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(Lucena, C贸rdoba): un h谩bitat achelense de cazadores en Andaluc铆a" class="work-thumbnail" src="https://attachments.academia-assets.com/53163279/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/33056322/La_cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_un_h%C3%A1bitat_achelense_de_cazadores_en_Andaluc%C3%ADa">La cueva del 脕ngel (Lucena, C贸rdoba): un h谩bitat achelense de cazadores en Andaluc铆a</a></div><div class="wp-workCard_item"><span>Menga Revista De Prehistoria De Andalucia</span><span>, 2012</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d59d5939f805aded2ab3214efcefcafa" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" 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href="https://www.academia.edu/33056319/Earliest_evidence_of_pollution_by_heavy_metals_in_archaeological_sites">Earliest evidence of pollution by heavy metals in archaeological sites</a></div><div class="wp-workCard_item"><span>Scientific Reports</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Homo species were exposed to a new biogeochemical environment when they began to occupy caves. He...</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 species were exposed to a new biogeochemical environment when they began to occupy caves. Here we report the first evidence of palaeopollution through geochemical analyses of heavy metals in four renowned archaeological caves of the Iberian Peninsula spanning the last million years of human evolution. Heavy metal contents reached high values due to natural (guano deposition) and anthropogenic factors (e.g. combustion) in restricted cave environments. The earliest anthropogenic pollution evidence is related to Neanderthal hearths from Gorham虝 s Cave (Gibraltar), being one of the first milestones in the so-called "Anthropocene". According to its heavy metal concentration, these sediments meet the present-day standards of "contaminated soil". Together with the former, the Gibraltar Vanguard Cave, shows Zn and Cu pollution ubiquitous across highly anthropic levels pointing to these elements as potential proxies for human activities. Pb concentrations in Magdalenian and Bronze age levels at El Pirulejo site can be similarly interpreted. Despite these high pollution levels, the contaminated soils might not have posed a major threat to Homo populations. Altogether, the data presented here indicate a long-term exposure of Homo to these elements, via fires, fumes and their ashes, which could have played certain role in environmental-pollution tolerance, a hitherto neglected influence.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a43e493ee18cbb735a7427c83c431e38" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163292,"asset_id":33056319,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163292/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="33056319"><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="33056319"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056319; 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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="33056316"><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/33056316/Caracterizaci%C3%B3n_mineral%C3%B3gica_del_relleno_de_edad_Pleistocena_de_la_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_"><img alt="Research paper thumbnail of Caracterizaci贸n mineral贸gica del relleno de edad Pleistocena de la Cueva del 脕ngel (Lucena, C贸rdoba)" class="work-thumbnail" src="https://attachments.academia-assets.com/53163290/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/33056316/Caracterizaci%C3%B3n_mineral%C3%B3gica_del_relleno_de_edad_Pleistocena_de_la_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_">Caracterizaci贸n mineral贸gica del relleno de edad Pleistocena de la Cueva del 脕ngel (Lucena, C贸rdoba)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">El relleno sedimentario del Pleistoceno del complejo k谩rstico de la cueva del 脕ngel se encuentra ...</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">El relleno sedimentario del Pleistoceno del complejo k谩rstico de la cueva del 脕ngel se encuentra ubicado en el extremo suroccidental de la Sierra de Araceli, en el t茅rmino municipal de Lucena (C贸rdoba). Dicho complejo k谩rstico encaja en una unidad carbon谩tica de calizas y dolom铆as del L铆as inferior y medio, pertenecientes al dominio Subb茅tico externo meridional de las Cordilleras B茅ticas. El relleno presenta m谩s de cuatro metros de potencia estratigr谩fica, donde alternan los dep贸sitos de origen qu铆mico (espeleotemas) con otros de origen mec谩nico, tanto naturales como antr贸picos (restos 贸seos e industria), que fueron acumulados en el interior de una cavidad. Dentro del relleno sedimentario se distinguen dos unidades. La primera se extiende desde el techo (-215 cm) hasta los -350 cm, presenta poco material arqueol贸gico y la fracci贸n gruesa es escasa. La segunda abarca desde -350 cm a la base actual del relleno; presenta gran cantidad de restos 贸seos, fragmentos de calcita e industria l铆tica, junto con una gran proporci贸n de constituyentes gruesos generalmente calc谩reos, sin alterar. En el presente trabajo se ha realizado el estudio textural y mineral贸gico de la secci贸n J/K, la m谩s representativa del relleno sedimentario, habi茅ndose analizado un total de 36 muestras. Los resultados del an谩lisis granulom茅trico indican una cierta homogeneidad textural en los constituyentes comprendidos entre 2 mm y la fracci贸n arcilla (<2 渭m), con predominio de la fracci贸n arena y limo. Los contenidos en carbonatos obtenidos por calcimetr铆a son generalmente superiores al 60%, coincidiendo con los resultados de difracci贸n de rayos X, donde la calcita es predominante junto a los filosilicatos, present谩ndose subordinados cuarzo y feldespatos. Destaca la presencia de hidroxiapatito con diverso grado de ordenamiento y en indicios, dolomita. El estudio de los minerales pesados ha puesto de manifiesto la abundancia de circ贸n, turmalina, distena y hornblenda, detect谩ndose tambi茅n opacos, granate, rutilo, esfena y andalucita. En la fracci贸n ligera se confirma el predominio del cuarzo acompa帽ado de feldespatos, micas y calcita, siendo destacable, por su frecuencia, la presencia de clastos redondeados de peque帽o tama帽o (0,125 mm) de restos 贸seos.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="cf7d579fddc723010be3b653d7d8d13c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163290,"asset_id":33056316,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163290/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="33056316"><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="33056316"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056316; 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This kind of evidence is more common in the Solutrean and Epi-Magdalenian occupations, with which most of the Palaeolithic art inside the cave has been associated. The recent publication by J.L. Sanchidri谩n of the use of hollows and Pecten sp. valves as possible points of illumination, indicates a close correlation between the occupations in the outer chambers and the use of deep parts of the cave in the full Glacial period.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="150f6620fefe9e128d76b92540d658ba" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163291,"asset_id":33056314,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163291/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="33056314"><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="33056314"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056314; 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La fauna se puede correlacionar con las asociaciones faun铆...</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">que reflejan la depredaci贸n selectiva. La fauna se puede correlacionar con las asociaciones faun铆sticas de Europa de finales del Pleistoceno Medio a principios del Pleistoceno Superior. El conjunto l铆tico de la cueva del 脕ngel parece encajar dentro de la diversidad regional de una bien desarrollada industria no-Levallois del Achelense Final. Una estimaci贸n preliminar de la edad 230Th/234U, la revisi贸n del conjunto l铆tico y la evidencia de la fauna, favorecen el posicionamiento cronol贸gico del sitio en un per铆odo que va desde el final del Pleistoceno Medio a principios del Pleistoceno Superior (MIS 11 -MIS 5). 3DODEUDV del 脕ngel, Cuaternario, Pleistoceno Medio, Achelense, Bison, carnicer铆a, hogar. 7+(+817(56 $EVWUDFW The Angel Cave archaeological site is an open-air sedimentary sequence, resultant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by horses, large bovids and cervids has been subjected to intense anthropic actions reflecting selective pre...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b80bc9cd4b9ff3b37f700d2e78a0d5a1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163293,"asset_id":33056313,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163293/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33056313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33056313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056313; 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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="8954694"><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/8954694/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_a_site_of_the_Middle_and_Early_Upper_Pleistocene_in_the_South_of_the_Iberian_Peninsula"><img alt="Research paper thumbnail of La Cueva del 脕ngel (Lucena, C贸rdoba), a site of the Middle and Early Upper Pleistocene in the South of the Iberian Peninsula" class="work-thumbnail" src="https://attachments.academia-assets.com/47937571/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/8954694/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_a_site_of_the_Middle_and_Early_Upper_Pleistocene_in_the_South_of_the_Iberian_Peninsula">La Cueva del 脕ngel (Lucena, C贸rdoba), a site of the Middle and Early Upper Pleistocene in the South of the Iberian Peninsula</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalahAbdessadok">Salah Abdessadok</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DanielBotella">Daniel Botella</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MiguelCaparros">Miguel Caparros</a></span></div><div class="wp-workCard_item"><span>Trabajos De Prehistoria</span><span>, 2006</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆t...</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">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆tico del sur de la Pen铆nsula Ib茅rica: la Cueva del 脕ngel (Lucena, C贸rdoba). Desde el descubrimiento en 1995 de su potencial arqueol贸gico, se ha excavado durante cuatro campa帽as y, hasta el momento, presenta un corte estratigr谩fico de unos 5 metros de potencia. Paralelamente se analiza la tecnolog铆a y tipolog铆a, la fauna, la geolog铆a de la cavidad y su relleno sedimentario. La fauna, la industria l铆tica y las dataciones absolutas sit煤an el yacimiento en el Pleistoceno medio y el Pleistoceno superior antiguo; lo que hace que esta cueva sea excepcional en la Pen铆nsula Ib茅rica.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="80d43a57357d28ba5ad099b95b033a38" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":47937571,"asset_id":8954694,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/47937571/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="8954694"><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="8954694"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8954694; 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Llasat</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">The Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collaps...</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 Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by Equus ferus, large bovids and cervids has been subjected to intense anthropic actions reflecting selective predation. The fauna may be correlated with European faunistic associations of the end of the Middle Pleistocene to the beginning of the Upper Pleistocene. The Cueva del Angel lithic assemblage (dominated by non-modified flakes and abundant retouched tools with the presence of 46 handaxes) appears to fit well within the regional diversity of a well developed non-Levallois final Acheulean industry. A preliminary 230 Th/ 234 U age estimate, the review of the lithic assemblage and faunal evidence would favour a chronological positioning of the site in a period stretching from the end of the Middle Pleistocene to the beginning of the Upper Pleistocene (MIS 11eMIS 5). The Acheulean lithic assemblage found at the Cueva del Angel fits very well with the hypothesis of a continuation of Acheulean cultural traditions in the site, distinct from the contemporaneous uniquely Mousterian complexes witnessed in other parts of the Iberian Peninsula, and Western Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b879d02daee5dcc6e21660bac388640a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49708230,"asset_id":4662477,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49708230/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="4662477"><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="4662477"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4662477; 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$(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="14398735"><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/14398735/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula"><img alt="Research paper thumbnail of The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula" class="work-thumbnail" src="https://attachments.academia-assets.com/38295172/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/14398735/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula">The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula</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://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/FilouxArnaud">Filoux Arnaud</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/GLlasat">G. Llasat</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LuisVerduBermejo">Luis Verdu Bermejo</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collaps...</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 Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by Equus ferus, large bovids and cervids has been subjected to intense anthropic actions reflecting selective predation. The fauna may be correlated with European faunistic associations of the end of the Middle Pleistocene to the beginning of the Upper Pleistocene. The Cueva del Angel lithic assemblage (dominated by non-modified flakes and abundant retouched tools with the presence of 46 handaxes) appears to fit well within the regional diversity of a well developed non-Levallois final Acheulean industry. A preliminary 230 Th/ 234 U age estimate, the review of the lithic assemblage and faunal evidence would favour a chronological positioning of the site in a period stretching from the end of the Middle Pleistocene to the beginning of the Upper Pleistocene (MIS 11eMIS 5). The Acheulean lithic assemblage found at the Cueva del Angel fits very well with the hypothesis of a continuation of Acheulean cultural traditions in the site, distinct from the contemporaneous uniquely Mousterian complexes witnessed in other parts of the Iberian Peninsula, and Western Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5a0457bb46f5b8c23d2abeff82904982" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38295172,"asset_id":14398735,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38295172/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="14398735"><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="14398735"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 14398735; 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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="14400584"><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/14400584/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_un_yacimiento_del_pleistoceno_medio_y_superior_del_sur_de_la_Pen%C3%ADnsula_Ib%C3%A9rica"><img alt="Research paper thumbnail of La Cueva del 脕ngel (Lucena, C贸rdoba), un yacimiento del pleistoceno medio y superior del sur de la Pen铆nsula Ib茅rica" class="work-thumbnail" src="https://attachments.academia-assets.com/38295687/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/14400584/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_un_yacimiento_del_pleistoceno_medio_y_superior_del_sur_de_la_Pen%C3%ADnsula_Ib%C3%A9rica">La Cueva del 脕ngel (Lucena, C贸rdoba), un yacimiento del pleistoceno medio y superior del sur de la Pen铆nsula Ib茅rica</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MuseoArqueologicoLucena">Museo Arqueologico Lucena</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆t...</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">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆tico del sur de la Pen铆nsula Ib茅rica: la Cueva del 脕ngel (Lucena, C贸rdoba). Desde el descubrimiento en 1995 de su potencial arqueol贸gico, se ha excavado durante cuatro campa帽as y, hasta el momento, presenta un corte estratigr谩fico de unos 5 metros de potencia. Paralelamente se analiza la tecnolog铆a y tipolog铆a, la fauna, la geolog铆a de la cavidad y su relleno sedimentario. La fauna, la industria l铆tica y las dataciones absolutas sit煤an el yacimiento en el Pleistoceno medio y el Pleistoceno superior antiguo; lo que hace que esta cueva sea excepcional en la Pen铆nsula Ib茅rica.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2daad5743abed11ef8fe83af45f8216e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38295687,"asset_id":14400584,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38295687/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="14400584"><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="14400584"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 14400584; 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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="33056319"><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/33056319/Earliest_evidence_of_pollution_by_heavy_metals_in_archaeological_sites"><img alt="Research paper thumbnail of Earliest evidence of pollution by heavy metals in archaeological sites" class="work-thumbnail" src="https://attachments.academia-assets.com/53163292/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/33056319/Earliest_evidence_of_pollution_by_heavy_metals_in_archaeological_sites">Earliest evidence of pollution by heavy metals in archaeological sites</a></div><div class="wp-workCard_item"><span>Scientific Reports</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Homo species were exposed to a new biogeochemical environment when they began to occupy caves. He...</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 species were exposed to a new biogeochemical environment when they began to occupy caves. Here we report the first evidence of palaeopollution through geochemical analyses of heavy metals in four renowned archaeological caves of the Iberian Peninsula spanning the last million years of human evolution. Heavy metal contents reached high values due to natural (guano deposition) and anthropogenic factors (e.g. combustion) in restricted cave environments. The earliest anthropogenic pollution evidence is related to Neanderthal hearths from Gorham虝 s Cave (Gibraltar), being one of the first milestones in the so-called "Anthropocene". According to its heavy metal concentration, these sediments meet the present-day standards of "contaminated soil". Together with the former, the Gibraltar Vanguard Cave, shows Zn and Cu pollution ubiquitous across highly anthropic levels pointing to these elements as potential proxies for human activities. Pb concentrations in Magdalenian and Bronze age levels at El Pirulejo site can be similarly interpreted. Despite these high pollution levels, the contaminated soils might not have posed a major threat to Homo populations. Altogether, the data presented here indicate a long-term exposure of Homo to these elements, via fires, fumes and their ashes, which could have played certain role in environmental-pollution tolerance, a hitherto neglected influence.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a43e493ee18cbb735a7427c83c431e38" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163292,"asset_id":33056319,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163292/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="33056319"><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="33056319"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056319; 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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="33056316"><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/33056316/Caracterizaci%C3%B3n_mineral%C3%B3gica_del_relleno_de_edad_Pleistocena_de_la_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_"><img alt="Research paper thumbnail of Caracterizaci贸n mineral贸gica del relleno de edad Pleistocena de la Cueva del 脕ngel (Lucena, C贸rdoba)" class="work-thumbnail" src="https://attachments.academia-assets.com/53163290/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/33056316/Caracterizaci%C3%B3n_mineral%C3%B3gica_del_relleno_de_edad_Pleistocena_de_la_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_">Caracterizaci贸n mineral贸gica del relleno de edad Pleistocena de la Cueva del 脕ngel (Lucena, C贸rdoba)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">El relleno sedimentario del Pleistoceno del complejo k谩rstico de la cueva del 脕ngel se encuentra ...</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">El relleno sedimentario del Pleistoceno del complejo k谩rstico de la cueva del 脕ngel se encuentra ubicado en el extremo suroccidental de la Sierra de Araceli, en el t茅rmino municipal de Lucena (C贸rdoba). Dicho complejo k谩rstico encaja en una unidad carbon谩tica de calizas y dolom铆as del L铆as inferior y medio, pertenecientes al dominio Subb茅tico externo meridional de las Cordilleras B茅ticas. El relleno presenta m谩s de cuatro metros de potencia estratigr谩fica, donde alternan los dep贸sitos de origen qu铆mico (espeleotemas) con otros de origen mec谩nico, tanto naturales como antr贸picos (restos 贸seos e industria), que fueron acumulados en el interior de una cavidad. Dentro del relleno sedimentario se distinguen dos unidades. La primera se extiende desde el techo (-215 cm) hasta los -350 cm, presenta poco material arqueol贸gico y la fracci贸n gruesa es escasa. La segunda abarca desde -350 cm a la base actual del relleno; presenta gran cantidad de restos 贸seos, fragmentos de calcita e industria l铆tica, junto con una gran proporci贸n de constituyentes gruesos generalmente calc谩reos, sin alterar. En el presente trabajo se ha realizado el estudio textural y mineral贸gico de la secci贸n J/K, la m谩s representativa del relleno sedimentario, habi茅ndose analizado un total de 36 muestras. Los resultados del an谩lisis granulom茅trico indican una cierta homogeneidad textural en los constituyentes comprendidos entre 2 mm y la fracci贸n arcilla (<2 渭m), con predominio de la fracci贸n arena y limo. Los contenidos en carbonatos obtenidos por calcimetr铆a son generalmente superiores al 60%, coincidiendo con los resultados de difracci贸n de rayos X, donde la calcita es predominante junto a los filosilicatos, present谩ndose subordinados cuarzo y feldespatos. Destaca la presencia de hidroxiapatito con diverso grado de ordenamiento y en indicios, dolomita. El estudio de los minerales pesados ha puesto de manifiesto la abundancia de circ贸n, turmalina, distena y hornblenda, detect谩ndose tambi茅n opacos, granate, rutilo, esfena y andalucita. En la fracci贸n ligera se confirma el predominio del cuarzo acompa帽ado de feldespatos, micas y calcita, siendo destacable, por su frecuencia, la presencia de clastos redondeados de peque帽o tama帽o (0,125 mm) de restos 贸seos.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="cf7d579fddc723010be3b653d7d8d13c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163290,"asset_id":33056316,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163290/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="33056316"><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="33056316"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056316; 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This kind of evidence is more common in the Solutrean and Epi-Magdalenian occupations, with which most of the Palaeolithic art inside the cave has been associated. The recent publication by J.L. Sanchidri谩n of the use of hollows and Pecten sp. valves as possible points of illumination, indicates a close correlation between the occupations in the outer chambers and the use of deep parts of the cave in the full Glacial period.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="150f6620fefe9e128d76b92540d658ba" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163291,"asset_id":33056314,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163291/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="33056314"><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="33056314"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056314; 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La fauna se puede correlacionar con las asociaciones faun铆...</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">que reflejan la depredaci贸n selectiva. La fauna se puede correlacionar con las asociaciones faun铆sticas de Europa de finales del Pleistoceno Medio a principios del Pleistoceno Superior. El conjunto l铆tico de la cueva del 脕ngel parece encajar dentro de la diversidad regional de una bien desarrollada industria no-Levallois del Achelense Final. Una estimaci贸n preliminar de la edad 230Th/234U, la revisi贸n del conjunto l铆tico y la evidencia de la fauna, favorecen el posicionamiento cronol贸gico del sitio en un per铆odo que va desde el final del Pleistoceno Medio a principios del Pleistoceno Superior (MIS 11 -MIS 5). 3DODEUDV del 脕ngel, Cuaternario, Pleistoceno Medio, Achelense, Bison, carnicer铆a, hogar. 7+(+817(56 $EVWUDFW The Angel Cave archaeological site is an open-air sedimentary sequence, resultant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by horses, large bovids and cervids has been subjected to intense anthropic actions reflecting selective pre...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b80bc9cd4b9ff3b37f700d2e78a0d5a1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":53163293,"asset_id":33056313,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/53163293/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="33056313"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="33056313"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 33056313; 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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="8954694"><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/8954694/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_a_site_of_the_Middle_and_Early_Upper_Pleistocene_in_the_South_of_the_Iberian_Peninsula"><img alt="Research paper thumbnail of La Cueva del 脕ngel (Lucena, C贸rdoba), a site of the Middle and Early Upper Pleistocene in the South of the Iberian Peninsula" class="work-thumbnail" src="https://attachments.academia-assets.com/47937571/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/8954694/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_a_site_of_the_Middle_and_Early_Upper_Pleistocene_in_the_South_of_the_Iberian_Peninsula">La Cueva del 脕ngel (Lucena, C贸rdoba), a site of the Middle and Early Upper Pleistocene in the South of the Iberian Peninsula</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SalahAbdessadok">Salah Abdessadok</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/DanielBotella">Daniel Botella</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MiguelCaparros">Miguel Caparros</a></span></div><div class="wp-workCard_item"><span>Trabajos De Prehistoria</span><span>, 2006</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆t...</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">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆tico del sur de la Pen铆nsula Ib茅rica: la Cueva del 脕ngel (Lucena, C贸rdoba). Desde el descubrimiento en 1995 de su potencial arqueol贸gico, se ha excavado durante cuatro campa帽as y, hasta el momento, presenta un corte estratigr谩fico de unos 5 metros de potencia. Paralelamente se analiza la tecnolog铆a y tipolog铆a, la fauna, la geolog铆a de la cavidad y su relleno sedimentario. La fauna, la industria l铆tica y las dataciones absolutas sit煤an el yacimiento en el Pleistoceno medio y el Pleistoceno superior antiguo; lo que hace que esta cueva sea excepcional en la Pen铆nsula Ib茅rica.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="80d43a57357d28ba5ad099b95b033a38" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":47937571,"asset_id":8954694,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/47937571/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="8954694"><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="8954694"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 8954694; 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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="4662477"><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/4662477/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula"><img alt="Research paper thumbnail of The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula" class="work-thumbnail" src="https://attachments.academia-assets.com/49708230/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/4662477/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula">The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/FilouxArnaud">Filoux Arnaud</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/SBailon">Salvador Bailon</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BoulbesNicolas">Nicolas Boulbes</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://mnhn.academia.edu/OlivierNotter">Olivier Notter</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/GLlasat">G. Llasat</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">The Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collaps...</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 Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by Equus ferus, large bovids and cervids has been subjected to intense anthropic actions reflecting selective predation. The fauna may be correlated with European faunistic associations of the end of the Middle Pleistocene to the beginning of the Upper Pleistocene. The Cueva del Angel lithic assemblage (dominated by non-modified flakes and abundant retouched tools with the presence of 46 handaxes) appears to fit well within the regional diversity of a well developed non-Levallois final Acheulean industry. A preliminary 230 Th/ 234 U age estimate, the review of the lithic assemblage and faunal evidence would favour a chronological positioning of the site in a period stretching from the end of the Middle Pleistocene to the beginning of the Upper Pleistocene (MIS 11eMIS 5). The Acheulean lithic assemblage found at the Cueva del Angel fits very well with the hypothesis of a continuation of Acheulean cultural traditions in the site, distinct from the contemporaneous uniquely Mousterian complexes witnessed in other parts of the Iberian Peninsula, and Western Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b879d02daee5dcc6e21660bac388640a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":49708230,"asset_id":4662477,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/49708230/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="4662477"><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="4662477"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4662477; 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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="14398735"><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/14398735/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula"><img alt="Research paper thumbnail of The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula" class="work-thumbnail" src="https://attachments.academia-assets.com/38295172/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/14398735/The_Cueva_del_Angel_Lucena_Spain_An_Acheulean_hunters_habitat_in_the_South_of_the_Iberian_Peninsula">The Cueva del Angel (Lucena, Spain): An Acheulean hunters habitat in the South of the Iberian Peninsula</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://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/FilouxArnaud">Filoux Arnaud</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/GLlasat">G. Llasat</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LuisVerduBermejo">Luis Verdu Bermejo</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collaps...</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 Cueva del Angel archaeological site is an open-air sedimentary sequence, remnant of a collapsed cave and part of a karst complex. The faunal assemblage dominated by Equus ferus, large bovids and cervids has been subjected to intense anthropic actions reflecting selective predation. The fauna may be correlated with European faunistic associations of the end of the Middle Pleistocene to the beginning of the Upper Pleistocene. The Cueva del Angel lithic assemblage (dominated by non-modified flakes and abundant retouched tools with the presence of 46 handaxes) appears to fit well within the regional diversity of a well developed non-Levallois final Acheulean industry. A preliminary 230 Th/ 234 U age estimate, the review of the lithic assemblage and faunal evidence would favour a chronological positioning of the site in a period stretching from the end of the Middle Pleistocene to the beginning of the Upper Pleistocene (MIS 11eMIS 5). The Acheulean lithic assemblage found at the Cueva del Angel fits very well with the hypothesis of a continuation of Acheulean cultural traditions in the site, distinct from the contemporaneous uniquely Mousterian complexes witnessed in other parts of the Iberian Peninsula, and Western Europe.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5a0457bb46f5b8c23d2abeff82904982" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38295172,"asset_id":14398735,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38295172/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="14398735"><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="14398735"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 14398735; 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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="14400584"><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/14400584/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_un_yacimiento_del_pleistoceno_medio_y_superior_del_sur_de_la_Pen%C3%ADnsula_Ib%C3%A9rica"><img alt="Research paper thumbnail of La Cueva del 脕ngel (Lucena, C贸rdoba), un yacimiento del pleistoceno medio y superior del sur de la Pen铆nsula Ib茅rica" class="work-thumbnail" src="https://attachments.academia-assets.com/38295687/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/14400584/La_Cueva_del_%C3%81ngel_Lucena_C%C3%B3rdoba_un_yacimiento_del_pleistoceno_medio_y_superior_del_sur_de_la_Pen%C3%ADnsula_Ib%C3%A9rica">La Cueva del 脕ngel (Lucena, C贸rdoba), un yacimiento del pleistoceno medio y superior del sur de la Pen铆nsula Ib茅rica</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/MuseoArqueologicoLucena">Museo Arqueologico Lucena</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://upo.academia.edu/GuadalupeMongeG%C3%B3mez">Guadalupe Monge-G贸mez</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆t...</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">En este art铆culo presentamos un avance de los trabajos realizados en un nuevo yacimiento paleol铆tico del sur de la Pen铆nsula Ib茅rica: la Cueva del 脕ngel (Lucena, C贸rdoba). Desde el descubrimiento en 1995 de su potencial arqueol贸gico, se ha excavado durante cuatro campa帽as y, hasta el momento, presenta un corte estratigr谩fico de unos 5 metros de potencia. Paralelamente se analiza la tecnolog铆a y tipolog铆a, la fauna, la geolog铆a de la cavidad y su relleno sedimentario. La fauna, la industria l铆tica y las dataciones absolutas sit煤an el yacimiento en el Pleistoceno medio y el Pleistoceno superior antiguo; lo que hace que esta cueva sea excepcional en la Pen铆nsula Ib茅rica.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2daad5743abed11ef8fe83af45f8216e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":38295687,"asset_id":14400584,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/38295687/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="14400584"><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="14400584"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 14400584; 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