Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years
It is widely assumed that the ventilation of the Southern Ocean played a crucial role in driving glacial‐interglacial atmospheric CO2‐levels. So far however, ventilation records from the Indian sector of the Southern Ocean, are widely missing. Here we present reconstructions of water residence times...
Published in: | Paleoceanography and Paleoclimatology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union (AGU)
2020
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00611/72351/71258.pdf https://archimer.ifremer.fr/doc/00611/72351/71259.jpg https://archimer.ifremer.fr/doc/00611/72351/71261.jpg https://archimer.ifremer.fr/doc/00611/72351/71262.jpg https://archimer.ifremer.fr/doc/00611/72351/71263.jpg https://archimer.ifremer.fr/doc/00611/72351/71264.jpg https://archimer.ifremer.fr/doc/00611/72351/71265.jpg https://archimer.ifremer.fr/doc/00611/72351/71266.pdf https://doi.org/10.1029/2019PA003733 https://archimer.ifremer.fr/doc/00611/72351/ |
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ftarchimer:oai:archimer.ifremer.fr:72351 |
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openpolar |
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 |
radiocarbon ventilation Southern Ocean Younger Dryas carbon cycle Indian Ocean |
spellingShingle |
radiocarbon ventilation Southern Ocean Younger Dryas carbon cycle Indian Ocean Ronge, Thomas A. Prange, M. Mollenhauer, Gesine Ellinghausen, Maret Kuhn, G. Tiedemann, R. Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
topic_facet |
radiocarbon ventilation Southern Ocean Younger Dryas carbon cycle Indian Ocean |
description |
It is widely assumed that the ventilation of the Southern Ocean played a crucial role in driving glacial‐interglacial atmospheric CO2‐levels. So far however, ventilation records from the Indian sector of the Southern Ocean, are widely missing. Here we present reconstructions of water residence times (depicted as ΔΔ14C and Δδ13C) for the last 32,000 years on sediment records from the Kerguelen Plateau and the Conrad Rise (~570‐2500 m water depth), along with simulated changes in ocean stratification from a transient climate model experiment. Our data indicate that Circumpolar Deep Waters in the Indian Ocean were part of the glacial carbon pool. At our sites, close to or bathed by upwelling deep‐waters, we find two pulses of decreasing ΔΔ14C and δ13C values (~21‐17ka; ~15‐12ka). Both transient pulses precede a similar pattern in downstream intermediate waters in the tropical Indian Ocean as well as rising atmospheric CO2 values. These findings suggest that 14C‐depleted, CO2‐rich Circumpolar Deep Water from the Indian Ocean contributed to the rise in atmospheric CO2 during HS1 and also the Younger Dryas, and that the southern Indian Ocean acted as a gateway for sequestered carbon to the atmosphere and tropical intermediate waters. Plain Language Summary By analyzing air bubbles trapped in glacial ice from Antarctica, we know the pattern of atmospheric CO2 for roughly the last 800,000 years. This record shows a distinctive pattern of warm interglacials with high values of atmospheric CO2 (~280 ppm) and cold glacials with CO2 as low as ~180 ppm. A leading hypothesis assumes that the CO2 that went “missing” from the atmosphere during the glacials was stored in the deep global ocean. Several studies suggest that during glacials, the main connection between the deep ocean and the surface/atmosphere – the Southern Ocean – was significantly interrupted or at least reduced. Until now, it was shown that the deglacial South Pacific, the Drake Passage, and the South Atlantic played a vital role in the release of the stored ... |
format |
Article in Journal/Newspaper |
author |
Ronge, Thomas A. Prange, M. Mollenhauer, Gesine Ellinghausen, Maret Kuhn, G. Tiedemann, R. |
author_facet |
Ronge, Thomas A. Prange, M. Mollenhauer, Gesine Ellinghausen, Maret Kuhn, G. Tiedemann, R. |
author_sort |
Ronge, Thomas A. |
title |
Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
title_short |
Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
title_full |
Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
title_fullStr |
Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
title_full_unstemmed |
Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years |
title_sort |
radiocarbon evidence for the contribution of the southern indian ocean to the evolution of atmospheric co 2 over the last 32,000 years |
publisher |
American Geophysical Union (AGU) |
publishDate |
2020 |
url |
https://archimer.ifremer.fr/doc/00611/72351/71258.pdf https://archimer.ifremer.fr/doc/00611/72351/71259.jpg https://archimer.ifremer.fr/doc/00611/72351/71261.jpg https://archimer.ifremer.fr/doc/00611/72351/71262.jpg https://archimer.ifremer.fr/doc/00611/72351/71263.jpg https://archimer.ifremer.fr/doc/00611/72351/71264.jpg https://archimer.ifremer.fr/doc/00611/72351/71265.jpg https://archimer.ifremer.fr/doc/00611/72351/71266.pdf https://doi.org/10.1029/2019PA003733 https://archimer.ifremer.fr/doc/00611/72351/ |
long_lat |
ENVELOPE(41.000,41.000,-53.000,-53.000) |
geographic |
Southern Ocean Kerguelen Drake Passage Pacific Indian Conrad Rise |
geographic_facet |
Southern Ocean Kerguelen Drake Passage Pacific Indian Conrad Rise |
genre |
Antarc* Antarctica Drake Passage Southern Ocean |
genre_facet |
Antarc* Antarctica Drake Passage Southern Ocean |
op_source |
Paleoceanography And Paleoclimatology (2572-4517) (American Geophysical Union (AGU)), 2020-03 , Vol. 35 , N. 3 , P. e2019PA003733 (16p.) |
op_relation |
https://archimer.ifremer.fr/doc/00611/72351/71258.pdf https://archimer.ifremer.fr/doc/00611/72351/71259.jpg https://archimer.ifremer.fr/doc/00611/72351/71261.jpg https://archimer.ifremer.fr/doc/00611/72351/71262.jpg https://archimer.ifremer.fr/doc/00611/72351/71263.jpg https://archimer.ifremer.fr/doc/00611/72351/71264.jpg https://archimer.ifremer.fr/doc/00611/72351/71265.jpg https://archimer.ifremer.fr/doc/00611/72351/71266.pdf doi:10.1029/2019PA003733 https://archimer.ifremer.fr/doc/00611/72351/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1029/2019PA003733 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
35 |
container_issue |
3 |
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1788057231394078720 |
spelling |
ftarchimer:oai:archimer.ifremer.fr:72351 2024-01-14T10:02:18+01:00 Radiocarbon Evidence for the Contribution of the Southern Indian Ocean to the Evolution of Atmospheric CO 2 over the last 32,000 years Ronge, Thomas A. Prange, M. Mollenhauer, Gesine Ellinghausen, Maret Kuhn, G. Tiedemann, R. 2020-03 application/pdf https://archimer.ifremer.fr/doc/00611/72351/71258.pdf https://archimer.ifremer.fr/doc/00611/72351/71259.jpg https://archimer.ifremer.fr/doc/00611/72351/71261.jpg https://archimer.ifremer.fr/doc/00611/72351/71262.jpg https://archimer.ifremer.fr/doc/00611/72351/71263.jpg https://archimer.ifremer.fr/doc/00611/72351/71264.jpg https://archimer.ifremer.fr/doc/00611/72351/71265.jpg https://archimer.ifremer.fr/doc/00611/72351/71266.pdf https://doi.org/10.1029/2019PA003733 https://archimer.ifremer.fr/doc/00611/72351/ eng eng American Geophysical Union (AGU) https://archimer.ifremer.fr/doc/00611/72351/71258.pdf https://archimer.ifremer.fr/doc/00611/72351/71259.jpg https://archimer.ifremer.fr/doc/00611/72351/71261.jpg https://archimer.ifremer.fr/doc/00611/72351/71262.jpg https://archimer.ifremer.fr/doc/00611/72351/71263.jpg https://archimer.ifremer.fr/doc/00611/72351/71264.jpg https://archimer.ifremer.fr/doc/00611/72351/71265.jpg https://archimer.ifremer.fr/doc/00611/72351/71266.pdf doi:10.1029/2019PA003733 https://archimer.ifremer.fr/doc/00611/72351/ info:eu-repo/semantics/openAccess restricted use Paleoceanography And Paleoclimatology (2572-4517) (American Geophysical Union (AGU)), 2020-03 , Vol. 35 , N. 3 , P. e2019PA003733 (16p.) radiocarbon ventilation Southern Ocean Younger Dryas carbon cycle Indian Ocean text Article info:eu-repo/semantics/article 2020 ftarchimer https://doi.org/10.1029/2019PA003733 2023-12-19T23:51:09Z It is widely assumed that the ventilation of the Southern Ocean played a crucial role in driving glacial‐interglacial atmospheric CO2‐levels. So far however, ventilation records from the Indian sector of the Southern Ocean, are widely missing. Here we present reconstructions of water residence times (depicted as ΔΔ14C and Δδ13C) for the last 32,000 years on sediment records from the Kerguelen Plateau and the Conrad Rise (~570‐2500 m water depth), along with simulated changes in ocean stratification from a transient climate model experiment. Our data indicate that Circumpolar Deep Waters in the Indian Ocean were part of the glacial carbon pool. At our sites, close to or bathed by upwelling deep‐waters, we find two pulses of decreasing ΔΔ14C and δ13C values (~21‐17ka; ~15‐12ka). Both transient pulses precede a similar pattern in downstream intermediate waters in the tropical Indian Ocean as well as rising atmospheric CO2 values. These findings suggest that 14C‐depleted, CO2‐rich Circumpolar Deep Water from the Indian Ocean contributed to the rise in atmospheric CO2 during HS1 and also the Younger Dryas, and that the southern Indian Ocean acted as a gateway for sequestered carbon to the atmosphere and tropical intermediate waters. Plain Language Summary By analyzing air bubbles trapped in glacial ice from Antarctica, we know the pattern of atmospheric CO2 for roughly the last 800,000 years. This record shows a distinctive pattern of warm interglacials with high values of atmospheric CO2 (~280 ppm) and cold glacials with CO2 as low as ~180 ppm. A leading hypothesis assumes that the CO2 that went “missing” from the atmosphere during the glacials was stored in the deep global ocean. Several studies suggest that during glacials, the main connection between the deep ocean and the surface/atmosphere – the Southern Ocean – was significantly interrupted or at least reduced. Until now, it was shown that the deglacial South Pacific, the Drake Passage, and the South Atlantic played a vital role in the release of the stored ... Article in Journal/Newspaper Antarc* Antarctica Drake Passage Southern Ocean Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Southern Ocean Kerguelen Drake Passage Pacific Indian Conrad Rise ENVELOPE(41.000,41.000,-53.000,-53.000) Paleoceanography and Paleoclimatology 35 3 |