Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...

The Yermak Plateau is located north of Svalbard at the entrance to the Arctic Ocean, i.e. in an area highly sensitive to climate change. A multi proxy approach was carried out on Core PS92/039-2 to study glacial-interglacial environmental changes at the northern Barents Sea margin during the last 16...

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Main Authors: Kremer, Anne, Stein, Ruediger, Fahl, Kirsten
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.884795
https://doi.pangaea.de/10.1594/PANGAEA.884795
id ftdatacite:10.1594/pangaea.884795
record_format openpolar
spelling ftdatacite:10.1594/pangaea.884795 2024-09-15T17:53:59+00:00 Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ... Kremer, Anne Stein, Ruediger Fahl, Kirsten 2018 application/zip https://dx.doi.org/10.1594/pangaea.884795 https://doi.pangaea.de/10.1594/PANGAEA.884795 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2017.12.016 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Kasten corer PS92 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2018 ftdatacite https://doi.org/10.1594/pangaea.88479510.1016/j.quascirev.2017.12.016 2024-07-03T13:11:36Z The Yermak Plateau is located north of Svalbard at the entrance to the Arctic Ocean, i.e. in an area highly sensitive to climate change. A multi proxy approach was carried out on Core PS92/039-2 to study glacial-interglacial environmental changes at the northern Barents Sea margin during the last 160 ka. The main emphasis was on the reconstruction of sea ice cover, based on the sea ice proxy IP25 and the related phytoplankton - sea ice index PIP25. Sea ice was present most of the time but showed significant temporal variability decisively affected by movements of the Svalbard Barents Sea Ice Sheet. For the first time, we prove the occurrence of seasonal sea ice at the eastern Yermak Plateau during glacial intervals, probably steered by a major northward advance of the ice sheet and the formation of a coastal polynya in front of it. Maximum accumulation of terrigenous organic carbon, IP25 and the phytoplankton biomarkers (brassicasterol, dinosterol, HBI III) can be correlated to distinct deglaciation events. ... : Supplement to: Kremer, Anne; Stein, Ruediger; Fahl, Kirsten; Ji, Z; Yang, Z; Wiers, Steffen; Matthiessen, Jens; Forwick, Matthias; Löwemark, Ludvig; O'Regan, Matthew; Chen, Jiaming; Snowball, Ian (2018): Changes in sea ice cover and ice sheet extent at the Yermak Plateau during the last 160 ka - Reconstructions from biomarker records. Quaternary Science Reviews, 182, 93-108 ... Article in Journal/Newspaper Arctic Ocean Barents Sea Climate change Ice Sheet Phytoplankton Sea ice Svalbard Svalbard-Barents Sea Ice sheet Yermak plateau DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Kasten corer
PS92
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Kasten corer
PS92
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Kremer, Anne
Stein, Ruediger
Fahl, Kirsten
Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
topic_facet Kasten corer
PS92
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The Yermak Plateau is located north of Svalbard at the entrance to the Arctic Ocean, i.e. in an area highly sensitive to climate change. A multi proxy approach was carried out on Core PS92/039-2 to study glacial-interglacial environmental changes at the northern Barents Sea margin during the last 160 ka. The main emphasis was on the reconstruction of sea ice cover, based on the sea ice proxy IP25 and the related phytoplankton - sea ice index PIP25. Sea ice was present most of the time but showed significant temporal variability decisively affected by movements of the Svalbard Barents Sea Ice Sheet. For the first time, we prove the occurrence of seasonal sea ice at the eastern Yermak Plateau during glacial intervals, probably steered by a major northward advance of the ice sheet and the formation of a coastal polynya in front of it. Maximum accumulation of terrigenous organic carbon, IP25 and the phytoplankton biomarkers (brassicasterol, dinosterol, HBI III) can be correlated to distinct deglaciation events. ... : Supplement to: Kremer, Anne; Stein, Ruediger; Fahl, Kirsten; Ji, Z; Yang, Z; Wiers, Steffen; Matthiessen, Jens; Forwick, Matthias; Löwemark, Ludvig; O'Regan, Matthew; Chen, Jiaming; Snowball, Ian (2018): Changes in sea ice cover and ice sheet extent at the Yermak Plateau during the last 160 ka - Reconstructions from biomarker records. Quaternary Science Reviews, 182, 93-108 ...
format Article in Journal/Newspaper
author Kremer, Anne
Stein, Ruediger
Fahl, Kirsten
author_facet Kremer, Anne
Stein, Ruediger
Fahl, Kirsten
author_sort Kremer, Anne
title Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
title_short Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
title_full Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
title_fullStr Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
title_full_unstemmed Organic-geochemical bulk parameter and biomarker distribution of sediment core PS92/039-2 ...
title_sort organic-geochemical bulk parameter and biomarker distribution of sediment core ps92/039-2 ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.884795
https://doi.pangaea.de/10.1594/PANGAEA.884795
genre Arctic Ocean
Barents Sea
Climate change
Ice Sheet
Phytoplankton
Sea ice
Svalbard
Svalbard-Barents Sea Ice sheet
Yermak plateau
genre_facet Arctic Ocean
Barents Sea
Climate change
Ice Sheet
Phytoplankton
Sea ice
Svalbard
Svalbard-Barents Sea Ice sheet
Yermak plateau
op_relation https://dx.doi.org/10.1016/j.quascirev.2017.12.016
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.88479510.1016/j.quascirev.2017.12.016
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