Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
SÁNCHEZ GOÑI, María Fernanda
École Pratique des Hautes Études [EPHE]
Environnements et Paléoenvironnements OCéaniques [EPOC]
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École Pratique des Hautes Études [EPHE]
Environnements et Paléoenvironnements OCéaniques [EPOC]
SÁNCHEZ GOÑI, María Fernanda
École Pratique des Hautes Études [EPHE]
Environnements et Paléoenvironnements OCéaniques [EPOC]
< Réduire
École Pratique des Hautes Études [EPHE]
Environnements et Paléoenvironnements OCéaniques [EPOC]
Langue
en
Article de revue
Ce document a été publié dans
Quaternary Research. 2022-05-30p. 1-18
Elsevier
Résumé en anglais
Evaluating synchronies between climate and cultural changes is a prerequisite for addressing the possible effect of environmental changes on human populations. Searching for synchronies during the Middle-Upper Paleolithic ...Lire la suite >
Evaluating synchronies between climate and cultural changes is a prerequisite for addressing the possible effect of environmental changes on human populations. Searching for synchronies during the Middle-Upper Paleolithic transition (ca. 48–36 ka) is hampered by the limits of radiocarbon dating techniques and the large chronological uncertainties affecting the archaeological and paleoclimatic records, as well by their low temporal resolution. Here, we present a high-resolution, pollen-based vegetation record from the Bay of Biscay, sea surface temperature changes, additional 14 C ages, and a new IRSL date on the fine-sediment fraction of Heinrich Stadial (HS) 6. The IRSL measurements give an age of ca. 54.0 ± 3.4 ka. The paleoclimatic results reveal a succession of rapid climatic changes during the Middle-Upper Paleolithic transition in SW France (i.e. D-O 12–8 and two distinct climatic phases during HS 4). Comparison of the new paleoclimatic record with chronologically well-constrained regional archaeological changes shows that no synchronies exist between cultural transitions and environmental changes. The disappearance of Neanderthals and the arrival of Homo sapiens in SW France encompassed a long-term forest opening, suggesting that Homo sapiens may have progressively replaced Neanderthals from D-O 10 to HS 4 through competition for the same ecological niches.< Réduire
Project ANR
Centre de Mathématiques Henri Lebesgue : fondements, interactions, applications et Formation - ANR-11-LABX-0020
Origine
Importé de halUnités de recherche