Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...

Quantitative records of Globorotalia puncticulata and Globorotalia inflata, the last two members of the Globorotalia (Globoconella) lineage, obtained from North Atlantic sediments collected at DSDP Site 552, ODP Site 659 and ODP Site 665, are used to examine fluctuations in the biogeographic distrib...

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Main Authors: Chapman, Mark R, Funnell, Brian M, Weaver, Philip PE
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1998
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.679415
https://doi.pangaea.de/10.1594/PANGAEA.679415
id ftdatacite:10.1594/pangaea.679415
record_format openpolar
spelling ftdatacite:10.1594/pangaea.679415 2024-09-09T19:54:51+00:00 Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ... Chapman, Mark R Funnell, Brian M Weaver, Philip PE 1998 application/zip https://dx.doi.org/10.1594/pangaea.679415 https://doi.pangaea.de/10.1594/PANGAEA.679415 en eng PANGAEA https://dx.doi.org/10.1016/s0377-8398(97)00041-8 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg81 Leg108 Glomar Challenger Joides Resolution Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1998 ftdatacite https://doi.org/10.1594/pangaea.67941510.1016/s0377-8398(97)00041-8 2024-08-01T10:50:55Z Quantitative records of Globorotalia puncticulata and Globorotalia inflata, the last two members of the Globorotalia (Globoconella) lineage, obtained from North Atlantic sediments collected at DSDP Site 552, ODP Site 659 and ODP Site 665, are used to examine fluctuations in the biogeographic distribution of these species in the Late Pliocene between 3 and 2 Ma. Abundance data indicate that prior to the expansion of Northern Hemisphere glaciation at about 2.5 Ma, Gr. puncticulata was an important component of the planktonic foraminiferal fauna and had a geographic distribution ranging from 2°N to at least 56°N in the North Atlantic. A previously undescribed 6 chambered variant of Gr. puncticulata is found at both Sites 659 and 665. The stratigraphic distribution of this morphotype is restricted, first occurring at 2.9 Ma and then disappearing when glacial intensity increased at 2.75 Ma (isotope stage 110). Similar declines in Gr. puncticulata abundances occurred during glacial isotope stages 102, 100, and 98 ... : Supplement to: Chapman, Mark R; Funnell, Brian M; Weaver, Philip PE (1998): Isolation, extinction and migration within Late Pliocene populations of the planktonic foraminiferal lineage Globorotalia (Globoconella) in the North Atlantic. Marine Micropaleontology, 33(3-4), 203-222 ... Article in Journal/Newspaper North Atlantic DataCite Weaver ENVELOPE(-153.833,-153.833,-86.967,-86.967)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Leg81
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Composite Core
Leg81
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Chapman, Mark R
Funnell, Brian M
Weaver, Philip PE
Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
topic_facet Composite Core
Leg81
Leg108
Glomar Challenger
Joides Resolution
Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description Quantitative records of Globorotalia puncticulata and Globorotalia inflata, the last two members of the Globorotalia (Globoconella) lineage, obtained from North Atlantic sediments collected at DSDP Site 552, ODP Site 659 and ODP Site 665, are used to examine fluctuations in the biogeographic distribution of these species in the Late Pliocene between 3 and 2 Ma. Abundance data indicate that prior to the expansion of Northern Hemisphere glaciation at about 2.5 Ma, Gr. puncticulata was an important component of the planktonic foraminiferal fauna and had a geographic distribution ranging from 2°N to at least 56°N in the North Atlantic. A previously undescribed 6 chambered variant of Gr. puncticulata is found at both Sites 659 and 665. The stratigraphic distribution of this morphotype is restricted, first occurring at 2.9 Ma and then disappearing when glacial intensity increased at 2.75 Ma (isotope stage 110). Similar declines in Gr. puncticulata abundances occurred during glacial isotope stages 102, 100, and 98 ... : Supplement to: Chapman, Mark R; Funnell, Brian M; Weaver, Philip PE (1998): Isolation, extinction and migration within Late Pliocene populations of the planktonic foraminiferal lineage Globorotalia (Globoconella) in the North Atlantic. Marine Micropaleontology, 33(3-4), 203-222 ...
format Article in Journal/Newspaper
author Chapman, Mark R
Funnell, Brian M
Weaver, Philip PE
author_facet Chapman, Mark R
Funnell, Brian M
Weaver, Philip PE
author_sort Chapman, Mark R
title Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
title_short Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
title_full Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
title_fullStr Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
title_full_unstemmed Late Pliocene stratigraphic distribution of Globoconella taxa in the North Atlantic ...
title_sort late pliocene stratigraphic distribution of globoconella taxa in the north atlantic ...
publisher PANGAEA
publishDate 1998
url https://dx.doi.org/10.1594/pangaea.679415
https://doi.pangaea.de/10.1594/PANGAEA.679415
long_lat ENVELOPE(-153.833,-153.833,-86.967,-86.967)
geographic Weaver
geographic_facet Weaver
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1016/s0377-8398(97)00041-8
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.67941510.1016/s0377-8398(97)00041-8
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