Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming
The role of the Southern Ocean in releasing CO2 (sequestered in the global ocean during the Last Glacial Maximum) into the atmosphere during deglaciation is an important topic for investigation of Earth's climate. Changes in global deep water circulation associated with upwelling of Circumpolar...
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ftarchimer:oai:archimer.ifremer.fr:76046 2023-05-15T13:47:36+02:00 Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming Gorbarenko, Sergey A. Shi, Xuefa Liu, Yanguang Zou, Jianjun Psheneva, Olga Yu. Bosin, Aleksandr A. Kirichenko, Ivan S. Artemova, Antonina V. Yanchenko, Elena A. Vasilenko, Yuriy P. 2020-12 application/pdf https://archimer.ifremer.fr/doc/00648/76046/76988.pdf https://doi.org/10.1016/j.gloplacha.2020.103315 https://archimer.ifremer.fr/doc/00648/76046/ eng eng Elsevier BV https://archimer.ifremer.fr/doc/00648/76046/76988.pdf doi:10.1016/j.gloplacha.2020.103315 https://archimer.ifremer.fr/doc/00648/76046/ info:eu-repo/semantics/openAccess restricted use Global And Planetary Change (0921-8181) (Elsevier BV), 2020-12 , Vol. 195 , P. 103315 (15p.) Productivity Sea ice condition Deep water ventilation Oxygen and carbon isotope ratio Stratigraphy Benthic foraminifera text Publication info:eu-repo/semantics/article 2020 ftarchimer https://doi.org/10.1016/j.gloplacha.2020.103315 2021-09-23T20:35:51Z The role of the Southern Ocean in releasing CO2 (sequestered in the global ocean during the Last Glacial Maximum) into the atmosphere during deglaciation is an important topic for investigation of Earth's climate. Changes in global deep water circulation associated with upwelling of Circumpolar Deep Water (CDW) around Antarctica may have played a part in the CO2 release, but remain poorly studied. The potential response of the Pacific Ocean, including the North Pacific, to upwelling of CDW with its vast reservoir of CO2 remains unresolved. Here we combine productivity proxies, oxygen and carbon isotope values in benthic and planktic foraminifera, data on the occurrence and abundance of ice-rafted debris, and benthic foraminiferal species composition in three sediment cores with published data for three cores from the Northern Emperor Rise for the Last Glacial Maximum, deglaciation and Holocene in order to elucidate the North Pacific role in CO2 redistribution in the past. Age models of the cores are based on radiocarbon data calibrated by 14C atmospheric plateau tuning. The calcium carbonate content in all cores increased abruptly around 14.5 ka, indicating an influx of relatively young water enriched in carbonate ion, oxygen and nutrients, and sourced in the Southern Oceans. A decrease in the extent of sea ice at the NER area during early deglaciation is reflected in sharp increases in the productivity of siliceous phytoplankton near the onset of Bølling/Allerød warming, possibly facilitated by the influx of Southern Ocean-sourced nutrient-rich waters. Article in Journal/Newspaper Antarc* Antarctica Sea ice Southern Ocean Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Ner ENVELOPE(6.622,6.622,62.612,62.612) Pacific Southern Ocean Global and Planetary Change 195 103315 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Productivity Sea ice condition Deep water ventilation Oxygen and carbon isotope ratio Stratigraphy Benthic foraminifera |
spellingShingle |
Productivity Sea ice condition Deep water ventilation Oxygen and carbon isotope ratio Stratigraphy Benthic foraminifera Gorbarenko, Sergey A. Shi, Xuefa Liu, Yanguang Zou, Jianjun Psheneva, Olga Yu. Bosin, Aleksandr A. Kirichenko, Ivan S. Artemova, Antonina V. Yanchenko, Elena A. Vasilenko, Yuriy P. Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
topic_facet |
Productivity Sea ice condition Deep water ventilation Oxygen and carbon isotope ratio Stratigraphy Benthic foraminifera |
description |
The role of the Southern Ocean in releasing CO2 (sequestered in the global ocean during the Last Glacial Maximum) into the atmosphere during deglaciation is an important topic for investigation of Earth's climate. Changes in global deep water circulation associated with upwelling of Circumpolar Deep Water (CDW) around Antarctica may have played a part in the CO2 release, but remain poorly studied. The potential response of the Pacific Ocean, including the North Pacific, to upwelling of CDW with its vast reservoir of CO2 remains unresolved. Here we combine productivity proxies, oxygen and carbon isotope values in benthic and planktic foraminifera, data on the occurrence and abundance of ice-rafted debris, and benthic foraminiferal species composition in three sediment cores with published data for three cores from the Northern Emperor Rise for the Last Glacial Maximum, deglaciation and Holocene in order to elucidate the North Pacific role in CO2 redistribution in the past. Age models of the cores are based on radiocarbon data calibrated by 14C atmospheric plateau tuning. The calcium carbonate content in all cores increased abruptly around 14.5 ka, indicating an influx of relatively young water enriched in carbonate ion, oxygen and nutrients, and sourced in the Southern Oceans. A decrease in the extent of sea ice at the NER area during early deglaciation is reflected in sharp increases in the productivity of siliceous phytoplankton near the onset of Bølling/Allerød warming, possibly facilitated by the influx of Southern Ocean-sourced nutrient-rich waters. |
format |
Article in Journal/Newspaper |
author |
Gorbarenko, Sergey A. Shi, Xuefa Liu, Yanguang Zou, Jianjun Psheneva, Olga Yu. Bosin, Aleksandr A. Kirichenko, Ivan S. Artemova, Antonina V. Yanchenko, Elena A. Vasilenko, Yuriy P. |
author_facet |
Gorbarenko, Sergey A. Shi, Xuefa Liu, Yanguang Zou, Jianjun Psheneva, Olga Yu. Bosin, Aleksandr A. Kirichenko, Ivan S. Artemova, Antonina V. Yanchenko, Elena A. Vasilenko, Yuriy P. |
author_sort |
Gorbarenko, Sergey A. |
title |
Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
title_short |
Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
title_full |
Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
title_fullStr |
Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
title_full_unstemmed |
Evidence of Southern Ocean influence into the far Northwest Pacific (Northern Emperor Rise) since the Bølling–Allerød warming |
title_sort |
evidence of southern ocean influence into the far northwest pacific (northern emperor rise) since the bølling–allerød warming |
publisher |
Elsevier BV |
publishDate |
2020 |
url |
https://archimer.ifremer.fr/doc/00648/76046/76988.pdf https://doi.org/10.1016/j.gloplacha.2020.103315 https://archimer.ifremer.fr/doc/00648/76046/ |
long_lat |
ENVELOPE(6.622,6.622,62.612,62.612) |
geographic |
Ner Pacific Southern Ocean |
geographic_facet |
Ner Pacific Southern Ocean |
genre |
Antarc* Antarctica Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctica Sea ice Southern Ocean |
op_source |
Global And Planetary Change (0921-8181) (Elsevier BV), 2020-12 , Vol. 195 , P. 103315 (15p.) |
op_relation |
https://archimer.ifremer.fr/doc/00648/76046/76988.pdf doi:10.1016/j.gloplacha.2020.103315 https://archimer.ifremer.fr/doc/00648/76046/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1016/j.gloplacha.2020.103315 |
container_title |
Global and Planetary Change |
container_volume |
195 |
container_start_page |
103315 |
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1766247520028065792 |