Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments
The Antarctic Ice Sheet is a key feature of the global climate engine today, and has been so for most of its 35 Myr or longer history. It influences global circulation (mainly through bottom water production), eustatic sea-level change, biological production and albedo. And yet the details of that h...
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ftnerc:oai:nora.nerc.ac.uk:503893 2023-05-15T13:48:08+02:00 Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments Barker, Peter Camerlenghi, Angelo Acton, Gary Brachfeld, Stephanie Cowan, Ellen Daniels, Jim Domack, Eugene Escutia, Carlota Evans, Andrew Eyles, Nick Guyodo, Yohan Iorio, Marina Iwai, Masao Kyte, Frank Lauer, Christine Maldonado, Andres Moerz, Tobias Osterman, Lisa Pudsey, Carol Schuffert, Jeff Sjunneskog, Charlotte Vigar, Kate Weinheimer, Amy Williams, Trevor Winter, Diane Wolf-Welling, Thomas 1998 http://nora.nerc.ac.uk/id/eprint/503893/ http://www-odp.tamu.edu/publications/citations/joides_j/joides_j_24_2.pdf#page=7 unknown Barker, Peter; Camerlenghi, Angelo; Acton, Gary; Brachfeld, Stephanie; Cowan, Ellen; Daniels, Jim; Domack, Eugene; Escutia, Carlota; Evans, Andrew; Eyles, Nick; Guyodo, Yohan; Iorio, Marina; Iwai, Masao; Kyte, Frank; Lauer, Christine; Maldonado, Andres; Moerz, Tobias; Osterman, Lisa; Pudsey, Carol; Schuffert, Jeff; Sjunneskog, Charlotte; Vigar, Kate; Weinheimer, Amy; Williams, Trevor; Winter, Diane; Wolf-Welling, Thomas. 1998 Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments. JOIDES Journal, 24 (2). 7-10. Publication - Article PeerReviewed 1998 ftnerc 2023-02-04T19:38:06Z The Antarctic Ice Sheet is a key feature of the global climate engine today, and has been so for most of its 35 Myr or longer history. It influences global circulation (mainly through bottom water production), eustatic sea-level change, biological production and albedo. And yet the details of that history are poorly known, despite two decades of measurement and interpretation of lowlatitude ice-volume proxies. The most effective of those proxy measurements, oxygen isotopes and sea-level change, are ambiguous, and disagree. Recently, a way out of this impasse has emerged, that is technically difficult but much more direct. It involves sampling and dating sediments transported beneath the grounded ice sheet and deposited seaward of the grounding line around the Antarctic margin. We now appreciate that the ice sheet “drains” mainly by rapid flow in ice streams that slide on a shearing bed of diamict. Over the life of the ice sheet, those glacially-transported sediments have formed progradational wedges on the outer continental shelf. They, and their derived sediments redeposited in drifts on the upper continental rise, should therefore contain a record of ice sheet advance to the continental shelf edge. The prograded wedge is essentially unsorted making it difficult to recover, and the topsets are prone to subsequent erosion. The drifts have formed by more continuous deposition of sorted silty clays that are easier to recover but less direct, needing clues from the wedge to aid interpretation. The two depositional environments are complementary. Additional useful features of the Antarctic margin are the deep basins eroded on the inner continental shelf during glacial maxima, which preserve an expanded Holocene record of climate change. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Sheet Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
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description |
The Antarctic Ice Sheet is a key feature of the global climate engine today, and has been so for most of its 35 Myr or longer history. It influences global circulation (mainly through bottom water production), eustatic sea-level change, biological production and albedo. And yet the details of that history are poorly known, despite two decades of measurement and interpretation of lowlatitude ice-volume proxies. The most effective of those proxy measurements, oxygen isotopes and sea-level change, are ambiguous, and disagree. Recently, a way out of this impasse has emerged, that is technically difficult but much more direct. It involves sampling and dating sediments transported beneath the grounded ice sheet and deposited seaward of the grounding line around the Antarctic margin. We now appreciate that the ice sheet “drains” mainly by rapid flow in ice streams that slide on a shearing bed of diamict. Over the life of the ice sheet, those glacially-transported sediments have formed progradational wedges on the outer continental shelf. They, and their derived sediments redeposited in drifts on the upper continental rise, should therefore contain a record of ice sheet advance to the continental shelf edge. The prograded wedge is essentially unsorted making it difficult to recover, and the topsets are prone to subsequent erosion. The drifts have formed by more continuous deposition of sorted silty clays that are easier to recover but less direct, needing clues from the wedge to aid interpretation. The two depositional environments are complementary. Additional useful features of the Antarctic margin are the deep basins eroded on the inner continental shelf during glacial maxima, which preserve an expanded Holocene record of climate change. |
format |
Article in Journal/Newspaper |
author |
Barker, Peter Camerlenghi, Angelo Acton, Gary Brachfeld, Stephanie Cowan, Ellen Daniels, Jim Domack, Eugene Escutia, Carlota Evans, Andrew Eyles, Nick Guyodo, Yohan Iorio, Marina Iwai, Masao Kyte, Frank Lauer, Christine Maldonado, Andres Moerz, Tobias Osterman, Lisa Pudsey, Carol Schuffert, Jeff Sjunneskog, Charlotte Vigar, Kate Weinheimer, Amy Williams, Trevor Winter, Diane Wolf-Welling, Thomas |
spellingShingle |
Barker, Peter Camerlenghi, Angelo Acton, Gary Brachfeld, Stephanie Cowan, Ellen Daniels, Jim Domack, Eugene Escutia, Carlota Evans, Andrew Eyles, Nick Guyodo, Yohan Iorio, Marina Iwai, Masao Kyte, Frank Lauer, Christine Maldonado, Andres Moerz, Tobias Osterman, Lisa Pudsey, Carol Schuffert, Jeff Sjunneskog, Charlotte Vigar, Kate Weinheimer, Amy Williams, Trevor Winter, Diane Wolf-Welling, Thomas Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
author_facet |
Barker, Peter Camerlenghi, Angelo Acton, Gary Brachfeld, Stephanie Cowan, Ellen Daniels, Jim Domack, Eugene Escutia, Carlota Evans, Andrew Eyles, Nick Guyodo, Yohan Iorio, Marina Iwai, Masao Kyte, Frank Lauer, Christine Maldonado, Andres Moerz, Tobias Osterman, Lisa Pudsey, Carol Schuffert, Jeff Sjunneskog, Charlotte Vigar, Kate Weinheimer, Amy Williams, Trevor Winter, Diane Wolf-Welling, Thomas |
author_sort |
Barker, Peter |
title |
Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
title_short |
Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
title_full |
Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
title_fullStr |
Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
title_full_unstemmed |
Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments |
title_sort |
antarctic glacial history and sea-level change - leg 178 samples antarctic peninsula margin sediments |
publishDate |
1998 |
url |
http://nora.nerc.ac.uk/id/eprint/503893/ http://www-odp.tamu.edu/publications/citations/joides_j/joides_j_24_2.pdf#page=7 |
geographic |
Antarctic The Antarctic Antarctic Peninsula |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Sheet |
op_relation |
Barker, Peter; Camerlenghi, Angelo; Acton, Gary; Brachfeld, Stephanie; Cowan, Ellen; Daniels, Jim; Domack, Eugene; Escutia, Carlota; Evans, Andrew; Eyles, Nick; Guyodo, Yohan; Iorio, Marina; Iwai, Masao; Kyte, Frank; Lauer, Christine; Maldonado, Andres; Moerz, Tobias; Osterman, Lisa; Pudsey, Carol; Schuffert, Jeff; Sjunneskog, Charlotte; Vigar, Kate; Weinheimer, Amy; Williams, Trevor; Winter, Diane; Wolf-Welling, Thomas. 1998 Antarctic glacial history and sea-level change - Leg 178 samples Antarctic Peninsula margin sediments. JOIDES Journal, 24 (2). 7-10. |
_version_ |
1766248707923116032 |