Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans
Highlights • Sub-Antarctic CO2 release contributed to early deglacial atmospheric CO2 rise. • No evidence for enhanced CO2 flux from the Sub-Antarctic during the Younger Dryas. • Large heterogeneity of CO2 flux from the Southern Ocean over the last 20 kyr. Over the last deglaciation there were two t...
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Online Access: | https://oceanrep.geomar.de/id/eprint/57270/ https://oceanrep.geomar.de/id/eprint/57270/1/Shuttleworth.pdf https://doi.org/10.1016/j.epsl.2020.116649 |
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ftoceanrep:oai:oceanrep.geomar.de:57270 2024-02-11T09:56:52+01:00 Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans Shuttleworth, R. Bostock, H.C. Chalk, T.B. Calvo, E. Jaccard, S.L. Pelejero, C. Martínez-García, A. Foster, G.L. 2021-01 text https://oceanrep.geomar.de/id/eprint/57270/ https://oceanrep.geomar.de/id/eprint/57270/1/Shuttleworth.pdf https://doi.org/10.1016/j.epsl.2020.116649 en eng Elsevier https://oceanrep.geomar.de/id/eprint/57270/1/Shuttleworth.pdf Shuttleworth, R., Bostock, H. C., Chalk, T. B., Calvo, E., Jaccard, S. L., Pelejero, C., Martínez-García, A. and Foster, G. L. (2021) Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans. Earth and Planetary Science Letters, 554 . Art.Nr. 116649. DOI 10.1016/j.epsl.2020.116649 <https://doi.org/10.1016/j.epsl.2020.116649>. doi:10.1016/j.epsl.2020.116649 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2021 ftoceanrep https://doi.org/10.1016/j.epsl.2020.116649 2024-01-15T00:26:12Z Highlights • Sub-Antarctic CO2 release contributed to early deglacial atmospheric CO2 rise. • No evidence for enhanced CO2 flux from the Sub-Antarctic during the Younger Dryas. • Large heterogeneity of CO2 flux from the Southern Ocean over the last 20 kyr. Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading hypotheses accounting for the increased accumulation of CO2 in the atmosphere at these times invoke deep ocean carbon being released from the Southern Ocean and an associated decline in the global efficiency of the biological carbon pump. Here we present new deglacial surface seawater pH and CO2sw records from the Sub-Antarctic regions of the Atlantic and Pacific oceans using boron isotopes measured on the planktic foraminifera Globigerina bulloides. These new data support the hypothesis that upwelling of carbon-rich water in the Sub-Antarctic occurred during Heinrich Stadial 1, and contributed to the initial increase in atmospheric CO2. The increase in CO2sw is coeval with a decline in biological productivity at both the Sub-Antarctic Atlantic and Pacific sites. However, there is no evidence for a significant outgassing of deep ocean carbon from the Sub-Antarctic during the rest of the deglacial, including the second period of atmospheric CO2 rise coeval with the Younger Dryas. This suggests that the second rapid increase in atmospheric CO2 is driven by processes operating elsewhere in the Southern Ocean, or another region. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Pacific Southern Ocean Earth and Planetary Science Letters 554 116649 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Highlights • Sub-Antarctic CO2 release contributed to early deglacial atmospheric CO2 rise. • No evidence for enhanced CO2 flux from the Sub-Antarctic during the Younger Dryas. • Large heterogeneity of CO2 flux from the Southern Ocean over the last 20 kyr. Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading hypotheses accounting for the increased accumulation of CO2 in the atmosphere at these times invoke deep ocean carbon being released from the Southern Ocean and an associated decline in the global efficiency of the biological carbon pump. Here we present new deglacial surface seawater pH and CO2sw records from the Sub-Antarctic regions of the Atlantic and Pacific oceans using boron isotopes measured on the planktic foraminifera Globigerina bulloides. These new data support the hypothesis that upwelling of carbon-rich water in the Sub-Antarctic occurred during Heinrich Stadial 1, and contributed to the initial increase in atmospheric CO2. The increase in CO2sw is coeval with a decline in biological productivity at both the Sub-Antarctic Atlantic and Pacific sites. However, there is no evidence for a significant outgassing of deep ocean carbon from the Sub-Antarctic during the rest of the deglacial, including the second period of atmospheric CO2 rise coeval with the Younger Dryas. This suggests that the second rapid increase in atmospheric CO2 is driven by processes operating elsewhere in the Southern Ocean, or another region. |
format |
Article in Journal/Newspaper |
author |
Shuttleworth, R. Bostock, H.C. Chalk, T.B. Calvo, E. Jaccard, S.L. Pelejero, C. Martínez-García, A. Foster, G.L. |
spellingShingle |
Shuttleworth, R. Bostock, H.C. Chalk, T.B. Calvo, E. Jaccard, S.L. Pelejero, C. Martínez-García, A. Foster, G.L. Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
author_facet |
Shuttleworth, R. Bostock, H.C. Chalk, T.B. Calvo, E. Jaccard, S.L. Pelejero, C. Martínez-García, A. Foster, G.L. |
author_sort |
Shuttleworth, R. |
title |
Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
title_short |
Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
title_full |
Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
title_fullStr |
Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
title_full_unstemmed |
Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans |
title_sort |
early deglacial co2 release from the sub-antarctic atlantic and pacific oceans |
publisher |
Elsevier |
publishDate |
2021 |
url |
https://oceanrep.geomar.de/id/eprint/57270/ https://oceanrep.geomar.de/id/eprint/57270/1/Shuttleworth.pdf https://doi.org/10.1016/j.epsl.2020.116649 |
geographic |
Antarctic Pacific Southern Ocean |
geographic_facet |
Antarctic Pacific Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_relation |
https://oceanrep.geomar.de/id/eprint/57270/1/Shuttleworth.pdf Shuttleworth, R., Bostock, H. C., Chalk, T. B., Calvo, E., Jaccard, S. L., Pelejero, C., Martínez-García, A. and Foster, G. L. (2021) Early deglacial CO2 release from the Sub-Antarctic Atlantic and Pacific oceans. Earth and Planetary Science Letters, 554 . Art.Nr. 116649. DOI 10.1016/j.epsl.2020.116649 <https://doi.org/10.1016/j.epsl.2020.116649>. doi:10.1016/j.epsl.2020.116649 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.epsl.2020.116649 |
container_title |
Earth and Planetary Science Letters |
container_volume |
554 |
container_start_page |
116649 |
_version_ |
1790606559272763392 |