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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Bibliographic Details
Main Authors: Chekhovskaya, Maria P, Basov, Ivan A
Format: Dataset
Language:English
Published: PANGAEA 1999
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.778849
https://doi.pangaea.de/10.1594/PANGAEA.778849
id ftdatacite:10.1594/pangaea.778849
record_format openpolar
spelling 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