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dc.contributor.authorMayoral, Eduardo
dc.contributor.authorDuveau, Jérémy
dc.contributor.authorSantos, Ana
dc.contributor.authorRodríguez Ramírez, Antonio
dc.contributor.authorMorales González, Juan Antonio
dc.contributor.authorDíaz Delgado, Ricardo
dc.contributor.authorRivera Silva, Jorge
dc.contributor.authorGómez Olivencia, Asier ORCID
dc.contributor.authorDíaz Martínez, Ignacio
dc.date.accessioned2022-11-29T18:15:28Z
dc.date.available2022-11-29T18:15:28Z
dc.date.issued2022-10
dc.identifier.citationScientific Reports 12 : (2022) // Article ID 17505es_ES
dc.identifier.issn2045-2322
dc.identifier.urihttp://hdl.handle.net/10810/58608
dc.description.abstractHominin footprints were recently discovered at Matalascanas (Huelva; South of Iberian Peninsula). They were dated thanks to a previous study in deposits of the Asperillo cliff to 106 +/- 19 ka, Upper Pleistocene, making Neandertals the most likely track-makers. In this paper, we report new Optically Stimulated Luminescence dating that places the hominin footprints surface in the range of 295.8 +/- 17 ka (MIS 9-MIS 8 transition, Middle Pleistocene). This new age implies that the possible track-makers are individuals more likely from the Neandertal evolutionary lineage. Regardless of the taxon attributed to the Matalascanas footprints, they supplement the existing partial fossil record for the European Middle Pleistocene Hominins being notably the first palaeoanthropological evidence (hominin skeleton or footprints) from the MIS 9 and MIS 8 transition discovered in the Iberian Peninsula, a moment of climatic evolution from warm to cool. Thus, the Matalascanas footprints represent a crucial record for understanding human occupations in Europe in the Pleistocene.es_ES
dc.description.sponsorshipWe thank the Territorial Delegation in Huelva of the Ministry of Agriculture, Livestock, Fisheries and Sustainable Development of the Junta de Andalucia for permission to conduct research. Furthermore, this work has been financial support from the Ministry of Science and Innovation of Spain (grant no. PID2019-104625RB-100), the Andalusian Government to the Research Group RNM276 and Basque Government to the Research Group EJ IT1418-19. In addition, AGO is supported by a Ramon y Cajal fellowship (RYC-2017-22558) and by the Ministry of Science and Innovation of Spain (grant no. PGC2018-093925-B-C33, MCI/AEI/FEDER, UE). We would also like to give special thanks to Alicia Medialdea Utande, Head of the Luminescence Research Line of the National Center for Research on Human Evolution-CENIEH, for her help and collaboration in the treatment and interpretation of the data.es_ES
dc.language.isoenges_ES
dc.publisherNaturees_ES
dc.relationinfo:eu-repo/grantAgreement/MICIU/RYC-2017-22558es_ES
dc.relationinfo:eu-repo/grantAgreement/MICIU/PGC2018-093925-B-C33es_ES
dc.relationinfo:eu-repo/grantAgreement/MICINN/PID2019-104625RB-100es_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectLos Huesoses_ES
dc.subjectlast neanderthalses_ES
dc.subjectdental remainses_ES
dc.subjectAcheulean sitees_ES
dc.subjectsimaes_ES
dc.subjectAtapuercaes_ES
dc.subjectluminescencees_ES
dc.subjectSpaines_ES
dc.subjectmorphologyes_ES
dc.subjectevolutiones_ES
dc.titleNew dating of the Matalascañas footprints provides new evidence of the Middle Pleistocene (MIS 9-8) hominin paleoecology in southern Europees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.holder© The Author(s) 2022. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http:// creativecommons. org/ licenses/ by/4. 0/.es_ES
dc.rights.holderAtribución 3.0 España*
dc.relation.publisherversionhttps://www.nature.com/articles/s41598-022-22524-2es_ES
dc.identifier.doi10.1038/s41598-022-22524-2
dc.departamentoesGeologíaes_ES
dc.departamentoeuGeologiaes_ES


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© The Author(s) 2022. This article is licensed under a Creative Commons Attribution 4.0 International
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Except where otherwise noted, this item's license is described as © The Author(s) 2022. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http:// creativecommons. org/ licenses/ by/4. 0/.