Benthic foraminifera and phytodetritus species in sediments from DSDP Leg 85, and ODP Legs 113 and 143

From late middle Eocene through earliest Oligocene, high-latitude regions cooled, and by the end of the period, continental ice sheets existed in Antarctica. Diversity of planktonic microorganisms declined, and modern groups of terrestrial vertebrates originated. Coeval faunal changes in deep-sea be...

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Bibliographic Details
Main Authors: Thomas, Ellen, Gooday, Andrew J
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1996
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.712704
https://doi.org/10.1594/PANGAEA.712704