RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY).
International audience Vanations of detailed grain size and magnetic susceptibility records in the Nussloch loess sequence (Rhine Valley), where the sedimentation rate is especially high (1 to 2m per ka on more than 10 m) are presented. This study leads to evidence more or less cyclic vanations of t...
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Main Authors: | , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | French |
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HAL CCSD
2002
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Online Access: | https://hal.science/hal-02497460 https://hal.science/hal-02497460/document https://hal.science/hal-02497460/file/quate_1142-2904_2002_num_13_3_1712.pdf https://doi.org/10.3406/quate.2002.1712 |
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ftunimontpellier:oai:HAL:hal-02497460v1 |
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openpolar |
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Open Polar |
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Université de Montpellier: HAL |
op_collection_id |
ftunimontpellier |
language |
French |
topic |
Loess grain-size rapid events Weichsehan Germany Nussloch événements rapides Weichselien Allemagne granulométne [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy |
spellingShingle |
Loess grain-size rapid events Weichsehan Germany Nussloch événements rapides Weichselien Allemagne granulométne [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy Antoine, Pierre Rousseau, Denis Didier Hatté, Christine Zöller, Ludwig Lang, Andréas Fontugne, Michel Moine, Olivier RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
topic_facet |
Loess grain-size rapid events Weichsehan Germany Nussloch événements rapides Weichselien Allemagne granulométne [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy |
description |
International audience Vanations of detailed grain size and magnetic susceptibility records in the Nussloch loess sequence (Rhine Valley), where the sedimentation rate is especially high (1 to 2m per ka on more than 10 m) are presented. This study leads to evidence more or less cyclic vanations of these indices between about 30 and 17 ka. These vanations, especially well expressed by the evolution of the IGR (% 20-50um / % <20um), are considered to be an indirect measurement of the aeohan dynamic intensity and of the sedimentation rate dunng loess deposition (high ratio in typical unweathered loess (Loess events LI to L8) / low ratio in tundra gleys horizons Gl to G8 (reduction or stop of the sedimentation, permafrost development.). On the basis of OSL, and of I4C dates on loess organic matter, we show that dunng the Upper Pleniglacial the loess deposition was especially fast and discontinuous, and resulted from a succession of rapid deposition phases, separated by stops or strong reduction of the aeohan flux sedimentation dunng some centunes. A temptative correlation with the Greenland dust record (GRIP) is proposed. In addition we can observe a parallel between Henrich 2 event and one of the main penod of loess deposition around 22-23 ka. Finally, the companson with the magnetic susceptibility record andthe grain-size data show that the period charactenzed by a high grain-size index, are also underlined by an increase in the amount of ferromagnetic minerals reworked from the Rhine alluvial plain located at the foot of the site (enhancement in the frequency of the storms from N-NW). L'étude des variations de la granulométrie et de la susceptibilité magnétique dans la séquence de Nussloch (Vallée du Rhin), où le taux de sédimentation est particulièrement élevé (1 à 2 m/ka sur plus de 10m), débouche sur la mise en évidence de variations plus ou moins cycliques entre 30 et 17 ka environ. Ces vanations, particulièrement bien soulignées par l'évolution du rapport % 20- 50um / % <20 um (indice IGR), sont ... |
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 des Sciences de l'Evolution de Montpellier (UMR ISEM) Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Géochrononologie Traceurs Archéométrie (GEOTRAC) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Universität Bayreuth Catholic University of Leuven = Katholieke Universiteit Leuven (KU Leuven) |
format |
Article in Journal/Newspaper |
author |
Antoine, Pierre Rousseau, Denis Didier Hatté, Christine Zöller, Ludwig Lang, Andréas Fontugne, Michel Moine, Olivier |
author_facet |
Antoine, Pierre Rousseau, Denis Didier Hatté, Christine Zöller, Ludwig Lang, Andréas Fontugne, Michel Moine, Olivier |
author_sort |
Antoine, Pierre |
title |
RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
title_short |
RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
title_full |
RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
title_fullStr |
RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
title_full_unstemmed |
RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). |
title_sort |
rapid aeolian events within the weichselian upper pleniglacial loess : the example of the nussloch sequence (rhine valley, germany). |
publisher |
HAL CCSD |
publishDate |
2002 |
url |
https://hal.science/hal-02497460 https://hal.science/hal-02497460/document https://hal.science/hal-02497460/file/quate_1142-2904_2002_num_13_3_1712.pdf https://doi.org/10.3406/quate.2002.1712 |
genre |
Greenland GRIP permafrost Tundra |
genre_facet |
Greenland GRIP permafrost Tundra |
op_source |
ISSN: 1142-2904 EISSN: 1965-0795 Quaternaire https://hal.science/hal-02497460 Quaternaire, 2002, 13 (3), pp.199-208. ⟨10.3406/quate.2002.1712⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.3406/quate.2002.1712 hal-02497460 https://hal.science/hal-02497460 https://hal.science/hal-02497460/document https://hal.science/hal-02497460/file/quate_1142-2904_2002_num_13_3_1712.pdf doi:10.3406/quate.2002.1712 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.3406/quate.2002.1712 |
container_title |
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13 |
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container_start_page |
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op_container_end_page |
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1799481094696861696 |
spelling |
ftunimontpellier:oai:HAL:hal-02497460v1 2024-05-19T07:41:29+00:00 RAPID AEOLIAN EVENTS WITHIN THE WEICHSELIAN UPPER PLENIGLACIAL LOESS : THE EXAMPLE OF THE NUSSLOCH SEQUENCE (RHINE VALLEY, GERMANY). Evènements éoliens rapides dans les Loess du Pléniglaciaire supérieur Weichselien : l'exemple de la séquence de Nussloch (vallée du Rhin-Allemagne) Antoine, Pierre Rousseau, Denis Didier Hatté, Christine Zöller, Ludwig Lang, Andréas Fontugne, Michel Moine, Olivier 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 des Sciences de l'Evolution de Montpellier (UMR ISEM) Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Géochrononologie Traceurs Archéométrie (GEOTRAC) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Universität Bayreuth Catholic University of Leuven = Katholieke Universiteit Leuven (KU Leuven) 2002 https://hal.science/hal-02497460 https://hal.science/hal-02497460/document https://hal.science/hal-02497460/file/quate_1142-2904_2002_num_13_3_1712.pdf https://doi.org/10.3406/quate.2002.1712 fr fre HAL CCSD AFEQ-CNF INQUA info:eu-repo/semantics/altIdentifier/doi/10.3406/quate.2002.1712 hal-02497460 https://hal.science/hal-02497460 https://hal.science/hal-02497460/document https://hal.science/hal-02497460/file/quate_1142-2904_2002_num_13_3_1712.pdf doi:10.3406/quate.2002.1712 info:eu-repo/semantics/OpenAccess ISSN: 1142-2904 EISSN: 1965-0795 Quaternaire https://hal.science/hal-02497460 Quaternaire, 2002, 13 (3), pp.199-208. ⟨10.3406/quate.2002.1712⟩ Loess grain-size rapid events Weichsehan Germany Nussloch événements rapides Weichselien Allemagne granulométne [SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy info:eu-repo/semantics/article Journal articles 2002 ftunimontpellier https://doi.org/10.3406/quate.2002.1712 2024-04-24T01:07:41Z International audience Vanations of detailed grain size and magnetic susceptibility records in the Nussloch loess sequence (Rhine Valley), where the sedimentation rate is especially high (1 to 2m per ka on more than 10 m) are presented. This study leads to evidence more or less cyclic vanations of these indices between about 30 and 17 ka. These vanations, especially well expressed by the evolution of the IGR (% 20-50um / % <20um), are considered to be an indirect measurement of the aeohan dynamic intensity and of the sedimentation rate dunng loess deposition (high ratio in typical unweathered loess (Loess events LI to L8) / low ratio in tundra gleys horizons Gl to G8 (reduction or stop of the sedimentation, permafrost development.). On the basis of OSL, and of I4C dates on loess organic matter, we show that dunng the Upper Pleniglacial the loess deposition was especially fast and discontinuous, and resulted from a succession of rapid deposition phases, separated by stops or strong reduction of the aeohan flux sedimentation dunng some centunes. A temptative correlation with the Greenland dust record (GRIP) is proposed. In addition we can observe a parallel between Henrich 2 event and one of the main penod of loess deposition around 22-23 ka. Finally, the companson with the magnetic susceptibility record andthe grain-size data show that the period charactenzed by a high grain-size index, are also underlined by an increase in the amount of ferromagnetic minerals reworked from the Rhine alluvial plain located at the foot of the site (enhancement in the frequency of the storms from N-NW). L'étude des variations de la granulométrie et de la susceptibilité magnétique dans la séquence de Nussloch (Vallée du Rhin), où le taux de sédimentation est particulièrement élevé (1 à 2 m/ka sur plus de 10m), débouche sur la mise en évidence de variations plus ou moins cycliques entre 30 et 17 ka environ. Ces vanations, particulièrement bien soulignées par l'évolution du rapport % 20- 50um / % <20 um (indice IGR), sont ... Article in Journal/Newspaper Greenland GRIP permafrost Tundra Université de Montpellier: HAL Quaternaire 13 3 199 208 |