Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...

Planktonic foraminiferal and nannoplankton stratigraphy of the Pliocene-Quatemary Sediments of the northern half of the Atlantic Ocean from the equator up to the Rockall Plateau and the Norwegian Sea, is considered. Lowlatitude zonations were used for the subdivision of the Pliocene and Quaternary S...

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Main Authors: Bylinskaya, M E, Golovina, L A, Krasheninnikov, Valery A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2002
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.758415
https://doi.pangaea.de/10.1594/PANGAEA.758415
id ftdatacite:10.1594/pangaea.758415
record_format openpolar
spelling ftdatacite:10.1594/pangaea.758415 2024-09-15T18:23:25+00:00 Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ... Bylinskaya, M E Golovina, L A Krasheninnikov, Valery A 2002 application/zip https://dx.doi.org/10.1594/pangaea.758415 https://doi.pangaea.de/10.1594/PANGAEA.758415 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Gravity corer Leg41 ANS3 Glomar Challenger Akademik Nikolaj Strakhov Archive of Ocean Data ARCOD Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 2002 ftdatacite https://doi.org/10.1594/pangaea.758415 2024-08-01T10:58:30Z Planktonic foraminiferal and nannoplankton stratigraphy of the Pliocene-Quatemary Sediments of the northern half of the Atlantic Ocean from the equator up to the Rockall Plateau and the Norwegian Sea, is considered. Lowlatitude zonations were used for the subdivision of the Pliocene and Quaternary Sediments of different climatic belts, and certain subglobal zonal units were recognized. Variations in the degree of resolution of the zonation in different latitudes were revealed; the resolution of zonal scales based on calcareous plankton diminishes northwards. Changes of taxonomic composition of the zonal foraminifer and nannoplankton assemblages within various latitudinal belts of the Atlantic were analyzed taking into consideration the influence of climatic factors and of local bionomic conditions. Correlation with the magnetostratigraphic time-scale permitted the establishment of the most reliable appearance and disappearance datums (datum planes) of planktonic foraminifer and nannoplankton species. ... : For planktonic foraminiferal data of DSDP Hole 41-366A see Krasheninnikov and Pflaumann (1978) dataset: doi:10.1594/PANGAEA.758414. ... Article in Journal/Newspaper North Atlantic Norwegian Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Drilling/drill rig
Gravity corer
Leg41
ANS3
Glomar Challenger
Akademik Nikolaj Strakhov
Archive of Ocean Data ARCOD
Deep Sea Drilling Project DSDP
spellingShingle Composite Core
Drilling/drill rig
Gravity corer
Leg41
ANS3
Glomar Challenger
Akademik Nikolaj Strakhov
Archive of Ocean Data ARCOD
Deep Sea Drilling Project DSDP
Bylinskaya, M E
Golovina, L A
Krasheninnikov, Valery A
Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
topic_facet Composite Core
Drilling/drill rig
Gravity corer
Leg41
ANS3
Glomar Challenger
Akademik Nikolaj Strakhov
Archive of Ocean Data ARCOD
Deep Sea Drilling Project DSDP
description Planktonic foraminiferal and nannoplankton stratigraphy of the Pliocene-Quatemary Sediments of the northern half of the Atlantic Ocean from the equator up to the Rockall Plateau and the Norwegian Sea, is considered. Lowlatitude zonations were used for the subdivision of the Pliocene and Quaternary Sediments of different climatic belts, and certain subglobal zonal units were recognized. Variations in the degree of resolution of the zonation in different latitudes were revealed; the resolution of zonal scales based on calcareous plankton diminishes northwards. Changes of taxonomic composition of the zonal foraminifer and nannoplankton assemblages within various latitudinal belts of the Atlantic were analyzed taking into consideration the influence of climatic factors and of local bionomic conditions. Correlation with the magnetostratigraphic time-scale permitted the establishment of the most reliable appearance and disappearance datums (datum planes) of planktonic foraminifer and nannoplankton species. ... : For planktonic foraminiferal data of DSDP Hole 41-366A see Krasheninnikov and Pflaumann (1978) dataset: doi:10.1594/PANGAEA.758414. ...
format Article in Journal/Newspaper
author Bylinskaya, M E
Golovina, L A
Krasheninnikov, Valery A
author_facet Bylinskaya, M E
Golovina, L A
Krasheninnikov, Valery A
author_sort Bylinskaya, M E
title Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
title_short Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
title_full Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
title_fullStr Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
title_full_unstemmed Microfossil occurrence in Pliocene-Quaternary sediments of the North Atlantic ...
title_sort microfossil occurrence in pliocene-quaternary sediments of the north atlantic ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.758415
https://doi.pangaea.de/10.1594/PANGAEA.758415
genre North Atlantic
Norwegian Sea
genre_facet North Atlantic
Norwegian 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.758415
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