Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...

The Kara Sea is an important area for paleo-climatic research since sea ice and brine formation take place on its shelf-two processes inducing supra-regional climatic implications and thereby connecting regional environmental variability with global climatic conditions. To gain information about pas...

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Main Authors: Hörner, Tanja, Stein, Ruediger, Fahl, Kirsten
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.887426
https://doi.pangaea.de/10.1594/PANGAEA.887426
id ftdatacite:10.1594/pangaea.887426
record_format openpolar
spelling ftdatacite:10.1594/pangaea.887426 2024-09-15T18:16:08+00:00 Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ... Hörner, Tanja Stein, Ruediger Fahl, Kirsten 2018 application/zip https://dx.doi.org/10.1594/pangaea.887426 https://doi.pangaea.de/10.1594/PANGAEA.887426 en eng PANGAEA https://dx.doi.org/10.1007/s41063-018-0040-4 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2018 ftdatacite https://doi.org/10.1594/pangaea.88742610.1007/s41063-018-0040-4 2024-08-01T10:54:59Z The Kara Sea is an important area for paleo-climatic research since sea ice and brine formation take place on its shelf-two processes inducing supra-regional climatic implications and thereby connecting regional environmental variability with global climatic conditions. To gain information about past sea ice coverage and variations, three sediment cores distributed in the southern and central parts of the marginal Sea were investigated. By applying the sea ice biomarker IP25 and the PIP25 index [phytoplankton biomarker (dinosterol)-IP25 index] post-glacial sea ice variability could be detected in the central Kara Sea (Core BP00-36/4), with most intense sea ice cover between 12.4 and 11.8 ka coinciding with the Younger Dryas (12.9-11.6 ka), and reduced sea ice cover between 10 and 8 ka during the Holocene Thermal Maximum. During the last ~7 ka, increasing sea ice indicators might indicate a Holocene cooling trend, probably induced by declining summer insolation. Furthermore, temporal changes in the fast ... : Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten (2018): Paleo-sea ice distribution and polynya variability on the Kara sea shelf during the last 12 ka. arktos - The Journal of Arctic Geosciences ... Article in Journal/Newspaper Kara Sea Phytoplankton Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
topic_facet Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The Kara Sea is an important area for paleo-climatic research since sea ice and brine formation take place on its shelf-two processes inducing supra-regional climatic implications and thereby connecting regional environmental variability with global climatic conditions. To gain information about past sea ice coverage and variations, three sediment cores distributed in the southern and central parts of the marginal Sea were investigated. By applying the sea ice biomarker IP25 and the PIP25 index [phytoplankton biomarker (dinosterol)-IP25 index] post-glacial sea ice variability could be detected in the central Kara Sea (Core BP00-36/4), with most intense sea ice cover between 12.4 and 11.8 ka coinciding with the Younger Dryas (12.9-11.6 ka), and reduced sea ice cover between 10 and 8 ka during the Holocene Thermal Maximum. During the last ~7 ka, increasing sea ice indicators might indicate a Holocene cooling trend, probably induced by declining summer insolation. Furthermore, temporal changes in the fast ... : Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten (2018): Paleo-sea ice distribution and polynya variability on the Kara sea shelf during the last 12 ka. arktos - The Journal of Arctic Geosciences ...
format Article in Journal/Newspaper
author Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
author_facet Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
author_sort Hörner, Tanja
title Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
title_short Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
title_full Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
title_fullStr Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
title_full_unstemmed Biomarker content and total organic carbon of sediment cores from the Kara Sea shelf ...
title_sort biomarker content and total organic carbon of sediment cores from the kara sea shelf ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.887426
https://doi.pangaea.de/10.1594/PANGAEA.887426
genre Kara Sea
Phytoplankton
Sea ice
genre_facet Kara Sea
Phytoplankton
Sea ice
op_relation https://dx.doi.org/10.1007/s41063-018-0040-4
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.88742610.1007/s41063-018-0040-4
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