Planktonic foraminifers in DSDP Holes 30-289 and 33-315A

The work is based on samples from Deep-Sea Drilling in the Pacific Ocean and from natural sections in its continental setting. Species composition of planktonic foraminifera from Maastrichtian sediments of the Pacific and South Atlantic oceans, as well as from marginal seas of Australia and New Zeal...

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Main Author: Sokolova, Ekaterina A
Format: Dataset
Language:English
Published: PANGAEA 1997
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.734520
https://doi.org/10.1594/PANGAEA.734520
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.734520
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.734520 2023-05-15T18:00:28+02:00 Planktonic foraminifers in DSDP Holes 30-289 and 33-315A Sokolova, Ekaterina A MEDIAN LATITUDE: 1.057867 * MEDIAN LONGITUDE: 172.832433 * SOUTH-BOUND LATITUDE: -0.498700 * WEST-BOUND LONGITUDE: 158.511500 * NORTH-BOUND LATITUDE: 4.171000 * EAST-BOUND LONGITUDE: -158.525700 * DATE/TIME START: 1973-05-31T00:00:00 * DATE/TIME END: 1973-11-13T00:00:00 1997-03-03 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.734520 https://doi.org/10.1594/PANGAEA.734520 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.734520 https://doi.org/10.1594/PANGAEA.734520 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Sokolova, Ekaterina A (1997): Paleoceanologic reconstructions of the Pacific Ocean for the end of Late Cretaceous (Maastrichtian) based on planktonic foraminifera. P.P. Shirshov Institute of Oceanology, Russian Acedemy of Sciences, Moscow. Ph.D. Thesis; Saidova, Kh.M. (Supervisor), 195 pp 30-289 33-315A Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg30 Leg33 North Pacific/FAN South Pacific/PLATEAU Dataset 1997 ftpangaea https://doi.org/10.1594/PANGAEA.734520 2023-01-20T07:31:41Z The work is based on samples from Deep-Sea Drilling in the Pacific Ocean and from natural sections in its continental setting. Species composition of planktonic foraminifera from Maastrichtian sediments of the Pacific and South Atlantic oceans, as well as from marginal seas of Australia and New Zealand and epicontinental basins of the northern hemisphere has been analysed. Two main issues: reconstruction of Maastrichtian climatic zonality, and reconstruction of Maastrichtian paleodepths. Four bipolar climatic zones have been distinguished. According to preservation of planktonic foraminifera and composition of their complexes three levels of dissolution have been identified. Dataset Planktonic foraminifera PANGAEA - Data Publisher for Earth & Environmental Science Pacific New Zealand ENVELOPE(158.511500,-158.525700,4.171000,-0.498700)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 30-289
33-315A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg30
Leg33
North Pacific/FAN
South Pacific/PLATEAU
spellingShingle 30-289
33-315A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg30
Leg33
North Pacific/FAN
South Pacific/PLATEAU
Sokolova, Ekaterina A
Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
topic_facet 30-289
33-315A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg30
Leg33
North Pacific/FAN
South Pacific/PLATEAU
description The work is based on samples from Deep-Sea Drilling in the Pacific Ocean and from natural sections in its continental setting. Species composition of planktonic foraminifera from Maastrichtian sediments of the Pacific and South Atlantic oceans, as well as from marginal seas of Australia and New Zealand and epicontinental basins of the northern hemisphere has been analysed. Two main issues: reconstruction of Maastrichtian climatic zonality, and reconstruction of Maastrichtian paleodepths. Four bipolar climatic zones have been distinguished. According to preservation of planktonic foraminifera and composition of their complexes three levels of dissolution have been identified.
format Dataset
author Sokolova, Ekaterina A
author_facet Sokolova, Ekaterina A
author_sort Sokolova, Ekaterina A
title Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
title_short Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
title_full Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
title_fullStr Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
title_full_unstemmed Planktonic foraminifers in DSDP Holes 30-289 and 33-315A
title_sort planktonic foraminifers in dsdp holes 30-289 and 33-315a
publisher PANGAEA
publishDate 1997
url https://doi.pangaea.de/10.1594/PANGAEA.734520
https://doi.org/10.1594/PANGAEA.734520
op_coverage MEDIAN LATITUDE: 1.057867 * MEDIAN LONGITUDE: 172.832433 * SOUTH-BOUND LATITUDE: -0.498700 * WEST-BOUND LONGITUDE: 158.511500 * NORTH-BOUND LATITUDE: 4.171000 * EAST-BOUND LONGITUDE: -158.525700 * DATE/TIME START: 1973-05-31T00:00:00 * DATE/TIME END: 1973-11-13T00:00:00
long_lat ENVELOPE(158.511500,-158.525700,4.171000,-0.498700)
geographic Pacific
New Zealand
geographic_facet Pacific
New Zealand
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
Supplement to: Sokolova, Ekaterina A (1997): Paleoceanologic reconstructions of the Pacific Ocean for the end of Late Cretaceous (Maastrichtian) based on planktonic foraminifera. P.P. Shirshov Institute of Oceanology, Russian Acedemy of Sciences, Moscow. Ph.D. Thesis; Saidova, Kh.M. (Supervisor), 195 pp
op_relation https://doi.pangaea.de/10.1594/PANGAEA.734520
https://doi.org/10.1594/PANGAEA.734520
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.734520
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