Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3347
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dc.contributor.authorRodríguez-Almagro, Manuel-
dc.contributor.authorArriolabengoa, Martín-
dc.contributor.authorVillalba de Alvarado, Mónica-
dc.contributor.authorArceredillo, Diego-
dc.contributor.authorGalán, Julia-
dc.contributor.authorFernández-Garcí}a, Mónica-
dc.contributor.authorVander Made, J.-
dc.contributor.authorEsteban, José Julián-
dc.contributor.authorArsuaga, Juan Luis-
dc.contributor.authorRios-Garaizar, Joseba-
dc.contributor.authorSala, Nohemi-
dc.contributor.authorGómez-Olivencia, Asier-
dc.date.accessioned2023-12-06-
dc.date.accessioned2024-11-15T11:41:37Z-
dc.date.issued2023-
dc.identifier.citationSSRN, 2023, [Preprint]es_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3347-
dc.description.abstractThe study of cold-adapted faunas in Iberia is of great interest for paleontologists because this peninsula represents the southernmost limit of distribution in western Europe of species such as mammoths, reindeer and woolly rhinoceros. Additionally, the direct dating of paleontological assemblages can provide important information regarding the paleoecology of Paleolithic humans. This study aims to study the fossil assemblage recovered on the surface of the Baio cave (Zestoa, Northern Iberia), which includes cold-adapted species remains.This site has yielded an assemblage that includes herbivores, carnivores and a small number of rodents. The radiocarbon dating of a reindeer and a red deer remains has yielded chronologies consistent with the Châtelperronian and Late Aurignacian occupations in the area, indicating a diachronic accumulation. Taphonomic observations suggest carnivores as the main accumulation agents, with a minimal human contribution, and the probable accumulation of some remains due to natural causes and/or the cave acting as a natural trap.This new evidence contributes to the existing record from other sites, such as Ekain and Mainea, suggesting severe climatic pulses during the transition from the Middle Paleolithic to the Upper Paleolithic, which coincides with a complex pattern of Neanderthal extinction and the replacement by modern humans.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.subjectPleistocenees_ES
dc.subjectRangifer taranduses_ES
dc.subjectIberian Peninsulaes_ES
dc.subjectTaphonomyes_ES
dc.titlePaleobiological and taphonomic analysis of a site with cold-adaptedfauna in Iberia: Baio (zestoa, Gipuzkoa, northern Iberianpeninsula)es_ES
dc.typeArticlees_ES
dc.identifier.doi10.2139/ssrn.4656055-
dc.relation.publisherversionhttps://doi.org/10.2139/ssrn.4656055es_ES
dc.date.available2024-11-15T11:41:37Z-
Appears in Collections:Paleobiología



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