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...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2012
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.783839 https://doi.pangaea.de/10.1594/PANGAEA.783839 |