Holocene palaeoceanographic evolution off West Greenland ...
Benthic foraminiferal assemblages from a core southwest of Disko Bugt provide a Holocene perspective (last ~7 ka BP) on ice-sheet/ocean interactions between the West Greenland Current (WGC) and the West Greenland ice sheet. Changes in the fauna reveal significant variations in the water mass propert...
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Online Access: | https://dx.doi.org/10.1594/pangaea.898319 https://doi.pangaea.de/10.1594/PANGAEA.898319 |
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ftdatacite:10.1594/pangaea.898319 2024-09-15T18:03:44+00:00 Holocene palaeoceanographic evolution off West Greenland ... Perner, Kerstin Moros, Matthias Jennings, Anne E Lloyd, Jeremy M Knudsen, Karen Luise 2019 application/zip https://dx.doi.org/10.1594/pangaea.898319 https://doi.pangaea.de/10.1594/PANGAEA.898319 en eng PANGAEA https://dx.doi.org/10.1177/0959683612460785 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Benthic foraminifera EGC GREENClim Holocene IC ocean forcing WGC article Collection Supplementary Publication Series of Datasets 2019 ftdatacite https://doi.org/10.1594/pangaea.89831910.1177/0959683612460785 2024-08-01T10:53:32Z Benthic foraminiferal assemblages from a core southwest of Disko Bugt provide a Holocene perspective (last ~7 ka BP) on ice-sheet/ocean interactions between the West Greenland Current (WGC) and the West Greenland ice sheet. Changes in the fauna reveal significant variations in the water mass properties (temperature and salinity) of the WGC through time. From 7.3 to 6.2 ka BP, a relatively warm/strong WGC influences ice-sheet melt in Disko Bugt and causes enhanced meltwater production, resulting in low surface-water productivity. The most favourable oceanographic conditions occur from 5.5 to 3.5 ka BP, associated with 'thermal optimum-like' conditions, encompassing minimum ice sheet extent in the Disko Bugt area. These conditions are attributed to: (1) reduced meltwater influence as the ice sheet is land based and (2) enhanced contribution of warm/saline water masses from the Irminger Current to the WGC. The transition into the late Holocene (last ~3.5 ka BP) is characterized by a cooling of oceanographic ... : Supplement to: Perner, Kerstin; Moros, Matthias; Jennings, Anne E; Lloyd, Jeremy M; Knudsen, Karen Luise (2013): Holocene palaeoceanographic evolution off West Greenland. The Holocene, 23(3), 374-387 ... Article in Journal/Newspaper Disko bugt Greenland Ice Sheet DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Benthic foraminifera EGC GREENClim Holocene IC ocean forcing WGC |
spellingShingle |
Benthic foraminifera EGC GREENClim Holocene IC ocean forcing WGC Perner, Kerstin Moros, Matthias Jennings, Anne E Lloyd, Jeremy M Knudsen, Karen Luise Holocene palaeoceanographic evolution off West Greenland ... |
topic_facet |
Benthic foraminifera EGC GREENClim Holocene IC ocean forcing WGC |
description |
Benthic foraminiferal assemblages from a core southwest of Disko Bugt provide a Holocene perspective (last ~7 ka BP) on ice-sheet/ocean interactions between the West Greenland Current (WGC) and the West Greenland ice sheet. Changes in the fauna reveal significant variations in the water mass properties (temperature and salinity) of the WGC through time. From 7.3 to 6.2 ka BP, a relatively warm/strong WGC influences ice-sheet melt in Disko Bugt and causes enhanced meltwater production, resulting in low surface-water productivity. The most favourable oceanographic conditions occur from 5.5 to 3.5 ka BP, associated with 'thermal optimum-like' conditions, encompassing minimum ice sheet extent in the Disko Bugt area. These conditions are attributed to: (1) reduced meltwater influence as the ice sheet is land based and (2) enhanced contribution of warm/saline water masses from the Irminger Current to the WGC. The transition into the late Holocene (last ~3.5 ka BP) is characterized by a cooling of oceanographic ... : Supplement to: Perner, Kerstin; Moros, Matthias; Jennings, Anne E; Lloyd, Jeremy M; Knudsen, Karen Luise (2013): Holocene palaeoceanographic evolution off West Greenland. The Holocene, 23(3), 374-387 ... |
format |
Article in Journal/Newspaper |
author |
Perner, Kerstin Moros, Matthias Jennings, Anne E Lloyd, Jeremy M Knudsen, Karen Luise |
author_facet |
Perner, Kerstin Moros, Matthias Jennings, Anne E Lloyd, Jeremy M Knudsen, Karen Luise |
author_sort |
Perner, Kerstin |
title |
Holocene palaeoceanographic evolution off West Greenland ... |
title_short |
Holocene palaeoceanographic evolution off West Greenland ... |
title_full |
Holocene palaeoceanographic evolution off West Greenland ... |
title_fullStr |
Holocene palaeoceanographic evolution off West Greenland ... |
title_full_unstemmed |
Holocene palaeoceanographic evolution off West Greenland ... |
title_sort |
holocene palaeoceanographic evolution off west greenland ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.898319 https://doi.pangaea.de/10.1594/PANGAEA.898319 |
genre |
Disko bugt Greenland Ice Sheet |
genre_facet |
Disko bugt Greenland Ice Sheet |
op_relation |
https://dx.doi.org/10.1177/0959683612460785 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.89831910.1177/0959683612460785 |
_version_ |
1810441218827485184 |