Water mass evolution of the Greenland Sea since late glacial times ...
Four sediment cores from the central and northern Greenland Sea basin, a crucial area for the renewal of North Atlantic deep water, were analyzed for planktic foraminiferal fauna, planktic and benthic stable oxygen and carbon iso- topes as well as ice-rafted debris to reconstruct the environ- mental...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2014
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.832368 https://doi.pangaea.de/10.1594/PANGAEA.832368 |
id |
ftdatacite:10.1594/pangaea.832368 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.832368 2023-12-31T10:07:17+01:00 Water mass evolution of the Greenland Sea since late glacial times ... Telesiński, Maciej Mateusz Spielhagen, Robert F Bauch, Henning A 2014 application/zip https://dx.doi.org/10.1594/pangaea.832368 https://doi.pangaea.de/10.1594/PANGAEA.832368 en eng PANGAEA https://dx.doi.org/10.5194/cp-10-123-2014 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Supplementary Publication Series of Datasets article Collection 2014 ftdatacite https://doi.org/10.1594/pangaea.83236810.5194/cp-10-123-2014 2023-12-01T11:07:06Z Four sediment cores from the central and northern Greenland Sea basin, a crucial area for the renewal of North Atlantic deep water, were analyzed for planktic foraminiferal fauna, planktic and benthic stable oxygen and carbon iso- topes as well as ice-rafted debris to reconstruct the environ- mental variability in the last 23 kyr. During the Last Glacial Maximum, the Greenland Sea was dominated by cold and sea-ice bearing surface water masses. Meltwater discharges from the surrounding ice sheets affected the area during the deglaciation, influencing the water mass circulation. During the Younger Dryas interval the last major freshwater event occurred in the region. The onset of the Holocene interglacial was marked by an increase in the advection of Atlantic Wa- ter and a rise in sea surface temperatures (SST). Although the thermal maximum was not reached simultaneously across the basin, benthic isotope data indicate that the rate of overturn- ing circulation reached a maximum in the central Greenland Sea ... : Supplement to: Telesiński, Maciej Mateusz; Spielhagen, Robert F; Bauch, Henning A (2014): Water mass evolution of the Greenland Sea since late glacial times. Climate of the Past, 10(1), 123-136 ... Article in Journal/Newspaper Greenland Greenland Sea North Atlantic Deep Water North Atlantic Sea ice DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
Four sediment cores from the central and northern Greenland Sea basin, a crucial area for the renewal of North Atlantic deep water, were analyzed for planktic foraminiferal fauna, planktic and benthic stable oxygen and carbon iso- topes as well as ice-rafted debris to reconstruct the environ- mental variability in the last 23 kyr. During the Last Glacial Maximum, the Greenland Sea was dominated by cold and sea-ice bearing surface water masses. Meltwater discharges from the surrounding ice sheets affected the area during the deglaciation, influencing the water mass circulation. During the Younger Dryas interval the last major freshwater event occurred in the region. The onset of the Holocene interglacial was marked by an increase in the advection of Atlantic Wa- ter and a rise in sea surface temperatures (SST). Although the thermal maximum was not reached simultaneously across the basin, benthic isotope data indicate that the rate of overturn- ing circulation reached a maximum in the central Greenland Sea ... : Supplement to: Telesiński, Maciej Mateusz; Spielhagen, Robert F; Bauch, Henning A (2014): Water mass evolution of the Greenland Sea since late glacial times. Climate of the Past, 10(1), 123-136 ... |
format |
Article in Journal/Newspaper |
author |
Telesiński, Maciej Mateusz Spielhagen, Robert F Bauch, Henning A |
spellingShingle |
Telesiński, Maciej Mateusz Spielhagen, Robert F Bauch, Henning A Water mass evolution of the Greenland Sea since late glacial times ... |
author_facet |
Telesiński, Maciej Mateusz Spielhagen, Robert F Bauch, Henning A |
author_sort |
Telesiński, Maciej Mateusz |
title |
Water mass evolution of the Greenland Sea since late glacial times ... |
title_short |
Water mass evolution of the Greenland Sea since late glacial times ... |
title_full |
Water mass evolution of the Greenland Sea since late glacial times ... |
title_fullStr |
Water mass evolution of the Greenland Sea since late glacial times ... |
title_full_unstemmed |
Water mass evolution of the Greenland Sea since late glacial times ... |
title_sort |
water mass evolution of the greenland sea since late glacial times ... |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.832368 https://doi.pangaea.de/10.1594/PANGAEA.832368 |
genre |
Greenland Greenland Sea North Atlantic Deep Water North Atlantic Sea ice |
genre_facet |
Greenland Greenland Sea North Atlantic Deep Water North Atlantic Sea ice |
op_relation |
https://dx.doi.org/10.5194/cp-10-123-2014 |
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.83236810.5194/cp-10-123-2014 |
_version_ |
1786839597561413632 |