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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Language: | English |
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HAL CCSD
2019
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Online Access: | https://hal.science/hal-02319847 |
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ftunivparis8:oai:HAL:hal-02319847v1 |
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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 |