Oceanographic investiations from the Sea of Ochotsk ...

The Sea of Okhotsk is a marginal sea of the Pacific Ocean, which is characterized by strong variations in the productivity and sediment supply due to sea ice transport and river input. Furthermore the variations in the hydrological cycle determine the formation of the SOIW (Sea of Okhotsk Intermedia...

Full description

Bibliographic Details
Main Author: Kaiser, André
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.743860
https://doi.pangaea.de/10.1594/PANGAEA.743860
id ftdatacite:10.1594/pangaea.743860
record_format openpolar
spelling ftdatacite:10.1594/pangaea.743860 2024-09-15T18:28:37+00:00 Oceanographic investiations from the Sea of Ochotsk ... Kaiser, André 2010 application/zip https://dx.doi.org/10.1594/pangaea.743860 https://doi.pangaea.de/10.1594/PANGAEA.743860 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 MultiCorer Gravity corer Kiel type Gravity corer POI Gravity corer Kasten corer LV27/GREGORY LV28 OK92 Akademik M.A. Lavrentyev Akademik A Nesmeyanov Kurile-Okhotsk Sea Marine Experiment KOMEX article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.743860 2024-08-01T11:08:49Z The Sea of Okhotsk is a marginal sea of the Pacific Ocean, which is characterized by strong variations in the productivity and sediment supply due to sea ice transport and river input. Furthermore the variations in the hydrological cycle determine the formation of the SOIW (Sea of Okhotsk Intermediate Water) which plays an important role in the ventilation processes in the intermediate water of the N-Pacific. Isotope data measured on planktonic and benthic foraminifera, sedimentological and geochemical studies of sediment cores and surface samples from the Sea of Okhotsk are used to reconstruct the paleoceanography during the past 350.000 years. The dating and correlation of the sediments are based on oxygen isotope stratigraphy, absolute ages, magnetic susceptibility as well as a detailled tephrachronology of the entire basin. The sedimentation rates are characterized by temporal and spatial variations. The maximum sedimentation rate takes place at the continental slope off Sakhalin due to the input of the ... : Supplement to: Kaiser, André (2001): Ozeanographie, Produktivität und Meereisverbreitung im Ochotskischen Meer während der letzten ca. 350 ka. Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 114 pp ... Article in Journal/Newspaper okhotsk sea Sakhalin Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic MultiCorer
Gravity corer Kiel type
Gravity corer POI
Gravity corer
Kasten corer
LV27/GREGORY
LV28
OK92
Akademik M.A. Lavrentyev
Akademik A Nesmeyanov
Kurile-Okhotsk Sea Marine Experiment KOMEX
spellingShingle MultiCorer
Gravity corer Kiel type
Gravity corer POI
Gravity corer
Kasten corer
LV27/GREGORY
LV28
OK92
Akademik M.A. Lavrentyev
Akademik A Nesmeyanov
Kurile-Okhotsk Sea Marine Experiment KOMEX
Kaiser, André
Oceanographic investiations from the Sea of Ochotsk ...
topic_facet MultiCorer
Gravity corer Kiel type
Gravity corer POI
Gravity corer
Kasten corer
LV27/GREGORY
LV28
OK92
Akademik M.A. Lavrentyev
Akademik A Nesmeyanov
Kurile-Okhotsk Sea Marine Experiment KOMEX
description The Sea of Okhotsk is a marginal sea of the Pacific Ocean, which is characterized by strong variations in the productivity and sediment supply due to sea ice transport and river input. Furthermore the variations in the hydrological cycle determine the formation of the SOIW (Sea of Okhotsk Intermediate Water) which plays an important role in the ventilation processes in the intermediate water of the N-Pacific. Isotope data measured on planktonic and benthic foraminifera, sedimentological and geochemical studies of sediment cores and surface samples from the Sea of Okhotsk are used to reconstruct the paleoceanography during the past 350.000 years. The dating and correlation of the sediments are based on oxygen isotope stratigraphy, absolute ages, magnetic susceptibility as well as a detailled tephrachronology of the entire basin. The sedimentation rates are characterized by temporal and spatial variations. The maximum sedimentation rate takes place at the continental slope off Sakhalin due to the input of the ... : Supplement to: Kaiser, André (2001): Ozeanographie, Produktivität und Meereisverbreitung im Ochotskischen Meer während der letzten ca. 350 ka. Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 114 pp ...
format Article in Journal/Newspaper
author Kaiser, André
author_facet Kaiser, André
author_sort Kaiser, André
title Oceanographic investiations from the Sea of Ochotsk ...
title_short Oceanographic investiations from the Sea of Ochotsk ...
title_full Oceanographic investiations from the Sea of Ochotsk ...
title_fullStr Oceanographic investiations from the Sea of Ochotsk ...
title_full_unstemmed Oceanographic investiations from the Sea of Ochotsk ...
title_sort oceanographic investiations from the sea of ochotsk ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.743860
https://doi.pangaea.de/10.1594/PANGAEA.743860
genre okhotsk sea
Sakhalin
Sea ice
genre_facet okhotsk sea
Sakhalin
Sea ice
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.743860
_version_ 1810470080423657472