Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...

With the examination of multinet catches (63 µm mesh size), the present study analyzes the distribution of planktonic foraminifera in Polar regions: the Labrador Sea, Greenland Sea at 75°N and Fram Strait at 80°N. The community of the planktonic foraminifera, which in the study area mainly consists...

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Main Author: Stangeew, Elena
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2001
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.706908
https://doi.pangaea.de/10.1594/PANGAEA.706908
id ftdatacite:10.1594/pangaea.706908
record_format openpolar
spelling ftdatacite:10.1594/pangaea.706908 2024-09-15T18:07:03+00:00 Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ... Stangeew, Elena 2001 application/zip https://dx.doi.org/10.1594/pangaea.706908 https://doi.pangaea.de/10.1594/PANGAEA.706908 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CTD/Rosette Multiple opening/closing net M39/4 ARK-XV/1 ARK-XV/2 Meteor 1986 Polarstern Helmholtz Centre for Ocean Research Kiel GEOMAR Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2001 ftdatacite https://doi.org/10.1594/pangaea.706908 2024-08-01T11:08:49Z With the examination of multinet catches (63 µm mesh size), the present study analyzes the distribution of planktonic foraminifera in Polar regions: the Labrador Sea, Greenland Sea at 75°N and Fram Strait at 80°N. The community of the planktonic foraminifera, which in the study area mainly consists of six species: left and right-coiling N. pachyderma, T. quinqueloba, G. bulloides, G. glutinata and G. uvula, is primarily controlled by the temperature in the different water masses. Besides hydrographic parameters, the changes in the horizontal and vertical distribution of N. pachyderma (s.) and T. quinqueloba as well as their shell size distribution in the study area are primarily influenced by the synchrone reproduction, which is coupled to the lunar cycle. Detailed examinations of the isotope signal in dependency on the shell size and weight for N. pachyderma (s.) and T. quinqueloba from plankton tows, indicated the weight or degree of calcification to not be the primary factor controlling the isotope signal ... : Supplement to: Stangeew, Elena (2001): Distribution and isotopic composition of living planktonic foraminifera N. pachyderma (sinistral) and T. quinqueloba in the high latitude North Atlantic. Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 90 pp ... Article in Journal/Newspaper Fram Strait Greenland Greenland Sea Labrador Sea North Atlantic Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic CTD/Rosette
Multiple opening/closing net
M39/4
ARK-XV/1
ARK-XV/2
Meteor 1986
Polarstern
Helmholtz Centre for Ocean Research Kiel GEOMAR
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle CTD/Rosette
Multiple opening/closing net
M39/4
ARK-XV/1
ARK-XV/2
Meteor 1986
Polarstern
Helmholtz Centre for Ocean Research Kiel GEOMAR
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Stangeew, Elena
Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
topic_facet CTD/Rosette
Multiple opening/closing net
M39/4
ARK-XV/1
ARK-XV/2
Meteor 1986
Polarstern
Helmholtz Centre for Ocean Research Kiel GEOMAR
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description With the examination of multinet catches (63 µm mesh size), the present study analyzes the distribution of planktonic foraminifera in Polar regions: the Labrador Sea, Greenland Sea at 75°N and Fram Strait at 80°N. The community of the planktonic foraminifera, which in the study area mainly consists of six species: left and right-coiling N. pachyderma, T. quinqueloba, G. bulloides, G. glutinata and G. uvula, is primarily controlled by the temperature in the different water masses. Besides hydrographic parameters, the changes in the horizontal and vertical distribution of N. pachyderma (s.) and T. quinqueloba as well as their shell size distribution in the study area are primarily influenced by the synchrone reproduction, which is coupled to the lunar cycle. Detailed examinations of the isotope signal in dependency on the shell size and weight for N. pachyderma (s.) and T. quinqueloba from plankton tows, indicated the weight or degree of calcification to not be the primary factor controlling the isotope signal ... : Supplement to: Stangeew, Elena (2001): Distribution and isotopic composition of living planktonic foraminifera N. pachyderma (sinistral) and T. quinqueloba in the high latitude North Atlantic. Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 90 pp ...
format Article in Journal/Newspaper
author Stangeew, Elena
author_facet Stangeew, Elena
author_sort Stangeew, Elena
title Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
title_short Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
title_full Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
title_fullStr Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
title_full_unstemmed Oceanography and stable isotopes on planktonic foraminifera from the North Atlantic ...
title_sort oceanography and stable isotopes on planktonic foraminifera from the north atlantic ...
publisher PANGAEA
publishDate 2001
url https://dx.doi.org/10.1594/pangaea.706908
https://doi.pangaea.de/10.1594/PANGAEA.706908
genre Fram Strait
Greenland
Greenland Sea
Labrador Sea
North Atlantic
Planktonic foraminifera
genre_facet Fram Strait
Greenland
Greenland Sea
Labrador Sea
North Atlantic
Planktonic foraminifera
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.706908
_version_ 1810444436475215872