Radiolarians of the Japan Sea

Fuente: PANGAEA
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Bibliographic Details
Main Author: Alexandrovich, Joanne M
Format: Dataset Open Access
Language:en
Published: PANGAEA 1992
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author Alexandrovich, Joanne M
author_facet Alexandrovich, Joanne M
collection Datos científicos de ciencias marinas y ambientales
contents Japan Sea ODP Leg 127 shipboard radiolarian biostratigraphic data are compiled and improved. The sequence of biostratigraphic events determined in sediments above the opal-A/opal-CT transition is illustrated graphically with depth-depth plots. The absence of biostratigraphic indicators from the North and subtropical Pacific and differences between the compositions of the Japan Sea and Pacific radiolarian assemblages suggest that the planktonic populations of the Japan Sea have been partially isolated from the Pacific since the late Miocene. Subtropical fauna in sediments younger than ~1.8 Ma at Site 797 record the occurrence of a paleo-Tsushima current. These same fauna record larger volumes of the paleo-Tsushima current, or warmer intervals during the colder glacial climate regime at Site 794. The variability of Pleistocene assemblage composition and preservation shows that radiolarian dissolution has played a large part in determining what is preserved. Preliminary taxonomic evaluations are made, and the stratigraphic and paleoceanographic implications of radiolarian species are discussed.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_771377
institution PANGAEA
language en
publishDate 1992
publisher PANGAEA
record_format pangaea
spellingShingle Radiolarians of the Japan Sea
Alexandrovich, Joanne M
127-794A; 127-794B; 127-795A; 127-795B; 127-796A; 127-796B; 127-797B; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg127; Ocean Drilling Program; ODP
Japan Sea ODP Leg 127 shipboard radiolarian biostratigraphic data are compiled and improved. The sequence of biostratigraphic events determined in sediments above the opal-A/opal-CT transition is illustrated graphically with depth-depth plots. The absence of biostratigraphic indicators from the North and subtropical Pacific and differences between the compositions of the Japan Sea and Pacific radiolarian assemblages suggest that the planktonic populations of the Japan Sea have been partially isolated from the Pacific since the late Miocene. Subtropical fauna in sediments younger than ~1.8 Ma at Site 797 record the occurrence of a paleo-Tsushima current. These same fauna record larger volumes of the paleo-Tsushima current, or warmer intervals during the colder glacial climate regime at Site 794. The variability of Pleistocene assemblage composition and preservation shows that radiolarian dissolution has played a large part in determining what is preserved. Preliminary taxonomic evaluations are made, and the stratigraphic and paleoceanographic implications of radiolarian species are discussed.
title Radiolarians of the Japan Sea
topic 127-794A; 127-794B; 127-795A; 127-795B; 127-796A; 127-796B; 127-797B; DRILL; Drilling/drill rig; Japan Sea; Joides Resolution; Leg127; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.771377