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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Online Access: | https://dx.doi.org/10.1594/pangaea.706908 https://doi.pangaea.de/10.1594/PANGAEA.706908 |
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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 |