Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay

Baffin Bay hosts the largest and most productive of the Arctic polynyas: the North Water (NOW). Despite its significance and active role in water mass formation, the history of the NOW beyond the observational era remains poorly known. We reconcile the previously unassessed relationship between long...

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Published in:Scientific Reports
Main Authors: Jackson, Rebecca, Kvorning, Anna Bang, Limoges, Audrey, Georgiadis, Eleanor, Olsen, Steffen M., Tallberg, Petra, Andersen, Thorbjorn J., Mikkelsen, Naja, Giraudeau, Jacques, Masse, Guillaume, Wacker, Lukas, Ribeiro, Sofia
Other Authors: Ecosystems and Environment Research Programme, Biosciences, Marine Ecosystems Research Group
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2021
Subjects:
Online Access:http://hdl.handle.net/10138/330945
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/330945 2024-01-07T09:41:27+01:00 Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay Jackson, Rebecca Kvorning, Anna Bang Limoges, Audrey Georgiadis, Eleanor Olsen, Steffen M. Tallberg, Petra Andersen, Thorbjorn J. Mikkelsen, Naja Giraudeau, Jacques Masse, Guillaume Wacker, Lukas Ribeiro, Sofia Ecosystems and Environment Research Programme Biosciences Marine Ecosystems Research Group 2021-06-14T13:45:01Z 17 application/pdf http://hdl.handle.net/10138/330945 eng eng Nature Publishing Group 10.1038/s41598-021-88517-9 We would like to thank the Network of Centres of Excellence, ArcticNet, Fondation Total, the French Agence Nationale de la Recherche ("GreenEdge" project) and crew of CCGS Amundsen on expeditions AMD15 and AMD16 for the collection and provision of the sediment cores. We thank Caroline Guilmette for carrying out the lipid biomarker analysis. This study was funded by the VILLUM Foundation, Denmark (grant VKR023454 to SR) and the ICE-ARC project from the European Union 7th Framework Programme, grant 603887. RJ is funded by the European Union's Horizon 2020 research and innovation programme under the Marie Skodowska-Curie grant agreement No. 846142. AL received financial support from NSERC-discovery grant (RGPIN-2018-03984). SMO has received funding from the National Centre for Climate Research (NCKF 2021) and from the European Union's Horizon 2020 research and innovation programme under grant agreement no. 727852. Jackson , R , Kvorning , A B , Limoges , A , Georgiadis , E , Olsen , S M , Tallberg , P , Andersen , T J , Mikkelsen , N , Giraudeau , J , Masse , G , Wacker , L & Ribeiro , S 2021 , ' Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay ' , Scientific Reports , vol. 11 , 10095 . https://doi.org/10.1038/s41598-021-88517-9 d85bd87e-1c2b-4019-89e8-0c7709bf5208 http://hdl.handle.net/10138/330945 000652602700004 cc_by openAccess info:eu-repo/semantics/openAccess NORTH WATER POLYNYA PALAEO SEA-ICE BENTHIC FORAMINIFERA NARES STRAIT BENTHONIC FORAMINIFERA DEEP-SEA GREENLAND SHELF ASSEMBLAGES STORFJORDEN 1171 Geosciences 1172 Environmental sciences Article publishedVersion 2021 ftunivhelsihelda 2023-12-14T00:08:32Z Baffin Bay hosts the largest and most productive of the Arctic polynyas: the North Water (NOW). Despite its significance and active role in water mass formation, the history of the NOW beyond the observational era remains poorly known. We reconcile the previously unassessed relationship between long-term NOW dynamics and ocean conditions by applying a multiproxy approach to two marine sediment cores from the region that, together, span the Holocene. Declining influence of Atlantic Water in the NOW is coeval with regional records that indicate the inception of a strong and recurrent polynya from similar to 4400 yrs BP, in line with Neoglacial cooling. During warmer Holocene intervals such as the Roman Warm Period, a weaker NOW is evident, and its reduced capacity to influence bottom ocean conditions facilitated northward penetration of Atlantic Water. Future warming in the Arctic may have negative consequences for this vital biological oasis, with the potential knock-on effect of warm water penetration further north and intensified melt of the marine-terminating glaciers that flank the coast of northwest Greenland. Peer reviewed Article in Journal/Newspaper Arctic Baffin Bay Baffin Bay Baffin Foraminifera* Greenland Nares strait Sea ice HELDA – University of Helsinki Open Repository Arctic Baffin Bay Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450) Scientific Reports 11 1
institution Open Polar
collection HELDA – University of Helsinki Open Repository
op_collection_id ftunivhelsihelda
language English
topic NORTH WATER POLYNYA
PALAEO SEA-ICE
BENTHIC FORAMINIFERA
NARES STRAIT
BENTHONIC FORAMINIFERA
DEEP-SEA
GREENLAND
SHELF
ASSEMBLAGES
STORFJORDEN
1171 Geosciences
1172 Environmental sciences
spellingShingle NORTH WATER POLYNYA
PALAEO SEA-ICE
BENTHIC FORAMINIFERA
NARES STRAIT
BENTHONIC FORAMINIFERA
DEEP-SEA
GREENLAND
SHELF
ASSEMBLAGES
STORFJORDEN
1171 Geosciences
1172 Environmental sciences
Jackson, Rebecca
Kvorning, Anna Bang
Limoges, Audrey
Georgiadis, Eleanor
Olsen, Steffen M.
Tallberg, Petra
Andersen, Thorbjorn J.
Mikkelsen, Naja
Giraudeau, Jacques
Masse, Guillaume
Wacker, Lukas
Ribeiro, Sofia
Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
topic_facet NORTH WATER POLYNYA
PALAEO SEA-ICE
BENTHIC FORAMINIFERA
NARES STRAIT
BENTHONIC FORAMINIFERA
DEEP-SEA
GREENLAND
SHELF
ASSEMBLAGES
STORFJORDEN
1171 Geosciences
1172 Environmental sciences
description Baffin Bay hosts the largest and most productive of the Arctic polynyas: the North Water (NOW). Despite its significance and active role in water mass formation, the history of the NOW beyond the observational era remains poorly known. We reconcile the previously unassessed relationship between long-term NOW dynamics and ocean conditions by applying a multiproxy approach to two marine sediment cores from the region that, together, span the Holocene. Declining influence of Atlantic Water in the NOW is coeval with regional records that indicate the inception of a strong and recurrent polynya from similar to 4400 yrs BP, in line with Neoglacial cooling. During warmer Holocene intervals such as the Roman Warm Period, a weaker NOW is evident, and its reduced capacity to influence bottom ocean conditions facilitated northward penetration of Atlantic Water. Future warming in the Arctic may have negative consequences for this vital biological oasis, with the potential knock-on effect of warm water penetration further north and intensified melt of the marine-terminating glaciers that flank the coast of northwest Greenland. Peer reviewed
author2 Ecosystems and Environment Research Programme
Biosciences
Marine Ecosystems Research Group
format Article in Journal/Newspaper
author Jackson, Rebecca
Kvorning, Anna Bang
Limoges, Audrey
Georgiadis, Eleanor
Olsen, Steffen M.
Tallberg, Petra
Andersen, Thorbjorn J.
Mikkelsen, Naja
Giraudeau, Jacques
Masse, Guillaume
Wacker, Lukas
Ribeiro, Sofia
author_facet Jackson, Rebecca
Kvorning, Anna Bang
Limoges, Audrey
Georgiadis, Eleanor
Olsen, Steffen M.
Tallberg, Petra
Andersen, Thorbjorn J.
Mikkelsen, Naja
Giraudeau, Jacques
Masse, Guillaume
Wacker, Lukas
Ribeiro, Sofia
author_sort Jackson, Rebecca
title Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
title_short Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
title_full Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
title_fullStr Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
title_full_unstemmed Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay
title_sort holocene polynya dynamics and their interaction with oceanic heat transport in northernmost baffin bay
publisher Nature Publishing Group
publishDate 2021
url http://hdl.handle.net/10138/330945
long_lat ENVELOPE(158.167,158.167,-81.450,-81.450)
geographic Arctic
Baffin Bay
Greenland
Nares
geographic_facet Arctic
Baffin Bay
Greenland
Nares
genre Arctic
Baffin Bay
Baffin Bay
Baffin
Foraminifera*
Greenland
Nares strait
Sea ice
genre_facet Arctic
Baffin Bay
Baffin Bay
Baffin
Foraminifera*
Greenland
Nares strait
Sea ice
op_relation 10.1038/s41598-021-88517-9
We would like to thank the Network of Centres of Excellence, ArcticNet, Fondation Total, the French Agence Nationale de la Recherche ("GreenEdge" project) and crew of CCGS Amundsen on expeditions AMD15 and AMD16 for the collection and provision of the sediment cores. We thank Caroline Guilmette for carrying out the lipid biomarker analysis. This study was funded by the VILLUM Foundation, Denmark (grant VKR023454 to SR) and the ICE-ARC project from the European Union 7th Framework Programme, grant 603887. RJ is funded by the European Union's Horizon 2020 research and innovation programme under the Marie Skodowska-Curie grant agreement No. 846142. AL received financial support from NSERC-discovery grant (RGPIN-2018-03984). SMO has received funding from the National Centre for Climate Research (NCKF 2021) and from the European Union's Horizon 2020 research and innovation programme under grant agreement no. 727852.
Jackson , R , Kvorning , A B , Limoges , A , Georgiadis , E , Olsen , S M , Tallberg , P , Andersen , T J , Mikkelsen , N , Giraudeau , J , Masse , G , Wacker , L & Ribeiro , S 2021 , ' Holocene polynya dynamics and their interaction with oceanic heat transport in northernmost Baffin Bay ' , Scientific Reports , vol. 11 , 10095 . https://doi.org/10.1038/s41598-021-88517-9
d85bd87e-1c2b-4019-89e8-0c7709bf5208
http://hdl.handle.net/10138/330945
000652602700004
op_rights cc_by
openAccess
info:eu-repo/semantics/openAccess
container_title Scientific Reports
container_volume 11
container_issue 1
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