Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures
The timing, nature, and causes of grounded ice-sheet retreat following the Last Glacial Maximum (LGM) in Marguerite Trough, west Antarctic Peninsula, and subsequent early Holocene ice-shelf decay, are presented in this paper. We use sedimentological, foraminiferal, geotechnical, and accelerator mass...
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ftuglasgow:oai:eprints.gla.ac.uk:70904 2023-05-15T13:31:54+02:00 Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures Kilfeather, A.A. Cofaigh, C.O. Lloyd, J.M. Dowdeswell, J.A. Xu, S. Moreton, S.G. 2011-05 http://eprints.gla.ac.uk/70904/ unknown Kilfeather, A.A., Cofaigh, C.O., Lloyd, J.M., Dowdeswell, J.A., Xu, S. <http://eprints.gla.ac.uk/view/author/12708.html> and Moreton, S.G. <http://eprints.gla.ac.uk/view/author/11570.html> (2011) Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures. Geological Society of America Bulletin <http://eprints.gla.ac.uk/view/journal_volume/Geological_Society_of_America_Bulletin.html>, 123(5-6), pp. 997-1015. (doi:10.1130/B30282.1 <http://dx.doi.org/10.1130/B30282.1>) Articles PeerReviewed 2011 ftuglasgow https://doi.org/10.1130/B30282.1 2021-09-23T22:48:48Z The timing, nature, and causes of grounded ice-sheet retreat following the Last Glacial Maximum (LGM) in Marguerite Trough, west Antarctic Peninsula, and subsequent early Holocene ice-shelf decay, are presented in this paper. We use sedimentological, foraminiferal, geotechnical, and accelerator mass spectrometer (AMS) radiocarbon data from marine cores from the mid-continental shelf, together with previously published AMS dates, to establish a sedimentological and chronological model. Initial ice-sheet retreat through the outer- and mid-shelf sectors of Marguerite Trough was under way by ca. 14 ka B.P., was rapid, and coincided with the sea-level rise of meltwater pulse 1a. An ice shelf formed during this retreat, and fine-grained, laminated muds reflecting meltwater-derived suspension settling and/or tidal pumping were deposited. During this time the ice sheet remained grounded on the inner shelf. Ice-shelf breakup and retreat of the calving front, from ca. 13.2 to 12.5 ka B.P., was slow (∼100 m a−1) across the outer- and mid-shelf, with calving bay conditions remaining for at least 3.5 ka. We interpret this ice-shelf decay to have been driven by an incursion of Weddell Sea Transitional Water onto the shelf. In contrast, grounding-line and ice-shelf retreat in the inner bay occurred from ca. 9.3 ka B.P. and was driven by Circumpolar Warm Deep Water encroaching onto the continental shelf. At this time the mid-shelf was an open-marine environment characterized by hemipelagic deposition. These findings highlight the importance of oceanographic controls in the breakup of Antarctic Peninsula ice shelves during the Holocene. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Sheet Ice Shelf Ice Shelves Weddell Sea University of Glasgow: Enlighten - Publications Antarctic Antarctic Peninsula Inner Bay ENVELOPE(-37.967,-37.967,-54.017,-54.017) Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Weddell Weddell Sea Geological Society of America Bulletin 123 5-6 997 1015 |
institution |
Open Polar |
collection |
University of Glasgow: Enlighten - Publications |
op_collection_id |
ftuglasgow |
language |
unknown |
description |
The timing, nature, and causes of grounded ice-sheet retreat following the Last Glacial Maximum (LGM) in Marguerite Trough, west Antarctic Peninsula, and subsequent early Holocene ice-shelf decay, are presented in this paper. We use sedimentological, foraminiferal, geotechnical, and accelerator mass spectrometer (AMS) radiocarbon data from marine cores from the mid-continental shelf, together with previously published AMS dates, to establish a sedimentological and chronological model. Initial ice-sheet retreat through the outer- and mid-shelf sectors of Marguerite Trough was under way by ca. 14 ka B.P., was rapid, and coincided with the sea-level rise of meltwater pulse 1a. An ice shelf formed during this retreat, and fine-grained, laminated muds reflecting meltwater-derived suspension settling and/or tidal pumping were deposited. During this time the ice sheet remained grounded on the inner shelf. Ice-shelf breakup and retreat of the calving front, from ca. 13.2 to 12.5 ka B.P., was slow (∼100 m a−1) across the outer- and mid-shelf, with calving bay conditions remaining for at least 3.5 ka. We interpret this ice-shelf decay to have been driven by an incursion of Weddell Sea Transitional Water onto the shelf. In contrast, grounding-line and ice-shelf retreat in the inner bay occurred from ca. 9.3 ka B.P. and was driven by Circumpolar Warm Deep Water encroaching onto the continental shelf. At this time the mid-shelf was an open-marine environment characterized by hemipelagic deposition. These findings highlight the importance of oceanographic controls in the breakup of Antarctic Peninsula ice shelves during the Holocene. |
format |
Article in Journal/Newspaper |
author |
Kilfeather, A.A. Cofaigh, C.O. Lloyd, J.M. Dowdeswell, J.A. Xu, S. Moreton, S.G. |
spellingShingle |
Kilfeather, A.A. Cofaigh, C.O. Lloyd, J.M. Dowdeswell, J.A. Xu, S. Moreton, S.G. Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
author_facet |
Kilfeather, A.A. Cofaigh, C.O. Lloyd, J.M. Dowdeswell, J.A. Xu, S. Moreton, S.G. |
author_sort |
Kilfeather, A.A. |
title |
Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
title_short |
Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
title_full |
Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
title_fullStr |
Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
title_full_unstemmed |
Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures |
title_sort |
ice-stream retreat and ice-shelf history in marguerite trough, antarctic peninsula: sedimentological and foraminiferal signatures |
publishDate |
2011 |
url |
http://eprints.gla.ac.uk/70904/ |
long_lat |
ENVELOPE(-37.967,-37.967,-54.017,-54.017) ENVELOPE(141.378,141.378,-66.787,-66.787) |
geographic |
Antarctic Antarctic Peninsula Inner Bay Marguerite Weddell Weddell Sea |
geographic_facet |
Antarctic Antarctic Peninsula Inner Bay Marguerite Weddell Weddell Sea |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Sheet Ice Shelf Ice Shelves Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Sheet Ice Shelf Ice Shelves Weddell Sea |
op_relation |
Kilfeather, A.A., Cofaigh, C.O., Lloyd, J.M., Dowdeswell, J.A., Xu, S. <http://eprints.gla.ac.uk/view/author/12708.html> and Moreton, S.G. <http://eprints.gla.ac.uk/view/author/11570.html> (2011) Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures. Geological Society of America Bulletin <http://eprints.gla.ac.uk/view/journal_volume/Geological_Society_of_America_Bulletin.html>, 123(5-6), pp. 997-1015. (doi:10.1130/B30282.1 <http://dx.doi.org/10.1130/B30282.1>) |
op_doi |
https://doi.org/10.1130/B30282.1 |
container_title |
Geological Society of America Bulletin |
container_volume |
123 |
container_issue |
5-6 |
container_start_page |
997 |
op_container_end_page |
1015 |
_version_ |
1766022282188161024 |