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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Main Authors: Nürnberg, Dirk, Tiedemann, Ralf
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2004
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.742366
https://doi.pangaea.de/10.1594/PANGAEA.742366
id ftdatacite:10.1594/pangaea.742366
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic 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
spellingShingle 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
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