Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica

International audience This study presents a high-resolution multi-proxy investigation of sediment core MD03-2601 and documents major glacier oscillations and deep water activity during the Holocene in the Adé lie Land region, East Antarctica. A comparison with surface ocean conditions reveals synch...

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Published in:Quaternary Science Reviews
Main Authors: Denis, Delphine, Crosta, Xavier, Schmidt, Sabine, Carson, Damien, S, Ganeshram, Raja, S, Renssen, Hans, Bout-Roumazeilles, Viviane, Zaragosi, Sébastien, Martin, Bernard, Cremer, Michel, Giraudeau, Jacques
Other Authors: Université Paris 1 Panthéon-Sorbonne (UP1), Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), University of Edinburgh (Edin.), Vrije Universiteit Amsterdam Amsterdam (VU), Processus et bilan des domaines sédimentaires (PBDS), Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de microbiologie et génétique moléculaires - UMR5100 (LMGM), Centre de Biologie Intégrative (CBI), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2009
Subjects:
Online Access:https://hal.science/hal-02105668
https://doi.org/10.1016/j.quascirev.2008.12.024
id ftutoulouse3hal:oai:HAL:hal-02105668v1
record_format openpolar
institution Open Polar
collection Université Toulouse III - Paul Sabatier: HAL-UPS
op_collection_id ftutoulouse3hal
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Denis, Delphine
Crosta, Xavier
Schmidt, Sabine
Carson, Damien, S
Ganeshram, Raja, S
Renssen, Hans
Bout-Roumazeilles, Viviane
Zaragosi, Sébastien
Martin, Bernard
Cremer, Michel
Giraudeau, Jacques
Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience This study presents a high-resolution multi-proxy investigation of sediment core MD03-2601 and documents major glacier oscillations and deep water activity during the Holocene in the Adé lie Land region, East Antarctica. A comparison with surface ocean conditions reveals synchronous changes of glaciers, sea ice and deep water formation at Milankovitch and sub-Milankovitch time scales. We report (1) a deglaciation of the Adé lie Land continental shelf from 11 to 8.5 cal ka BP, which occurred in two phases of effective glacier grounding-line retreat at 10.6 and 9 cal ka BP, associated with active deep water formation; (2) a rapid glacier and sea ice readvance centred around 7.7 cal ka BP; and (3) five rapid expansions of the glacier-sea ice systems, during the Mid to Late Holocene, associated to a long-term increase of deep water formation. At Milankovich time scales, we show that the precessionnal component of insolation at high and low latitudes explains the major trend of the glacier-sea ice-ocean system throughout the Holocene, in the Adé lie Land region. In addition, the orbitally-forced seasonality seems to control the coastal deep water formation via the sea ice-ocean coupling, which could lead to opposite patterns between north and south high latitudes during the Mid to Late Holocene. At sub-Milankovitch time scales, there are eight events of glacier-sea ice retreat and expansion that occurred during atmospheric cooling events over East Antarctica. Comparisons of our results with other peri-Antarctic records and model simulations from high southern latitudes may suggest that our interpretation on glacier-sea ice-ocean interactions and their Holocene evolutions reflect a more global Antarctic Holocene pattern.
author2 Université Paris 1 Panthéon-Sorbonne (UP1)
Environnements et Paléoenvironnements OCéaniques (EPOC)
Observatoire aquitain des sciences de l'univers (OASU)
Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)
University of Edinburgh (Edin.)
Vrije Universiteit Amsterdam Amsterdam (VU)
Processus et bilan des domaines sédimentaires (PBDS)
Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de microbiologie et génétique moléculaires - UMR5100 (LMGM)
Centre de Biologie Intégrative (CBI)
Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Denis, Delphine
Crosta, Xavier
Schmidt, Sabine
Carson, Damien, S
Ganeshram, Raja, S
Renssen, Hans
Bout-Roumazeilles, Viviane
Zaragosi, Sébastien
Martin, Bernard
Cremer, Michel
Giraudeau, Jacques
author_facet Denis, Delphine
Crosta, Xavier
Schmidt, Sabine
Carson, Damien, S
Ganeshram, Raja, S
Renssen, Hans
Bout-Roumazeilles, Viviane
Zaragosi, Sébastien
Martin, Bernard
Cremer, Michel
Giraudeau, Jacques
author_sort Denis, Delphine
title Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
title_short Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
title_full Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
title_fullStr Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
title_full_unstemmed Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica
title_sort holocene glacier and deep water dynamics, adélie land region, east antarctica
publisher HAL CCSD
publishDate 2009
url https://hal.science/hal-02105668
https://doi.org/10.1016/j.quascirev.2008.12.024
genre Antarc*
Antarctic
Antarctica
East Antarctica
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Sea ice
op_source ISSN: 0277-3791
EISSN: 1873-457X
Quaternary Science Reviews
https://hal.science/hal-02105668
Quaternary Science Reviews, 2009, 28 (13-14), pp.1291-1303. ⟨10.1016/j.quascirev.2008.12.024⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2008.12.024
hal-02105668
https://hal.science/hal-02105668
doi:10.1016/j.quascirev.2008.12.024
op_doi https://doi.org/10.1016/j.quascirev.2008.12.024
container_title Quaternary Science Reviews
container_volume 28
container_issue 13-14
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op_container_end_page 1303
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spelling ftutoulouse3hal:oai:HAL:hal-02105668v1 2024-05-19T07:31:42+00:00 Holocene glacier and deep water dynamics, Adélie Land region, East Antarctica Denis, Delphine Crosta, Xavier Schmidt, Sabine Carson, Damien, S Ganeshram, Raja, S Renssen, Hans Bout-Roumazeilles, Viviane Zaragosi, Sébastien Martin, Bernard Cremer, Michel Giraudeau, Jacques Université Paris 1 Panthéon-Sorbonne (UP1) Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) University of Edinburgh (Edin.) Vrije Universiteit Amsterdam Amsterdam (VU) Processus et bilan des domaines sédimentaires (PBDS) Université de Lille, Sciences et Technologies-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de microbiologie et génétique moléculaires - UMR5100 (LMGM) Centre de Biologie Intégrative (CBI) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS) 2009 https://hal.science/hal-02105668 https://doi.org/10.1016/j.quascirev.2008.12.024 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2008.12.024 hal-02105668 https://hal.science/hal-02105668 doi:10.1016/j.quascirev.2008.12.024 ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-02105668 Quaternary Science Reviews, 2009, 28 (13-14), pp.1291-1303. ⟨10.1016/j.quascirev.2008.12.024⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2009 ftutoulouse3hal https://doi.org/10.1016/j.quascirev.2008.12.024 2024-04-25T01:16:18Z International audience This study presents a high-resolution multi-proxy investigation of sediment core MD03-2601 and documents major glacier oscillations and deep water activity during the Holocene in the Adé lie Land region, East Antarctica. A comparison with surface ocean conditions reveals synchronous changes of glaciers, sea ice and deep water formation at Milankovitch and sub-Milankovitch time scales. We report (1) a deglaciation of the Adé lie Land continental shelf from 11 to 8.5 cal ka BP, which occurred in two phases of effective glacier grounding-line retreat at 10.6 and 9 cal ka BP, associated with active deep water formation; (2) a rapid glacier and sea ice readvance centred around 7.7 cal ka BP; and (3) five rapid expansions of the glacier-sea ice systems, during the Mid to Late Holocene, associated to a long-term increase of deep water formation. At Milankovich time scales, we show that the precessionnal component of insolation at high and low latitudes explains the major trend of the glacier-sea ice-ocean system throughout the Holocene, in the Adé lie Land region. In addition, the orbitally-forced seasonality seems to control the coastal deep water formation via the sea ice-ocean coupling, which could lead to opposite patterns between north and south high latitudes during the Mid to Late Holocene. At sub-Milankovitch time scales, there are eight events of glacier-sea ice retreat and expansion that occurred during atmospheric cooling events over East Antarctica. Comparisons of our results with other peri-Antarctic records and model simulations from high southern latitudes may suggest that our interpretation on glacier-sea ice-ocean interactions and their Holocene evolutions reflect a more global Antarctic Holocene pattern. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Sea ice Université Toulouse III - Paul Sabatier: HAL-UPS Quaternary Science Reviews 28 13-14 1291 1303