Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core

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 tech...

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Published in:Quaternary Research
Main Authors: FOURCADE, Tiffanie, SÁNCHEZ GOÑI, María Fernanda, LAHAYE, Christelle, ROSSIGNOL, Linda, PHILIPPE, Anne
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2022
Subjects:
Online Access:https://doi.org/10.1017/qua.2022.21
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spelling ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/148044 2024-09-09T19:57:33+00:00 Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core FOURCADE, Tiffanie SÁNCHEZ GOÑI, María Fernanda LAHAYE, Christelle ROSSIGNOL, Linda PHILIPPE, Anne 2022-05-30 https://doi.org/10.1017/qua.2022.21 en eng Elsevier 0033-5894 doi:10.1017/qua.2022.21 Sciences de l'environnement/Milieux et Changements globaux Sciences de l'Homme et Société/Archéologie et Préhistoire Article de revue 2022 ftoskarbordeaux https://doi.org/10.1017/qua.2022.21 2024-06-16T23:39:57Z 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. Centre de Mathématiques Henri Lebesgue : fondements, interactions, applications et Formation Article in Journal/Newspaper North Atlantic OSKAR Bordeaux (Open Science Knowledge ARchive) Quaternary Research 110 147 164
institution Open Polar
collection OSKAR Bordeaux (Open Science Knowledge ARchive)
op_collection_id ftoskarbordeaux
language English
topic Sciences de l'environnement/Milieux et Changements globaux
Sciences de l'Homme et Société/Archéologie et Préhistoire
spellingShingle Sciences de l'environnement/Milieux et Changements globaux
Sciences de l'Homme et Société/Archéologie et Préhistoire
FOURCADE, Tiffanie
SÁNCHEZ GOÑI, María Fernanda
LAHAYE, Christelle
ROSSIGNOL, Linda
PHILIPPE, Anne
Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
topic_facet Sciences de l'environnement/Milieux et Changements globaux
Sciences de l'Homme et Société/Archéologie et Préhistoire
description 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. Centre de Mathématiques Henri Lebesgue : fondements, interactions, applications et Formation
format Article in Journal/Newspaper
author FOURCADE, Tiffanie
SÁNCHEZ GOÑI, María Fernanda
LAHAYE, Christelle
ROSSIGNOL, Linda
PHILIPPE, Anne
author_facet FOURCADE, Tiffanie
SÁNCHEZ GOÑI, María Fernanda
LAHAYE, Christelle
ROSSIGNOL, Linda
PHILIPPE, Anne
author_sort FOURCADE, Tiffanie
title Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
title_short Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
title_full Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
title_fullStr Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
title_full_unstemmed Environmental changes in SW France during the Middle to Upper Paleolithic transition from the pollen analysis of an eastern North Atlantic deep-sea core
title_sort environmental changes in sw france during the middle to upper paleolithic transition from the pollen analysis of an eastern north atlantic deep-sea core
publisher Elsevier
publishDate 2022
url https://doi.org/10.1017/qua.2022.21
genre North Atlantic
genre_facet North Atlantic
op_relation 0033-5894
doi:10.1017/qua.2022.21
op_doi https://doi.org/10.1017/qua.2022.21
container_title Quaternary Research
container_volume 110
container_start_page 147
op_container_end_page 164
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