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...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2008
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.695350 https://doi.pangaea.de/10.1594/PANGAEA.695350 |
_version_ | 1821804574916214784 |
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author | Vogt, Christoph Knies, Jochen |
author_facet | Vogt, Christoph Knies, Jochen |
author_sort | Vogt, Christoph |
collection | DataCite |
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 |
genre | Arctic Arctic Ocean laptev Sea ice |
genre_facet | Arctic Arctic Ocean laptev Sea ice |
geographic | Arctic Arctic Ocean Breaker |
geographic_facet | Arctic Arctic Ocean Breaker |
id | ftdatacite:10.1594/pangaea.695350 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-67.257,-67.257,-67.874,-67.874) |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.1594/pangaea.69535010.1016/j.margeo.2008.01.006 |
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 |
publishDate | 2008 |
publisher | PANGAEA |
record_format | openpolar |
spelling | ftdatacite:10.1594/pangaea.695350 2025-01-16T20:09:46+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 Arctic Ocean laptev Sea ice DataCite Arctic Arctic Ocean Breaker ENVELOPE(-67.257,-67.257,-67.874,-67.874) |
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 ... |
title | 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_short | Clay mineralogy of sediment cores from the Arctic Ocean ... |
title_sort | clay mineralogy of sediment cores from the arctic ocean ... |
topic | MultiCorer Giant box corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
topic_facet | MultiCorer Giant box corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
url | https://dx.doi.org/10.1594/pangaea.695350 https://doi.pangaea.de/10.1594/PANGAEA.695350 |