Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability
Data from cores collected from sites that were beneath the Ross Ice Shelf until 2000 and 2002 indicate that sub-ice shelf lithofacies are distinguishable from sub-glacial and glacial marine facies. Glacial marine sediment is characterized by diatom-rich, low-density, olive-green, sandy-muds, whereas...
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ftunivnebraskali:oai:digitalcommons.unl.edu:andrillaffiliates-1009 2023-11-12T04:18:53+01:00 Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability Boyd, L. W. Bartek, L. R. Luyendyk, B. P. Wilson, D. 2007-01-01T08:00:00Z application/pdf https://digitalcommons.unl.edu/andrillaffiliates/10 https://digitalcommons.unl.edu/context/andrillaffiliates/article/1009/viewcontent/Luyendyk_AAKCW_2007_Contrasting_sub_ice.pdf unknown DigitalCommons@University of Nebraska - Lincoln https://digitalcommons.unl.edu/andrillaffiliates/10 https://digitalcommons.unl.edu/context/andrillaffiliates/article/1009/viewcontent/Luyendyk_AAKCW_2007_Contrasting_sub_ice.pdf Related Publications from ANDRILL Affiliates Environmental Indicators and Impact Assessment text 2007 ftunivnebraskali 2023-10-30T10:48:58Z Data from cores collected from sites that were beneath the Ross Ice Shelf until 2000 and 2002 indicate that sub-ice shelf lithofacies are distinguishable from sub-glacial and glacial marine facies. Glacial marine sediment is characterized by diatom-rich, low-density, olive-green, sandy-muds, whereas sub-ice shelf sediment is defined by a lack of diatoms and muds that are enriched in silt and fine sand. Sub-glacial sediment is composed of diatom-poor, high density, coarse grained sandy-mud, rich in fine to coarse sized pebbles. Repetitive, fining-up packages, composed of fine-sand/silty-mud (distal sub ice-shelf deposits), grading into coarse pebbly-mud (sub ice-shelf proximal to the grounding line), suggest cyclicity in the movement of the grounding line over the last 11,000 yrs in the eastern Ross Sea. This research may facilitate a new understanding of ice-shelf dynamics, and possibly refine the current models for the Ross Ice Shelf’s recent glacial history. Text Ice Shelf Ross Ice Shelf Ross Sea University of Nebraska-Lincoln: DigitalCommons@UNL Ross Sea Ross Ice Shelf |
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University of Nebraska-Lincoln: DigitalCommons@UNL |
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ftunivnebraskali |
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topic |
Environmental Indicators and Impact Assessment |
spellingShingle |
Environmental Indicators and Impact Assessment Boyd, L. W. Bartek, L. R. Luyendyk, B. P. Wilson, D. Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
topic_facet |
Environmental Indicators and Impact Assessment |
description |
Data from cores collected from sites that were beneath the Ross Ice Shelf until 2000 and 2002 indicate that sub-ice shelf lithofacies are distinguishable from sub-glacial and glacial marine facies. Glacial marine sediment is characterized by diatom-rich, low-density, olive-green, sandy-muds, whereas sub-ice shelf sediment is defined by a lack of diatoms and muds that are enriched in silt and fine sand. Sub-glacial sediment is composed of diatom-poor, high density, coarse grained sandy-mud, rich in fine to coarse sized pebbles. Repetitive, fining-up packages, composed of fine-sand/silty-mud (distal sub ice-shelf deposits), grading into coarse pebbly-mud (sub ice-shelf proximal to the grounding line), suggest cyclicity in the movement of the grounding line over the last 11,000 yrs in the eastern Ross Sea. This research may facilitate a new understanding of ice-shelf dynamics, and possibly refine the current models for the Ross Ice Shelf’s recent glacial history. |
format |
Text |
author |
Boyd, L. W. Bartek, L. R. Luyendyk, B. P. Wilson, D. |
author_facet |
Boyd, L. W. Bartek, L. R. Luyendyk, B. P. Wilson, D. |
author_sort |
Boyd, L. W. |
title |
Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
title_short |
Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
title_full |
Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
title_fullStr |
Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
title_full_unstemmed |
Contrasting sub-ice shelf, sub glacial and glacial marine deposition: Implications for ice shelf stability |
title_sort |
contrasting sub-ice shelf, sub glacial and glacial marine deposition: implications for ice shelf stability |
publisher |
DigitalCommons@University of Nebraska - Lincoln |
publishDate |
2007 |
url |
https://digitalcommons.unl.edu/andrillaffiliates/10 https://digitalcommons.unl.edu/context/andrillaffiliates/article/1009/viewcontent/Luyendyk_AAKCW_2007_Contrasting_sub_ice.pdf |
geographic |
Ross Sea Ross Ice Shelf |
geographic_facet |
Ross Sea Ross Ice Shelf |
genre |
Ice Shelf Ross Ice Shelf Ross Sea |
genre_facet |
Ice Shelf Ross Ice Shelf Ross Sea |
op_source |
Related Publications from ANDRILL Affiliates |
op_relation |
https://digitalcommons.unl.edu/andrillaffiliates/10 https://digitalcommons.unl.edu/context/andrillaffiliates/article/1009/viewcontent/Luyendyk_AAKCW_2007_Contrasting_sub_ice.pdf |
_version_ |
1782335418722680832 |