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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Online Access: | https://dx.doi.org/10.1594/pangaea.679415 https://doi.pangaea.de/10.1594/PANGAEA.679415 |
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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 |
_version_ |
1809924300326567936 |