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| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.contributor.author | Richard, Maïlys | - |
| dc.contributor.author | Val Blanco, Miren del | - |
| dc.contributor.author | Fewlass, Helen | - |
| dc.contributor.author | Sinet-Mathiot, Virginie | - |
| dc.contributor.author | Lanos, Philippe | - |
| dc.contributor.author | Pons-Branchu, Edwige | - |
| dc.contributor.author | Puaud, Simon | - |
| dc.contributor.author | Hublin, Jean-Jacques | - |
| dc.contributor.author | Moncel, Marie-Hélène | - |
| dc.date.accessioned | 2024-08-05 | - |
| dc.date.accessioned | 2024-09-03T13:01:53Z | - |
| dc.date.issued | 2024-09 | - |
| dc.identifier.citation | Scientific Reports, 2024, 14, 20474 | es_ES |
| dc.identifier.issn | 2045-2322 | - |
| dc.identifier.uri | https://cir.cenieh.es/handle/20.500.12136/3319 | - |
| dc.description.abstract | The emergence of the Middle Palaeolithic, and its variability over time and space are key questions in the field of prehistoric archaeology. Many sites have been documented in the south-eastern margins of the Massif central and the middle Rhône valley, a migration path that connects Northern Europe with the Mediterranean. Well-dated, long stratigraphic sequences are essential to understand Neanderthals dynamics and demise, and potential interactions with Homo sapiens in the area, such as the one displayed at the Maras rock shelter (“Abri du Maras”). The site is characterised by exceptional preservation of archaeological remains, including bones dated using radiocarbon (14C) and teeth using electron spin resonance combined with uranium series (ESR/U-series). Optically stimulated luminescence was used to date the sedimentary deposits. By combining the new ages with previous ones using Bayesian modelling, we are able to clarify the occupation time over a period spanning 200,000 years. Between ca. 250 and 40 ka, the site has been used as a long-term residence by Neanderthals, specifically during three interglacial periods: first during marine isotopic stage (MIS) 7, between 247 ± 34 and 223 ± 33 ka, and then recurrently during MIS 5 (between 127 ± 17 and 90 ± 9 ka) and MIS 3 (up to 39,280 cal BP). | es_ES |
| dc.description.sponsorship | The Service Régional de l’Archéologie, Auvergne-Rhône-Alpes, Ministère de la Culture for supporting fieldwork and analyses, PANOPLY (Plateforme Analytique Géosciences Paris Saclay) for the use of the MC-ICPMS at the LSCE. We thank A. Dapoigny for support with U-Th measurements (LSCE). ZooMS analyses performed in Leipzig (MPI-EVA) were financially supported by the Max Planck Society, and we thank M. Munoz-Alegre for assistance with the MALDI-TOF MS instrument (Univ. of Cambridge). Many thanks to M.J. Alonso, M. Duval, A. Medialdea and D. Moreno (CENIEH) for access to the ESR and OSL facilities at the CENIEH. V.S.-M. is supported by a Fyssen Foundation postdoctoral fellowship (2023-2025). | es_ES |
| dc.language.iso | en | es_ES |
| dc.publisher | Nature Portfolio | es_ES |
| dc.rights | info:eu-repo/semantics/openAccess | es_ES |
| dc.rights | Atribución 3.0 Estados Unidos de América | * |
| dc.rights.uri | http://creativecommons.org/licenses/by/3.0/us/ | * |
| dc.subject | Chronology | es_ES |
| dc.subject | Neanderthal | es_ES |
| dc.subject | Luminescence | es_ES |
| dc.subject | Radiocarbon | es_ES |
| dc.subject | Electron spin resonance | es_ES |
| dc.subject | Uranium-series | es_ES |
| dc.title | Multi-method dating reveals 200 ka of Middle Palaeolithic occupation at Maras rock shelter, Rhône Valley, France | es_ES |
| dc.type | Article | es_ES |
| dc.identifier.doi | 10.1038/s41598-024-69380-w | - |
| dc.relation.publisherversion | https://doi.org/10.1038/s41598-024-69380-w | es_ES |
| dc.date.available | 2024-09-03T13:01:53Z | - |
| Aparece en las colecciones: | Datación por Luminiscencia Geocronología y Geología Series de Uranio | |
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| Fichero | Descripción | Tamaño | Formato | |
|---|---|---|---|---|
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