Physical properties of sediment cores from the Arctic Ocean ...
Sediments of the Arctic Ocean are recorders of oceanographic and climatic evolution in the northern hemisphere, The sedimentary history is reflected in the sediment physical properties, thus knowledge about them is a key to its Interpretation particularly within the Quaternary.In this study, 29 sedi...
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ftdatacite:10.1594/pangaea.871084 2024-09-15T17:53:05+00:00 Physical properties of sediment cores from the Arctic Ocean ... Bergmann, Uwe 2017 application/zip https://dx.doi.org/10.1594/pangaea.871084 https://doi.pangaea.de/10.1594/PANGAEA.871084 en eng PANGAEA https://dx.doi.org/10.2312/bzp_0183_1996 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Giant piston 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 2017 ftdatacite https://doi.org/10.1594/pangaea.87108410.2312/bzp_0183_1996 2024-07-03T13:11:36Z Sediments of the Arctic Ocean are recorders of oceanographic and climatic evolution in the northern hemisphere, The sedimentary history is reflected in the sediment physical properties, thus knowledge about them is a key to its Interpretation particularly within the Quaternary.In this study, 29 sediment cores from the eastern Arctic Ocean were investigated On porosity, wet bulk density and ten cores on compressional (P-) wave velocity. Analysis of these parameters permits interpretations about the sedimentary conditions in the Amundsen and Makarov Basins and on the Lomonosov Ridge, Yermak Plateau and Morris Jesup Rise.The distribution of 25 sediment cores throughout abyssal hill and abyssal plain locations of the eastern Arctic Ocean show specific distribution patterns of wet bulk densities and porosities which characterize the sedimentary regions. On the Yermak Plateau undisturbed pelagic sedimentation predominates. The Lomonosov Ridge and the Morris Jesup Rise are characterized by winnowing. On the Gakkel ... : Supplement to: Bergmann, Uwe (1996): Interpretation digitaler Parasound Echolotaufzeichnungen im östlichen Arktischen Ozean auf der Grundlage physikalischer Sedimenteigenschaften (Interpretation of digital Parasound echosounder records of the eastern Arctic Ocean on the basis of sediment physical properties). Berichte zur Polarforschung = Reports on Polar Research, 183, 164 pp ... Article in Journal/Newspaper Arctic Ocean Arktis* Lomonosov Ridge Yermak plateau DataCite |
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DataCite |
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ftdatacite |
language |
English |
topic |
Gravity corer Kiel type Giant piston corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Gravity corer Kiel type Giant piston corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN Bergmann, Uwe Physical properties of sediment cores from the Arctic Ocean ... |
topic_facet |
Gravity corer Kiel type Giant piston corer Kasten corer ARK-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Quaternary Environment of the Eurasian North QUEEN |
description |
Sediments of the Arctic Ocean are recorders of oceanographic and climatic evolution in the northern hemisphere, The sedimentary history is reflected in the sediment physical properties, thus knowledge about them is a key to its Interpretation particularly within the Quaternary.In this study, 29 sediment cores from the eastern Arctic Ocean were investigated On porosity, wet bulk density and ten cores on compressional (P-) wave velocity. Analysis of these parameters permits interpretations about the sedimentary conditions in the Amundsen and Makarov Basins and on the Lomonosov Ridge, Yermak Plateau and Morris Jesup Rise.The distribution of 25 sediment cores throughout abyssal hill and abyssal plain locations of the eastern Arctic Ocean show specific distribution patterns of wet bulk densities and porosities which characterize the sedimentary regions. On the Yermak Plateau undisturbed pelagic sedimentation predominates. The Lomonosov Ridge and the Morris Jesup Rise are characterized by winnowing. On the Gakkel ... : Supplement to: Bergmann, Uwe (1996): Interpretation digitaler Parasound Echolotaufzeichnungen im östlichen Arktischen Ozean auf der Grundlage physikalischer Sedimenteigenschaften (Interpretation of digital Parasound echosounder records of the eastern Arctic Ocean on the basis of sediment physical properties). Berichte zur Polarforschung = Reports on Polar Research, 183, 164 pp ... |
format |
Article in Journal/Newspaper |
author |
Bergmann, Uwe |
author_facet |
Bergmann, Uwe |
author_sort |
Bergmann, Uwe |
title |
Physical properties of sediment cores from the Arctic Ocean ... |
title_short |
Physical properties of sediment cores from the Arctic Ocean ... |
title_full |
Physical properties of sediment cores from the Arctic Ocean ... |
title_fullStr |
Physical properties of sediment cores from the Arctic Ocean ... |
title_full_unstemmed |
Physical properties of sediment cores from the Arctic Ocean ... |
title_sort |
physical properties of sediment cores from the arctic ocean ... |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.871084 https://doi.pangaea.de/10.1594/PANGAEA.871084 |
genre |
Arctic Ocean Arktis* Lomonosov Ridge Yermak plateau |
genre_facet |
Arctic Ocean Arktis* Lomonosov Ridge Yermak plateau |
op_relation |
https://dx.doi.org/10.2312/bzp_0183_1996 |
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.87108410.2312/bzp_0183_1996 |
_version_ |
1810295087117107200 |