a low incidence of post-depositional alterations. The documented use-wear allowed us to identify the active edges, the kinematics and, more rarely, the worked material. Chopping activities were documented on two large artefacts suggesting a specific utility of those tools.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1c7c7343a36f6d9396cb40cf6b954dc0" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899219,"asset_id":94444829,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899219/download_file?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="94444829"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444829"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444829; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444829]").text(description); $(".js-view-count[data-work-id=94444829]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444829; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444829']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "1c7c7343a36f6d9396cb40cf6b954dc0" } } $('.js-work-strip[data-work-id=94444829]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444829,"title":"Microwear study of quartzite artefacts: preliminary results from the Middle Pleistocene site of Payre (South-eastern France)","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","ai_title_tag":"Microwear Analysis of Quartzite Artefacts from Payre","grobid_abstract":"Preliminary functional results obtained from the quartzite assemblage of the Early Middle Palaeolithic site of Payre (South-eastern France) are presented. In an area rich in flint, hominins at Payre also collected quartzite in their local environment, specifically along the Rhône River banks. Although the Payre lithic assemblage is largely composed of flint, quartzite was introduced in the site mainly as large cutting tools knapped outside. This fact pointed out an apparently highly differential treatment of the raw material types available in the region. A major concern is to understand the reason why. Is there any functional reason for the introduction of those artefacts, perhaps to perform specific activities related to the toughness of quartzite? Or is there any functional differentiation among the various raw materials? Use-wear analysis is a useful tool for better understanding human technological choices and strategies of lithic raw material management. Before attempting to extensively apply use-wear analysis on the quartzite assemblage, we analysed a limited sample to evaluate the general surface preservation. A specific experimental programme with the same local quartzite was carried out in order to provide a reliable comparative reference for interpreting use-wear evidence on archaeological implements. Methodological difficulties related to use-wear analysis applied to quartzite artefacts are also discussed. Both Optical light microscopy (OLM) and Scanning Electron Microscopy (SEM) were employed in this study; however, interpretations were elaborated considering principally SEM micro-graphs. The analysis of the archaeological material showed a good state of preservation of the surfaces with a low incidence of post-depositional alterations. The documented use-wear allowed us to identify the active edges, the kinematics and, more rarely, the worked material. Chopping activities were documented on two large artefacts suggesting a specific utility of those tools.","publication_date":{"day":null,"month":null,"year":2016,"errors":{}},"publication_name":"Archaeological and Anthropological Sciences","grobid_abstract_attachment_id":96899219},"translated_abstract":null,"internal_url":"https://www.academia.edu/94444829/Microwear_study_of_quartzite_artefacts_preliminary_results_from_the_Middle_Pleistocene_site_of_Payre_South_eastern_France_","translated_internal_url":"","created_at":"2023-01-06T02:34:56.052-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":96899219,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899219/thumbnails/1.jpg","file_name":"s12520-016-0368-220230106-1-t7umg0.pdf","download_url":"https://www.academia.edu/attachments/96899219/download_file","bulk_download_file_name":"Microwear_study_of_quartzite_artefacts_p.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899219/s12520-016-0368-220230106-1-t7umg0-libre.pdf?1673003252=\u0026response-content-disposition=attachment%3B+filename%3DMicrowear_study_of_quartzite_artefacts_p.pdf\u0026Expires=1738769132\u0026Signature=bYCzFCICz8tgh92--t55Y5pt9nV2-nE3PGuVrFAqsxGR0Oo5y2C-eTiS-3MNDm8K6kXZRGQ8Dt-IT8cfzcgEcqemSoEsp0IKvGEmf1Djnr~U0camse2spnil-Gza1PYkX36SB4g17C4ZIbDhA93W7RNyP8gmaBChvSOV1bFiwJOG58SoyG6k6mLXV1DJ2EjV6RZDiVJm-LcOhiWmjDa1uRXCPWm4wCCNlqzVhsJ7bBkKk4vQrPKiScGGKyw6tO46OF22RZgLfoswXhG146~gNbDKB1iTE-y1ZaoPdDjC5MI2UqgOYRPDHP2b7hr7oW~LzP4OJsqFTmgkl4q8cKDAgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Microwear_study_of_quartzite_artefacts_preliminary_results_from_the_Middle_Pleistocene_site_of_Payre_South_eastern_France_","translated_slug":"","page_count":20,"language":"en","content_type":"Work","summary":"Preliminary functional results obtained from the quartzite assemblage of the Early Middle Palaeolithic site of Payre (South-eastern France) are presented. In an area rich in flint, hominins at Payre also collected quartzite in their local environment, specifically along the Rhône River banks. Although the Payre lithic assemblage is largely composed of flint, quartzite was introduced in the site mainly as large cutting tools knapped outside. This fact pointed out an apparently highly differential treatment of the raw material types available in the region. A major concern is to understand the reason why. Is there any functional reason for the introduction of those artefacts, perhaps to perform specific activities related to the toughness of quartzite? Or is there any functional differentiation among the various raw materials? Use-wear analysis is a useful tool for better understanding human technological choices and strategies of lithic raw material management. Before attempting to extensively apply use-wear analysis on the quartzite assemblage, we analysed a limited sample to evaluate the general surface preservation. A specific experimental programme with the same local quartzite was carried out in order to provide a reliable comparative reference for interpreting use-wear evidence on archaeological implements. Methodological difficulties related to use-wear analysis applied to quartzite artefacts are also discussed. Both Optical light microscopy (OLM) and Scanning Electron Microscopy (SEM) were employed in this study; however, interpretations were elaborated considering principally SEM micro-graphs. The analysis of the archaeological material showed a good state of preservation of the surfaces with a low incidence of post-depositional alterations. The documented use-wear allowed us to identify the active edges, the kinematics and, more rarely, the worked material. Chopping activities were documented on two large artefacts suggesting a specific utility of those tools.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[{"id":96899219,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899219/thumbnails/1.jpg","file_name":"s12520-016-0368-220230106-1-t7umg0.pdf","download_url":"https://www.academia.edu/attachments/96899219/download_file","bulk_download_file_name":"Microwear_study_of_quartzite_artefacts_p.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899219/s12520-016-0368-220230106-1-t7umg0-libre.pdf?1673003252=\u0026response-content-disposition=attachment%3B+filename%3DMicrowear_study_of_quartzite_artefacts_p.pdf\u0026Expires=1738769132\u0026Signature=bYCzFCICz8tgh92--t55Y5pt9nV2-nE3PGuVrFAqsxGR0Oo5y2C-eTiS-3MNDm8K6kXZRGQ8Dt-IT8cfzcgEcqemSoEsp0IKvGEmf1Djnr~U0camse2spnil-Gza1PYkX36SB4g17C4ZIbDhA93W7RNyP8gmaBChvSOV1bFiwJOG58SoyG6k6mLXV1DJ2EjV6RZDiVJm-LcOhiWmjDa1uRXCPWm4wCCNlqzVhsJ7bBkKk4vQrPKiScGGKyw6tO46OF22RZgLfoswXhG146~gNbDKB1iTE-y1ZaoPdDjC5MI2UqgOYRPDHP2b7hr7oW~LzP4OJsqFTmgkl4q8cKDAgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":30254,"name":"Pleistocene","url":"https://www.academia.edu/Documents/in/Pleistocene"}],"urls":[{"id":27796548,"url":"http://link.springer.com/article/10.1007/s12520-016-0368-2/fulltext.html"}]}, 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="94444828"><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/94444828/Monitoring_and_interpreting_the_use_wear_formation_processes_on_quartzite_flakes_through_sequential_experiments"><img alt="Research paper thumbnail of Monitoring and interpreting the use-wear formation processes on quartzite flakes through sequential experiments" class="work-thumbnail" src="https://attachments.academia-assets.com/96899210/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/94444828/Monitoring_and_interpreting_the_use_wear_formation_processes_on_quartzite_flakes_through_sequential_experiments">Monitoring and interpreting the use-wear formation processes on quartzite flakes through sequential experiments</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2017</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Sequential experiments were performed with quartzite flakes with the main purpose of monitoring u...</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">Sequential experiments were performed with quartzite flakes with the main purpose of monitoring usewear formation processes. The two main objectives of this research were the construction of a wide reference collection to serve for future functional interpretations of the archaeological material and to achieve a better comprehension of the mechanical behaviour of quartzite when subjected to the stress applied in determined prehistoric tasks (e.g., sawing, scraping bone, wood, etc.). The two objectives are strictly related because the appearance of wear on the tool edges resulting from those tasks would be dependant on the mechanical behaviour of the rock in question. Concepts from tribology were used to provide an explanatory framework. As mechanical behaviour of solid materials always depends on their mechanical proprieties which are unique, each raw material should be treated individually in use-wear analysis. For this reason, there is an urgent need to create a reliable and objective system to identify and interpret wear due to use on quartzite. For data recording, we resorted to both optical and electron microscopes (OLM and SEM) to present a wide photographic documentation and to compare the adequacy and complementarity of those microscopic techniques for microwear studies. Furthermore, both the experimental residues of the worked materials and the rock particles detached from the active edges were analysed to understand their role as interfacial medium affecting use-wear formation. EDX (Energy-Dispersive X-ray spectroscopy) was used to document the presence of rock particles detached from the tools edges and then embedded in the residues of the worked materials. The results from analysing the experimental flakes allowed us to infer more closely the mechanical behaviour of quartzite. As a final point, the potential of OLM and SEM for analysing quartzite surfaces was evaluated and it emerged that the combination of the two techniques in an integrated approach is a feasible choice, though the application of SEM is always desirable in order to get more trustworthy results.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c0f00b5ad006ae5da75a6917becf673c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899210,"asset_id":94444828,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899210/download_file?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="94444828"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444828"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444828; 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</script> <div class="js-work-strip profile--work_container" data-work-id="94444824"><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/94444824/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools"><img alt="Research paper thumbnail of Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools" class="work-thumbnail" src="https://attachments.academia-assets.com/96899209/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/94444824/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools">Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools</a></div><div class="wp-workCard_item"><span>Journal of Lithic Studies</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">While many experimental studies have been done on siliceous and metamorphic rocks for both use-we...</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">While many experimental studies have been done on siliceous and metamorphic rocks for both use-wear and post depositional surface modification (PDSM) events, little is known about such experiments on volcanic materials (other than obsidian), and on basalt in particular. Here we present the preliminary results of several experiments related to: a) evidence for basalt use (e.g., butchery and fresh hide scraping) and the subsequent characteristic use-wear patterns that can be seen; and b) postdepositional surface modifications caused by bear (Ursidae) trampling on experimental basalt flakes and subsequent use of these flakes for a tumbling experiment in a special tumbling machine. The results of these experiments were compared to better understand some surface modifications noted on the Middle to Upper Pleistocene lithic assemblages of the Azokh Cave site (Nagorno Karabagh, Lesser Caucasus). Although some aspects of both events (use-wear and PDSM) remain to be studied in depth, the experiments have improved our understanding of the effects of use-wear and post-depositional trampling and tumbling on basalt lithic artefacts. In particular, it has allowed us to recognise mechanical alterations (e.g., cracks, striations, fractures, edge damage) caused by trampling and tumbling and to note differences between these modifications and those caused by use. In particular, the experiments have shown that macroscopic modifications are rarely diagnostic, especially those observed after use. Microscopic wear features such as edge rounding, polish, abrasion and striations were the most evident types of alteration on basalt flakes, although occurring at different times and from different types of use. Distribution and orientation of alterations may be key in distinguishing use-wear from post-depositional alterations on basalt artefacts.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="21030f9f6a974c94ece762c22025cd09" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899209,"asset_id":94444824,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899209/download_file?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="94444824"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444824"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444824; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444824]").text(description); $(".js-view-count[data-work-id=94444824]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444824; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444824']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "21030f9f6a974c94ece762c22025cd09" } } $('.js-work-strip[data-work-id=94444824]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444824,"title":"Reality and confusion in the recognition of post-depositional alterations and use-wear: an experimental approach on basalt tools","translated_title":"","metadata":{"publisher":"Edinburgh University Library","grobid_abstract":"While many experimental studies have been done on siliceous and metamorphic rocks for both use-wear and post depositional surface modification (PDSM) events, little is known about such experiments on volcanic materials (other than obsidian), and on basalt in particular. Here we present the preliminary results of several experiments related to: a) evidence for basalt use (e.g., butchery and fresh hide scraping) and the subsequent characteristic use-wear patterns that can be seen; and b) postdepositional surface modifications caused by bear (Ursidae) trampling on experimental basalt flakes and subsequent use of these flakes for a tumbling experiment in a special tumbling machine. The results of these experiments were compared to better understand some surface modifications noted on the Middle to Upper Pleistocene lithic assemblages of the Azokh Cave site (Nagorno Karabagh, Lesser Caucasus). Although some aspects of both events (use-wear and PDSM) remain to be studied in depth, the experiments have improved our understanding of the effects of use-wear and post-depositional trampling and tumbling on basalt lithic artefacts. In particular, it has allowed us to recognise mechanical alterations (e.g., cracks, striations, fractures, edge damage) caused by trampling and tumbling and to note differences between these modifications and those caused by use. In particular, the experiments have shown that macroscopic modifications are rarely diagnostic, especially those observed after use. Microscopic wear features such as edge rounding, polish, abrasion and striations were the most evident types of alteration on basalt flakes, although occurring at different times and from different types of use. Distribution and orientation of alterations may be key in distinguishing use-wear from post-depositional alterations on basalt artefacts.","publication_date":{"day":null,"month":null,"year":2014,"errors":{}},"publication_name":"Journal of Lithic Studies","grobid_abstract_attachment_id":96899209},"translated_abstract":null,"internal_url":"https://www.academia.edu/94444824/Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools","translated_internal_url":"","created_at":"2023-01-06T02:34:55.512-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":96899209,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899209/thumbnails/1.jpg","file_name":"2bae5332511fa04962a49f8495ba72d183f3.pdf","download_url":"https://www.academia.edu/attachments/96899209/download_file","bulk_download_file_name":"Reality_and_confusion_in_the_recognition.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899209/2bae5332511fa04962a49f8495ba72d183f3-libre.pdf?1673003251=\u0026response-content-disposition=attachment%3B+filename%3DReality_and_confusion_in_the_recognition.pdf\u0026Expires=1738797871\u0026Signature=NEpLetp0j~auO-1G3oCDmTyxgYSQcVwdMRY0ZdBkqgYDN6fikI3RD4q3nQ7wT68jy9OLvaYw-pB8fYbEEnhCKvFak0SjZAt8SINaCvosEI23YNiXO1sk5zguCr9tC~YDvaOBuSPa-NhRXeIS7qZtXxKD~DM7JrmrYauwk7ibLBdCOO4MxSpUUmQ~dfb0ag8cB1Cx6QZ~Oq41ZwAJO41DegGpyocamlMU-7FlcXKkO9j3Xc79Y1NqBB08tEkgbJjou4bfewKgD6PO1S13v1Q55EkGrZKicowwU~-9S-S5HwsewGSQ7xm68zq2NgYMGb4ilRgW6fhtpeOcra7UXsUW0w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Reality_and_confusion_in_the_recognition_of_post_depositional_alterations_and_use_wear_an_experimental_approach_on_basalt_tools","translated_slug":"","page_count":24,"language":"en","content_type":"Work","summary":"While many experimental studies have been done on siliceous and metamorphic rocks for both use-wear and post depositional surface modification (PDSM) events, little is known about such experiments on volcanic materials (other than obsidian), and on basalt in particular. Here we present the preliminary results of several experiments related to: a) evidence for basalt use (e.g., butchery and fresh hide scraping) and the subsequent characteristic use-wear patterns that can be seen; and b) postdepositional surface modifications caused by bear (Ursidae) trampling on experimental basalt flakes and subsequent use of these flakes for a tumbling experiment in a special tumbling machine. The results of these experiments were compared to better understand some surface modifications noted on the Middle to Upper Pleistocene lithic assemblages of the Azokh Cave site (Nagorno Karabagh, Lesser Caucasus). Although some aspects of both events (use-wear and PDSM) remain to be studied in depth, the experiments have improved our understanding of the effects of use-wear and post-depositional trampling and tumbling on basalt lithic artefacts. In particular, it has allowed us to recognise mechanical alterations (e.g., cracks, striations, fractures, edge damage) caused by trampling and tumbling and to note differences between these modifications and those caused by use. In particular, the experiments have shown that macroscopic modifications are rarely diagnostic, especially those observed after use. Microscopic wear features such as edge rounding, polish, abrasion and striations were the most evident types of alteration on basalt flakes, although occurring at different times and from different types of use. Distribution and orientation of alterations may be key in distinguishing use-wear from post-depositional alterations on basalt artefacts.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[{"id":96899209,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899209/thumbnails/1.jpg","file_name":"2bae5332511fa04962a49f8495ba72d183f3.pdf","download_url":"https://www.academia.edu/attachments/96899209/download_file","bulk_download_file_name":"Reality_and_confusion_in_the_recognition.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899209/2bae5332511fa04962a49f8495ba72d183f3-libre.pdf?1673003251=\u0026response-content-disposition=attachment%3B+filename%3DReality_and_confusion_in_the_recognition.pdf\u0026Expires=1738797871\u0026Signature=NEpLetp0j~auO-1G3oCDmTyxgYSQcVwdMRY0ZdBkqgYDN6fikI3RD4q3nQ7wT68jy9OLvaYw-pB8fYbEEnhCKvFak0SjZAt8SINaCvosEI23YNiXO1sk5zguCr9tC~YDvaOBuSPa-NhRXeIS7qZtXxKD~DM7JrmrYauwk7ibLBdCOO4MxSpUUmQ~dfb0ag8cB1Cx6QZ~Oq41ZwAJO41DegGpyocamlMU-7FlcXKkO9j3Xc79Y1NqBB08tEkgbJjou4bfewKgD6PO1S13v1Q55EkGrZKicowwU~-9S-S5HwsewGSQ7xm68zq2NgYMGb4ilRgW6fhtpeOcra7UXsUW0w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":395,"name":"Experimental Archaeology","url":"https://www.academia.edu/Documents/in/Experimental_Archaeology"},{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":127334,"name":"Lithic Studies","url":"https://www.academia.edu/Documents/in/Lithic_Studies"},{"id":205576,"name":"Basalt","url":"https://www.academia.edu/Documents/in/Basalt"},{"id":466993,"name":"Confusion","url":"https://www.academia.edu/Documents/in/Confusion"}],"urls":[]}, dispatcherData: dispatcherData }); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=94444823]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444823,"title":"Contribución del yacimiento Galería (Sierra de Atapuerca) al Cuaternario Ibérico","internal_url":"https://www.academia.edu/94444823/Contribuci%C3%B3n_del_yacimiento_Galer%C3%ADa_Sierra_de_Atapuerca_al_Cuaternario_Ib%C3%A9rico","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="94444822"><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/94444822/Applying_SEM_to_the_study_of_use_wear_on_unmodified_shell_tools_an_experimental_approach"><img alt="Research paper thumbnail of Applying SEM to the study of use-wear on unmodified shell tools: an experimental approach" 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/94444822/Applying_SEM_to_the_study_of_use_wear_on_unmodified_shell_tools_an_experimental_approach">Applying SEM to the study of use-wear on unmodified shell tools: an experimental approach</a></div><div class="wp-workCard_item"><span>Journal of Archaeological Science</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Although in prehistoric archaeology the evidence provided by molluscs has often been stu...</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">Abstract Although in prehistoric archaeology the evidence provided by molluscs has often been studied, few works have focused on the functional analysis of shells as tools. A number of prehistoric sites around the world are producing evidence from retouched shells that indicates that they were used for certain operations. In recent years, several experimental studies have been conducted for the purpose of gaining insight into the processes involved in shell tool production and use. This paper focuses on the procedures and the preliminary results of a program of use-wear experiments based on SEM analysis, and corroborates that non-retouched shells can also yield interesting results and can be used as a reference against which archaeological materials can be compared.</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="94444822"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444822"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444822; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=94444822]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444822,"title":"Applying SEM to the study of use-wear on unmodified shell tools: an experimental approach","internal_url":"https://www.academia.edu/94444822/Applying_SEM_to_the_study_of_use_wear_on_unmodified_shell_tools_an_experimental_approach","owner_id":2858486,"coauthors_can_edit":true,"owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[]}, 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="94444821"><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/94444821/The_nature_of_technological_changes_The_Middle_Pleistocene_stone_tool_assemblages_from_Galer%C3%ADa_and_Gran_Dolina_subunit_TD10_1_Atapuerca_Spain_"><img alt="Research paper thumbnail of The nature of technological changes: The Middle Pleistocene stone tool assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain)" class="work-thumbnail" src="https://attachments.academia-assets.com/96899212/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/94444821/The_nature_of_technological_changes_The_Middle_Pleistocene_stone_tool_assemblages_from_Galer%C3%ADa_and_Gran_Dolina_subunit_TD10_1_Atapuerca_Spain_">The nature of technological changes: The Middle Pleistocene stone tool assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain)</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This article focuses on the origins for technological variation during the Middle Pleistocene thr...</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 article focuses on the origins for technological variation during the Middle Pleistocene through the analysis of the lithic assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain). The technological study was organized into three main levels of analysis. The first stage consisted of the technological characterization of the whole assemblage (e.g. the general composition of each sample, the exploitation and shaping methods used, and the characteristics of each item). The second stage involved the morphometric analysis of the large tools, mainly handaxes and cleavers, given the significance of these instruments in Middle Pleistocene assemblages. In this case, we combined traditional technical and metrical analyses with current morphometric methods. Lastly, taking into account the general characteristics of these sites, the third stage consisted of assessing how the different occupational strategies affected the lithic representation. These analyses allowed us to define three technological groups. The first includes unit Galería-GIIa, which corresponds to the appearance of the Acheulean in the Atapuerca caves. The second is represented by the rest of the sequence of the Galería site, mainly the upper part of the sequence (unit GIII). And the third technological corresponds to Gran Dolina-subunit TD10.1. Thus, the Galería sequence shows the technological evolution of the Acheulean over a period of 250 ka. Furthermore, subunit TD10.1 represents a new occupational strategy combining traditional Acheulean tools with more evolved technical strategies.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="71a585ab05c00d342473b49f89840c02" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":96899212,"asset_id":94444821,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/96899212/download_file?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="94444821"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="94444821"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 94444821; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=94444821]").text(description); $(".js-view-count[data-work-id=94444821]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 94444821; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='94444821']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "71a585ab05c00d342473b49f89840c02" } } $('.js-work-strip[data-work-id=94444821]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":94444821,"title":"The nature of technological changes: The Middle Pleistocene stone tool assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain)","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"This article focuses on the origins for technological variation during the Middle Pleistocene through the analysis of the lithic assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain). The technological study was organized into three main levels of analysis. The first stage consisted of the technological characterization of the whole assemblage (e.g. the general composition of each sample, the exploitation and shaping methods used, and the characteristics of each item). The second stage involved the morphometric analysis of the large tools, mainly handaxes and cleavers, given the significance of these instruments in Middle Pleistocene assemblages. In this case, we combined traditional technical and metrical analyses with current morphometric methods. Lastly, taking into account the general characteristics of these sites, the third stage consisted of assessing how the different occupational strategies affected the lithic representation. These analyses allowed us to define three technological groups. The first includes unit Galería-GIIa, which corresponds to the appearance of the Acheulean in the Atapuerca caves. The second is represented by the rest of the sequence of the Galería site, mainly the upper part of the sequence (unit GIII). And the third technological corresponds to Gran Dolina-subunit TD10.1. Thus, the Galería sequence shows the technological evolution of the Acheulean over a period of 250 ka. Furthermore, subunit TD10.1 represents a new occupational strategy combining traditional Acheulean tools with more evolved technical strategies.","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Quaternary International","grobid_abstract_attachment_id":96899212},"translated_abstract":null,"internal_url":"https://www.academia.edu/94444821/The_nature_of_technological_changes_The_Middle_Pleistocene_stone_tool_assemblages_from_Galer%C3%ADa_and_Gran_Dolina_subunit_TD10_1_Atapuerca_Spain_","translated_internal_url":"","created_at":"2023-01-06T02:34:55.146-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2858486,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":96899212,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899212/thumbnails/1.jpg","file_name":"j.quaint.2015.03.00620230106-1-1pxqpvh.pdf","download_url":"https://www.academia.edu/attachments/96899212/download_file","bulk_download_file_name":"The_nature_of_technological_changes_The.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899212/j.quaint.2015.03.00620230106-1-1pxqpvh-libre.pdf?1673003248=\u0026response-content-disposition=attachment%3B+filename%3DThe_nature_of_technological_changes_The.pdf\u0026Expires=1738769133\u0026Signature=OLcbhQuVDyTKBQcOvZIi6yrI~GOYkAziuWcbGK0BwgXViypHi4zviDOGG4b2bphuOOpfQo9ZI~r~0WAzYa9QDeh4IYG7tGRZJVgFC9RKbU7KM3mSTz-W2COThdtS3aPN1nZMgbY-XVQYUBJJO-akwZIGEIeNpNxVoEFY0Xw1j5qsaa3Rpzvn45oOd4MF5l3429zYZECzQaSQNofk1RP~5zMTm2heiESSjY1nWub7g~ovHLkDzGHkukV6RLQ1mGp-pbAI4cJm7ecJvg~iwqFAC1wNzjvOdmC2wN46DWjzEy3AlBPHHTScLiTJRZM55G5iIy~XctgqjnCKZW~xvuPZEA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_nature_of_technological_changes_The_Middle_Pleistocene_stone_tool_assemblages_from_Galería_and_Gran_Dolina_subunit_TD10_1_Atapuerca_Spain_","translated_slug":"","page_count":20,"language":"en","content_type":"Work","summary":"This article focuses on the origins for technological variation during the Middle Pleistocene through the analysis of the lithic assemblages from Galería and Gran Dolina-subunit TD10.1 (Atapuerca, Spain). The technological study was organized into three main levels of analysis. The first stage consisted of the technological characterization of the whole assemblage (e.g. the general composition of each sample, the exploitation and shaping methods used, and the characteristics of each item). The second stage involved the morphometric analysis of the large tools, mainly handaxes and cleavers, given the significance of these instruments in Middle Pleistocene assemblages. In this case, we combined traditional technical and metrical analyses with current morphometric methods. Lastly, taking into account the general characteristics of these sites, the third stage consisted of assessing how the different occupational strategies affected the lithic representation. These analyses allowed us to define three technological groups. The first includes unit Galería-GIIa, which corresponds to the appearance of the Acheulean in the Atapuerca caves. The second is represented by the rest of the sequence of the Galería site, mainly the upper part of the sequence (unit GIII). And the third technological corresponds to Gran Dolina-subunit TD10.1. Thus, the Galería sequence shows the technological evolution of the Acheulean over a period of 250 ka. Furthermore, subunit TD10.1 represents a new occupational strategy combining traditional Acheulean tools with more evolved technical strategies.","owner":{"id":2858486,"first_name":"Andreu","middle_initials":null,"last_name":"Ollé","page_name":"AndreuOllé","domain_name":"iphes","created_at":"2012-12-08T06:18:23.703-08:00","display_name":"Andreu Ollé","url":"https://iphes.academia.edu/AndreuOll%C3%A9"},"attachments":[{"id":96899212,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/96899212/thumbnails/1.jpg","file_name":"j.quaint.2015.03.00620230106-1-1pxqpvh.pdf","download_url":"https://www.academia.edu/attachments/96899212/download_file","bulk_download_file_name":"The_nature_of_technological_changes_The.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/96899212/j.quaint.2015.03.00620230106-1-1pxqpvh-libre.pdf?1673003248=\u0026response-content-disposition=attachment%3B+filename%3DThe_nature_of_technological_changes_The.pdf\u0026Expires=1738769133\u0026Signature=OLcbhQuVDyTKBQcOvZIi6yrI~GOYkAziuWcbGK0BwgXViypHi4zviDOGG4b2bphuOOpfQo9ZI~r~0WAzYa9QDeh4IYG7tGRZJVgFC9RKbU7KM3mSTz-W2COThdtS3aPN1nZMgbY-XVQYUBJJO-akwZIGEIeNpNxVoEFY0Xw1j5qsaa3Rpzvn45oOd4MF5l3429zYZECzQaSQNofk1RP~5zMTm2heiESSjY1nWub7g~ovHLkDzGHkukV6RLQ1mGp-pbAI4cJm7ecJvg~iwqFAC1wNzjvOdmC2wN46DWjzEy3AlBPHHTScLiTJRZM55G5iIy~XctgqjnCKZW~xvuPZEA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":30254,"name":"Pleistocene","url":"https://www.academia.edu/Documents/in/Pleistocene"},{"id":35587,"name":"Quaternary","url":"https://www.academia.edu/Documents/in/Quaternary"},{"id":77502,"name":"Early Pleistocene","url":"https://www.academia.edu/Documents/in/Early_Pleistocene"},{"id":80691,"name":"Raw materials","url":"https://www.academia.edu/Documents/in/Raw_materials"},{"id":138930,"name":"Acheulean","url":"https://www.academia.edu/Documents/in/Acheulean"},{"id":185242,"name":"Raw Material","url":"https://www.academia.edu/Documents/in/Raw_Material"},{"id":390272,"name":"Occupation Type","url":"https://www.academia.edu/Documents/in/Occupation_Type"},{"id":1930970,"name":"Technological Evolution","url":"https://www.academia.edu/Documents/in/Technological_Evolution"},{"id":2949810,"name":"Large Cutting Tools","url":"https://www.academia.edu/Documents/in/Large_Cutting_Tools"}],"urls":[{"id":27796544,"url":"https://api.elsevier.com/content/article/PII:S1040618215001901?httpAccept=text/xml"}]}, 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="4253372" id="conferenceabstracts"><div class="js-work-strip profile--work_container" data-work-id="19579330"><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/19579330/Traceological_analysis_of_a_singular_artifact_The_rock_crystal_point_from_O_Achadizo_Boiro_A_Coru%C3%B1a_Galicia_"><img alt="Research paper thumbnail of Traceological analysis of a singular artifact. The rock crystal point from O Achadizo (Boiro, A Coruña, Galicia)" class="work-thumbnail" src="https://attachments.academia-assets.com/40708798/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/19579330/Traceological_analysis_of_a_singular_artifact_The_rock_crystal_point_from_O_Achadizo_Boiro_A_Coru%C3%B1a_Galicia_">Traceological analysis of a singular artifact. The rock crystal point from O Achadizo (Boiro, A Coruña, Galicia)</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://ub.academia.edu/JuanLuisFern%C3%A1ndezMarchena">Juan Luis Fernández Marchena</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://usc-es.academia.edu/AlbaAnt%C3%ADaRodr%C3%ADguezN%C3%B3voa">Alba Antía Rodríguez Nóvoa</a>, <a class="" data-click-track="profile-work-strip-authors" rel="nofollow" href="https://usc-es.academia.edu/CrisSeoane">Cristina Seoane Novo</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://usc-es.academia.edu/EstevoAmadoRodr%C3%ADguez">Estevo Amado Rodríguez</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="cd76a4e2df9b9016e09f663fa5c59d6c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":40708798,"asset_id":19579330,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/40708798/download_file?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="19579330"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="19579330"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 19579330; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=19579330]").text(description); $(".js-view-count[data-work-id=19579330]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 19579330; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='19579330']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "cd76a4e2df9b9016e09f663fa5c59d6c" } } $('.js-work-strip[data-work-id=19579330]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":19579330,"title":"Traceological analysis of a singular artifact. The rock crystal point from O Achadizo (Boiro, A Coruña, Galicia)","internal_url":"https://www.academia.edu/19579330/Traceological_analysis_of_a_singular_artifact_The_rock_crystal_point_from_O_Achadizo_Boiro_A_Coru%C3%B1a_Galicia_","owner_id":1003485,"coauthors_can_edit":true,"owner":{"id":1003485,"first_name":"Juan Luis","middle_initials":null,"last_name":"Fernández Marchena","page_name":"JuanLuisFernándezMarchena","domain_name":"ub","created_at":"2011-12-01T05:28:06.088-08:00","display_name":"Juan Luis Fernández Marchena","url":"https://ub.academia.edu/JuanLuisFern%C3%A1ndezMarchena"},"attachments":[{"id":40708798,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/40708798/thumbnails/1.jpg","file_name":"ISKM-2015_-_Fernandez_Marchena_et_al_-_O_Achadizo.pdf","download_url":"https://www.academia.edu/attachments/40708798/download_file","bulk_download_file_name":"Traceological_analysis_of_a_singular_art.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/40708798/ISKM-2015_-_Fernandez_Marchena_et_al_-_O_Achadizo-libre.pdf?1449673529=\u0026response-content-disposition=attachment%3B+filename%3DTraceological_analysis_of_a_singular_art.pdf\u0026Expires=1739769008\u0026Signature=cCE5k8zvzwIZFbp1D~iNvlcIrN4G5XcVnC250K02fr4QW2Ge9~KrlPi5cKxlg2Qb8-C~vo3HcTsHV0-vca9GVJqCvVP-saf~3lzG12M4J7ETzRCQaISY55gek1LFusvfFn-EPNruqX4vioEJMDvCehBl-dXrxtuyIAC6LfOt6ijXlux1sZy4DpuKm50lL~IEjko-BZdSdENAIw57nqpLuA7FuE2Q~ae7yUevlsbRWRZLYT609OqExmxSFY823UW60blMyO~7QFz-8eJkawwrjwXuvQgvrwTKFcRUBJEEXGUdbBuyZKzPxDKvIP9XzHZDWJUXsty3-ktAohZtre81aA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, 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="5148114" id="poster"><div class="js-work-strip profile--work_container" data-work-id="24952802"><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/24952802/Human_predatory_behaviour_and_social_implications_of_bison_communal_hunting_at_Gran_Dolina_TD10_2_Atapuerca_"><img alt="Research paper thumbnail of Human predatory behaviour and social implications of bison communal hunting at Gran Dolina TD10.2 (Atapuerca)" class="work-thumbnail" src="https://attachments.academia-assets.com/45283546/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/24952802/Human_predatory_behaviour_and_social_implications_of_bison_communal_hunting_at_Gran_Dolina_TD10_2_Atapuerca_">Human predatory behaviour and social implications of bison communal hunting at Gran Dolina TD10.2 (Atapuerca)</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/AntonioRodr%C3%ADguezHidalgo">Antonio Rodríguez-Hidalgo</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/PalmiraSaladieBalleste">Palmira Saladié</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Zooarcheological research informs us about not only subsistence but social behavior in the past. ...</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">Zooarcheological research informs us about not only subsistence but social behavior in the past. Following Driver (1), the social organization of hunting parties, the type of predation (number and rate of animal slaughtered), and the technology used (tactics and tools) must be taken into account to identify and classify the hunting methods in prehistory. In these sense, communal hunting is a technique that implies the participation of several people, including those that usually don’t participate in hunting parties as, children and elders, for killing several prey animals in a single event, often seasonally (1, 2, and 3). In this sense zooarcheological testing of this hunting practice provides valuable information about cognitive development, social integration, cooperation among group members, and other interesting aspects of behavior beyond the strictly economical.<br />Here we present the faunal analysis of the "bison bone bed" layer from TD10.2 sub-unit (Gran Dolina site, Atapuerca, Spain) based on zooarchaeology and taphonomical archaeology  methods (4). To obtain the results we have taken into account taxonomic diversity rates, skeletal profiles, mortality profiles, seasonality, statistical approaches to density mediated attrition and taphonomic modifications in bone surfaces.<br />The taxonomic and anatomical composition indicates a monospecific assemblage heavily dominated by axial elements of Bison sp. The abundance of anthropogenic modifications are in concordance with early and primary access to the carcasses and the development of systematic butchering focused on the exploitation of meat and fat and the transportation of high yield elements to somewhere near the cave. Together with a catastrophic and seasonal mortality pattern, our research suggests the procurement of bison by communal hunting as early as circa 400 ka B.P. <br />Ethnographic, ethnohistorical, and archeological analogies allowed us to interpret the "bison bone bed" as a kill-butchering site used for several seasonal events of mass communal hunting in which herds of bison were slaughtered to be exploited intensively by the hominines that occupied the cave. The repeated seasonal use of one location on the landscape for the development of specific tasks can be related with a modern logistical like pattern of resource management. In the same way, the early existence of mass communal hunting as a predation technique inform us about the emergence of cognitive, technological, and social skills similar to those exhibited by other modern communal hunters.<br />Evidence from monospecific faunal assemblages largely dominated by large ungulates that exhibit a high number of animals slaughtered, catastrophic mortality profiles, seasonal mortality, systematic exploitation of carcasses, and transport of elements of high utility is common features used to infer communal hunting in the MP, Upper Paleolithic, and recent times (5). These characteristics are fully consistent with those observed in the faunal assemblage of the TD10.2 "bison bone bed", suggesting that cognitive and technological capabilities required for successful communal hunting of large ungulates was fully developed in the pre-Neanderthal populations of Atapuerca as early as the Middle Pleistocene.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e41b0dcce4eac73aed0b0eac1a8ad22c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":45283546,"asset_id":24952802,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/45283546/download_file?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="24952802"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="24952802"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 24952802; 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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="7832236" id="callforpapers"><div class="js-work-strip profile--work_container" data-work-id="35494714"><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/35494714/Call_for_abstracts_SESSION_438_Not_only_use_Application_of_functional_methods_for_a_better_comprehension_of_operative_chains"><img alt="Research paper thumbnail of Call for abstracts SESSION 438: Not only use. Application of functional methods for a better comprehension of operative chains" class="work-thumbnail" src="https://attachments.academia-assets.com/55357820/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/35494714/Call_for_abstracts_SESSION_438_Not_only_use_Application_of_functional_methods_for_a_better_comprehension_of_operative_chains">Call for abstracts SESSION 438: Not only use. Application of functional methods for a better comprehension of operative chains</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://ub.academia.edu/JuanLuisFern%C3%A1ndezMarchena">Juan Luis Fernández Marchena</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the past few years, new approaches emerged in wear studies including a wide variety of new ana...</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 past few years, new approaches emerged in wear studies including a wide variety of new analytical methods. Moreover, these studies have been frequently supported by experimental data in order to better interpret the archaeological record. The growing interest in understanding the function of objects has also enhanced to expand the materials (e.g. rock, shell, bone, metal, pottery) and types of objects (e.g. cutting tools, scrapers, ornaments, vessels) analysed. One of the aims of this session is to bring together different methodologies used in wear studies and to take advantages of multidisciplinary studies of traces of different origin (i.e. technological marks, use-wear, post-depositional alteration marks and residues). Finally, in this session we aim to discuss the reconstruction of operative chain starting from object manufacture to its use and discard at the site. Therefore, we invite presentations related to the study of marks resulting from production, use and post-depositional processes that will attempt to integrate different activities and different raw materials in both experimental and archaeological assemblages. We also welcome contributions on the application of new methodologies with high diagnostic value to analyse traces of different origin. Combination of different methodologies and microscopic study techniques will be one of the central issues in this session. 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Furthermore, the development of new experiments and experimental protocols related to the formation of different traces on artefacts of different raw materials will have an important role within this session.","owner":{"id":1003485,"first_name":"Juan Luis","middle_initials":null,"last_name":"Fernández Marchena","page_name":"JuanLuisFernándezMarchena","domain_name":"ub","created_at":"2011-12-01T05:28:06.088-08:00","display_name":"Juan Luis Fernández Marchena","url":"https://ub.academia.edu/JuanLuisFern%C3%A1ndezMarchena"},"attachments":[{"id":55357820,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/55357820/thumbnails/1.jpg","file_name":"EAA_Session_438_-_Not_only_use.pdf","download_url":"https://www.academia.edu/attachments/55357820/download_file","bulk_download_file_name":"Call_for_abstracts_SESSION_438_Not_only.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/55357820/EAA_Session_438_-_Not_only_use-libre.pdf?1513967954=\u0026response-content-disposition=attachment%3B+filename%3DCall_for_abstracts_SESSION_438_Not_only.pdf\u0026Expires=1738769133\u0026Signature=dQAvYv4whOgHtM1yPu6m47F7xJ84A6ElAFL1HX3ArXL3koBHLVsIFoMpbYti5cvgUY-KOv7x77xdo85JZK9UoZIN8DN-GBxO5MU0sqf2jNUQpkBFg3UBi2BMk8l44Oi1t53cCKwMELlvTWo9PXAhGof9NT1VoMPAnq62wvYgLwmRxLoUTL3RY82FIzak0wlX17uVzLRCo08BHm9bOQ0nqCYRZ2F460eZM~RNkR6ni~Jjf7iExInsI9SC2DSfgitX8c~vNHa-n241mphe0353Wz8HQXef~w7S12raShdmlHdDUcC1PrSdob0VBq5Bq6mrTfObW~E1UtmWdKZZm-UyOw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":371,"name":"Functional Analysis","url":"https://www.academia.edu/Documents/in/Functional_Analysis"},{"id":399,"name":"Prehistoric Archaeology","url":"https://www.academia.edu/Documents/in/Prehistoric_Archaeology"},{"id":2213,"name":"Pottery (Archaeology)","url":"https://www.academia.edu/Documents/in/Pottery_Archaeology_"},{"id":15328,"name":"Use Wear Analysis","url":"https://www.academia.edu/Documents/in/Use_Wear_Analysis"},{"id":28020,"name":"Residue Analysis (Archaeology)","url":"https://www.academia.edu/Documents/in/Residue_Analysis_Archaeology_"},{"id":28899,"name":"Residue and Use-Wear Analysis","url":"https://www.academia.edu/Documents/in/Residue_and_Use-Wear_Analysis"},{"id":41464,"name":"Traceology","url":"https://www.academia.edu/Documents/in/Traceology"},{"id":229325,"name":"Traceologie","url":"https://www.academia.edu/Documents/in/Traceologie"},{"id":238372,"name":"Tracéologie Osseuse","url":"https://www.academia.edu/Documents/in/Traceologie_Osseuse"},{"id":297514,"name":"Butchery Marks, Experimental Archaeology, Traceology","url":"https://www.academia.edu/Documents/in/Butchery_Marks_Experimental_Archaeology_Traceology"},{"id":363279,"name":"Tracéologie","url":"https://www.academia.edu/Documents/in/Trac%C3%A9ologie"},{"id":412553,"name":"Analyse Fonctionnelle, Traceology","url":"https://www.academia.edu/Documents/in/Analyse_Fonctionnelle_Traceology"},{"id":446310,"name":"Pottery traceology","url":"https://www.academia.edu/Documents/in/Pottery_traceology"},{"id":462125,"name":"Traceología","url":"https://www.academia.edu/Documents/in/Traceologia"},{"id":520465,"name":"Bone tools and Use-wear Analisys","url":"https://www.academia.edu/Documents/in/Bone_tools_and_Use-wear_Analisys"}],"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="8285961" id="conferencepresentations"><div class="js-work-strip profile--work_container" data-work-id="37670908"><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/37670908/Objectifying_processes_The_multivariate_analyses_of_the_Acheulean_Tools_in_the_Western_Europe"><img alt="Research paper thumbnail of Objectifying processes: The multivariate analyses of the Acheulean Tools in the Western Europe" class="work-thumbnail" src="https://attachments.academia-assets.com/57659769/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/37670908/Objectifying_processes_The_multivariate_analyses_of_the_Acheulean_Tools_in_the_Western_Europe">Objectifying processes: The multivariate analyses of the Acheulean Tools in the Western Europe</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://iphes.academia.edu/PaulaGarc%C3%ADaMedrano">Paula García-Medrano</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span>IEEE INTERNATIONAL CONFERENCE ON METROLOGY FOR ARCHAEOLOGY AND CULTURAL HERITAGE</span><span>, Oct 22, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3dc583d9e422a77e5a491009f8a21949" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":57659769,"asset_id":37670908,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/57659769/download_file?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="37670908"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="37670908"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 37670908; 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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="36817246"><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/36817246/The_Western_European_Acheulean_a_new_methodological_approach_for_the_study_of_the_Middle_Pleistocene_occupation_of_Europe"><img alt="Research paper thumbnail of The Western European Acheulean: a new methodological approach for the study of the Middle Pleistocene occupation of Europe" class="work-thumbnail" src="https://attachments.academia-assets.com/56768274/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/36817246/The_Western_European_Acheulean_a_new_methodological_approach_for_the_study_of_the_Middle_Pleistocene_occupation_of_Europe">The Western European Acheulean: a new methodological approach for the study of the Middle Pleistocene occupation of Europe</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://iphes.academia.edu/PaulaGarc%C3%ADaMedrano">Paula García-Medrano</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span>XVIII UISPP WORLD CONGRESS, PARIS</span><span>, Jun 5, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Acheulean technology marked a revolution and its presence can be clearly tracked along the Eu...</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 Acheulean technology marked a revolution and its presence can be clearly tracked along the European seaboard from the Iberian Peninsula to Great Britain , mainly between 700 to 300ka. Nevertheless , to go beyond the local perspective and gain a regional point of view requires a deep understanding of the underlying technology to identify the differences or similarities in processes and traditions of manufacture. The different criteria to analyze and to categorize the results make it difficult to compare data from different research traditions. Although many technological approaches have been developed , there are still differences in method between the different countries. The British research has been based on the typological system of Wymer or the morphometric system of Roe for the analysis and classification of handaxes , as well ason the simple description of shaping sequences developed by Newcomer and Wenban-Smith. In turn , the French traditions are mainly based on the ty-pological view proposed by Bordes , on the complex approach of the chaine operatoire , and on the techno-functional approach proposed by Bó ' eda. Meanwhile , the Spanish tradition has been highly influenced by the French school , with significant methodological developments coming from the Logical Analytic System. This work proposes a common method of analysis for the study of Large Cutting Tools from several sites in UK and France (La Noira , Brandon Fields , Cagny Le Garenne , Elveden , Swanscombe , La Celle , Saint Pierre les Elbeuf , Menez Dregan) , based on a selection of technological attributes from the main traditions of lithic analysis (typological , technological , morphometrical and sequential) that are considered to be specially significant. The attributes will be those which give more information about the Large Cutting Tools and how they have been produced. Each tool will be analyzed as a unit and also divided in its three main morpho-potential sections: distal , medium and proximal parts. In addition , taking advantage of new technologies and combining the basic technological analysis with 3D models , will allow us to standardize the process of measurement and documentation of the pieces more objectively. The measurements obtained will be man-aged through an open-access data base in order to promote the accumulative information of Western European sites.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0015379231ac8e1e2e8df501d1c34df8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":56768274,"asset_id":36817246,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/56768274/download_file?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="36817246"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36817246"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36817246; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36817246]").text(description); $(".js-view-count[data-work-id=36817246]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36817246; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36817246']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "0015379231ac8e1e2e8df501d1c34df8" } } $('.js-work-strip[data-work-id=36817246]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36817246,"title":"The Western European Acheulean: a new methodological approach for the study of the Middle Pleistocene occupation of Europe","translated_title":"","metadata":{"abstract":"The Acheulean technology marked a revolution and its presence can be clearly tracked along the European seaboard from the Iberian Peninsula to Great Britain , mainly between 700 to 300ka. Nevertheless , to go beyond the local perspective and gain a regional point of view requires a deep understanding of the underlying technology to identify the differences or similarities in processes and traditions of manufacture. The different criteria to analyze and to categorize the results make it difficult to compare data from different research traditions. Although many technological approaches have been developed , there are still differences in method between the different countries. The British research has been based on the typological system of Wymer or the morphometric system of Roe for the analysis and classification of handaxes , as well ason the simple description of shaping sequences developed by Newcomer and Wenban-Smith. In turn , the French traditions are mainly based on the ty-pological view proposed by Bordes , on the complex approach of the chaine operatoire , and on the techno-functional approach proposed by Bó ' eda. Meanwhile , the Spanish tradition has been highly influenced by the French school , with significant methodological developments coming from the Logical Analytic System. This work proposes a common method of analysis for the study of Large Cutting Tools from several sites in UK and France (La Noira , Brandon Fields , Cagny Le Garenne , Elveden , Swanscombe , La Celle , Saint Pierre les Elbeuf , Menez Dregan) , based on a selection of technological attributes from the main traditions of lithic analysis (typological , technological , morphometrical and sequential) that are considered to be specially significant. The attributes will be those which give more information about the Large Cutting Tools and how they have been produced. Each tool will be analyzed as a unit and also divided in its three main morpho-potential sections: distal , medium and proximal parts. In addition , taking advantage of new technologies and combining the basic technological analysis with 3D models , will allow us to standardize the process of measurement and documentation of the pieces more objectively. The measurements obtained will be man-aged through an open-access data base in order to promote the accumulative information of Western European sites.","location":"Paris","event_date":{"day":5,"month":6,"year":2018,"errors":{}},"organization":"XVIII UISPP WORLD CONGRESS, PARIS","publication_date":{"day":5,"month":6,"year":2018,"errors":{}},"publication_name":"XVIII UISPP WORLD CONGRESS, PARIS"},"translated_abstract":"The Acheulean technology marked a revolution and its presence can be clearly tracked along the European seaboard from the Iberian Peninsula to Great Britain , mainly between 700 to 300ka. 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The morphological variability of Large Cutting Tools during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. The Quarry 1/B sample is ideal for assessing the role of some key raw material characteristics (size, form, and homogeneity of the flint nodules) in the shaping process, and to ascertain if they represent real constraints in the production of a handaxe. In addition, because of the large number of handaxes and the intensity of the thinning process at Boxgrove, we aimed to assess the extent to which reduction intensity affected the final shape as proposed by some authors. In Q1/B we found both rough-outs (N=62) and finished tools (N=358). Each piece was systematically measured, and the data subjected to statistical analyses. The morphological variability was analysed using a geometric morphometrics methodology and PCA. In addition , we developed an experimental programme aimed to replicate the Boxgrove shaping strategies, which was especially focused on assessing the raw material role within these processes. Our results show that the knapping strategies were flexible and adapted to the blank's physical characteristics and attributes. These affect the reduction strategy but there is no clear relationship between the initial morphology of the blank and the specific final handaxe shape. Throughout the experimental programme, we also explored the knapper's capacity to solve problems arising from reduction accidents and mistakes, which led to re-configuring the knapping strategy to achieve a " mental template ". The idea set in the knapper's mind was consistent and persistent along the whole process; no substantial morphological differences related to reduction intensity were noticed within the Boxgrove Q1/B handaxes. Only the most invasive distal shaping, usually through tranchet removals, generated minor variations in shape. Thus, systematic re-sharpening as the cause of shape variation seems highly unlikely, and it could be more related to the short use-life of the Boxgrove handaxes.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d07cd4fe7b4b3dff29232b88de597361" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":56767552,"asset_id":36816643,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/56767552/download_file?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="36816643"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36816643"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36816643; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36816643]").text(description); $(".js-view-count[data-work-id=36816643]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 36816643; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='36816643']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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: "d07cd4fe7b4b3dff29232b88de597361" } } $('.js-work-strip[data-work-id=36816643]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":36816643,"title":"The cultural pattern and question of morphological variability of handaxes: Boxgrove Q1/B (Sussex, UK)","translated_title":"","metadata":{"abstract":"Boxgrove –c.500ka– represents one of the richest and more interesting sites at which to analyse shaping strategies and morphological variability inthe European Middle Pleistocene handaxes, due to the high quantity of finished handaxes and also to the presence of complete operative chains. The morphological variability of Large Cutting Tools during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. The Quarry 1/B sample is ideal for assessing the role of some key raw material characteristics (size, form, and homogeneity of the flint nodules) in the shaping process, and to ascertain if they represent real constraints in the production of a handaxe. In addition, because of the large number of handaxes and the intensity of the thinning process at Boxgrove, we aimed to assess the extent to which reduction intensity affected the final shape as proposed by some authors. In Q1/B we found both rough-outs (N=62) and finished tools (N=358). Each piece was systematically measured, and the data subjected to statistical analyses. The morphological variability was analysed using a geometric morphometrics methodology and PCA. In addition , we developed an experimental programme aimed to replicate the Boxgrove shaping strategies, which was especially focused on assessing the raw material role within these processes. Our results show that the knapping strategies were flexible and adapted to the blank's physical characteristics and attributes. These affect the reduction strategy but there is no clear relationship between the initial morphology of the blank and the specific final handaxe shape. Throughout the experimental programme, we also explored the knapper's capacity to solve problems arising from reduction accidents and mistakes, which led to re-configuring the knapping strategy to achieve a \" mental template \". The idea set in the knapper's mind was consistent and persistent along the whole process; no substantial morphological differences related to reduction intensity were noticed within the Boxgrove Q1/B handaxes. Only the most invasive distal shaping, usually through tranchet removals, generated minor variations in shape. Thus, systematic re-sharpening as the cause of shape variation seems highly unlikely, and it could be more related to the short use-life of the Boxgrove handaxes.","location":"Paris","event_date":{"day":7,"month":6,"year":2018,"errors":{}},"organization":"XVIII UISPP WORLD CONGRESS, PARIS","publication_date":{"day":null,"month":null,"year":2018,"errors":{}},"publication_name":"XVIII UISPP WORLD CONGRESS, PARIS"},"translated_abstract":"Boxgrove –c.500ka– represents one of the richest and more interesting sites at which to analyse shaping strategies and morphological variability inthe European Middle Pleistocene handaxes, due to the high quantity of finished handaxes and also to the presence of complete operative chains. The morphological variability of Large Cutting Tools during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. The Quarry 1/B sample is ideal for assessing the role of some key raw material characteristics (size, form, and homogeneity of the flint nodules) in the shaping process, and to ascertain if they represent real constraints in the production of a handaxe. In addition, because of the large number of handaxes and the intensity of the thinning process at Boxgrove, we aimed to assess the extent to which reduction intensity affected the final shape as proposed by some authors. In Q1/B we found both rough-outs (N=62) and finished tools (N=358). Each piece was systematically measured, and the data subjected to statistical analyses. The morphological variability was analysed using a geometric morphometrics methodology and PCA. In addition , we developed an experimental programme aimed to replicate the Boxgrove shaping strategies, which was especially focused on assessing the raw material role within these processes. Our results show that the knapping strategies were flexible and adapted to the blank's physical characteristics and attributes. These affect the reduction strategy but there is no clear relationship between the initial morphology of the blank and the specific final handaxe shape. Throughout the experimental programme, we also explored the knapper's capacity to solve problems arising from reduction accidents and mistakes, which led to re-configuring the knapping strategy to achieve a \" mental template \". The idea set in the knapper's mind was consistent and persistent along the whole process; no substantial morphological differences related to reduction intensity were noticed within the Boxgrove Q1/B handaxes. Only the most invasive distal shaping, usually through tranchet removals, generated minor variations in shape. Thus, systematic re-sharpening as the cause of shape variation seems highly unlikely, and it could be more related to the short use-life of the Boxgrove handaxes.","internal_url":"https://www.academia.edu/36816643/The_cultural_pattern_and_question_of_morphological_variability_of_handaxes_Boxgrove_Q1_B_Sussex_UK_","translated_internal_url":"","created_at":"2018-06-10T11:29:57.416-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":8555584,"coauthors_can_edit":true,"document_type":"conference_presentation","co_author_tags":[{"id":31517508,"work_id":36816643,"tagging_user_id":8555584,"tagged_user_id":4299579,"co_author_invite_id":null,"email":"n***4@ntlworld.com","display_order":1,"name":"Nick Ashton","title":"The cultural pattern and question of morphological variability of handaxes: Boxgrove Q1/B (Sussex, UK)"},{"id":31517509,"work_id":36816643,"tagging_user_id":8555584,"tagged_user_id":2858486,"co_author_invite_id":null,"email":"a***e@iphes.cat","affiliation":"Institut Català de Paleoecologia Humana i Evolució Social","display_order":2,"name":"Andreu Ollé","title":"The cultural pattern and question of morphological variability of handaxes: Boxgrove Q1/B (Sussex, UK)"}],"downloadable_attachments":[{"id":56767552,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/56767552/thumbnails/1.jpg","file_name":"The_cultural_pattern_and_question_of_morphological_variability_of_handaxes.pdf","download_url":"https://www.academia.edu/attachments/56767552/download_file","bulk_download_file_name":"The_cultural_pattern_and_question_of_mor.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/56767552/The_cultural_pattern_and_question_of_morphological_variability_of_handaxes-libre.pdf?1528655588=\u0026response-content-disposition=attachment%3B+filename%3DThe_cultural_pattern_and_question_of_mor.pdf\u0026Expires=1738627787\u0026Signature=NhQ4J4UNpwEzXf7DROu-~TZkrnrwNkdxmzkWWQRrNzIMQWl1o3-MJWvrFkdkuqRlivlwn~HiUTmDfLNE8oT-dm7X7GcbBxUsOPFXvVMygUMCKy535hf4qKVcEa3UXyB-tx821DgMCS9tscxBs-4Dww2wB5vPj8ldj~UqknxVK~ZYgKxaO~l4~jsnwRTobLR3SIMZwv7hgT4PR-cuzVJFD3z8gAIRxHfPv8I9JtzSPEGE9ZS1MKQccqh9Su3ziI1F-JSR41RkOng27FXwJtm5Uz7SpOeqcOU5dNYJf9I-iq951J~DJjbJRwWoisFBYo9VzGQlRzoNswetA2gcXUMzGA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_cultural_pattern_and_question_of_morphological_variability_of_handaxes_Boxgrove_Q1_B_Sussex_UK_","translated_slug":"","page_count":2,"language":"en","content_type":"Work","summary":"Boxgrove –c.500ka– represents one of the richest and more interesting sites at which to analyse shaping strategies and morphological variability inthe European Middle Pleistocene handaxes, due to the high quantity of finished handaxes and also to the presence of complete operative chains. The morphological variability of Large Cutting Tools during the Middle Pleistocene has been traditionally associated with two main variables: raw material constraints and reduction intensity. The Quarry 1/B sample is ideal for assessing the role of some key raw material characteristics (size, form, and homogeneity of the flint nodules) in the shaping process, and to ascertain if they represent real constraints in the production of a handaxe. In addition, because of the large number of handaxes and the intensity of the thinning process at Boxgrove, we aimed to assess the extent to which reduction intensity affected the final shape as proposed by some authors. In Q1/B we found both rough-outs (N=62) and finished tools (N=358). Each piece was systematically measured, and the data subjected to statistical analyses. The morphological variability was analysed using a geometric morphometrics methodology and PCA. In addition , we developed an experimental programme aimed to replicate the Boxgrove shaping strategies, which was especially focused on assessing the raw material role within these processes. Our results show that the knapping strategies were flexible and adapted to the blank's physical characteristics and attributes. These affect the reduction strategy but there is no clear relationship between the initial morphology of the blank and the specific final handaxe shape. Throughout the experimental programme, we also explored the knapper's capacity to solve problems arising from reduction accidents and mistakes, which led to re-configuring the knapping strategy to achieve a \" mental template \". The idea set in the knapper's mind was consistent and persistent along the whole process; no substantial morphological differences related to reduction intensity were noticed within the Boxgrove Q1/B handaxes. Only the most invasive distal shaping, usually through tranchet removals, generated minor variations in shape. Thus, systematic re-sharpening as the cause of shape variation seems highly unlikely, and it could be more related to the short use-life of the Boxgrove handaxes.","owner":{"id":8555584,"first_name":"Paula","middle_initials":null,"last_name":"García-Medrano","page_name":"PaulaGarcíaMedrano","domain_name":"iphes","created_at":"2014-01-23T23:24:26.232-08:00","display_name":"Paula García-Medrano","url":"https://iphes.academia.edu/PaulaGarc%C3%ADaMedrano"},"attachments":[{"id":56767552,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/56767552/thumbnails/1.jpg","file_name":"The_cultural_pattern_and_question_of_morphological_variability_of_handaxes.pdf","download_url":"https://www.academia.edu/attachments/56767552/download_file","bulk_download_file_name":"The_cultural_pattern_and_question_of_mor.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/56767552/The_cultural_pattern_and_question_of_morphological_variability_of_handaxes-libre.pdf?1528655588=\u0026response-content-disposition=attachment%3B+filename%3DThe_cultural_pattern_and_question_of_mor.pdf\u0026Expires=1738627787\u0026Signature=NhQ4J4UNpwEzXf7DROu-~TZkrnrwNkdxmzkWWQRrNzIMQWl1o3-MJWvrFkdkuqRlivlwn~HiUTmDfLNE8oT-dm7X7GcbBxUsOPFXvVMygUMCKy535hf4qKVcEa3UXyB-tx821DgMCS9tscxBs-4Dww2wB5vPj8ldj~UqknxVK~ZYgKxaO~l4~jsnwRTobLR3SIMZwv7hgT4PR-cuzVJFD3z8gAIRxHfPv8I9JtzSPEGE9ZS1MKQccqh9Su3ziI1F-JSR41RkOng27FXwJtm5Uz7SpOeqcOU5dNYJf9I-iq951J~DJjbJRwWoisFBYo9VzGQlRzoNswetA2gcXUMzGA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":19536,"name":"Morphometry","url":"https://www.academia.edu/Documents/in/Morphometry"},{"id":80691,"name":"Raw materials","url":"https://www.academia.edu/Documents/in/Raw_materials"},{"id":138930,"name":"Acheulean","url":"https://www.academia.edu/Documents/in/Acheulean"},{"id":145236,"name":"Middle Pleistocene","url":"https://www.academia.edu/Documents/in/Middle_Pleistocene"},{"id":338207,"name":"Handaxes","url":"https://www.academia.edu/Documents/in/Handaxes"},{"id":539291,"name":"Boxgrove","url":"https://www.academia.edu/Documents/in/Boxgrove"}],"urls":[]}, dispatcherData: dispatcherData }); 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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="36582285"><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/36582285/The_Mental_Template_Middle_Pleistocene_handaxe_shaping_strategies"><img alt="Research paper thumbnail of The Mental Template: Middle Pleistocene handaxe shaping strategies" 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/36582285/The_Mental_Template_Middle_Pleistocene_handaxe_shaping_strategies">The Mental Template: Middle Pleistocene handaxe shaping strategies</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://iphes.academia.edu/PaulaGarc%C3%ADaMedrano">Paula García-Medrano</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://iphes.academia.edu/AndreuOll%C3%A9">Andreu Ollé</a></span></div><div class="wp-workCard_item"><span>ESHE</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The morphological variability of Large Cutting Tools during the Middle Pleistocene has been tradi...</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 morphological variability of Large Cutting Tools during the Middle Pleistocene has been traditionally associated with two main variables: the raw material constraints and the reduction intensity. Boxgrove –c.500ka– represents one of the richest and more interesting sites at which to analyse shaping strategies and morphological variability in European Middle Pleistocene handaxes, due to the huge quantity of finished handaxes and also to the presence of complete operative chains. For this paper, we have focused on the entire handaxe sample from the excavations at Quarry 1/B.</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="36582285"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="36582285"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 36582285; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=36582285]").text(description); 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