Age determination of sediments cores from the East Greenland continental margin ...
Stable isotope records, and sedimentological and organic-geochemical investigations of marine sediments from the east Greenland Sea at 70°N provide important information about glacial-interglacial variations of paleoenvironments through the last 225 kyr. The oxygen isotope records established on the...
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ftdatacite:10.1594/pangaea.707391 2024-06-09T07:45:39+00:00 Age determination of sediments cores from the East Greenland continental margin ... Nam, Seung-Il Stein, Ruediger Grobe, Hannes Hubberten, Hans-Wolfgang 1995 application/zip https://dx.doi.org/10.1594/pangaea.707391 https://doi.pangaea.de/10.1594/PANGAEA.707391 en eng PANGAEA https://dx.doi.org/10.1016/0025-3227(94)00070-2 https://dx.doi.org/10.2312/bzp_0241_1997 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Collection article Supplementary Publication Series of Datasets 1995 ftdatacite https://doi.org/10.1594/pangaea.70739110.1016/0025-3227(94)00070-210.2312/bzp_0241_1997 2024-05-13T14:00:09Z Stable isotope records, and sedimentological and organic-geochemical investigations of marine sediments from the east Greenland Sea at 70°N provide important information about glacial-interglacial variations of paleoenvironments through the last 225 kyr. The oxygen isotope records established on the planktonic foraminifer N. pachyderma sin. show some excursions from the global climate pattern, probably due to local/regional overprint by meltwater supply. The cold, low-saline East Greenland Current and fluctuations in sea-ice covering were a crucial element controlling the carbonate production in the subsurface/surface water column in the east Greenland Sea over the last 225 kyr. The beginning of Termination Ia is AMS 14C dated at about 15.8 kyr B.P. and interpreted as a Greenland Ice Sheet meltwater signal. The stage 2/3 boundary is dated at about 25 kyr B.P. The timing of the onset of the last deglacial meltwater event is about 800 years earlier than that of the Barents Shelf Ice Sheet meltwater signal ... : Supplement to: Nam, Seung-Il; Stein, Ruediger; Grobe, Hannes; Hubberten, Hans-Wolfgang (1995): Late Quaternary glacial-interglacial changes in sediment composition at the East Greenland continental margin and their paleoceanographic implications. Marine Geology, 122(3), 243-262 ... Article in Journal/Newspaper East Greenland east greenland current Greenland Greenland Sea Ice Sheet Sea ice DataCite Metadata Store (German National Library of Science and Technology) Greenland Hannes ENVELOPE(18.064,18.064,69.390,69.390) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
spellingShingle |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Nam, Seung-Il Stein, Ruediger Grobe, Hannes Hubberten, Hans-Wolfgang Age determination of sediments cores from the East Greenland continental margin ... |
topic_facet |
Gravity corer Kiel type ARK-V/3b Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
Stable isotope records, and sedimentological and organic-geochemical investigations of marine sediments from the east Greenland Sea at 70°N provide important information about glacial-interglacial variations of paleoenvironments through the last 225 kyr. The oxygen isotope records established on the planktonic foraminifer N. pachyderma sin. show some excursions from the global climate pattern, probably due to local/regional overprint by meltwater supply. The cold, low-saline East Greenland Current and fluctuations in sea-ice covering were a crucial element controlling the carbonate production in the subsurface/surface water column in the east Greenland Sea over the last 225 kyr. The beginning of Termination Ia is AMS 14C dated at about 15.8 kyr B.P. and interpreted as a Greenland Ice Sheet meltwater signal. The stage 2/3 boundary is dated at about 25 kyr B.P. The timing of the onset of the last deglacial meltwater event is about 800 years earlier than that of the Barents Shelf Ice Sheet meltwater signal ... : Supplement to: Nam, Seung-Il; Stein, Ruediger; Grobe, Hannes; Hubberten, Hans-Wolfgang (1995): Late Quaternary glacial-interglacial changes in sediment composition at the East Greenland continental margin and their paleoceanographic implications. Marine Geology, 122(3), 243-262 ... |
format |
Article in Journal/Newspaper |
author |
Nam, Seung-Il Stein, Ruediger Grobe, Hannes Hubberten, Hans-Wolfgang |
author_facet |
Nam, Seung-Il Stein, Ruediger Grobe, Hannes Hubberten, Hans-Wolfgang |
author_sort |
Nam, Seung-Il |
title |
Age determination of sediments cores from the East Greenland continental margin ... |
title_short |
Age determination of sediments cores from the East Greenland continental margin ... |
title_full |
Age determination of sediments cores from the East Greenland continental margin ... |
title_fullStr |
Age determination of sediments cores from the East Greenland continental margin ... |
title_full_unstemmed |
Age determination of sediments cores from the East Greenland continental margin ... |
title_sort |
age determination of sediments cores from the east greenland continental margin ... |
publisher |
PANGAEA |
publishDate |
1995 |
url |
https://dx.doi.org/10.1594/pangaea.707391 https://doi.pangaea.de/10.1594/PANGAEA.707391 |
long_lat |
ENVELOPE(18.064,18.064,69.390,69.390) |
geographic |
Greenland Hannes |
geographic_facet |
Greenland Hannes |
genre |
East Greenland east greenland current Greenland Greenland Sea Ice Sheet Sea ice |
genre_facet |
East Greenland east greenland current Greenland Greenland Sea Ice Sheet Sea ice |
op_relation |
https://dx.doi.org/10.1016/0025-3227(94)00070-2 https://dx.doi.org/10.2312/bzp_0241_1997 |
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.70739110.1016/0025-3227(94)00070-210.2312/bzp_0241_1997 |
_version_ |
1801375112861057024 |