Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka
In order to contribute to our understanding of the linkage between climate and ocean circulation we have studied benthic foraminifera from near the northern end of the Faeroe–Shetland Channel covering isotope stages 6 to lower stage 3 (∼150–55 ka). Our records demonstrate shifts between recurring as...
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crwiley:10.1046/j.1365-3121.1999.00226.x 2024-09-15T18:09:37+00:00 Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka Rasmussen, T.L. Balbon, E. Thomsen, E. Labeyrie, L. Van Weering, T.C.E. 1999 http://dx.doi.org/10.1046/j.1365-3121.1999.00226.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.1999.00226.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1999.00226.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Terra Nova volume 11, issue 2-3, page 61-66 ISSN 0954-4879 1365-3121 journal-article 1999 crwiley https://doi.org/10.1046/j.1365-3121.1999.00226.x 2024-07-25T04:23:06Z In order to contribute to our understanding of the linkage between climate and ocean circulation we have studied benthic foraminifera from near the northern end of the Faeroe–Shetland Channel covering isotope stages 6 to lower stage 3 (∼150–55 ka). Our records demonstrate shifts between recurring assemblages, which on millennial timescales monitor the outflow history of Norwegian Sea Deep Water. The records show that the outflow is closely linked to the climate of the region as documented in the Greenland ice cores. Outflow was relatively strong during all major warmer interstadials whereas there was no outflow during the colder stadials. During isotope substage 5e outflow was stable for ∼10–12 kyr with significant changes at the beginning and end only. Article in Journal/Newspaper Greenland Greenland ice cores Norwegian Sea Wiley Online Library Terra Nova 11 2-3 61 66 |
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Open Polar |
collection |
Wiley Online Library |
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crwiley |
language |
English |
description |
In order to contribute to our understanding of the linkage between climate and ocean circulation we have studied benthic foraminifera from near the northern end of the Faeroe–Shetland Channel covering isotope stages 6 to lower stage 3 (∼150–55 ka). Our records demonstrate shifts between recurring assemblages, which on millennial timescales monitor the outflow history of Norwegian Sea Deep Water. The records show that the outflow is closely linked to the climate of the region as documented in the Greenland ice cores. Outflow was relatively strong during all major warmer interstadials whereas there was no outflow during the colder stadials. During isotope substage 5e outflow was stable for ∼10–12 kyr with significant changes at the beginning and end only. |
format |
Article in Journal/Newspaper |
author |
Rasmussen, T.L. Balbon, E. Thomsen, E. Labeyrie, L. Van Weering, T.C.E. |
spellingShingle |
Rasmussen, T.L. Balbon, E. Thomsen, E. Labeyrie, L. Van Weering, T.C.E. Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
author_facet |
Rasmussen, T.L. Balbon, E. Thomsen, E. Labeyrie, L. Van Weering, T.C.E. |
author_sort |
Rasmussen, T.L. |
title |
Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
title_short |
Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
title_full |
Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
title_fullStr |
Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
title_full_unstemmed |
Climate records and changes in deep outflow from the Norwegian Sea ∼150–55 ka |
title_sort |
climate records and changes in deep outflow from the norwegian sea ∼150–55 ka |
publisher |
Wiley |
publishDate |
1999 |
url |
http://dx.doi.org/10.1046/j.1365-3121.1999.00226.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.1999.00226.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1999.00226.x |
genre |
Greenland Greenland ice cores Norwegian Sea |
genre_facet |
Greenland Greenland ice cores Norwegian Sea |
op_source |
Terra Nova volume 11, issue 2-3, page 61-66 ISSN 0954-4879 1365-3121 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1046/j.1365-3121.1999.00226.x |
container_title |
Terra Nova |
container_volume |
11 |
container_issue |
2-3 |
container_start_page |
61 |
op_container_end_page |
66 |
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1810447190223486976 |