Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum

International audience The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting its evolution since the Last Glacial Maximum (LGM) is important for understanding its present-day and future behaviour. As part of a community effort, we review geological evidenc...

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Published in:Quaternary Science Reviews
Main Authors: Mackintosh, Andrew N., Verleyen, Elie, O'Brien, Philip E., White, Duanne A., Jones, R. Selwyn, Mckay, Robert, Dunbar, Robert, Gore, Damian B., Fink, David, Post, Alexandra L., Miura, Hideki, Leventer, Amy, Goodwin, Ian, Hodgson, Dominic A., Lilly, Katherine, Crosta, Xavier, Golledge, Nicholas R., Wagner, Bernd, Berg, Sonja, van Ommen, Tas, Zwartz, Dan, Roberts, Stephen J., Vyverman, Wim, Massé, Guillaume
Other Authors: 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), Biogéochimie-Traceurs-Paléoclimat (BTP), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal.science/hal-02105571
https://doi.org/10.1016/j.quascirev.2013.07.024
id ftepunivpsaclay:oai:HAL:hal-02105571v1
record_format openpolar
institution Open Polar
collection École Polytechnique, Université Paris-Saclay: HAL
op_collection_id ftepunivpsaclay
language English
topic Sea level rise
Antarctica
Last Glacial Maximum
Ice sheet
[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
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle Sea level rise
Antarctica
Last Glacial Maximum
Ice sheet
[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
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Mackintosh, Andrew N.
Verleyen, Elie
O'Brien, Philip E.
White, Duanne A.
Jones, R. Selwyn
Mckay, Robert
Dunbar, Robert
Gore, Damian B.
Fink, David
Post, Alexandra L.
Miura, Hideki
Leventer, Amy
Goodwin, Ian
Hodgson, Dominic A.
Lilly, Katherine
Crosta, Xavier
Golledge, Nicholas R.
Wagner, Bernd
Berg, Sonja
van Ommen, Tas
Zwartz, Dan
Roberts, Stephen J.
Vyverman, Wim
Massé, Guillaume
Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
topic_facet Sea level rise
Antarctica
Last Glacial Maximum
Ice sheet
[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
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting its evolution since the Last Glacial Maximum (LGM) is important for understanding its present-day and future behaviour. As part of a community effort, we review geological evidence from East Antarctica that constrains the ice sheet history throughout this period (∼30,000 years ago to present). This includes terrestrial cosmogenic nuclide dates from previously glaciated regions, 14C chronologies from glacial and post-glacial deposits onshore and on the continental shelf, and ice sheet thickness changes inferred from ice cores and continental-scale ice sheet models. We also include new 14C dates from the George V Land – Terre Adélie Coast shelf. We show that the EAIS advanced to the continental shelf margin in some parts of East Antarctica, and that the ice sheet characteristically thickened by 300–400 m near the present-day coastline at these sites. This advance was associated with the formation of low-gradient ice streams that grounded at depths of >1 km below sea level on the inner continental shelf. The Lambert/Amery system thickened by a greater amount (800 m) near its present-day grounding zone, but did not advance beyond the inner continental shelf. At other sites in coastal East Antarctica (e.g. Bunger Hills, Larsemann Hills), very little change in the ice sheet margin occurred at the LGM, perhaps because ice streams accommodated any excess ice build up, leaving adjacent, ice-free areas relatively unaffected. Evidence from nunataks indicates that the amount of ice sheet thickening diminished inland at the LGM, an observation supported by ice cores, which suggest that interior ice sheet domes were ∼100 m lower than present at this time. Ice sheet recession may have started ∼18,000 years ago in the Lambert/Amery glacial system, and by ∼14,000 years ago in Mac.Robertson Land. These early pulses of deglaciation may have been responses to abrupt sea-level rise events such as Meltwater ...
author2 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)
Biogéochimie-Traceurs-Paléoclimat (BTP)
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Mackintosh, Andrew N.
Verleyen, Elie
O'Brien, Philip E.
White, Duanne A.
Jones, R. Selwyn
Mckay, Robert
Dunbar, Robert
Gore, Damian B.
Fink, David
Post, Alexandra L.
Miura, Hideki
Leventer, Amy
Goodwin, Ian
Hodgson, Dominic A.
Lilly, Katherine
Crosta, Xavier
Golledge, Nicholas R.
Wagner, Bernd
Berg, Sonja
van Ommen, Tas
Zwartz, Dan
Roberts, Stephen J.
Vyverman, Wim
Massé, Guillaume
author_facet Mackintosh, Andrew N.
Verleyen, Elie
O'Brien, Philip E.
White, Duanne A.
Jones, R. Selwyn
Mckay, Robert
Dunbar, Robert
Gore, Damian B.
Fink, David
Post, Alexandra L.
Miura, Hideki
Leventer, Amy
Goodwin, Ian
Hodgson, Dominic A.
Lilly, Katherine
Crosta, Xavier
Golledge, Nicholas R.
Wagner, Bernd
Berg, Sonja
van Ommen, Tas
Zwartz, Dan
Roberts, Stephen J.
Vyverman, Wim
Massé, Guillaume
author_sort Mackintosh, Andrew N.
title Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
title_short Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
title_full Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
title_fullStr Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
title_full_unstemmed Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum
title_sort retreat history of the east antarctic ice sheet since the last glacial maximum
publisher HAL CCSD
publishDate 2014
url https://hal.science/hal-02105571
https://doi.org/10.1016/j.quascirev.2013.07.024
genre Antarc*
Antarctic
Antarctica
East Antarctica
George V Land
Ice Sheet
Mac.Robertson Land
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
George V Land
Ice Sheet
Mac.Robertson Land
op_source ISSN: 0277-3791
EISSN: 1873-457X
Quaternary Science Reviews
https://hal.science/hal-02105571
Quaternary Science Reviews, 2014, 100, pp.10-30. ⟨10.1016/j.quascirev.2013.07.024⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2013.07.024
hal-02105571
https://hal.science/hal-02105571
doi:10.1016/j.quascirev.2013.07.024
WOS: 000342252700002
op_doi https://doi.org/10.1016/j.quascirev.2013.07.024
container_title Quaternary Science Reviews
container_volume 100
container_start_page 10
op_container_end_page 30
_version_ 1799469425849532416
spelling ftepunivpsaclay:oai:HAL:hal-02105571v1 2024-05-19T07:31:34+00:00 Retreat history of the East Antarctic Ice Sheet since the Last Glacial Maximum Mackintosh, Andrew N. Verleyen, Elie O'Brien, Philip E. White, Duanne A. Jones, R. Selwyn Mckay, Robert Dunbar, Robert Gore, Damian B. Fink, David Post, Alexandra L. Miura, Hideki Leventer, Amy Goodwin, Ian Hodgson, Dominic A. Lilly, Katherine Crosta, Xavier Golledge, Nicholas R. Wagner, Bernd Berg, Sonja van Ommen, Tas Zwartz, Dan Roberts, Stephen J. Vyverman, Wim Massé, Guillaume 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) Biogéochimie-Traceurs-Paléoclimat (BTP) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2014 https://hal.science/hal-02105571 https://doi.org/10.1016/j.quascirev.2013.07.024 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2013.07.024 hal-02105571 https://hal.science/hal-02105571 doi:10.1016/j.quascirev.2013.07.024 WOS: 000342252700002 ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-02105571 Quaternary Science Reviews, 2014, 100, pp.10-30. ⟨10.1016/j.quascirev.2013.07.024⟩ Sea level rise Antarctica Last Glacial Maximum Ice sheet [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 [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2014 ftepunivpsaclay https://doi.org/10.1016/j.quascirev.2013.07.024 2024-04-25T00:50:03Z International audience The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting its evolution since the Last Glacial Maximum (LGM) is important for understanding its present-day and future behaviour. As part of a community effort, we review geological evidence from East Antarctica that constrains the ice sheet history throughout this period (∼30,000 years ago to present). This includes terrestrial cosmogenic nuclide dates from previously glaciated regions, 14C chronologies from glacial and post-glacial deposits onshore and on the continental shelf, and ice sheet thickness changes inferred from ice cores and continental-scale ice sheet models. We also include new 14C dates from the George V Land – Terre Adélie Coast shelf. We show that the EAIS advanced to the continental shelf margin in some parts of East Antarctica, and that the ice sheet characteristically thickened by 300–400 m near the present-day coastline at these sites. This advance was associated with the formation of low-gradient ice streams that grounded at depths of >1 km below sea level on the inner continental shelf. The Lambert/Amery system thickened by a greater amount (800 m) near its present-day grounding zone, but did not advance beyond the inner continental shelf. At other sites in coastal East Antarctica (e.g. Bunger Hills, Larsemann Hills), very little change in the ice sheet margin occurred at the LGM, perhaps because ice streams accommodated any excess ice build up, leaving adjacent, ice-free areas relatively unaffected. Evidence from nunataks indicates that the amount of ice sheet thickening diminished inland at the LGM, an observation supported by ice cores, which suggest that interior ice sheet domes were ∼100 m lower than present at this time. Ice sheet recession may have started ∼18,000 years ago in the Lambert/Amery glacial system, and by ∼14,000 years ago in Mac.Robertson Land. These early pulses of deglaciation may have been responses to abrupt sea-level rise events such as Meltwater ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica George V Land Ice Sheet Mac.Robertson Land École Polytechnique, Université Paris-Saclay: HAL Quaternary Science Reviews 100 10 30