Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific

Polycystine radiolarians were investigated in 66 samples from 5 box-cores spanning the last ca. 40,000 years from the western (approx. 160°E) and the central (136°W) equatorial Pacific. The assemblages investigated show clear differences associated with the geographic locations of the sites: the cen...

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Main Author: Boltovskoy, Demetrio
Language:unknown
Published: 1991
Subjects:
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v86_n3-4_p227_Boltovskoy
https://hdl.handle.net/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy
id ftunibueairesbd:paper:paper_00310182_v86_n3-4_p227_Boltovskoy
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spelling ftunibueairesbd:paper:paper_00310182_v86_n3-4_p227_Boltovskoy 2023-05-15T18:00:58+02:00 Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific Boltovskoy, Demetrio 1991 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v86_n3-4_p227_Boltovskoy https://hdl.handle.net/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v86_n3-4_p227_Boltovskoy http://hdl.handle.net/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy biogeography equatorial ocean Holocene palaeoecology Pleistocene primary production radiolarian Pacific 1991 ftunibueairesbd https://doi.org/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy 2023-02-16T02:01:10Z Polycystine radiolarians were investigated in 66 samples from 5 box-cores spanning the last ca. 40,000 years from the western (approx. 160°E) and the central (136°W) equatorial Pacific. The assemblages investigated show clear differences associated with the geographic locations of the sites: the central Pacific is characterized by higher specific diverities, much higher absolute abundances of shells per gram of dry bulk sediment, and by conspicuously better radiolarian preservation. The differences involved also include significant changes in the relative proportions of several radiolarian species (these accounting for approx. 25% of total individuals), families and orders. These dissimilarities are chiefly attributed to differences in the primary production of the two zones and to enhanced advection of colder-water species characteristics of the California Current to the central equatorial Pacific. In both areas, downcore faunal changes, if present at all, are so weak that background noise from random sample-to-sample variations almost completely masks them. There do not seem to be any noticeable shifts associated with the 18 k.y. level. Inconclusive evidences of environmental changes at 30-20 k.y. B.P. are suggested in some of the cores by the increase in the proportions of several species characteristic of colder northeastern Pacific waters and by lower radiolarian accumulation rates; these changes seem to be paralleled by shifts in the isotopic composition of planktonic Foraminifera. © 1991. Fil:Boltovskoy, D. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Other/Unknown Material Planktonic foraminifera Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Argentina Pacific
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language unknown
topic biogeography
equatorial ocean
Holocene
palaeoecology
Pleistocene
primary production
radiolarian
Pacific
spellingShingle biogeography
equatorial ocean
Holocene
palaeoecology
Pleistocene
primary production
radiolarian
Pacific
Boltovskoy, Demetrio
Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
topic_facet biogeography
equatorial ocean
Holocene
palaeoecology
Pleistocene
primary production
radiolarian
Pacific
description Polycystine radiolarians were investigated in 66 samples from 5 box-cores spanning the last ca. 40,000 years from the western (approx. 160°E) and the central (136°W) equatorial Pacific. The assemblages investigated show clear differences associated with the geographic locations of the sites: the central Pacific is characterized by higher specific diverities, much higher absolute abundances of shells per gram of dry bulk sediment, and by conspicuously better radiolarian preservation. The differences involved also include significant changes in the relative proportions of several radiolarian species (these accounting for approx. 25% of total individuals), families and orders. These dissimilarities are chiefly attributed to differences in the primary production of the two zones and to enhanced advection of colder-water species characteristics of the California Current to the central equatorial Pacific. In both areas, downcore faunal changes, if present at all, are so weak that background noise from random sample-to-sample variations almost completely masks them. There do not seem to be any noticeable shifts associated with the 18 k.y. level. Inconclusive evidences of environmental changes at 30-20 k.y. B.P. are suggested in some of the cores by the increase in the proportions of several species characteristic of colder northeastern Pacific waters and by lower radiolarian accumulation rates; these changes seem to be paralleled by shifts in the isotopic composition of planktonic Foraminifera. © 1991. Fil:Boltovskoy, D. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
author Boltovskoy, Demetrio
author_facet Boltovskoy, Demetrio
author_sort Boltovskoy, Demetrio
title Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
title_short Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
title_full Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
title_fullStr Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
title_full_unstemmed Holocene-Upper Pleistocene radiolarian biogeography and paleoecology of the equatorial Pacific
title_sort holocene-upper pleistocene radiolarian biogeography and paleoecology of the equatorial pacific
publishDate 1991
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v86_n3-4_p227_Boltovskoy
https://hdl.handle.net/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy
geographic Argentina
Pacific
geographic_facet Argentina
Pacific
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v86_n3-4_p227_Boltovskoy
http://hdl.handle.net/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy
op_doi https://doi.org/20.500.12110/paper_00310182_v86_n3-4_p227_Boltovskoy
_version_ 1766170271657492480