Abundance of benthic Foraminifera in the Kara Sea ...

Taxonomic composition and structure of assemblages of the present-day benthic Foraminifera in the Kara Sea has been studied on the base of 37 samples of surface sediments. Three assemblages have been distinguished by composition of dominant species. The assemblage Cribrostomoides subglobosus-Tritaxi...

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Main Author: Khusid, Tatyana A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1996
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.760664
https://doi.pangaea.de/10.1594/PANGAEA.760664
id ftdatacite:10.1594/pangaea.760664
record_format openpolar
spelling ftdatacite:10.1594/pangaea.760664 2024-09-15T18:16:08+00:00 Abundance of benthic Foraminifera in the Kara Sea ... Khusid, Tatyana A 1996 application/zip https://dx.doi.org/10.1594/pangaea.760664 https://doi.pangaea.de/10.1594/PANGAEA.760664 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Grab Gravity corer Box corer Multiple investigations DM49 PSh12 Dmitry Mendeleev Professor Shtokman Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 1996 ftdatacite https://doi.org/10.1594/pangaea.760664 2024-08-01T10:59:28Z Taxonomic composition and structure of assemblages of the present-day benthic Foraminifera in the Kara Sea has been studied on the base of 37 samples of surface sediments. Three assemblages have been distinguished by composition of dominant species. The assemblage Cribrostomoides subglobosus-Tritaxis nana with prevalence of agglutinating forms, typical for abyssal areas of the World Ocean, occurs in brown oozes in the deep western part of the sea at depths 70-375 m under conditions of considerable bottom stratification. The assemblage Elphidium clavatum-Cassidulina reniforme consists predominantly of species with calcareous shells and is characterized by a wide range of species; this assemblage occurs in the eastern part of the sea at depths 30-90 m in a well-aerated area. Species typical for sublittoral areas of polar regions are dominant. The assemblage Elphidium clavatum-Haynesina orbiculare occupies the littoral estuarine part of the sea. This assemblage is poor in species and not abundant, and it occurs ... : Supplement to: Khusid, Tatyana A (1996): Benthic Foraminifera assemblages in the Kara Sea. Translated from Okeanologiya, 1996, 36(5), 759-765, Oceanology, 36(5), 716-722 ... Article in Journal/Newspaper Kara Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Grab
Gravity corer
Box corer
Multiple investigations
DM49
PSh12
Dmitry Mendeleev
Professor Shtokman
Archive of Ocean Data ARCOD
spellingShingle Grab
Gravity corer
Box corer
Multiple investigations
DM49
PSh12
Dmitry Mendeleev
Professor Shtokman
Archive of Ocean Data ARCOD
Khusid, Tatyana A
Abundance of benthic Foraminifera in the Kara Sea ...
topic_facet Grab
Gravity corer
Box corer
Multiple investigations
DM49
PSh12
Dmitry Mendeleev
Professor Shtokman
Archive of Ocean Data ARCOD
description Taxonomic composition and structure of assemblages of the present-day benthic Foraminifera in the Kara Sea has been studied on the base of 37 samples of surface sediments. Three assemblages have been distinguished by composition of dominant species. The assemblage Cribrostomoides subglobosus-Tritaxis nana with prevalence of agglutinating forms, typical for abyssal areas of the World Ocean, occurs in brown oozes in the deep western part of the sea at depths 70-375 m under conditions of considerable bottom stratification. The assemblage Elphidium clavatum-Cassidulina reniforme consists predominantly of species with calcareous shells and is characterized by a wide range of species; this assemblage occurs in the eastern part of the sea at depths 30-90 m in a well-aerated area. Species typical for sublittoral areas of polar regions are dominant. The assemblage Elphidium clavatum-Haynesina orbiculare occupies the littoral estuarine part of the sea. This assemblage is poor in species and not abundant, and it occurs ... : Supplement to: Khusid, Tatyana A (1996): Benthic Foraminifera assemblages in the Kara Sea. Translated from Okeanologiya, 1996, 36(5), 759-765, Oceanology, 36(5), 716-722 ...
format Article in Journal/Newspaper
author Khusid, Tatyana A
author_facet Khusid, Tatyana A
author_sort Khusid, Tatyana A
title Abundance of benthic Foraminifera in the Kara Sea ...
title_short Abundance of benthic Foraminifera in the Kara Sea ...
title_full Abundance of benthic Foraminifera in the Kara Sea ...
title_fullStr Abundance of benthic Foraminifera in the Kara Sea ...
title_full_unstemmed Abundance of benthic Foraminifera in the Kara Sea ...
title_sort abundance of benthic foraminifera in the kara sea ...
publisher PANGAEA
publishDate 1996
url https://dx.doi.org/10.1594/pangaea.760664
https://doi.pangaea.de/10.1594/PANGAEA.760664
genre Kara Sea
genre_facet Kara Sea
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.760664
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