Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal
Abstract The Antarctic Cold Reversal (ACR; 14.7 to 13 thousand years ago; ka) phase of the last deglaciation saw a pause in the rise of atmospheric CO2 and Antarctic temperature, that contrasted with warming in the North. A reexpansion of sea ice and a northward shift in the position of the westerly...
Published in: | Paleoceanography and Paleoclimatology |
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2021
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Online Access: | https://hdl.handle.net/1983/31d0240d-9520-4c20-91f9-9deab762f989 https://research-information.bris.ac.uk/en/publications/31d0240d-9520-4c20-91f9-9deab762f989 https://doi.org/10.1029/2021PA004288 https://research-information.bris.ac.uk/ws/files/299437688/Stewart_et_al._2021_ACR_PA004288.pdf |
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ftubristolcris:oai:research-information.bris.ac.uk:publications/31d0240d-9520-4c20-91f9-9deab762f989 2024-05-12T07:56:23+00:00 Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal Stewart, Joseph A. Li, Tao Spooner, Peter T. Burke, Andrea Chen, Tianyu Roberts, Jenny Rae, James W. B. Peck, Victoria Kender, Sev Liu, Qian Robinson, Laura F. 2021-10-19 application/pdf https://hdl.handle.net/1983/31d0240d-9520-4c20-91f9-9deab762f989 https://research-information.bris.ac.uk/en/publications/31d0240d-9520-4c20-91f9-9deab762f989 https://doi.org/10.1029/2021PA004288 https://research-information.bris.ac.uk/ws/files/299437688/Stewart_et_al._2021_ACR_PA004288.pdf eng eng https://research-information.bris.ac.uk/en/publications/31d0240d-9520-4c20-91f9-9deab762f989 info:eu-repo/semantics/openAccess Stewart , J A , Li , T , Spooner , P T , Burke , A , Chen , T , Roberts , J , Rae , J W B , Peck , V , Kender , S , Liu , Q & Robinson , L F 2021 , ' Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal ' , Paleoceanography and Paleoclimatology , vol. 36 , no. 10 , e2021PA004288 . https://doi.org/10.1029/2021PA004288 coral foraminifera Drake Passage deglacial article 2021 ftubristolcris https://doi.org/10.1029/2021PA004288 2024-04-17T14:34:42Z Abstract The Antarctic Cold Reversal (ACR; 14.7 to 13 thousand years ago; ka) phase of the last deglaciation saw a pause in the rise of atmospheric CO2 and Antarctic temperature, that contrasted with warming in the North. A reexpansion of sea ice and a northward shift in the position of the westerly winds in the Southern Ocean are well-documented, but the response of deep-sea biota and the primary drivers of habitat viability remain unclear. Here, we present a new perspective on ecological changes in the deglacial Southern Ocean, including multifaunal benthic assemblage (foraminifera and cold-water corals) and coral geochemical data (Ba/Ca and δ11B) from the Drake Passage. Our records show that, during the ACR, peak abundances of thick-walled benthic foraminifera Uvigerina bifurcata and corals are observed at shallow depths in the sub-Antarctic (?300 m), while coral populations at greater depths and further south diminished. Our ecological and geochemical data indicate that habitat shifts were dictated by (a) a northward migration of food supply (primary production) into the sub-Antarctic Zone and (b) poorly oxygenated seawater at depth during this Antarctic cooling interval. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Sea ice Southern Ocean University of Bristol: Bristol Research Antarctic Southern Ocean The Antarctic Drake Passage Paleoceanography and Paleoclimatology 36 10 |
institution |
Open Polar |
collection |
University of Bristol: Bristol Research |
op_collection_id |
ftubristolcris |
language |
English |
topic |
coral foraminifera Drake Passage deglacial |
spellingShingle |
coral foraminifera Drake Passage deglacial Stewart, Joseph A. Li, Tao Spooner, Peter T. Burke, Andrea Chen, Tianyu Roberts, Jenny Rae, James W. B. Peck, Victoria Kender, Sev Liu, Qian Robinson, Laura F. Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
topic_facet |
coral foraminifera Drake Passage deglacial |
description |
Abstract The Antarctic Cold Reversal (ACR; 14.7 to 13 thousand years ago; ka) phase of the last deglaciation saw a pause in the rise of atmospheric CO2 and Antarctic temperature, that contrasted with warming in the North. A reexpansion of sea ice and a northward shift in the position of the westerly winds in the Southern Ocean are well-documented, but the response of deep-sea biota and the primary drivers of habitat viability remain unclear. Here, we present a new perspective on ecological changes in the deglacial Southern Ocean, including multifaunal benthic assemblage (foraminifera and cold-water corals) and coral geochemical data (Ba/Ca and δ11B) from the Drake Passage. Our records show that, during the ACR, peak abundances of thick-walled benthic foraminifera Uvigerina bifurcata and corals are observed at shallow depths in the sub-Antarctic (?300 m), while coral populations at greater depths and further south diminished. Our ecological and geochemical data indicate that habitat shifts were dictated by (a) a northward migration of food supply (primary production) into the sub-Antarctic Zone and (b) poorly oxygenated seawater at depth during this Antarctic cooling interval. |
format |
Article in Journal/Newspaper |
author |
Stewart, Joseph A. Li, Tao Spooner, Peter T. Burke, Andrea Chen, Tianyu Roberts, Jenny Rae, James W. B. Peck, Victoria Kender, Sev Liu, Qian Robinson, Laura F. |
author_facet |
Stewart, Joseph A. Li, Tao Spooner, Peter T. Burke, Andrea Chen, Tianyu Roberts, Jenny Rae, James W. B. Peck, Victoria Kender, Sev Liu, Qian Robinson, Laura F. |
author_sort |
Stewart, Joseph A. |
title |
Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
title_short |
Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
title_full |
Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
title_fullStr |
Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
title_full_unstemmed |
Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal |
title_sort |
productivity and dissolved oxygen controls on the southern ocean deep-sea benthos during the antarctic cold reversal |
publishDate |
2021 |
url |
https://hdl.handle.net/1983/31d0240d-9520-4c20-91f9-9deab762f989 https://research-information.bris.ac.uk/en/publications/31d0240d-9520-4c20-91f9-9deab762f989 https://doi.org/10.1029/2021PA004288 https://research-information.bris.ac.uk/ws/files/299437688/Stewart_et_al._2021_ACR_PA004288.pdf |
geographic |
Antarctic Southern Ocean The Antarctic Drake Passage |
geographic_facet |
Antarctic Southern Ocean The Antarctic Drake Passage |
genre |
Antarc* Antarctic Drake Passage Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Drake Passage Sea ice Southern Ocean |
op_source |
Stewart , J A , Li , T , Spooner , P T , Burke , A , Chen , T , Roberts , J , Rae , J W B , Peck , V , Kender , S , Liu , Q & Robinson , L F 2021 , ' Productivity and Dissolved Oxygen Controls on the Southern Ocean Deep-Sea Benthos During the Antarctic Cold Reversal ' , Paleoceanography and Paleoclimatology , vol. 36 , no. 10 , e2021PA004288 . https://doi.org/10.1029/2021PA004288 |
op_relation |
https://research-information.bris.ac.uk/en/publications/31d0240d-9520-4c20-91f9-9deab762f989 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2021PA004288 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
36 |
container_issue |
10 |
_version_ |
1798836437782626304 |