Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation
Deep-sea sediment core FR1/97 GC-12 is located 990 mbsl in the northern Tasman Sea, southwest Pacific, where Antarctic Intermediate Water (AAIW) presently impinges the continental slope of the southern Great Barrier Reef. Analysis of carbon (δ13C) and ox
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American Geophysical Union
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Online Access: | http://hdl.handle.net/1885/86792 https://doi.org/10.1029/2004PA001047 https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg |
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/86792 2024-01-14T10:01:14+01:00 Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation Bostock, Helen Opdyke, Bradley Gagan, Michael Fifield, L Keith http://hdl.handle.net/1885/86792 https://doi.org/10.1029/2004PA001047 https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg unknown American Geophysical Union 0883-8305 http://hdl.handle.net/1885/86792 doi:10.1029/2004PA001047 https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg Paleoceanography Keywords: carbon isotope deglaciation foraminifera intermediate water Last Glacial Maximum paleoceanography oceanic regions Pacific Ocean Pacific Ocean (Northwest) World Foraminifera d13C AAIW Journal article ftanucanberra https://doi.org/10.1029/2004PA001047 2023-12-15T09:33:36Z Deep-sea sediment core FR1/97 GC-12 is located 990 mbsl in the northern Tasman Sea, southwest Pacific, where Antarctic Intermediate Water (AAIW) presently impinges the continental slope of the southern Great Barrier Reef. Analysis of carbon (δ13C) and ox Article in Journal/Newspaper Antarc* Antarctic Australian National University: ANU Digital Collections Antarctic Pacific Paleoceanography 19 4 n/a n/a |
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Open Polar |
collection |
Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
topic |
Keywords: carbon isotope deglaciation foraminifera intermediate water Last Glacial Maximum paleoceanography oceanic regions Pacific Ocean Pacific Ocean (Northwest) World Foraminifera d13C AAIW |
spellingShingle |
Keywords: carbon isotope deglaciation foraminifera intermediate water Last Glacial Maximum paleoceanography oceanic regions Pacific Ocean Pacific Ocean (Northwest) World Foraminifera d13C AAIW Bostock, Helen Opdyke, Bradley Gagan, Michael Fifield, L Keith Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
topic_facet |
Keywords: carbon isotope deglaciation foraminifera intermediate water Last Glacial Maximum paleoceanography oceanic regions Pacific Ocean Pacific Ocean (Northwest) World Foraminifera d13C AAIW |
description |
Deep-sea sediment core FR1/97 GC-12 is located 990 mbsl in the northern Tasman Sea, southwest Pacific, where Antarctic Intermediate Water (AAIW) presently impinges the continental slope of the southern Great Barrier Reef. Analysis of carbon (δ13C) and ox |
format |
Article in Journal/Newspaper |
author |
Bostock, Helen Opdyke, Bradley Gagan, Michael Fifield, L Keith |
author_facet |
Bostock, Helen Opdyke, Bradley Gagan, Michael Fifield, L Keith |
author_sort |
Bostock, Helen |
title |
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
title_short |
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
title_full |
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
title_fullStr |
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
title_full_unstemmed |
Carbon isotope evidence for changes in Antarctic Intermediate Water circulation and ocean ventilation in the southwest Pacific during the last deglaciation |
title_sort |
carbon isotope evidence for changes in antarctic intermediate water circulation and ocean ventilation in the southwest pacific during the last deglaciation |
publisher |
American Geophysical Union |
url |
http://hdl.handle.net/1885/86792 https://doi.org/10.1029/2004PA001047 https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg |
geographic |
Antarctic Pacific |
geographic_facet |
Antarctic Pacific |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Paleoceanography |
op_relation |
0883-8305 http://hdl.handle.net/1885/86792 doi:10.1029/2004PA001047 https://openresearch-repository.anu.edu.au/bitstream/1885/86792/5/MigratedxPub15783_2004.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/86792/7/01_Bostock_Carbon_isotope_evidence_for_2004.pdf.jpg |
op_doi |
https://doi.org/10.1029/2004PA001047 |
container_title |
Paleoceanography |
container_volume |
19 |
container_issue |
4 |
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n/a |
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n/a |
_version_ |
1788067039540150272 |