Antarctic erosion history reconstructed by Terre Adélie moraine geochronology
International audience We report apatitefission-track and10Be terrestrial cosmogenic nuclide (TCN) dating of14 moraine boulders originating from inland Terre Adélie, East Antarctica. These data show coolingof the Proterozoic Terre Adélie craton at <∼120°C between 350 and 300 Ma, suggesting > 4...
Published in: | Antarctic Science |
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Main Authors: | , , , , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2020
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Online Access: | https://hal.science/hal-02894535 https://doi.org/10.1017/S095410202000036X |
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ftunivnantes:oai:HAL:hal-02894535v1 |
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institution |
Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDU]Sciences of the Universe [physics] [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
[SDU]Sciences of the Universe [physics] [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Voisine, Encelyn Rolland, Yann Bernet, Matthias Carcaillet, Julien Duclaux, Guillaume Bascou, Jerôme Sue, Christian Balvay, Mélanie Ménot, René-Pierre Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
topic_facet |
[SDU]Sciences of the Universe [physics] [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience We report apatitefission-track and10Be terrestrial cosmogenic nuclide (TCN) dating of14 moraine boulders originating from inland Terre Adélie, East Antarctica. These data show coolingof the Proterozoic Terre Adélie craton at <∼120°C between 350 and 300 Ma, suggesting > 4 kmtemperate glacial erosion during the Late Palaeozoic Ice Age, followed by nearly null Mesozoicerosion and low glacial erosion (< 2 km) in the Cenozoic. Based on glacialflux maps, the origin of theboulders may be located∼400 km upstream. Preliminary TCN (10Be) datings of moraine boulderscluster within the last 30 ka. Cosmogenic ages from the Lacroix Nunatak suggest a main deglaciationafter the Younger Dryas atc.10 ka, while those of Cap Prud'homme mostly cluster at 0.6 ka, inagreement with an exhumation of boulders during the Little Ice Age. |
author2 |
Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA) Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) Laboratoire Magmas et Volcans (LMV) Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS) Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) |
format |
Article in Journal/Newspaper |
author |
Voisine, Encelyn Rolland, Yann Bernet, Matthias Carcaillet, Julien Duclaux, Guillaume Bascou, Jerôme Sue, Christian Balvay, Mélanie Ménot, René-Pierre |
author_facet |
Voisine, Encelyn Rolland, Yann Bernet, Matthias Carcaillet, Julien Duclaux, Guillaume Bascou, Jerôme Sue, Christian Balvay, Mélanie Ménot, René-Pierre |
author_sort |
Voisine, Encelyn |
title |
Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
title_short |
Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
title_full |
Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
title_fullStr |
Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
title_full_unstemmed |
Antarctic erosion history reconstructed by Terre Adélie moraine geochronology |
title_sort |
antarctic erosion history reconstructed by terre adélie moraine geochronology |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.science/hal-02894535 https://doi.org/10.1017/S095410202000036X |
long_lat |
ENVELOPE(-63.983,-63.983,-65.050,-65.050) ENVELOPE(141.317,141.317,-66.844,-66.844) ENVELOPE(139.000,139.000,-67.000,-67.000) ENVELOPE(138.991,138.991,-59.999,-59.999) |
geographic |
Antarctic East Antarctica Lacroix Lacroix Nunatak Terre Adélie Terre-Adélie |
geographic_facet |
Antarctic East Antarctica Lacroix Lacroix Nunatak Terre Adélie Terre-Adélie |
genre |
Antarc* Antarctic Antarctic Science Antarctica East Antarctica |
genre_facet |
Antarc* Antarctic Antarctic Science Antarctica East Antarctica |
op_source |
ISSN: 0954-1020 EISSN: 1365-2079 Antarctic Science https://hal.science/hal-02894535 Antarctic Science, 2020, 32 (5), pp.382-395. ⟨10.1017/S095410202000036X⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1017/S095410202000036X hal-02894535 https://hal.science/hal-02894535 doi:10.1017/S095410202000036X |
op_doi |
https://doi.org/10.1017/S095410202000036X |
container_title |
Antarctic Science |
container_volume |
32 |
container_issue |
5 |
container_start_page |
382 |
op_container_end_page |
395 |
_version_ |
1766086342279692288 |
spelling |
ftunivnantes:oai:HAL:hal-02894535v1 2023-05-15T13:36:58+02:00 Antarctic erosion history reconstructed by Terre Adélie moraine geochronology Voisine, Encelyn Rolland, Yann Bernet, Matthias Carcaillet, Julien Duclaux, Guillaume Bascou, Jerôme Sue, Christian Balvay, Mélanie Ménot, René-Pierre Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre (ISTerre) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA) Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) Laboratoire Magmas et Volcans (LMV) Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS) Laboratoire Chrono-environnement (UMR 6249) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) 2020 https://hal.science/hal-02894535 https://doi.org/10.1017/S095410202000036X en eng HAL CCSD Cambridge University Press (CUP) info:eu-repo/semantics/altIdentifier/doi/10.1017/S095410202000036X hal-02894535 https://hal.science/hal-02894535 doi:10.1017/S095410202000036X ISSN: 0954-1020 EISSN: 1365-2079 Antarctic Science https://hal.science/hal-02894535 Antarctic Science, 2020, 32 (5), pp.382-395. ⟨10.1017/S095410202000036X⟩ [SDU]Sciences of the Universe [physics] [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2020 ftunivnantes https://doi.org/10.1017/S095410202000036X 2023-01-25T00:26:45Z International audience We report apatitefission-track and10Be terrestrial cosmogenic nuclide (TCN) dating of14 moraine boulders originating from inland Terre Adélie, East Antarctica. These data show coolingof the Proterozoic Terre Adélie craton at <∼120°C between 350 and 300 Ma, suggesting > 4 kmtemperate glacial erosion during the Late Palaeozoic Ice Age, followed by nearly null Mesozoicerosion and low glacial erosion (< 2 km) in the Cenozoic. Based on glacialflux maps, the origin of theboulders may be located∼400 km upstream. Preliminary TCN (10Be) datings of moraine boulderscluster within the last 30 ka. Cosmogenic ages from the Lacroix Nunatak suggest a main deglaciationafter the Younger Dryas atc.10 ka, while those of Cap Prud'homme mostly cluster at 0.6 ka, inagreement with an exhumation of boulders during the Little Ice Age. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica East Antarctica Université de Nantes: HAL-UNIV-NANTES Antarctic East Antarctica Lacroix ENVELOPE(-63.983,-63.983,-65.050,-65.050) Lacroix Nunatak ENVELOPE(141.317,141.317,-66.844,-66.844) Terre Adélie ENVELOPE(139.000,139.000,-67.000,-67.000) Terre-Adélie ENVELOPE(138.991,138.991,-59.999,-59.999) Antarctic Science 32 5 382 395 |