Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation
For its greenhouse effects, atmospheric CO 2 can critically influence the global climate on millennial and centennial timescales. Pleistocene atmospheric CO 2 variations must involve changes in ocean storage of carbon, but the mechanisms and pathways of carbon transfer between the oceanic and atmosp...
Published in: | Nature Geoscience |
---|---|
Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2022
|
Subjects: | |
Online Access: | https://research-portal.st-andrews.ac.uk/en/publications/f126d5cd-7b1f-473e-a5ea-b023f4bb7e2a https://doi.org/10.1038/s41561-022-00910-9 |
id |
ftunstandrewcris:oai:research-portal.st-andrews.ac.uk:publications/f126d5cd-7b1f-473e-a5ea-b023f4bb7e2a |
---|---|
record_format |
openpolar |
spelling |
ftunstandrewcris:oai:research-portal.st-andrews.ac.uk:publications/f126d5cd-7b1f-473e-a5ea-b023f4bb7e2a 2024-10-13T14:01:46+00:00 Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation Yu, Jimin Oppo, Delia W. Jin, Zhangdong Lacerra, Matthew Ji, Xuan Umling, Natalie E. Lund, David C. McCave, Nick Menviel, Laurie Shao, Jun Xu, Chen 2022-04-01 https://research-portal.st-andrews.ac.uk/en/publications/f126d5cd-7b1f-473e-a5ea-b023f4bb7e2a https://doi.org/10.1038/s41561-022-00910-9 eng eng info:eu-repo/semantics/restrictedAccess Yu , J , Oppo , D W , Jin , Z , Lacerra , M , Ji , X , Umling , N E , Lund , D C , McCave , N , Menviel , L , Shao , J & Xu , C 2022 , ' Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation ' , Nature Geoscience , vol. 15 , no. 4 , pp. 293-299 . https://doi.org/10.1038/s41561-022-00910-9 article 2022 ftunstandrewcris https://doi.org/10.1038/s41561-022-00910-9 2024-09-26T14:11:27Z For its greenhouse effects, atmospheric CO 2 can critically influence the global climate on millennial and centennial timescales. Pleistocene atmospheric CO 2 variations must involve changes in ocean storage of carbon, but the mechanisms and pathways of carbon transfer between the oceanic and atmospheric reservoirs are poorly understood due, in part, to complications associated with interpretation of carbonate system proxy data. Here we employ a recently developed approach to reconstruct upper Atlantic air–sea CO 2 exchange signatures through the last deglaciation. Using this approach, proxy and model data each suggest that there was a net release of CO 2 via the Atlantic sector of the Southern Ocean during the early deglaciation, which probably contributed to the millennial-scale atmospheric CO 2 rise during Heinrich Stadial 1 at ~18.0–14.7 kyr ago. Moreover, our data reveal a previously unrecognized mechanism for the centennial-scale atmospheric CO 2 rise at the onset of the Bølling warming event around 14.7 kyr ago, namely, the expansion of Antarctic Intermediate Water, a water mass that is especially inefficient at sequestering atmospheric CO 2 . Our findings highlight the role of the Southern Ocean outgassing and intermediate water-mass production and volume variations in governing millennial- and centennial-timescale atmospheric CO 2 rises during the last deglaciation. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean University of St Andrews: Research Portal Antarctic Southern Ocean Nature Geoscience 15 4 293 299 |
institution |
Open Polar |
collection |
University of St Andrews: Research Portal |
op_collection_id |
ftunstandrewcris |
language |
English |
description |
For its greenhouse effects, atmospheric CO 2 can critically influence the global climate on millennial and centennial timescales. Pleistocene atmospheric CO 2 variations must involve changes in ocean storage of carbon, but the mechanisms and pathways of carbon transfer between the oceanic and atmospheric reservoirs are poorly understood due, in part, to complications associated with interpretation of carbonate system proxy data. Here we employ a recently developed approach to reconstruct upper Atlantic air–sea CO 2 exchange signatures through the last deglaciation. Using this approach, proxy and model data each suggest that there was a net release of CO 2 via the Atlantic sector of the Southern Ocean during the early deglaciation, which probably contributed to the millennial-scale atmospheric CO 2 rise during Heinrich Stadial 1 at ~18.0–14.7 kyr ago. Moreover, our data reveal a previously unrecognized mechanism for the centennial-scale atmospheric CO 2 rise at the onset of the Bølling warming event around 14.7 kyr ago, namely, the expansion of Antarctic Intermediate Water, a water mass that is especially inefficient at sequestering atmospheric CO 2 . Our findings highlight the role of the Southern Ocean outgassing and intermediate water-mass production and volume variations in governing millennial- and centennial-timescale atmospheric CO 2 rises during the last deglaciation. |
format |
Article in Journal/Newspaper |
author |
Yu, Jimin Oppo, Delia W. Jin, Zhangdong Lacerra, Matthew Ji, Xuan Umling, Natalie E. Lund, David C. McCave, Nick Menviel, Laurie Shao, Jun Xu, Chen |
spellingShingle |
Yu, Jimin Oppo, Delia W. Jin, Zhangdong Lacerra, Matthew Ji, Xuan Umling, Natalie E. Lund, David C. McCave, Nick Menviel, Laurie Shao, Jun Xu, Chen Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
author_facet |
Yu, Jimin Oppo, Delia W. Jin, Zhangdong Lacerra, Matthew Ji, Xuan Umling, Natalie E. Lund, David C. McCave, Nick Menviel, Laurie Shao, Jun Xu, Chen |
author_sort |
Yu, Jimin |
title |
Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
title_short |
Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
title_full |
Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
title_fullStr |
Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
title_full_unstemmed |
Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation |
title_sort |
millennial and centennial co 2 release from the southern ocean during the last deglaciation |
publishDate |
2022 |
url |
https://research-portal.st-andrews.ac.uk/en/publications/f126d5cd-7b1f-473e-a5ea-b023f4bb7e2a https://doi.org/10.1038/s41561-022-00910-9 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
Yu , J , Oppo , D W , Jin , Z , Lacerra , M , Ji , X , Umling , N E , Lund , D C , McCave , N , Menviel , L , Shao , J & Xu , C 2022 , ' Millennial and centennial CO 2 release from the Southern Ocean during the last deglaciation ' , Nature Geoscience , vol. 15 , no. 4 , pp. 293-299 . https://doi.org/10.1038/s41561-022-00910-9 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1038/s41561-022-00910-9 |
container_title |
Nature Geoscience |
container_volume |
15 |
container_issue |
4 |
container_start_page |
293 |
op_container_end_page |
299 |
_version_ |
1812812785259642880 |