Siliceous microfossil assemblage and accumulation rate variations across the Middle Eocene Climatic Optimum at ODP Site 171-1051

The Middle Eocene Climatic Optimum (MECO; ~ 40 million years ago [Ma]) is one of the most prominent transient global warming events in the Paleogene. Although the event is well documented in geochemical and isotopic proxy records at many locations, the marine biotic response to the MECO remains poor...

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Bibliographic Details
Main Authors: Witkowski, Jakub, Bohaty, Steven M, Edgar, Kirsty M, Harwood, David M
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2014
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.828089
https://doi.org/10.1594/PANGAEA.828089