Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating
International audience The chronology of the late Pleistocene glaciation in the Massif Central, France, is not well documented and there are divergent hypotheses regarding the timing of glacial events in this area. This study aims at reconstructing the chronology of late Pleistocene glacier fluctuat...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2022
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Online Access: | https://hal.science/hal-03667340 https://hal.science/hal-03667340/document https://hal.science/hal-03667340/file/Ancrenaz-etal-2022_JQSR.pdf https://doi.org/10.1016/j.quascirev.2022.107500 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
Late Pleistocene glacial geochronology cosmogenic exposure dating moraine plateau icefield Massif Central Aubrac [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
Late Pleistocene glacial geochronology cosmogenic exposure dating moraine plateau icefield Massif Central Aubrac [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Ancrenaz, Arthur Braucher, Regis Defive, Emmanuelle Poiraud, Alexandre Steiger, Johannes Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
topic_facet |
Late Pleistocene glacial geochronology cosmogenic exposure dating moraine plateau icefield Massif Central Aubrac [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
International audience The chronology of the late Pleistocene glaciation in the Massif Central, France, is not well documented and there are divergent hypotheses regarding the timing of glacial events in this area. This study aims at reconstructing the chronology of late Pleistocene glacier fluctuations in the Aubrac massif. We present a new set of Be-10 and Al-26 exposure ages from twenty erratic boulders embedded in six glacial landforms. Glacial landforms were sampled to determine the timing of three glacial stades and the deglaciation of the Aubrac Mountains. These new data allowed us to constrain the timing of: (i) the Local Last Glacial Maximum, which is coeval to the early part of Marine Isotopic Stage 2 (MIS 2) (28-24 ka), and (ii) the Grandvals and Bouquincan stades, which are both coeval with the later part of MIS 2 (24-16 ka). Deglaciation occurred during Heinrich Stadial 1 (18-15.6 ka). This new direct glacial chronology is supported by regional paleoenvironmental proxies and it updates the chronostratigraphic framework available for the southwestern Massif Central. Western European atmospheric circulation changes (i.e., a southward shift in North Atlantic storm tracks and Mediterranean influences) during MIS 2 were identified as significant factors controlling glacier growth in the Aubrac Mountains as well as other glaciated mountains within the southwestern Massif Central, such as the Cantal, Margeride and Lozère mountains. 2 |
author2 |
Paléoenvironnement et Géoarchéologie (GEOLAB-PG) Laboratoire de Géographie Physique et Environnementale (GEOLAB) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Dynamiques Géoenvironnementales Actuelles (GEOLAB-DGA) |
format |
Article in Journal/Newspaper |
author |
Ancrenaz, Arthur Braucher, Regis Defive, Emmanuelle Poiraud, Alexandre Steiger, Johannes |
author_facet |
Ancrenaz, Arthur Braucher, Regis Defive, Emmanuelle Poiraud, Alexandre Steiger, Johannes |
author_sort |
Ancrenaz, Arthur |
title |
Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
title_short |
Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
title_full |
Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
title_fullStr |
Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
title_full_unstemmed |
Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating |
title_sort |
last glacial fluctuations in the southwestern massif central, aubrac (france): first direct chronology from cosmogenic 10 be and 26 al exposure dating |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-03667340 https://hal.science/hal-03667340/document https://hal.science/hal-03667340/file/Ancrenaz-etal-2022_JQSR.pdf https://doi.org/10.1016/j.quascirev.2022.107500 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 0277-3791 Quaternary Science Reviews https://hal.science/hal-03667340 Quaternary Science Reviews, 2022, 285, pp.107500. ⟨10.1016/j.quascirev.2022.107500⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2022.107500 hal-03667340 https://hal.science/hal-03667340 https://hal.science/hal-03667340/document https://hal.science/hal-03667340/file/Ancrenaz-etal-2022_JQSR.pdf doi:10.1016/j.quascirev.2022.107500 WOS: 000803072100008 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2022.107500 |
container_title |
Quaternary Science Reviews |
container_volume |
285 |
container_start_page |
107500 |
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1785570586995458048 |
spelling |
ftinsu:oai:HAL:hal-03667340v1 2023-12-17T10:46:54+01:00 Last glacial fluctuations in the southwestern Massif Central, Aubrac (France): first direct chronology from cosmogenic 10 Be and 26 Al exposure dating Ancrenaz, Arthur Braucher, Regis Defive, Emmanuelle Poiraud, Alexandre Steiger, Johannes Paléoenvironnement et Géoarchéologie (GEOLAB-PG) Laboratoire de Géographie Physique et Environnementale (GEOLAB) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) Dynamiques Géoenvironnementales Actuelles (GEOLAB-DGA) 2022 https://hal.science/hal-03667340 https://hal.science/hal-03667340/document https://hal.science/hal-03667340/file/Ancrenaz-etal-2022_JQSR.pdf https://doi.org/10.1016/j.quascirev.2022.107500 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2022.107500 hal-03667340 https://hal.science/hal-03667340 https://hal.science/hal-03667340/document https://hal.science/hal-03667340/file/Ancrenaz-etal-2022_JQSR.pdf doi:10.1016/j.quascirev.2022.107500 WOS: 000803072100008 info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 Quaternary Science Reviews https://hal.science/hal-03667340 Quaternary Science Reviews, 2022, 285, pp.107500. ⟨10.1016/j.quascirev.2022.107500⟩ Late Pleistocene glacial geochronology cosmogenic exposure dating moraine plateau icefield Massif Central Aubrac [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2022 ftinsu https://doi.org/10.1016/j.quascirev.2022.107500 2023-11-22T17:31:38Z International audience The chronology of the late Pleistocene glaciation in the Massif Central, France, is not well documented and there are divergent hypotheses regarding the timing of glacial events in this area. This study aims at reconstructing the chronology of late Pleistocene glacier fluctuations in the Aubrac massif. We present a new set of Be-10 and Al-26 exposure ages from twenty erratic boulders embedded in six glacial landforms. Glacial landforms were sampled to determine the timing of three glacial stades and the deglaciation of the Aubrac Mountains. These new data allowed us to constrain the timing of: (i) the Local Last Glacial Maximum, which is coeval to the early part of Marine Isotopic Stage 2 (MIS 2) (28-24 ka), and (ii) the Grandvals and Bouquincan stades, which are both coeval with the later part of MIS 2 (24-16 ka). Deglaciation occurred during Heinrich Stadial 1 (18-15.6 ka). This new direct glacial chronology is supported by regional paleoenvironmental proxies and it updates the chronostratigraphic framework available for the southwestern Massif Central. Western European atmospheric circulation changes (i.e., a southward shift in North Atlantic storm tracks and Mediterranean influences) during MIS 2 were identified as significant factors controlling glacier growth in the Aubrac Mountains as well as other glaciated mountains within the southwestern Massif Central, such as the Cantal, Margeride and Lozère mountains. 2 Article in Journal/Newspaper North Atlantic Institut national des sciences de l'Univers: HAL-INSU Quaternary Science Reviews 285 107500 |