Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation
Comparison of marine, lacustrine, and terrestrial records from twenty-four sites suggests the existence of a 'Younger Dryas'-type climate oscillation just prior to the Oxygen Isotope Stage 6/5e boundary. These records include results from biostratigraphic, pedostratigraphic, and speleothem...
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Online Access: | http://hdl.handle.net/2078.1/47120 https://doi.org/10.1016/0277-3791(95)00086-0 |
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ftunivlouvain:oai:dial.uclouvain.be:boreal:47120 2023-05-15T15:35:03+02:00 Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation Seidenkrantz, MS Bornmalm, L Johnsen, SJ Knudsen, KL Kuijpers, A Lauritzen, SE Leroy, SAG. Mergeai, I Schweger, C Vanvlietlanoe, B. UCL 1996 http://hdl.handle.net/2078.1/47120 https://doi.org/10.1016/0277-3791(95)00086-0 eng eng Pergamon-elsevier Science Ltd boreal:47120 http://hdl.handle.net/2078.1/47120 doi:10.1016/0277-3791(95)00086-0 urn:ISSN:0277-3791 urn:EISSN:1873-457X info:eu-repo/semantics/restrictedAccess Quaternary Science Reviews, Vol. 15, no. 1, p. 63-75 (1996) info:eu-repo/semantics/article 1996 ftunivlouvain https://doi.org/10.1016/0277-3791(95)00086-0 2022-08-11T23:22:50Z Comparison of marine, lacustrine, and terrestrial records from twenty-four sites suggests the existence of a 'Younger Dryas'-type climate oscillation just prior to the Oxygen Isotope Stage 6/5e boundary. These records include results from biostratigraphic, pedostratigraphic, and speleothem studies, as well as analyses of stable isotope compositions of marine records and ice cores. The climate oscillation is named after the warm Zeifen Interstadial and the cold Kattegat Stadial. The Zeifen Interstadial may be related to a major meltwater pulse in the Baffin Bay-Labrador Sea-Norwegian Sea region. The climate oscillation is presumably in part a result of a variation in ocean circulation, especially in the strength of the North Atlantic Drift, but changes in the atmospheric circulation also played an important role. The geographically widespread distribution of the oscillation suggests that the two-step deglaciation influenced both the northern and southern hemispheres. (C) 1996 Elsevier Science Ltd Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Labrador Sea North Atlantic Norwegian Sea DIAL@UCLouvain (Université catholique de Louvain) Baffin Bay Kattegat ENVELOPE(9.692,9.692,63.563,63.563) Norwegian Sea Quaternary Science Reviews 15 1 63 75 |
institution |
Open Polar |
collection |
DIAL@UCLouvain (Université catholique de Louvain) |
op_collection_id |
ftunivlouvain |
language |
English |
description |
Comparison of marine, lacustrine, and terrestrial records from twenty-four sites suggests the existence of a 'Younger Dryas'-type climate oscillation just prior to the Oxygen Isotope Stage 6/5e boundary. These records include results from biostratigraphic, pedostratigraphic, and speleothem studies, as well as analyses of stable isotope compositions of marine records and ice cores. The climate oscillation is named after the warm Zeifen Interstadial and the cold Kattegat Stadial. The Zeifen Interstadial may be related to a major meltwater pulse in the Baffin Bay-Labrador Sea-Norwegian Sea region. The climate oscillation is presumably in part a result of a variation in ocean circulation, especially in the strength of the North Atlantic Drift, but changes in the atmospheric circulation also played an important role. The geographically widespread distribution of the oscillation suggests that the two-step deglaciation influenced both the northern and southern hemispheres. (C) 1996 Elsevier Science Ltd |
author2 |
UCL |
format |
Article in Journal/Newspaper |
author |
Seidenkrantz, MS Bornmalm, L Johnsen, SJ Knudsen, KL Kuijpers, A Lauritzen, SE Leroy, SAG. Mergeai, I Schweger, C Vanvlietlanoe, B. |
spellingShingle |
Seidenkrantz, MS Bornmalm, L Johnsen, SJ Knudsen, KL Kuijpers, A Lauritzen, SE Leroy, SAG. Mergeai, I Schweger, C Vanvlietlanoe, B. Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
author_facet |
Seidenkrantz, MS Bornmalm, L Johnsen, SJ Knudsen, KL Kuijpers, A Lauritzen, SE Leroy, SAG. Mergeai, I Schweger, C Vanvlietlanoe, B. |
author_sort |
Seidenkrantz, MS |
title |
Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
title_short |
Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
title_full |
Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
title_fullStr |
Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
title_full_unstemmed |
Two-step deglaciation at the oxygen isotope stage 6/5e transition: The Zeifen-Kattegat climate oscillation |
title_sort |
two-step deglaciation at the oxygen isotope stage 6/5e transition: the zeifen-kattegat climate oscillation |
publisher |
Pergamon-elsevier Science Ltd |
publishDate |
1996 |
url |
http://hdl.handle.net/2078.1/47120 https://doi.org/10.1016/0277-3791(95)00086-0 |
long_lat |
ENVELOPE(9.692,9.692,63.563,63.563) |
geographic |
Baffin Bay Kattegat Norwegian Sea |
geographic_facet |
Baffin Bay Kattegat Norwegian Sea |
genre |
Baffin Bay Baffin Bay Baffin Labrador Sea North Atlantic Norwegian Sea |
genre_facet |
Baffin Bay Baffin Bay Baffin Labrador Sea North Atlantic Norwegian Sea |
op_source |
Quaternary Science Reviews, Vol. 15, no. 1, p. 63-75 (1996) |
op_relation |
boreal:47120 http://hdl.handle.net/2078.1/47120 doi:10.1016/0277-3791(95)00086-0 urn:ISSN:0277-3791 urn:EISSN:1873-457X |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/0277-3791(95)00086-0 |
container_title |
Quaternary Science Reviews |
container_volume |
15 |
container_issue |
1 |
container_start_page |
63 |
op_container_end_page |
75 |
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1766365350484508672 |