Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ...
Based on analyses of taxonomic composition of planktonic foraminifera and oxygen isotopic composition of their shells in the sediment core V34-90 from the eastern slope of the USSR Academy of Sciences Rise in the southeast Sea of Okhotsk the main climatic and hydrological variations over the past 20...
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Online Access: | https://dx.doi.org/10.1594/pangaea.778849 https://doi.pangaea.de/10.1594/PANGAEA.778849 |
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ftdatacite:10.1594/pangaea.778849 2024-02-27T08:42:56+00:00 Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... Chekhovskaya, Maria P Basov, Ivan A 1999 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.778849 https://doi.pangaea.de/10.1594/PANGAEA.778849 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Foraminifera, planktic Neogloboquadrina pachyderma sinistral Neogloboquadrina pachyderma dextral Globigerina bulloides Globigerina quinqueloba Globigerinita uvula Globigerina scitula Globigerina glutinata Gravity corer Age, 14C conventional Counting, foraminifera, planktic Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 1999 ftdatacite https://doi.org/10.1594/pangaea.778849 2024-02-01T16:16:58Z Based on analyses of taxonomic composition of planktonic foraminifera and oxygen isotopic composition of their shells in the sediment core V34-90 from the eastern slope of the USSR Academy of Sciences Rise in the southeast Sea of Okhotsk the main climatic and hydrological variations over the past 20 Ka have been traced and dated by the radiocarbon method. The followed periods have been revealed: glacial (20-12.5 Ka), deglaciation (12.5-8.0 Ka) with a pronounced cooling event (Late Drias about 10.8 Ka) and post deglaciation (last 8.0 Ka). ... : >0 = species is present. ... Dataset Neogloboquadrina pachyderma Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Okhotsk |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Foraminifera, planktic Neogloboquadrina pachyderma sinistral Neogloboquadrina pachyderma dextral Globigerina bulloides Globigerina quinqueloba Globigerinita uvula Globigerina scitula Globigerina glutinata Gravity corer Age, 14C conventional Counting, foraminifera, planktic Archive of Ocean Data ARCOD |
spellingShingle |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Foraminifera, planktic Neogloboquadrina pachyderma sinistral Neogloboquadrina pachyderma dextral Globigerina bulloides Globigerina quinqueloba Globigerinita uvula Globigerina scitula Globigerina glutinata Gravity corer Age, 14C conventional Counting, foraminifera, planktic Archive of Ocean Data ARCOD Chekhovskaya, Maria P Basov, Ivan A Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
topic_facet |
DEPTH, sediment/rock Depth, top/min Depth, bottom/max Age, dated Foraminifera, planktic Neogloboquadrina pachyderma sinistral Neogloboquadrina pachyderma dextral Globigerina bulloides Globigerina quinqueloba Globigerinita uvula Globigerina scitula Globigerina glutinata Gravity corer Age, 14C conventional Counting, foraminifera, planktic Archive of Ocean Data ARCOD |
description |
Based on analyses of taxonomic composition of planktonic foraminifera and oxygen isotopic composition of their shells in the sediment core V34-90 from the eastern slope of the USSR Academy of Sciences Rise in the southeast Sea of Okhotsk the main climatic and hydrological variations over the past 20 Ka have been traced and dated by the radiocarbon method. The followed periods have been revealed: glacial (20-12.5 Ka), deglaciation (12.5-8.0 Ka) with a pronounced cooling event (Late Drias about 10.8 Ka) and post deglaciation (last 8.0 Ka). ... : >0 = species is present. ... |
format |
Dataset |
author |
Chekhovskaya, Maria P Basov, Ivan A |
author_facet |
Chekhovskaya, Maria P Basov, Ivan A |
author_sort |
Chekhovskaya, Maria P |
title |
Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
title_short |
Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
title_full |
Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
title_fullStr |
Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
title_full_unstemmed |
Isotope age and relative abundance of planktonic foraminifera in Core Vulk-34-90, Sea of Okhotsk ... |
title_sort |
isotope age and relative abundance of planktonic foraminifera in core vulk-34-90, sea of okhotsk ... |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://dx.doi.org/10.1594/pangaea.778849 https://doi.pangaea.de/10.1594/PANGAEA.778849 |
geographic |
Okhotsk |
geographic_facet |
Okhotsk |
genre |
Neogloboquadrina pachyderma Planktonic foraminifera |
genre_facet |
Neogloboquadrina pachyderma 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.778849 |
_version_ |
1792050799030829056 |