Organic geochemistry on sediment profiles from the Arctic Ocean ...
During the ARCTIC '91-Expedition with RV 'Polarstern', several Multicorer and Kastenlot-cores were recovered along a profile crossing the eastern part of the Arctic Ocean. The investigated cores consist mainly of clayey-silty sediments, and some units with a higher sand content. In th...
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ftdatacite:10.1594/pangaea.729809 2024-09-15T17:38:51+00:00 Organic geochemistry on sediment profiles from the Arctic Ocean ... Schubert, Carsten J 2009 application/zip https://dx.doi.org/10.1594/pangaea.729809 https://doi.pangaea.de/10.1594/PANGAEA.729809 en eng PANGAEA https://dx.doi.org/10.2312/bzp_0177_1995 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 MultiCorer Giant box corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.72980910.2312/bzp_0177_1995 2024-07-03T13:10:33Z During the ARCTIC '91-Expedition with RV 'Polarstern', several Multicorer and Kastenlot-cores were recovered along a profile crossing the eastern part of the Arctic Ocean. The investigated cores consist mainly of clayey-silty sediments, and some units with a higher sand content. In this thesis, detailed sedimentological and organic-geochemical investigations were performed. In part, the near surface sediments were AMS-14C dated making it possible to Interpret the results of the organic-geochemical investigations in terms of climatic changes (isotopic stage 2 to the Holocene). The more or less absence of foraminifers within the long cores prevented the development of an oxygen isotope stratigraphy. Only the results of core PS2174-5 from the Amundsen-Basin could be discussed in terms of the climatic change that could be dated back to oxygen isotope stage 7.Detailed organic-geochemical investigations in the central Arctic Ocean are rare. Therefore, several different organic-geochemical methods were used to ... : Supplement to: Schubert, Carsten J (1995): Organischer Kohlenstoff in spätquartären Sedimenten des Arktischen Ozeans: Terrigener Eintrag und marine Produktivität (Organic carbon in late Quaternary Arctic Ocean sediments: Terrigenous supply and marine productivity). Berichte zur Polarforschung = Reports on Polar Research, 177, 178 pp ... Article in Journal/Newspaper amundsen basin Arctic Ocean Arktis* DataCite |
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collection |
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op_collection_id |
ftdatacite |
language |
English |
topic |
MultiCorer Giant box corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
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MultiCorer Giant box corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Schubert, Carsten J Organic geochemistry on sediment profiles from the Arctic Ocean ... |
topic_facet |
MultiCorer Giant box corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
During the ARCTIC '91-Expedition with RV 'Polarstern', several Multicorer and Kastenlot-cores were recovered along a profile crossing the eastern part of the Arctic Ocean. The investigated cores consist mainly of clayey-silty sediments, and some units with a higher sand content. In this thesis, detailed sedimentological and organic-geochemical investigations were performed. In part, the near surface sediments were AMS-14C dated making it possible to Interpret the results of the organic-geochemical investigations in terms of climatic changes (isotopic stage 2 to the Holocene). The more or less absence of foraminifers within the long cores prevented the development of an oxygen isotope stratigraphy. Only the results of core PS2174-5 from the Amundsen-Basin could be discussed in terms of the climatic change that could be dated back to oxygen isotope stage 7.Detailed organic-geochemical investigations in the central Arctic Ocean are rare. Therefore, several different organic-geochemical methods were used to ... : Supplement to: Schubert, Carsten J (1995): Organischer Kohlenstoff in spätquartären Sedimenten des Arktischen Ozeans: Terrigener Eintrag und marine Produktivität (Organic carbon in late Quaternary Arctic Ocean sediments: Terrigenous supply and marine productivity). Berichte zur Polarforschung = Reports on Polar Research, 177, 178 pp ... |
format |
Article in Journal/Newspaper |
author |
Schubert, Carsten J |
author_facet |
Schubert, Carsten J |
author_sort |
Schubert, Carsten J |
title |
Organic geochemistry on sediment profiles from the Arctic Ocean ... |
title_short |
Organic geochemistry on sediment profiles from the Arctic Ocean ... |
title_full |
Organic geochemistry on sediment profiles from the Arctic Ocean ... |
title_fullStr |
Organic geochemistry on sediment profiles from the Arctic Ocean ... |
title_full_unstemmed |
Organic geochemistry on sediment profiles from the Arctic Ocean ... |
title_sort |
organic geochemistry on sediment profiles from the arctic ocean ... |
publisher |
PANGAEA |
publishDate |
2009 |
url |
https://dx.doi.org/10.1594/pangaea.729809 https://doi.pangaea.de/10.1594/PANGAEA.729809 |
genre |
amundsen basin Arctic Ocean Arktis* |
genre_facet |
amundsen basin Arctic Ocean Arktis* |
op_relation |
https://dx.doi.org/10.2312/bzp_0177_1995 |
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.72980910.2312/bzp_0177_1995 |
_version_ |
1810475727673360384 |