The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic

International audience In Northern France Quaternary loess-palaeosol sequences represent the main deposits in which Palaeolithic sites are generally recovered. The oldest loess, dating from the Middle Pleistocene, are generally preserved in sedimentary traps formed by the junction between the chalky...

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Main Authors: Antoine, Pierre, Coutard, Sylvie, Locht, Jean‑luc, Goval, Emilie, Hérisson, David, Moine, Olivier, Bahain, Jean-Jacques
Other Authors: Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Institut national de recherches archéologiques préventives (Inrap), Ministère de la Culture et de la Communication, Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS), Anthropologie des techniques, des espaces et des territoires au Pliocène et au Pléistocène (AnTET), Archéologies et Sciences de l'Antiquité (ArScAn), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)-Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS), Muséum national d'Histoire naturelle (MNHN)
Format: Conference Object
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.science/hal-02319847
id ftunivparis8:oai:HAL:hal-02319847v1
record_format openpolar
institution Open Polar
collection Université Paris 8 Vincennes-Saint-Denis: HAL
op_collection_id ftunivparis8
language English
topic Loess
Archaeology
Prehistory
Palaeolithic
Archéologie
Paléolithique
Préhistoire
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
spellingShingle Loess
Archaeology
Prehistory
Palaeolithic
Archéologie
Paléolithique
Préhistoire
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
Antoine, Pierre
Coutard, Sylvie
Locht, Jean‑luc
Goval, Emilie
Hérisson, David
Moine, Olivier
Bahain, Jean-Jacques
The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
topic_facet Loess
Archaeology
Prehistory
Palaeolithic
Archéologie
Paléolithique
Préhistoire
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory
description International audience In Northern France Quaternary loess-palaeosol sequences represent the main deposits in which Palaeolithic sites are generally recovered. The oldest loess, dating from the Middle Pleistocene, are generally preserved in sedimentary traps formed by the junction between the chalky slopes and the alluvial formations of the Somme River fluvial terrace system or by deep sinkholes (3-5 m) resulting from the dissolution of the chalky substratum on the plateaus. They are mainly resulting from local deflation processes reworking the top of sandy fluvial deposits. A large extension of typical calcareous loess over the whole landscape is only observed from the end of the Saalian (ca. 150-135 ka). The heavy mineral content of these aeolian deposits testifies to a distant transport from the polar desert areas of the dried Eastern Channel (≥ 100 km). Following the last Interglacial (Eemian), the Last glacial (Weichselian) is represented by a sub-continuous loess cover rising up to 7-8 m in thickness in the best locations as leeward slopes. In this large area, pedostratigraphic sequences from the last Interglacial-glacial cycle have been intensely studied, especially in the frame of rescue archaeological programs that have provided hundreds of individual sequences from test-pits or excavations and numerous archaeological layers. The pedostratigraphic sequences from the last Interglacial-glacial cycle exhibit a regular pedosedimentary pattern including well identified pedological and periglacial marker horizons that can be followed towards the East at least in Belgium and Germany. This approach leads to a detailed pedostratigraphic and chronostratigraphic scheme that represents a unique database to discuss the relations between Palaeolithic occupations and environment in Europe. It can be summarised by the succession of four main chrono-climatic phases following the erosion of the eemian brown leached soil during MIS 5d: (1) Early-glacial (112-72 ka) including a phase with grey forest soils (Early-glacial ...
author2 Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP)
Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)
Institut national de recherches archéologiques préventives (Inrap)
Ministère de la Culture et de la Communication
Histoire naturelle de l'Homme préhistorique (HNHP)
Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS)
Anthropologie des techniques, des espaces et des territoires au Pliocène et au Pléistocène (AnTET)
Archéologies et Sciences de l'Antiquité (ArScAn)
Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)-Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)
Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)
Centre National de la Recherche Scientifique (CNRS)
Muséum national d'Histoire naturelle (MNHN)
format Conference Object
author Antoine, Pierre
Coutard, Sylvie
Locht, Jean‑luc
Goval, Emilie
Hérisson, David
Moine, Olivier
Bahain, Jean-Jacques
author_facet Antoine, Pierre
Coutard, Sylvie
Locht, Jean‑luc
Goval, Emilie
Hérisson, David
Moine, Olivier
Bahain, Jean-Jacques
author_sort Antoine, Pierre
title The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
title_short The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
title_full The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
title_fullStr The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
title_full_unstemmed The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic
title_sort last 400 ka in loess-palaeosols records from northern france: environmental background and dating of the palaeolithic
publisher HAL CCSD
publishDate 2019
url https://hal.science/hal-02319847
op_coverage Aachen, Germany
genre polar desert
genre_facet polar desert
op_source Loess and Archeology
https://hal.science/hal-02319847
Loess and Archeology, Nov 2019, Aachen, Germany
op_relation hal-02319847
https://hal.science/hal-02319847
_version_ 1802649320861728768
spelling ftunivparis8:oai:HAL:hal-02319847v1 2024-06-23T07:56:19+00:00 The last 400 ka in loess-palaeosols records from Northern France: environmental background and dating of the Palaeolithic Antoine, Pierre Coutard, Sylvie Locht, Jean‑luc Goval, Emilie Hérisson, David Moine, Olivier Bahain, Jean-Jacques Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Institut national de recherches archéologiques préventives (Inrap) Ministère de la Culture et de la Communication Histoire naturelle de l'Homme préhistorique (HNHP) Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS) Anthropologie des techniques, des espaces et des territoires au Pliocène et au Pléistocène (AnTET) Archéologies et Sciences de l'Antiquité (ArScAn) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS)-Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris 8 Vincennes-Saint-Denis (UP8)-Université Paris Nanterre (UPN)-Ministère de la Culture et de la Communication (MCC)-Centre National de la Recherche Scientifique (CNRS) Centre National de la Recherche Scientifique (CNRS) Muséum national d'Histoire naturelle (MNHN) Aachen, Germany 2019-11-28 https://hal.science/hal-02319847 en eng HAL CCSD hal-02319847 https://hal.science/hal-02319847 Loess and Archeology https://hal.science/hal-02319847 Loess and Archeology, Nov 2019, Aachen, Germany Loess Archaeology Prehistory Palaeolithic Archéologie Paléolithique Préhistoire [SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory info:eu-repo/semantics/conferenceObject Conference papers 2019 ftunivparis8 2024-06-10T23:54:11Z International audience In Northern France Quaternary loess-palaeosol sequences represent the main deposits in which Palaeolithic sites are generally recovered. The oldest loess, dating from the Middle Pleistocene, are generally preserved in sedimentary traps formed by the junction between the chalky slopes and the alluvial formations of the Somme River fluvial terrace system or by deep sinkholes (3-5 m) resulting from the dissolution of the chalky substratum on the plateaus. They are mainly resulting from local deflation processes reworking the top of sandy fluvial deposits. A large extension of typical calcareous loess over the whole landscape is only observed from the end of the Saalian (ca. 150-135 ka). The heavy mineral content of these aeolian deposits testifies to a distant transport from the polar desert areas of the dried Eastern Channel (≥ 100 km). Following the last Interglacial (Eemian), the Last glacial (Weichselian) is represented by a sub-continuous loess cover rising up to 7-8 m in thickness in the best locations as leeward slopes. In this large area, pedostratigraphic sequences from the last Interglacial-glacial cycle have been intensely studied, especially in the frame of rescue archaeological programs that have provided hundreds of individual sequences from test-pits or excavations and numerous archaeological layers. The pedostratigraphic sequences from the last Interglacial-glacial cycle exhibit a regular pedosedimentary pattern including well identified pedological and periglacial marker horizons that can be followed towards the East at least in Belgium and Germany. This approach leads to a detailed pedostratigraphic and chronostratigraphic scheme that represents a unique database to discuss the relations between Palaeolithic occupations and environment in Europe. It can be summarised by the succession of four main chrono-climatic phases following the erosion of the eemian brown leached soil during MIS 5d: (1) Early-glacial (112-72 ka) including a phase with grey forest soils (Early-glacial ... Conference Object polar desert Université Paris 8 Vincennes-Saint-Denis: HAL