Sedimentology of the Okhotsk Sea ...
On the basis of two sedimentary records from the central Sea of Okhotsk, we reconstruct the closely coupled glacial/interglacial changes in terrigenous flux, marine productivity, and sea ice coverage over the past 1.1 Myr. The correspondance of our sedimentary records to the China loess grain size r...
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Online Access: | https://dx.doi.org/10.1594/pangaea.742366 https://doi.pangaea.de/10.1594/PANGAEA.742366 |
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ftdatacite:10.1594/pangaea.742366 2024-09-15T18:28:36+00:00 Sedimentology of the Okhotsk Sea ... Nürnberg, Dirk Tiedemann, Ralf 2004 application/zip https://dx.doi.org/10.1594/pangaea.742366 https://doi.pangaea.de/10.1594/PANGAEA.742366 en eng PANGAEA https://dx.doi.org/10.1029/2004pa001023 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Giant piston corer LV28 MD122 Akademik M.A. Lavrentyev Marion Dufresne 1995 International Marine Global Change Study IMAGES Kurile-Okhotsk Sea Marine Experiment KOMEX article Collection Supplementary Publication Series of Datasets 2004 ftdatacite https://doi.org/10.1594/pangaea.74236610.1029/2004pa001023 2024-07-03T13:10:33Z On the basis of two sedimentary records from the central Sea of Okhotsk, we reconstruct the closely coupled glacial/interglacial changes in terrigenous flux, marine productivity, and sea ice coverage over the past 1.1 Myr. The correspondance of our sedimentary records to the China loess grain size record (China loess particle timescale, CHILOPARTS) suggests that environmental changes in both the Sea of Okhotsk area and in SE Asia were closely related via the Siberian atmospheric high-pressure cell. During full glacial times our records point to a strong Siberian High causing northerly wind directions, the extension of the sea ice cover, and a reduced Amur River discharge. Deglacial maxima of terrigenous flux were succeeded by or synchronous to high-productivity events. Marine productivity was strengthened during glacial terminations because of an effective nutrient utilization at times of enhanced water column stratification and high nutrient supply from fluvial runoff and sea ice thawing. During ... : Supplement to: Nürnberg, Dirk; Tiedemann, Ralf (2004): Environmental change in the Sea of Okhotsk during the last 1.1 million years. Paleoceanography, 19(4), PA4011 ... Article in Journal/Newspaper okhotsk sea Sea ice DataCite |
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English |
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Gravity corer Giant piston corer LV28 MD122 Akademik M.A. Lavrentyev Marion Dufresne 1995 International Marine Global Change Study IMAGES Kurile-Okhotsk Sea Marine Experiment KOMEX |
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Gravity corer Giant piston corer LV28 MD122 Akademik M.A. Lavrentyev Marion Dufresne 1995 International Marine Global Change Study IMAGES Kurile-Okhotsk Sea Marine Experiment KOMEX Nürnberg, Dirk Tiedemann, Ralf Sedimentology of the Okhotsk Sea ... |
topic_facet |
Gravity corer Giant piston corer LV28 MD122 Akademik M.A. Lavrentyev Marion Dufresne 1995 International Marine Global Change Study IMAGES Kurile-Okhotsk Sea Marine Experiment KOMEX |
description |
On the basis of two sedimentary records from the central Sea of Okhotsk, we reconstruct the closely coupled glacial/interglacial changes in terrigenous flux, marine productivity, and sea ice coverage over the past 1.1 Myr. The correspondance of our sedimentary records to the China loess grain size record (China loess particle timescale, CHILOPARTS) suggests that environmental changes in both the Sea of Okhotsk area and in SE Asia were closely related via the Siberian atmospheric high-pressure cell. During full glacial times our records point to a strong Siberian High causing northerly wind directions, the extension of the sea ice cover, and a reduced Amur River discharge. Deglacial maxima of terrigenous flux were succeeded by or synchronous to high-productivity events. Marine productivity was strengthened during glacial terminations because of an effective nutrient utilization at times of enhanced water column stratification and high nutrient supply from fluvial runoff and sea ice thawing. During ... : Supplement to: Nürnberg, Dirk; Tiedemann, Ralf (2004): Environmental change in the Sea of Okhotsk during the last 1.1 million years. Paleoceanography, 19(4), PA4011 ... |
format |
Article in Journal/Newspaper |
author |
Nürnberg, Dirk Tiedemann, Ralf |
author_facet |
Nürnberg, Dirk Tiedemann, Ralf |
author_sort |
Nürnberg, Dirk |
title |
Sedimentology of the Okhotsk Sea ... |
title_short |
Sedimentology of the Okhotsk Sea ... |
title_full |
Sedimentology of the Okhotsk Sea ... |
title_fullStr |
Sedimentology of the Okhotsk Sea ... |
title_full_unstemmed |
Sedimentology of the Okhotsk Sea ... |
title_sort |
sedimentology of the okhotsk sea ... |
publisher |
PANGAEA |
publishDate |
2004 |
url |
https://dx.doi.org/10.1594/pangaea.742366 https://doi.pangaea.de/10.1594/PANGAEA.742366 |
genre |
okhotsk sea Sea ice |
genre_facet |
okhotsk sea Sea ice |
op_relation |
https://dx.doi.org/10.1029/2004pa001023 |
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.74236610.1029/2004pa001023 |
_version_ |
1810470064530391040 |