Mg/Ca and stable isotope record of benthic foraminifera of the Paleocene-Eocene Thermal Maximum

A rapid increase in greenhouse gas levels is thought to have fueled global warming at the Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios indicate that bottom waters warmed by 4° to 5°C, similar to tropical and subtropical surface ocean waters, implying no amplificati...

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Bibliographic Details
Main Authors: Tripati, Aradhna K, Elderfield, Henry
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2005
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738241
https://doi.org/10.1594/PANGAEA.738241