Foraminiferal Mg/Ca and Mn/Ca ratios across the Eocene-Oligocene transition

Constraining the magnitude of high-latitude temperature change across the Eocene-Oligocene transition (EOT) is essential for quantifying the magnitude of Antarctic ice-sheet expansion and understanding regional climate response to this event. To this end, we constructed high-resolution stable oxygen...

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Bibliographic Details
Main Authors: Bohaty, Steven M, Zachos, James C, Delaney, Margaret Lois
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2012
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.783839
https://doi.org/10.1594/PANGAEA.783839