The Marine Geological Imprint of Antarctic Ice Shelves

Reductions in the thickness and extent of Antarctic ice shelves are triggering increased discharge of marine-terminating glaciers. While the impacts of recent changes are well documented, their role in modulating past ice-sheet dynamics remains poorly constrained. This reflects two persistent issues...

Full description

Bibliographic Details
Main Authors: Smith, James A., Graham, Alastair G., Post, Alix L., Hillenbrand, Claus-Dieter, Bart, Philip J., Powell, Ross D.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2019
Subjects:
Online Access:https://digitalcommons.usf.edu/msc_facpub/1524
https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2534&context=msc_facpub
id ftunisfloridatam:oai:digitalcommons.usf.edu:msc_facpub-2534
record_format openpolar
spelling ftunisfloridatam:oai:digitalcommons.usf.edu:msc_facpub-2534 2023-05-15T14:04:11+02:00 The Marine Geological Imprint of Antarctic Ice Shelves Smith, James A. Graham, Alastair G. Post, Alix L. Hillenbrand, Claus-Dieter Bart, Philip J. Powell, Ross D. 2019-01-01T08:00:00Z application/pdf https://digitalcommons.usf.edu/msc_facpub/1524 https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2534&context=msc_facpub unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/msc_facpub/1524 https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2534&context=msc_facpub http://creativecommons.org/licenses/by/4.0/ CC-BY Marine Science Faculty Publications Climate sciences Environmental sciences Ocean sciences Scientific community Life Sciences article 2019 ftunisfloridatam 2022-01-20T18:40:12Z Reductions in the thickness and extent of Antarctic ice shelves are triggering increased discharge of marine-terminating glaciers. While the impacts of recent changes are well documented, their role in modulating past ice-sheet dynamics remains poorly constrained. This reflects two persistent issues; first, the effective discrimination of sediments and landforms solely attributable to sub-ice-shelf deposition, and second, challenges in dating these records. Recent progress in deciphering the geological imprint of Antarctic ice shelves is summarised, including advances in dating methods and proxies to reconstruct drivers of change. Finally, we identify several challenges to overcome to fully exploit the paleo record. The recent collapses of ice shelves in Antarctica due to warming make it essential to understand past ice shelf conditions and mechanisms. Here Smith and colleagues review the latest progress in deciphering the geological imprint of Antarctic ice shelves via sediments, landforms and proxy indicators. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Digital Commons University of South Florida (USF) Antarctic
institution Open Polar
collection Digital Commons University of South Florida (USF)
op_collection_id ftunisfloridatam
language unknown
topic Climate sciences
Environmental sciences
Ocean sciences
Scientific community
Life Sciences
spellingShingle Climate sciences
Environmental sciences
Ocean sciences
Scientific community
Life Sciences
Smith, James A.
Graham, Alastair G.
Post, Alix L.
Hillenbrand, Claus-Dieter
Bart, Philip J.
Powell, Ross D.
The Marine Geological Imprint of Antarctic Ice Shelves
topic_facet Climate sciences
Environmental sciences
Ocean sciences
Scientific community
Life Sciences
description Reductions in the thickness and extent of Antarctic ice shelves are triggering increased discharge of marine-terminating glaciers. While the impacts of recent changes are well documented, their role in modulating past ice-sheet dynamics remains poorly constrained. This reflects two persistent issues; first, the effective discrimination of sediments and landforms solely attributable to sub-ice-shelf deposition, and second, challenges in dating these records. Recent progress in deciphering the geological imprint of Antarctic ice shelves is summarised, including advances in dating methods and proxies to reconstruct drivers of change. Finally, we identify several challenges to overcome to fully exploit the paleo record. The recent collapses of ice shelves in Antarctica due to warming make it essential to understand past ice shelf conditions and mechanisms. Here Smith and colleagues review the latest progress in deciphering the geological imprint of Antarctic ice shelves via sediments, landforms and proxy indicators.
format Article in Journal/Newspaper
author Smith, James A.
Graham, Alastair G.
Post, Alix L.
Hillenbrand, Claus-Dieter
Bart, Philip J.
Powell, Ross D.
author_facet Smith, James A.
Graham, Alastair G.
Post, Alix L.
Hillenbrand, Claus-Dieter
Bart, Philip J.
Powell, Ross D.
author_sort Smith, James A.
title The Marine Geological Imprint of Antarctic Ice Shelves
title_short The Marine Geological Imprint of Antarctic Ice Shelves
title_full The Marine Geological Imprint of Antarctic Ice Shelves
title_fullStr The Marine Geological Imprint of Antarctic Ice Shelves
title_full_unstemmed The Marine Geological Imprint of Antarctic Ice Shelves
title_sort marine geological imprint of antarctic ice shelves
publisher Digital Commons @ University of South Florida
publishDate 2019
url https://digitalcommons.usf.edu/msc_facpub/1524
https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2534&context=msc_facpub
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
op_source Marine Science Faculty Publications
op_relation https://digitalcommons.usf.edu/msc_facpub/1524
https://digitalcommons.usf.edu/cgi/viewcontent.cgi?article=2534&context=msc_facpub
op_rights http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
_version_ 1766275208482652160