Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period
The Fram Strait is the only deep gateway between the Arctic Ocean and the Nordic Seas and thus is a key area to study past changes in ocean circulation and the marine carbon cycle. Here, we study deep ocean temperature, δ18O, carbonate chemistry (i.e., carbonate ion concentration [CO3 2−]), and nutr...
Published in: | Paleoceanography and Paleoclimatology |
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American Geophysical Union
2021
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Online Access: | https://boris.unibe.ch/157943/1/Ezat_Deep_ocean_storage_of_heat_and_CO2_at_Fram_Strait__Paleoocean_Paleoclim_2021_.pdf https://boris.unibe.ch/157943/ |
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ftunivbern:oai:boris.unibe.ch:157943 2023-08-20T04:03:01+02:00 Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period Ezat, Mohamed M. Rasmussen, Tine L. Hain, Mathis P. Greaves, Mervyn Rae, James W. B. Zamelczyk, Katarzyna Marchitto, Thomas M. Szidat, Sönke Skinner, Luke C. 2021 application/pdf https://boris.unibe.ch/157943/1/Ezat_Deep_ocean_storage_of_heat_and_CO2_at_Fram_Strait__Paleoocean_Paleoclim_2021_.pdf https://boris.unibe.ch/157943/ eng eng American Geophysical Union https://boris.unibe.ch/157943/ info:eu-repo/semantics/openAccess Ezat, Mohamed M.; Rasmussen, Tine L.; Hain, Mathis P.; Greaves, Mervyn; Rae, James W. B.; Zamelczyk, Katarzyna; Marchitto, Thomas M.; Szidat, Sönke; Skinner, Luke C. (2021). Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period. Paleoceanography and paleoclimatology, 36(8) American Geophysical Union 10.1029/2021PA004216 <http://dx.doi.org/10.1029/2021PA004216> 540 Chemistry info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2021 ftunivbern https://doi.org/10.1029/2021PA004216 2023-07-31T22:07:53Z The Fram Strait is the only deep gateway between the Arctic Ocean and the Nordic Seas and thus is a key area to study past changes in ocean circulation and the marine carbon cycle. Here, we study deep ocean temperature, δ18O, carbonate chemistry (i.e., carbonate ion concentration [CO3 2−]), and nutrient content in the Fram Strait during the late glacial (35,000–19,000 years BP) and the Holocene based on benthic foraminiferal geochemistry and carbon cycle modeling. Our results indicate a thickening of Atlantic water penetrating into the northern Nordic Seas, forming a subsurface Atlantic intermediate water layer reaching to at least ∼2,600 m water depth during most of the late glacial period. The recirculating Atlantic layer was characterized by relatively high [CO3 2−] and low δ13C during the late glacial, and provides evidence for a Nordic Seas source to the glacial North Atlantic intermediate water flowing at 2,000–3,000 m water depth, most likely via the Denmark Strait. In addition, we discuss evidence for enhanced terrestrial carbon input to the Nordic Seas at ∼23.5 ka. Comparing our δ13C and qualitative [CO3 2−] records with results of carbon cycle box modeling suggests that the total terrestrial CO2 release during this carbon input event was low, slow, or directly to the atmosphere. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Denmark Strait Foraminifera* Fram Strait Nordic Seas North Atlantic BORIS (Bern Open Repository and Information System, University of Bern) Arctic Arctic Ocean Paleoceanography and Paleoclimatology 36 8 |
institution |
Open Polar |
collection |
BORIS (Bern Open Repository and Information System, University of Bern) |
op_collection_id |
ftunivbern |
language |
English |
topic |
540 Chemistry |
spellingShingle |
540 Chemistry Ezat, Mohamed M. Rasmussen, Tine L. Hain, Mathis P. Greaves, Mervyn Rae, James W. B. Zamelczyk, Katarzyna Marchitto, Thomas M. Szidat, Sönke Skinner, Luke C. Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
topic_facet |
540 Chemistry |
description |
The Fram Strait is the only deep gateway between the Arctic Ocean and the Nordic Seas and thus is a key area to study past changes in ocean circulation and the marine carbon cycle. Here, we study deep ocean temperature, δ18O, carbonate chemistry (i.e., carbonate ion concentration [CO3 2−]), and nutrient content in the Fram Strait during the late glacial (35,000–19,000 years BP) and the Holocene based on benthic foraminiferal geochemistry and carbon cycle modeling. Our results indicate a thickening of Atlantic water penetrating into the northern Nordic Seas, forming a subsurface Atlantic intermediate water layer reaching to at least ∼2,600 m water depth during most of the late glacial period. The recirculating Atlantic layer was characterized by relatively high [CO3 2−] and low δ13C during the late glacial, and provides evidence for a Nordic Seas source to the glacial North Atlantic intermediate water flowing at 2,000–3,000 m water depth, most likely via the Denmark Strait. In addition, we discuss evidence for enhanced terrestrial carbon input to the Nordic Seas at ∼23.5 ka. Comparing our δ13C and qualitative [CO3 2−] records with results of carbon cycle box modeling suggests that the total terrestrial CO2 release during this carbon input event was low, slow, or directly to the atmosphere. |
format |
Article in Journal/Newspaper |
author |
Ezat, Mohamed M. Rasmussen, Tine L. Hain, Mathis P. Greaves, Mervyn Rae, James W. B. Zamelczyk, Katarzyna Marchitto, Thomas M. Szidat, Sönke Skinner, Luke C. |
author_facet |
Ezat, Mohamed M. Rasmussen, Tine L. Hain, Mathis P. Greaves, Mervyn Rae, James W. B. Zamelczyk, Katarzyna Marchitto, Thomas M. Szidat, Sönke Skinner, Luke C. |
author_sort |
Ezat, Mohamed M. |
title |
Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
title_short |
Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
title_full |
Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
title_fullStr |
Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
title_full_unstemmed |
Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period |
title_sort |
deep ocean storage of heat and co2 in the fram strait, arctic ocean during the last glacial period |
publisher |
American Geophysical Union |
publishDate |
2021 |
url |
https://boris.unibe.ch/157943/1/Ezat_Deep_ocean_storage_of_heat_and_CO2_at_Fram_Strait__Paleoocean_Paleoclim_2021_.pdf https://boris.unibe.ch/157943/ |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Arctic Ocean Denmark Strait Foraminifera* Fram Strait Nordic Seas North Atlantic |
genre_facet |
Arctic Arctic Arctic Ocean Denmark Strait Foraminifera* Fram Strait Nordic Seas North Atlantic |
op_source |
Ezat, Mohamed M.; Rasmussen, Tine L.; Hain, Mathis P.; Greaves, Mervyn; Rae, James W. B.; Zamelczyk, Katarzyna; Marchitto, Thomas M.; Szidat, Sönke; Skinner, Luke C. (2021). Deep Ocean Storage of Heat and CO2 in the Fram Strait, Arctic Ocean During the Last Glacial Period. Paleoceanography and paleoclimatology, 36(8) American Geophysical Union 10.1029/2021PA004216 <http://dx.doi.org/10.1029/2021PA004216> |
op_relation |
https://boris.unibe.ch/157943/ |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2021PA004216 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
36 |
container_issue |
8 |
_version_ |
1774713498280919040 |