Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data
Abstract Planktonic foraminiferal evidence suggests that the ocean front systems between Polar and Atlantic surface waters in the Norwegian Sea generally were located closer to Greenland during Oxygen Isotope Substage 5e than in the Holocene. During both these periods oscillations have occurred in t...
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crwiley:10.1002/jqs.3390100408 2024-06-02T08:07:27+00:00 Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data Sejrup, Hans Petter Haflidason, Haflidi Kristensen, Dorthe Klitgaard Johnsen, Sigfus J. 1995 http://dx.doi.org/10.1002/jqs.3390100408 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390100408 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390100408 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 10, issue 4, page 385-390 ISSN 0267-8179 1099-1417 journal-article 1995 crwiley https://doi.org/10.1002/jqs.3390100408 2024-05-03T11:15:02Z Abstract Planktonic foraminiferal evidence suggests that the ocean front systems between Polar and Atlantic surface waters in the Norwegian Sea generally were located closer to Greenland during Oxygen Isotope Substage 5e than in the Holocene. During both these periods oscillations have occurred in the position of the fronts. In the western Norwegian Sea region, the substage 5e influence of warm Atlantic waters was interrupted by a return to polar conditions. These findings support both ice‐core data and evidence from Europe that the last interglacial was a period of rapid climatic shifts. Article in Journal/Newspaper Greenland ice core Norwegian Sea Wiley Online Library Greenland Norwegian Sea Journal of Quaternary Science 10 4 385 390 |
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Wiley Online Library |
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language |
English |
description |
Abstract Planktonic foraminiferal evidence suggests that the ocean front systems between Polar and Atlantic surface waters in the Norwegian Sea generally were located closer to Greenland during Oxygen Isotope Substage 5e than in the Holocene. During both these periods oscillations have occurred in the position of the fronts. In the western Norwegian Sea region, the substage 5e influence of warm Atlantic waters was interrupted by a return to polar conditions. These findings support both ice‐core data and evidence from Europe that the last interglacial was a period of rapid climatic shifts. |
format |
Article in Journal/Newspaper |
author |
Sejrup, Hans Petter Haflidason, Haflidi Kristensen, Dorthe Klitgaard Johnsen, Sigfus J. |
spellingShingle |
Sejrup, Hans Petter Haflidason, Haflidi Kristensen, Dorthe Klitgaard Johnsen, Sigfus J. Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
author_facet |
Sejrup, Hans Petter Haflidason, Haflidi Kristensen, Dorthe Klitgaard Johnsen, Sigfus J. |
author_sort |
Sejrup, Hans Petter |
title |
Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
title_short |
Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
title_full |
Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
title_fullStr |
Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
title_full_unstemmed |
Last interglacial and Holocene climatic development in the Norwegian Sea region: Ocean front movements and ice‐core data |
title_sort |
last interglacial and holocene climatic development in the norwegian sea region: ocean front movements and ice‐core data |
publisher |
Wiley |
publishDate |
1995 |
url |
http://dx.doi.org/10.1002/jqs.3390100408 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390100408 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390100408 |
geographic |
Greenland Norwegian Sea |
geographic_facet |
Greenland Norwegian Sea |
genre |
Greenland ice core Norwegian Sea |
genre_facet |
Greenland ice core Norwegian Sea |
op_source |
Journal of Quaternary Science volume 10, issue 4, page 385-390 ISSN 0267-8179 1099-1417 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jqs.3390100408 |
container_title |
Journal of Quaternary Science |
container_volume |
10 |
container_issue |
4 |
container_start_page |
385 |
op_container_end_page |
390 |
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1800752538528514048 |