Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ...
A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and paleoceanographic variability during the last ~9 ka in the eastern Fram Strait. Our multiproxy evidence suggests that the establishment of the modern oceanographic configuration in the eastern Fram St...
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Online Access: | https://dx.doi.org/10.1594/pangaea.810415 https://doi.pangaea.de/10.1594/PANGAEA.810415 |
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ftdatacite:10.1594/pangaea.810415 2023-10-01T03:54:08+02:00 Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... Werner, Kirstin Spielhagen, Robert F Bauch, Dorothea Hass, H Christian Kandiano, Evgenia S 2013 application/zip https://dx.doi.org/10.1594/pangaea.810415 https://doi.pangaea.de/10.1594/PANGAEA.810415 en eng PANGAEA https://dx.doi.org/10.1002/palo.20028 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Integrierte Analyse zwischeneiszeitlicher Klimadynamik INTERDYNAMIK Supplementary Publication Series of Datasets article Collection 2013 ftdatacite https://doi.org/10.1594/pangaea.81041510.1002/palo.20028 2023-09-04T14:52:34Z A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and paleoceanographic variability during the last ~9 ka in the eastern Fram Strait. Our multiproxy evidence suggests that the establishment of the modern oceanographic configuration in the eastern Fram Strait occurred stepwise, in response to the postglacial sea-level rise and the related onset of modern sea-ice production on the shallow Siberian shelves. The late Early and Mid Holocene interval (9 to 5 ka) was generally characterized by relatively unstable conditions. High abundance of the subpolar planktic foraminifer species Turborotalita quinqueloba implies strong intensity of Atlantic Water (AW) inflow with high productivity and/or high AW temperatures, resulting in a strong heat flux to the Arctic. A series of short-lived cooling events (8.2, 6.9. and 6.1 ka) occurred superimposed on the warm late Early and Mid Holocene conditions. Our proxy data imply that simultaneous to the complete postglacial flooding ... : Supplement to: Werner, Kirstin; Spielhagen, Robert F; Bauch, Dorothea; Hass, H Christian; Kandiano, Evgenia S (2013): Atlantic Water advection versus sea-ice advances in the eastern Fram Strait during the last 9 ka: Multiproxy evidence for a two-phase Holocene. Paleoceanography, 28(2), 283-295 ... Article in Journal/Newspaper Arctic Foraminifera* Fram Strait Sea ice Spitsbergen DataCite Metadata Store (German National Library of Science and Technology) Arctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Integrierte Analyse zwischeneiszeitlicher Klimadynamik INTERDYNAMIK |
spellingShingle |
Integrierte Analyse zwischeneiszeitlicher Klimadynamik INTERDYNAMIK Werner, Kirstin Spielhagen, Robert F Bauch, Dorothea Hass, H Christian Kandiano, Evgenia S Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
topic_facet |
Integrierte Analyse zwischeneiszeitlicher Klimadynamik INTERDYNAMIK |
description |
A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and paleoceanographic variability during the last ~9 ka in the eastern Fram Strait. Our multiproxy evidence suggests that the establishment of the modern oceanographic configuration in the eastern Fram Strait occurred stepwise, in response to the postglacial sea-level rise and the related onset of modern sea-ice production on the shallow Siberian shelves. The late Early and Mid Holocene interval (9 to 5 ka) was generally characterized by relatively unstable conditions. High abundance of the subpolar planktic foraminifer species Turborotalita quinqueloba implies strong intensity of Atlantic Water (AW) inflow with high productivity and/or high AW temperatures, resulting in a strong heat flux to the Arctic. A series of short-lived cooling events (8.2, 6.9. and 6.1 ka) occurred superimposed on the warm late Early and Mid Holocene conditions. Our proxy data imply that simultaneous to the complete postglacial flooding ... : Supplement to: Werner, Kirstin; Spielhagen, Robert F; Bauch, Dorothea; Hass, H Christian; Kandiano, Evgenia S (2013): Atlantic Water advection versus sea-ice advances in the eastern Fram Strait during the last 9 ka: Multiproxy evidence for a two-phase Holocene. Paleoceanography, 28(2), 283-295 ... |
format |
Article in Journal/Newspaper |
author |
Werner, Kirstin Spielhagen, Robert F Bauch, Dorothea Hass, H Christian Kandiano, Evgenia S |
author_facet |
Werner, Kirstin Spielhagen, Robert F Bauch, Dorothea Hass, H Christian Kandiano, Evgenia S |
author_sort |
Werner, Kirstin |
title |
Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
title_short |
Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
title_full |
Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
title_fullStr |
Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
title_full_unstemmed |
Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2 ... |
title_sort |
age determination, planktic foraminifera and stable istopes of sediment core msm05/5_712-2 ... |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://dx.doi.org/10.1594/pangaea.810415 https://doi.pangaea.de/10.1594/PANGAEA.810415 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Foraminifera* Fram Strait Sea ice Spitsbergen |
genre_facet |
Arctic Foraminifera* Fram Strait Sea ice Spitsbergen |
op_relation |
https://dx.doi.org/10.1002/palo.20028 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.81041510.1002/palo.20028 |
_version_ |
1778521490730254336 |