The Quaternary coversands of southwest France

International audience Detailed stratigraphic analysis and numerical dating (OSL, IRSL, ESR, 14C) of Pleistocene coversands in southwest France enable the construction of a renewed chronostratigraphic framework for sand deposition. The chronological data obtained from sandsheet units testify to the...

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Published in:Quaternary Science Reviews
Main Authors: Sitzia, Luca, Bertran, Pascal, Bahain, Jean-Jacques, Bateman, Mark D., Hernandez, Marion, Garon, Henri, Lafontaine, Guillaume, Mercier, Norbert, Leroyer, Chantal, Queffelec, Alain, Voinchet, Pierre
Other Authors: De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie (PACEA), Université de Bordeaux (UB)-Centre National de la Recherche Scientifique (CNRS), Institut national de recherches archéologiques préventives (Inrap), Muséum national d'Histoire naturelle (MNHN), Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Université de Perpignan Via Domitia (UPVD), University of Sheffield Sheffield, Institut de Recherches sur les Archéomatériaux (IRAMAT), Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Université Bordeaux Montaigne-Centre National de la Recherche Scientifique (CNRS), Université Laval Québec (ULaval), Centre de Recherche en Archéologie, Archéosciences, Histoire (CReAAH), Le Mans Université (UM)-Université de Nantes - UFR Histoire, Histoire de l'Art et Archéologie (UFR HHAA), Université de Nantes (UN)-Université de Nantes (UN)-Université de Rennes 2 (UR2), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
ESR
OSL
Online Access:https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/file/Sitzia-etal_2015.pdf
https://doi.org/10.1016/j.quascirev.2015.06.019
id ftccsdartic:oai:HAL:hal-01201992v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic Middle and Late Pleistocene
ESR
Coversand
Palaeosols
OSL
Southwest France
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
spellingShingle Middle and Late Pleistocene
ESR
Coversand
Palaeosols
OSL
Southwest France
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
Sitzia, Luca
Bertran, Pascal
Bahain, Jean-Jacques
Bateman, Mark D.
Hernandez, Marion
Garon, Henri
Lafontaine, Guillaume,
Mercier, Norbert
Leroyer, Chantal
Queffelec, Alain
Voinchet, Pierre
The Quaternary coversands of southwest France
topic_facet Middle and Late Pleistocene
ESR
Coversand
Palaeosols
OSL
Southwest France
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
description International audience Detailed stratigraphic analysis and numerical dating (OSL, IRSL, ESR, 14C) of Pleistocene coversands in southwest France enable the construction of a renewed chronostratigraphic framework for sand deposition. The chronological data obtained from sandsheet units testify to the development of transgressive dunefields since at least the Middle Pleistocene (MIS 10). Three main phases of accumulation occurred during the Last Glacial. The oldest one (64–42 ka) is associated with wet sandsheet facies, histic horizons and zibar-type dune fields, which reflect deposition in a context strongly influenced by the groundwater table. The Late Pleniglacial (24–14 ka) corresponds to the main phase of coversand extension in a drier context. Silty gley horizons suggest, however, local interruptions of sand drifting during GS 2.1. Lateglacial stabilization of the coversands may not have occurred before GI-1c (Allerød), which was typified by the development of cumulic arenosols. These were covered by parabolic dunes during the Younger Dryas. The variations in extent of the emerged continental shelf during the glacial–interglacial cycles may explain the uneven geographical distribution of sand deposition through time. Because of coastline retreat up to 100 km north of 45°N during the LGM lowstand, the coversands were unable to reach the northern part of the basin. Comparison with other European regions highlights stronger affinities of the French record with Portugal than with the Netherlands and Great Britain, probably because of reduced influence of permafrost
author2 De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie (PACEA)
Université de Bordeaux (UB)-Centre National de la Recherche Scientifique (CNRS)
Institut national de recherches archéologiques préventives (Inrap)
Muséum national d'Histoire naturelle (MNHN)
Histoire naturelle de l'Homme préhistorique (HNHP)
Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Université de Perpignan Via Domitia (UPVD)
University of Sheffield Sheffield
Institut de Recherches sur les Archéomatériaux (IRAMAT)
Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Université Bordeaux Montaigne-Centre National de la Recherche Scientifique (CNRS)
Université Laval Québec (ULaval)
Centre de Recherche en Archéologie, Archéosciences, Histoire (CReAAH)
Le Mans Université (UM)-Université de Nantes - UFR Histoire, Histoire de l'Art et Archéologie (UFR HHAA)
Université de Nantes (UN)-Université de Nantes (UN)-Université de Rennes 2 (UR2)
Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Université de Rennes 1 (UR1)
Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC)
format Article in Journal/Newspaper
author Sitzia, Luca
Bertran, Pascal
Bahain, Jean-Jacques
Bateman, Mark D.
Hernandez, Marion
Garon, Henri
Lafontaine, Guillaume,
Mercier, Norbert
Leroyer, Chantal
Queffelec, Alain
Voinchet, Pierre
author_facet Sitzia, Luca
Bertran, Pascal
Bahain, Jean-Jacques
Bateman, Mark D.
Hernandez, Marion
Garon, Henri
Lafontaine, Guillaume,
Mercier, Norbert
Leroyer, Chantal
Queffelec, Alain
Voinchet, Pierre
author_sort Sitzia, Luca
title The Quaternary coversands of southwest France
title_short The Quaternary coversands of southwest France
title_full The Quaternary coversands of southwest France
title_fullStr The Quaternary coversands of southwest France
title_full_unstemmed The Quaternary coversands of southwest France
title_sort quaternary coversands of southwest france
publisher HAL CCSD
publishDate 2015
url https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/file/Sitzia-etal_2015.pdf
https://doi.org/10.1016/j.quascirev.2015.06.019
genre permafrost
genre_facet permafrost
op_source ISSN: 0277-3791
Quaternary Science Reviews
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992
Quaternary Science Reviews, Elsevier, 2015, 124, pp.84-105. ⟨10.1016/j.quascirev.2015.06.019⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2015.06.019
hal-01201992
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/file/Sitzia-etal_2015.pdf
doi:10.1016/j.quascirev.2015.06.019
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.quascirev.2015.06.019
container_title Quaternary Science Reviews
container_volume 124
container_start_page 84
op_container_end_page 105
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spelling ftccsdartic:oai:HAL:hal-01201992v1 2023-05-15T17:58:03+02:00 The Quaternary coversands of southwest France Sitzia, Luca Bertran, Pascal Bahain, Jean-Jacques Bateman, Mark D. Hernandez, Marion Garon, Henri Lafontaine, Guillaume, Mercier, Norbert Leroyer, Chantal Queffelec, Alain Voinchet, Pierre De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie (PACEA) Université de Bordeaux (UB)-Centre National de la Recherche Scientifique (CNRS) Institut national de recherches archéologiques préventives (Inrap) Muséum national d'Histoire naturelle (MNHN) Histoire naturelle de l'Homme préhistorique (HNHP) Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS)-Université de Perpignan Via Domitia (UPVD) University of Sheffield Sheffield Institut de Recherches sur les Archéomatériaux (IRAMAT) Université de Technologie de Belfort-Montbeliard (UTBM)-Université d'Orléans (UO)-Université Bordeaux Montaigne-Centre National de la Recherche Scientifique (CNRS) Université Laval Québec (ULaval) Centre de Recherche en Archéologie, Archéosciences, Histoire (CReAAH) Le Mans Université (UM)-Université de Nantes - UFR Histoire, Histoire de l'Art et Archéologie (UFR HHAA) Université de Nantes (UN)-Université de Nantes (UN)-Université de Rennes 2 (UR2) Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Université de Rennes 1 (UR1) Université de Rennes (UNIV-RENNES)-Centre National de la Recherche Scientifique (CNRS)-Ministère de la Culture (MC) 2015 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/document https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/file/Sitzia-etal_2015.pdf https://doi.org/10.1016/j.quascirev.2015.06.019 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2015.06.019 hal-01201992 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992 https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/document https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992/file/Sitzia-etal_2015.pdf doi:10.1016/j.quascirev.2015.06.019 info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 Quaternary Science Reviews https://hal-univ-rennes1.archives-ouvertes.fr/hal-01201992 Quaternary Science Reviews, Elsevier, 2015, 124, pp.84-105. ⟨10.1016/j.quascirev.2015.06.019⟩ Middle and Late Pleistocene ESR Coversand Palaeosols OSL Southwest France [SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology info:eu-repo/semantics/article Journal articles 2015 ftccsdartic https://doi.org/10.1016/j.quascirev.2015.06.019 2021-12-19T01:05:26Z International audience Detailed stratigraphic analysis and numerical dating (OSL, IRSL, ESR, 14C) of Pleistocene coversands in southwest France enable the construction of a renewed chronostratigraphic framework for sand deposition. The chronological data obtained from sandsheet units testify to the development of transgressive dunefields since at least the Middle Pleistocene (MIS 10). Three main phases of accumulation occurred during the Last Glacial. The oldest one (64–42 ka) is associated with wet sandsheet facies, histic horizons and zibar-type dune fields, which reflect deposition in a context strongly influenced by the groundwater table. The Late Pleniglacial (24–14 ka) corresponds to the main phase of coversand extension in a drier context. Silty gley horizons suggest, however, local interruptions of sand drifting during GS 2.1. Lateglacial stabilization of the coversands may not have occurred before GI-1c (Allerød), which was typified by the development of cumulic arenosols. These were covered by parabolic dunes during the Younger Dryas. The variations in extent of the emerged continental shelf during the glacial–interglacial cycles may explain the uneven geographical distribution of sand deposition through time. Because of coastline retreat up to 100 km north of 45°N during the LGM lowstand, the coversands were unable to reach the northern part of the basin. Comparison with other European regions highlights stronger affinities of the French record with Portugal than with the Netherlands and Great Britain, probably because of reduced influence of permafrost Article in Journal/Newspaper permafrost Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Quaternary Science Reviews 124 84 105