In situ foraminifera in grounding zone diamict: A working hypothesis
© 2016 Antarctic Science Ltd. The ice-proximal diamict sediment deposited on the foreset of a grounding zone wedge in Glomar Challenger Basin on the eastern Ross Sea continental shelf yielded a low abundance assemblage of foraminifera at two piston core sites. We found 302 small well-preserved speci...
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Online Access: | https://digitalcommons.lsu.edu/geo_pubs/1046 https://doi.org/10.1017/S0954102016000055 |
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ftlouisianastuir:oai:digitalcommons.lsu.edu:geo_pubs-2045 2023-06-11T04:06:52+02:00 In situ foraminifera in grounding zone diamict: A working hypothesis Bart, Philip J. Coquereau, Laura Warny, Sophie Majewski, Wojciech 2016-08-01T07:00:00Z https://digitalcommons.lsu.edu/geo_pubs/1046 https://doi.org/10.1017/S0954102016000055 unknown LSU Digital Commons https://digitalcommons.lsu.edu/geo_pubs/1046 doi:10.1017/S0954102016000055 Faculty Publications continental shelf grounding zone wedge ice sheet Last Glacial Maximum Ross Sea West Antarctica text 2016 ftlouisianastuir https://doi.org/10.1017/S0954102016000055 2023-05-28T18:17:27Z © 2016 Antarctic Science Ltd. The ice-proximal diamict sediment deposited on the foreset of a grounding zone wedge in Glomar Challenger Basin on the eastern Ross Sea continental shelf yielded a low abundance assemblage of foraminifera at two piston core sites. We found 302 small well-preserved specimens representing 18 species of benthic foraminifera from 825 ml of sediment. Only three poorly preserved specimens of the planktonic foraminifera Neogloboquadrina pachyderma (sinistral) were found. Our combined analyses of preservation state, assemblage composition and stable isotopes suggest that the benthic foraminifera may be in situ. This possibility is of interest to palaeoclimatologists who use ice-proximal sediments on the Antarctic continental shelves to radiocarbon date the post-glacial retreat history. Text Antarc* Antarctic Antarctica Ice Sheet Neogloboquadrina pachyderma Planktonic foraminifera Ross Sea West Antarctica LSU Digital Commons (Louisiana State University) Antarctic The Antarctic Ross Sea West Antarctica Glomar Challenger Basin ENVELOPE(180.000,180.000,-77.750,-77.750) Antarctic Science 28 4 313 321 |
institution |
Open Polar |
collection |
LSU Digital Commons (Louisiana State University) |
op_collection_id |
ftlouisianastuir |
language |
unknown |
topic |
continental shelf grounding zone wedge ice sheet Last Glacial Maximum Ross Sea West Antarctica |
spellingShingle |
continental shelf grounding zone wedge ice sheet Last Glacial Maximum Ross Sea West Antarctica Bart, Philip J. Coquereau, Laura Warny, Sophie Majewski, Wojciech In situ foraminifera in grounding zone diamict: A working hypothesis |
topic_facet |
continental shelf grounding zone wedge ice sheet Last Glacial Maximum Ross Sea West Antarctica |
description |
© 2016 Antarctic Science Ltd. The ice-proximal diamict sediment deposited on the foreset of a grounding zone wedge in Glomar Challenger Basin on the eastern Ross Sea continental shelf yielded a low abundance assemblage of foraminifera at two piston core sites. We found 302 small well-preserved specimens representing 18 species of benthic foraminifera from 825 ml of sediment. Only three poorly preserved specimens of the planktonic foraminifera Neogloboquadrina pachyderma (sinistral) were found. Our combined analyses of preservation state, assemblage composition and stable isotopes suggest that the benthic foraminifera may be in situ. This possibility is of interest to palaeoclimatologists who use ice-proximal sediments on the Antarctic continental shelves to radiocarbon date the post-glacial retreat history. |
format |
Text |
author |
Bart, Philip J. Coquereau, Laura Warny, Sophie Majewski, Wojciech |
author_facet |
Bart, Philip J. Coquereau, Laura Warny, Sophie Majewski, Wojciech |
author_sort |
Bart, Philip J. |
title |
In situ foraminifera in grounding zone diamict: A working hypothesis |
title_short |
In situ foraminifera in grounding zone diamict: A working hypothesis |
title_full |
In situ foraminifera in grounding zone diamict: A working hypothesis |
title_fullStr |
In situ foraminifera in grounding zone diamict: A working hypothesis |
title_full_unstemmed |
In situ foraminifera in grounding zone diamict: A working hypothesis |
title_sort |
in situ foraminifera in grounding zone diamict: a working hypothesis |
publisher |
LSU Digital Commons |
publishDate |
2016 |
url |
https://digitalcommons.lsu.edu/geo_pubs/1046 https://doi.org/10.1017/S0954102016000055 |
long_lat |
ENVELOPE(180.000,180.000,-77.750,-77.750) |
geographic |
Antarctic The Antarctic Ross Sea West Antarctica Glomar Challenger Basin |
geographic_facet |
Antarctic The Antarctic Ross Sea West Antarctica Glomar Challenger Basin |
genre |
Antarc* Antarctic Antarctica Ice Sheet Neogloboquadrina pachyderma Planktonic foraminifera Ross Sea West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Neogloboquadrina pachyderma Planktonic foraminifera Ross Sea West Antarctica |
op_source |
Faculty Publications |
op_relation |
https://digitalcommons.lsu.edu/geo_pubs/1046 doi:10.1017/S0954102016000055 |
op_doi |
https://doi.org/10.1017/S0954102016000055 |
container_title |
Antarctic Science |
container_volume |
28 |
container_issue |
4 |
container_start_page |
313 |
op_container_end_page |
321 |
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1768379060278263808 |