(Table 1) Ostracode assemblage parameters in sediments of ODP Hole 113-689
During the late Paleocene thermal maximum (ca. 55.50 Ma) mid-bathyal ostracodes at Maud Rise in the Southern Ocean (Ocean Drilling Program Site 689) underwent a sudden, dramatic turnover synchronous with a global extinction in deep-sea benthic foraminifers and with large-scale, short-lived negative...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1996
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.712029 https://doi.org/10.1594/PANGAEA.712029 |