Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes
Sea-surface conditions in northeastern Fram Strait since the last glacial maximum (LGM) were reconstructed from cores MSM5/5-712-2 and PS2863/1-2 based on palynological assemblages, ecological preferences of dinocysts and application of the modern analog technique. Dinocyst in LGM sediments are spar...
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Online Access: | https://oceanrep.geomar.de/id/eprint/44151/ https://oceanrep.geomar.de/id/eprint/44151/1/Falardeau.pdf https://doi.org/10.1016/j.quascirev.2018.06.030 |
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ftoceanrep:oai:oceanrep.geomar.de:44151 2023-05-15T15:13:59+02:00 Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes Falardeau, Jade de Vernal, Anne Spielhagen, Robert F. 2018-09-01 text https://oceanrep.geomar.de/id/eprint/44151/ https://oceanrep.geomar.de/id/eprint/44151/1/Falardeau.pdf https://doi.org/10.1016/j.quascirev.2018.06.030 en eng Elsevier https://oceanrep.geomar.de/id/eprint/44151/1/Falardeau.pdf Falardeau, J., de Vernal, A. and Spielhagen, R. F. (2018) Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes. Quaternary Science Reviews, 195 . pp. 133-152. DOI 10.1016/j.quascirev.2018.06.030 <https://doi.org/10.1016/j.quascirev.2018.06.030>. doi:10.1016/j.quascirev.2018.06.030 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2018 ftoceanrep https://doi.org/10.1016/j.quascirev.2018.06.030 2023-04-07T15:41:11Z Sea-surface conditions in northeastern Fram Strait since the last glacial maximum (LGM) were reconstructed from cores MSM5/5-712-2 and PS2863/1-2 based on palynological assemblages, ecological preferences of dinocysts and application of the modern analog technique. Dinocyst in LGM sediments are sparse, but their assemblages reflect mild summer conditions. Given the regional context and evidence from other tracers, the dinocyst assemblages of the LGM could relate to regional fluxes of dinocysts during exceptional mild summers. From 19 to 14.7 ka, dinocyst data suggest very cold conditions with extensive sea-ice cover, while abundant reworked palynomorphs indicate intense glacial erosion. An abrupt transition at 14.7-14.5 ka was marked by a peak in summer temperatures coinciding with a rapidly deposited sediment layer related to a regional meltwater plume event in western Svalbard. From 14.7 to 12.6 ka, large seasonal temperature contrasts with mild summers and cold winters together with low salinity indicate continuous melting of the Svalbard Barents Sea ice sheet fostered by warm climate. At 12.6 ka, the regional onset of the Younger Dryas was marked by cooling and increased salinity. On a regional scale, the 12.6-12 ka interval corresponds to an important transition involving enhanced circulation of Arctic waters around Svalbard and establishment of coastal fronts along its northern and western margins. Modern-like oceanic conditions with relatively high salinity and low seasonal temperature contrast developed at about 7.6 ka. Since then, a slight cooling is observed, especially in winter. This study offers a comprehensive picture of the deglacial phases in eastern Fram Strait with unique data on the sea-surface salinity, which controls surface water stratification and plays an important role in ocean circulation. Article in Journal/Newspaper Arctic Barents Sea Fram Strait Ice Sheet Sea ice Svalbard Svalbard-Barents Sea Ice sheet OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Barents Sea Svalbard Quaternary Science Reviews 195 133 152 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Sea-surface conditions in northeastern Fram Strait since the last glacial maximum (LGM) were reconstructed from cores MSM5/5-712-2 and PS2863/1-2 based on palynological assemblages, ecological preferences of dinocysts and application of the modern analog technique. Dinocyst in LGM sediments are sparse, but their assemblages reflect mild summer conditions. Given the regional context and evidence from other tracers, the dinocyst assemblages of the LGM could relate to regional fluxes of dinocysts during exceptional mild summers. From 19 to 14.7 ka, dinocyst data suggest very cold conditions with extensive sea-ice cover, while abundant reworked palynomorphs indicate intense glacial erosion. An abrupt transition at 14.7-14.5 ka was marked by a peak in summer temperatures coinciding with a rapidly deposited sediment layer related to a regional meltwater plume event in western Svalbard. From 14.7 to 12.6 ka, large seasonal temperature contrasts with mild summers and cold winters together with low salinity indicate continuous melting of the Svalbard Barents Sea ice sheet fostered by warm climate. At 12.6 ka, the regional onset of the Younger Dryas was marked by cooling and increased salinity. On a regional scale, the 12.6-12 ka interval corresponds to an important transition involving enhanced circulation of Arctic waters around Svalbard and establishment of coastal fronts along its northern and western margins. Modern-like oceanic conditions with relatively high salinity and low seasonal temperature contrast developed at about 7.6 ka. Since then, a slight cooling is observed, especially in winter. This study offers a comprehensive picture of the deglacial phases in eastern Fram Strait with unique data on the sea-surface salinity, which controls surface water stratification and plays an important role in ocean circulation. |
format |
Article in Journal/Newspaper |
author |
Falardeau, Jade de Vernal, Anne Spielhagen, Robert F. |
spellingShingle |
Falardeau, Jade de Vernal, Anne Spielhagen, Robert F. Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
author_facet |
Falardeau, Jade de Vernal, Anne Spielhagen, Robert F. |
author_sort |
Falardeau, Jade |
title |
Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
title_short |
Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
title_full |
Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
title_fullStr |
Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
title_full_unstemmed |
Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes |
title_sort |
paleoceanography of northeastern fram strait since the last glacial maximum: palynological evidence of large amplitude changes |
publisher |
Elsevier |
publishDate |
2018 |
url |
https://oceanrep.geomar.de/id/eprint/44151/ https://oceanrep.geomar.de/id/eprint/44151/1/Falardeau.pdf https://doi.org/10.1016/j.quascirev.2018.06.030 |
geographic |
Arctic Barents Sea Svalbard |
geographic_facet |
Arctic Barents Sea Svalbard |
genre |
Arctic Barents Sea Fram Strait Ice Sheet Sea ice Svalbard Svalbard-Barents Sea Ice sheet |
genre_facet |
Arctic Barents Sea Fram Strait Ice Sheet Sea ice Svalbard Svalbard-Barents Sea Ice sheet |
op_relation |
https://oceanrep.geomar.de/id/eprint/44151/1/Falardeau.pdf Falardeau, J., de Vernal, A. and Spielhagen, R. F. (2018) Paleoceanography of northeastern Fram Strait since the last glacial maximum: Palynological evidence of large amplitude changes. Quaternary Science Reviews, 195 . pp. 133-152. DOI 10.1016/j.quascirev.2018.06.030 <https://doi.org/10.1016/j.quascirev.2018.06.030>. doi:10.1016/j.quascirev.2018.06.030 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.quascirev.2018.06.030 |
container_title |
Quaternary Science Reviews |
container_volume |
195 |
container_start_page |
133 |
op_container_end_page |
152 |
_version_ |
1766344482491465728 |