Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2
The paleoproductivity in the Southern Ocean plays a crucial role in controlling the atmospheric CO2 concentration. Here, we present the sediment record of gravity core ANT37-C5/6-07, which was retrieved from the Cosmonaut Sea (CS), Indian Ocean sector of the Southern Ocean. We found that the change...
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ftdoajarticles:oai:doaj.org/article:4fa3260083e347dbbb5337f9527d7d6c 2023-11-12T04:06:26+01:00 Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 Liangming Hu Yi Zhang Yizhuo Wang Pengyun Ma Wendong Wu Qian Ge Yeping Bian Xibin Han 2023-10-01T00:00:00Z https://doi.org/10.3389/fmars.2023.1215048 https://doaj.org/article/4fa3260083e347dbbb5337f9527d7d6c EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/fmars.2023.1215048/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2023.1215048 https://doaj.org/article/4fa3260083e347dbbb5337f9527d7d6c Frontiers in Marine Science, Vol 10 (2023) paleoproductivity oxygenation last glacial maximum carbon cycling Cosmonaut Sea Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2023 ftdoajarticles https://doi.org/10.3389/fmars.2023.1215048 2023-10-22T00:42:45Z The paleoproductivity in the Southern Ocean plays a crucial role in controlling the atmospheric CO2 concentration. Here, we present the sediment record of gravity core ANT37-C5/6-07, which was retrieved from the Cosmonaut Sea (CS), Indian Ocean sector of the Southern Ocean. We found that the change in the oxygen concentration in the CS bottom water is strongly correlated with the atmospheric CO2 fluctuations since the Last Glacial Maximum (LGM). Based on the change in the export production, we reconstructed the evolution history of the deep-water ventilation/upwelling in the study area. During the LGM, a large amount of respiratory carbon was stored in the deep Southern Ocean due to the effect of the low export productivity and restricted ventilation. The oxygen concentration was also low at this time. Despite the increase in paleoproductivity, the biological pump efficiency remained at a low level during the Last Deglaciation. Vast quantities of CO2 were released into the atmosphere through enhanced upwelling. The recovery of ventilation during this period facilitated the supply of oxygen-rich surface water to the deep ocean. Moreover, signals were identified during the transitions between the Heinrich Stage 1 (HS1), Antarctic Cold Reverse (ACR), and Younger Drays (YD) periods. During the Holocene, the productivity increased overall, and the oxygen in the bottom water was consumed but still remained at a high level. This may have been caused by the enhanced ventilation and/or the prevalence of East Cosmonaut Polynya (ECP) near Cape Ann. Article in Journal/Newspaper Antarc* Antarctic Cosmonaut sea Southern Ocean Directory of Open Access Journals: DOAJ Articles Antarctic Cape Ann ENVELOPE(51.367,51.367,-66.167,-66.167) Indian Southern Ocean Frontiers in Marine Science 10 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
paleoproductivity oxygenation last glacial maximum carbon cycling Cosmonaut Sea Science Q General. Including nature conservation geographical distribution QH1-199.5 |
spellingShingle |
paleoproductivity oxygenation last glacial maximum carbon cycling Cosmonaut Sea Science Q General. Including nature conservation geographical distribution QH1-199.5 Liangming Hu Yi Zhang Yizhuo Wang Pengyun Ma Wendong Wu Qian Ge Yeping Bian Xibin Han Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
topic_facet |
paleoproductivity oxygenation last glacial maximum carbon cycling Cosmonaut Sea Science Q General. Including nature conservation geographical distribution QH1-199.5 |
description |
The paleoproductivity in the Southern Ocean plays a crucial role in controlling the atmospheric CO2 concentration. Here, we present the sediment record of gravity core ANT37-C5/6-07, which was retrieved from the Cosmonaut Sea (CS), Indian Ocean sector of the Southern Ocean. We found that the change in the oxygen concentration in the CS bottom water is strongly correlated with the atmospheric CO2 fluctuations since the Last Glacial Maximum (LGM). Based on the change in the export production, we reconstructed the evolution history of the deep-water ventilation/upwelling in the study area. During the LGM, a large amount of respiratory carbon was stored in the deep Southern Ocean due to the effect of the low export productivity and restricted ventilation. The oxygen concentration was also low at this time. Despite the increase in paleoproductivity, the biological pump efficiency remained at a low level during the Last Deglaciation. Vast quantities of CO2 were released into the atmosphere through enhanced upwelling. The recovery of ventilation during this period facilitated the supply of oxygen-rich surface water to the deep ocean. Moreover, signals were identified during the transitions between the Heinrich Stage 1 (HS1), Antarctic Cold Reverse (ACR), and Younger Drays (YD) periods. During the Holocene, the productivity increased overall, and the oxygen in the bottom water was consumed but still remained at a high level. This may have been caused by the enhanced ventilation and/or the prevalence of East Cosmonaut Polynya (ECP) near Cape Ann. |
format |
Article in Journal/Newspaper |
author |
Liangming Hu Yi Zhang Yizhuo Wang Pengyun Ma Wendong Wu Qian Ge Yeping Bian Xibin Han |
author_facet |
Liangming Hu Yi Zhang Yizhuo Wang Pengyun Ma Wendong Wu Qian Ge Yeping Bian Xibin Han |
author_sort |
Liangming Hu |
title |
Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
title_short |
Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
title_full |
Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
title_fullStr |
Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
title_full_unstemmed |
Paleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO2 |
title_sort |
paleoproductivity and deep-sea oxygenation in cosmonaut sea since the last glacial maximum: impact on atmospheric co2 |
publisher |
Frontiers Media S.A. |
publishDate |
2023 |
url |
https://doi.org/10.3389/fmars.2023.1215048 https://doaj.org/article/4fa3260083e347dbbb5337f9527d7d6c |
long_lat |
ENVELOPE(51.367,51.367,-66.167,-66.167) |
geographic |
Antarctic Cape Ann Indian Southern Ocean |
geographic_facet |
Antarctic Cape Ann Indian Southern Ocean |
genre |
Antarc* Antarctic Cosmonaut sea Southern Ocean |
genre_facet |
Antarc* Antarctic Cosmonaut sea Southern Ocean |
op_source |
Frontiers in Marine Science, Vol 10 (2023) |
op_relation |
https://www.frontiersin.org/articles/10.3389/fmars.2023.1215048/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2023.1215048 https://doaj.org/article/4fa3260083e347dbbb5337f9527d7d6c |
op_doi |
https://doi.org/10.3389/fmars.2023.1215048 |
container_title |
Frontiers in Marine Science |
container_volume |
10 |
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1782327537670553600 |