Clay mineralogy of sediment cores from the Arctic Ocean ...

This study focuses on sedimentological investigations of sediment cores recovered during the international Arctic'91, expeditions with the German research ice breaker RV “Polarstern” to the European sector of the Arctic Ocean. Here, we deduce the last glacial/interglacial changes in transport m...

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Main Authors: Vogt, Christoph, Knies, Jochen
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.695350
https://doi.pangaea.de/10.1594/PANGAEA.695350
id ftdatacite:10.1594/pangaea.695350
record_format openpolar
spelling ftdatacite:10.1594/pangaea.695350 2024-09-15T17:53:12+00:00 Clay mineralogy of sediment cores from the Arctic Ocean ... Vogt, Christoph Knies, Jochen 2008 application/zip https://dx.doi.org/10.1594/pangaea.695350 https://doi.pangaea.de/10.1594/PANGAEA.695350 en eng PANGAEA https://dx.doi.org/10.1016/j.margeo.2008.01.006 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 MultiCorer Giant box corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2008 ftdatacite https://doi.org/10.1594/pangaea.69535010.1016/j.margeo.2008.01.006 2024-07-03T13:10:33Z This study focuses on sedimentological investigations of sediment cores recovered during the international Arctic'91, expeditions with the German research ice breaker RV “Polarstern” to the European sector of the Arctic Ocean. Here, we deduce the last glacial/interglacial changes in transport mechanism and sedimentation from the clay mineral group smectite. We choose the smectites as an example of how sediment mineralogy can be linked with particular source regions (the Kara and Laptev seas), distinct transport mechanism (sea ice and surface currents) and sedimentation processes. Smectite contents in Arctic sediments discussed for two time slices, including the Last Glacial Maximum (LGM), and the last deglaciation (Termination I), reveal the highest variability subsequent to the retreat of the Eurasian ice sheets. Our results show that smectite anomalies in the Eurasian Basin are associated with distinct meltwater pulses and occurred around 13.5-13.0 14C ka B.P. Compelling evidence is provided that these ... : Supplement to: Vogt, Christoph; Knies, Jochen (2008): Sediment dynamics in the Eurasian Arctic Ocean during the last deglaciation - The clay mineral group smectite perspective. Marine Geology, 250(3-4), 211-222 ... Article in Journal/Newspaper Arctic Ocean laptev Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic MultiCorer
Giant box corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle MultiCorer
Giant box corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Vogt, Christoph
Knies, Jochen
Clay mineralogy of sediment cores from the Arctic Ocean ...
topic_facet MultiCorer
Giant box corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description This study focuses on sedimentological investigations of sediment cores recovered during the international Arctic'91, expeditions with the German research ice breaker RV “Polarstern” to the European sector of the Arctic Ocean. Here, we deduce the last glacial/interglacial changes in transport mechanism and sedimentation from the clay mineral group smectite. We choose the smectites as an example of how sediment mineralogy can be linked with particular source regions (the Kara and Laptev seas), distinct transport mechanism (sea ice and surface currents) and sedimentation processes. Smectite contents in Arctic sediments discussed for two time slices, including the Last Glacial Maximum (LGM), and the last deglaciation (Termination I), reveal the highest variability subsequent to the retreat of the Eurasian ice sheets. Our results show that smectite anomalies in the Eurasian Basin are associated with distinct meltwater pulses and occurred around 13.5-13.0 14C ka B.P. Compelling evidence is provided that these ... : Supplement to: Vogt, Christoph; Knies, Jochen (2008): Sediment dynamics in the Eurasian Arctic Ocean during the last deglaciation - The clay mineral group smectite perspective. Marine Geology, 250(3-4), 211-222 ...
format Article in Journal/Newspaper
author Vogt, Christoph
Knies, Jochen
author_facet Vogt, Christoph
Knies, Jochen
author_sort Vogt, Christoph
title Clay mineralogy of sediment cores from the Arctic Ocean ...
title_short Clay mineralogy of sediment cores from the Arctic Ocean ...
title_full Clay mineralogy of sediment cores from the Arctic Ocean ...
title_fullStr Clay mineralogy of sediment cores from the Arctic Ocean ...
title_full_unstemmed Clay mineralogy of sediment cores from the Arctic Ocean ...
title_sort clay mineralogy of sediment cores from the arctic ocean ...
publisher PANGAEA
publishDate 2008
url https://dx.doi.org/10.1594/pangaea.695350
https://doi.pangaea.de/10.1594/PANGAEA.695350
genre Arctic Ocean
laptev
Sea ice
genre_facet Arctic Ocean
laptev
Sea ice
op_relation https://dx.doi.org/10.1016/j.margeo.2008.01.006
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.69535010.1016/j.margeo.2008.01.006
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