Sea surface temperatures and UK37 of three sediment cores from the Arctic Ocean ...

Sediment proxy data from the Norwegian, Greenland, and Iceland seas (Nordic seas) are presented to evaluate surface water temperature (SST) differences between Holocene and Eemian times and to deduce from these data the particular mode of surface water circulation. Records from planktic foraminifera...

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Bibliographic Details
Main Authors: Bauch, Henning A, Erlenkeuser, Helmut, Fahl, Kirsten, Spielhagen, Robert F, Weinelt, Mara, Andruleit, Harald, Henrich, Rüdiger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1999
Subjects:
Kasten corer
Gravity corer Kiel type
M13/2
M7/5
ARK-II/5
Meteor 1986
Polarstern
Helmholtz Centre for Ocean Research Kiel GEOMAR
Quaternary Environment of the Eurasian North QUEEN
Arctic
Arctic Ocean
Greenland
Mara
Norwegian Sea
Foraminifera*
Fram Strait
Iceberg*
Iceland
Nordic Seas
Online Access:https://dx.doi.org/10.1594/pangaea.728295
https://doi.pangaea.de/10.1594/PANGAEA.728295
Description
Summary:Sediment proxy data from the Norwegian, Greenland, and Iceland seas (Nordic seas) are presented to evaluate surface water temperature (SST) differences between Holocene and Eemian times and to deduce from these data the particular mode of surface water circulation. Records from planktic foraminiferal assemblages, CaCO3 content, oxygen isotopes of foraminifera, and iceberg-rafted debris form the main basis of interpretation. All results indicate for the Eemian comparatively cooler northern Nordic seas than for the Holocene due to a reduction in the northwardly flow of Atlantic surface water towards Fram Strait and the Arctic Ocean. Therefore, the cold polar water flow from the Arctic Ocean was less influencial in the southwestern Nordic seas during this time. As can be further deduced from the Eemian data, slightly higher Eemian SSTs are interpreted for the western Iceland Sea compared to the Norwegian Sea (ca. south of 70°N). This Eemian situation is in contrast to the Holocene when the main mass of warmest ... : Supplement to: Bauch, Henning A; Erlenkeuser, Helmut; Fahl, Kirsten; Spielhagen, Robert F; Weinelt, Mara; Andruleit, Harald; Henrich, Rüdiger (1999): Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic and sub-Arctic regions. Palaeogeography, Palaeoclimatology, Palaeoecology, 145(1-3), 95-117 ...

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