Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/3537
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dc.contributor.authorRodríguez-Almagro, Manuel-
dc.contributor.authorArriolabengoa, Martin-
dc.contributor.authorVillalba de Alvarado, Mónica-
dc.contributor.authorArceredillo, Diego-
dc.contributor.authorGalán, Julia-
dc.contributor.authorMade, Jan van der-
dc.contributor.authorFernández-García, Mónica-
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.accessioned2025-
dc.date.accessioned2025-11-13T11:25:26Z-
dc.date.issued2025-02-
dc.identifier.citationGeobios, 88–89, 205–217es_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/3537-
dc.description.abstractThe study of cold-adapted faunas in Iberia is of great interest to palaeontologists because this peninsula represents the southernmost limit of the distribution in Western Europe of species such as mammoth, reindeer and woolly rhinoceros. Additionally, the direct dating of these palaeontological assemblages can provide important information regarding the palaeoecology of Palaeolithic humans. In this study, we examine the fossil assemblage recovered from the floor of the Baio cave (Zestoa, northern Iberia), which includes the remains of cold-adapted species. This site has yielded an assemblage that includes herbivores, carnivores and a small number of rodents. Our radiocarbon dating of the remains of a reindeer and a red deer yielded chronologies consistent with the Châtelperronian and Late Aurignacian occupations in the area, indicating a diachronic accumulation. Taphonomic observations suggest carnivores as being the main accumulation agents, with a minimal human contribution, along with 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 records from other sites, such as Ekain and Mainea, suggesting severe climatic pulses during the transition from the Middle to the Upper Palaeolithic, which coincides with a complex pattern of Neandertal extinction and their replacement by modern humans.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.subjectRangifer taranduses_ES
dc.subjectTaphonomyes_ES
dc.subjectIberian Peninsulaes_ES
dc.subjectPleistocenees_ES
dc.titlePalaeobiological and taphonomic analysis of a site hosting a cold-adapted fauna in Iberia: The Baio cave (Zestoa, Gipuzkoa, northern Iberian Peninsula)es_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.geobios.2024.05.008-
dc.relation.publisherversionhttps://doi.org/10.1016/j.geobios.2024.05.008es_ES
dc.date.available2025-11-13T11:25:26Z-
Appears in Collections:Paleobiología

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