Ostracoda in surface sediments of the Arctic Ocean ...

Ostracodes were studied from deep Arctic Ocean cores obtained during the Arctic 91 expedition of the Polarstern to the Nansen, Amundsen and Makarov Basins, the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau, in order to investigate their distribution in Arctic Ocean deep water (AODW) and appl...

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Main Authors: Cronin, Thomas M, Holtz, Thomas R, Whatley, Robin C
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1994
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.728604
https://doi.pangaea.de/10.1594/PANGAEA.728604
id ftdatacite:10.1594/pangaea.728604
record_format openpolar
spelling ftdatacite:10.1594/pangaea.728604 2024-09-15T17:53:07+00:00 Ostracoda in surface sediments of the Arctic Ocean ... Cronin, Thomas M Holtz, Thomas R Whatley, Robin C 1994 application/zip https://dx.doi.org/10.1594/pangaea.728604 https://doi.pangaea.de/10.1594/PANGAEA.728604 en eng PANGAEA https://dx.doi.org/10.1016/0025-3227(94)90188-0 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box 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 1994 ftdatacite https://doi.org/10.1594/pangaea.72860410.1016/0025-3227(94)90188-0 2024-07-03T13:10:33Z Ostracodes were studied from deep Arctic Ocean cores obtained during the Arctic 91 expedition of the Polarstern to the Nansen, Amundsen and Makarov Basins, the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau, in order to investigate their distribution in Arctic Ocean deep water (AODW) and apply these data to paleoceanographic reconstruction of bottom water masses during the Quaternary. Analyses of coretop assemblages from Arctic 91 boxcores indicate the following: ostracodes are common at all depths between 1000 and 4500 m, and species distribution is strongly influenced by water mass characteristics and bathymetry; quantitative analyses comparing Eurasian and Canada Basin assemblages indicate that distinct assemblages inhabit regions east and west of the Lomonosov Ridge, a barrier especially important to species living in lower AODW; deep Eurasian Basin assemblages are more similar to those living in Greenland Sea deep water (GSDW) than those in Canada Basin deep water; two upper AODW assemblages were ... : Supplement to: Cronin, Thomas M; Holtz, Thomas R; Whatley, Robin C (1994): Quaternary paleoceanography of the deep Arctic Ocean based on quantitative analysis of Ostracoda. Marine Geology, 119(3-4), 305-332 ... Article in Journal/Newspaper Arctic Ocean canada basin Greenland Greenland Sea Lomonosov Ridge Yermak plateau DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Giant box corer
Kasten corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
spellingShingle Giant box corer
Kasten corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
Cronin, Thomas M
Holtz, Thomas R
Whatley, Robin C
Ostracoda in surface sediments of the Arctic Ocean ...
topic_facet Giant box corer
Kasten corer
ARK-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Quaternary Environment of the Eurasian North QUEEN
description Ostracodes were studied from deep Arctic Ocean cores obtained during the Arctic 91 expedition of the Polarstern to the Nansen, Amundsen and Makarov Basins, the Lomonosov Ridge, Morris Jesup Rise and Yermak Plateau, in order to investigate their distribution in Arctic Ocean deep water (AODW) and apply these data to paleoceanographic reconstruction of bottom water masses during the Quaternary. Analyses of coretop assemblages from Arctic 91 boxcores indicate the following: ostracodes are common at all depths between 1000 and 4500 m, and species distribution is strongly influenced by water mass characteristics and bathymetry; quantitative analyses comparing Eurasian and Canada Basin assemblages indicate that distinct assemblages inhabit regions east and west of the Lomonosov Ridge, a barrier especially important to species living in lower AODW; deep Eurasian Basin assemblages are more similar to those living in Greenland Sea deep water (GSDW) than those in Canada Basin deep water; two upper AODW assemblages were ... : Supplement to: Cronin, Thomas M; Holtz, Thomas R; Whatley, Robin C (1994): Quaternary paleoceanography of the deep Arctic Ocean based on quantitative analysis of Ostracoda. Marine Geology, 119(3-4), 305-332 ...
format Article in Journal/Newspaper
author Cronin, Thomas M
Holtz, Thomas R
Whatley, Robin C
author_facet Cronin, Thomas M
Holtz, Thomas R
Whatley, Robin C
author_sort Cronin, Thomas M
title Ostracoda in surface sediments of the Arctic Ocean ...
title_short Ostracoda in surface sediments of the Arctic Ocean ...
title_full Ostracoda in surface sediments of the Arctic Ocean ...
title_fullStr Ostracoda in surface sediments of the Arctic Ocean ...
title_full_unstemmed Ostracoda in surface sediments of the Arctic Ocean ...
title_sort ostracoda in surface sediments of the arctic ocean ...
publisher PANGAEA
publishDate 1994
url https://dx.doi.org/10.1594/pangaea.728604
https://doi.pangaea.de/10.1594/PANGAEA.728604
genre Arctic Ocean
canada basin
Greenland
Greenland Sea
Lomonosov Ridge
Yermak plateau
genre_facet Arctic Ocean
canada basin
Greenland
Greenland Sea
Lomonosov Ridge
Yermak plateau
op_relation https://dx.doi.org/10.1016/0025-3227(94)90188-0
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.72860410.1016/0025-3227(94)90188-0
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