Sedimentology of three cores recovered off the northwest of Svalbard ...
Three cores recovered off the northwest of Svalbard were studied with respect to glacial/interglacial changes of clay and bulk mineralogy, lithology and organic geochemistry. The cores cover the Late Quaternary Marine Isotope Stages (MIS) 6-1 (ca. 170,000 years) and are located in the vicinity of th...
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ftdatacite:10.1594/pangaea.728244 2024-09-15T17:53:30+00:00 Sedimentology of three cores recovered off the northwest of Svalbard ... Vogt, Christoph Knies, Jochen Spielhagen, Robert F Stein, Ruediger 2001 application/zip https://dx.doi.org/10.1594/pangaea.728244 https://doi.pangaea.de/10.1594/PANGAEA.728244 en eng PANGAEA https://dx.doi.org/10.1016/s0921-8181(01)00111-4 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Gravity corer Kiel type Kasten corer ARK-VIII/2 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 2001 ftdatacite https://doi.org/10.1594/pangaea.72824410.1016/s0921-8181(01)00111-4 2024-07-03T13:10:33Z Three cores recovered off the northwest of Svalbard were studied with respect to glacial/interglacial changes of clay and bulk mineralogy, lithology and organic geochemistry. The cores cover the Late Quaternary Marine Isotope Stages (MIS) 6-1 (ca. 170,000 years) and are located in the vicinity of the Polar Front which separates the warm Atlantic water of the Westspitsbergen Current and the cold Polar Water of the Transpolar Drift. Globally driven changes in the paleoenvironment like the variable advection of warm Atlantic water into the Arctic Ocean can be distinguished from regional events by means of source mineral signatures and organic geochemistry data. In particular, a combination of high organic carbon and low carbonate contents, high C/N-ratios, a particular lithology and a distinct bulk and clay mineral assemblage can be related to Svalbard ice sheet developments between 23,000 and 19,500 14C years. This complex sediment pattern has been traced to the northwest of Spitsbergen as far north as 82°N. ... : Supplement to: Vogt, Christoph; Knies, Jochen; Spielhagen, Robert F; Stein, Ruediger (2001): Detailed mineralogical evidence for two nearly identical glacial/deglacial cycles and Atlantic Water advection to the Arctic Ocean during the last 90,000 years. Global and Planetary Change, QUEEN special issue, 31(1-4), 23-44 ... Article in Journal/Newspaper Arctic Ocean Ice Sheet Svalbard Spitsbergen DataCite |
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collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Giant box corer Gravity corer Kiel type Kasten corer ARK-VIII/2 ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Giant box corer Gravity corer Kiel type Kasten corer ARK-VIII/2 ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Vogt, Christoph Knies, Jochen Spielhagen, Robert F Stein, Ruediger Sedimentology of three cores recovered off the northwest of Svalbard ... |
topic_facet |
Giant box corer Gravity corer Kiel type Kasten corer ARK-VIII/2 ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
Three cores recovered off the northwest of Svalbard were studied with respect to glacial/interglacial changes of clay and bulk mineralogy, lithology and organic geochemistry. The cores cover the Late Quaternary Marine Isotope Stages (MIS) 6-1 (ca. 170,000 years) and are located in the vicinity of the Polar Front which separates the warm Atlantic water of the Westspitsbergen Current and the cold Polar Water of the Transpolar Drift. Globally driven changes in the paleoenvironment like the variable advection of warm Atlantic water into the Arctic Ocean can be distinguished from regional events by means of source mineral signatures and organic geochemistry data. In particular, a combination of high organic carbon and low carbonate contents, high C/N-ratios, a particular lithology and a distinct bulk and clay mineral assemblage can be related to Svalbard ice sheet developments between 23,000 and 19,500 14C years. This complex sediment pattern has been traced to the northwest of Spitsbergen as far north as 82°N. ... : Supplement to: Vogt, Christoph; Knies, Jochen; Spielhagen, Robert F; Stein, Ruediger (2001): Detailed mineralogical evidence for two nearly identical glacial/deglacial cycles and Atlantic Water advection to the Arctic Ocean during the last 90,000 years. Global and Planetary Change, QUEEN special issue, 31(1-4), 23-44 ... |
format |
Article in Journal/Newspaper |
author |
Vogt, Christoph Knies, Jochen Spielhagen, Robert F Stein, Ruediger |
author_facet |
Vogt, Christoph Knies, Jochen Spielhagen, Robert F Stein, Ruediger |
author_sort |
Vogt, Christoph |
title |
Sedimentology of three cores recovered off the northwest of Svalbard ... |
title_short |
Sedimentology of three cores recovered off the northwest of Svalbard ... |
title_full |
Sedimentology of three cores recovered off the northwest of Svalbard ... |
title_fullStr |
Sedimentology of three cores recovered off the northwest of Svalbard ... |
title_full_unstemmed |
Sedimentology of three cores recovered off the northwest of Svalbard ... |
title_sort |
sedimentology of three cores recovered off the northwest of svalbard ... |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://dx.doi.org/10.1594/pangaea.728244 https://doi.pangaea.de/10.1594/PANGAEA.728244 |
genre |
Arctic Ocean Ice Sheet Svalbard Spitsbergen |
genre_facet |
Arctic Ocean Ice Sheet Svalbard Spitsbergen |
op_relation |
https://dx.doi.org/10.1016/s0921-8181(01)00111-4 |
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.72824410.1016/s0921-8181(01)00111-4 |
_version_ |
1810429343294291968 |