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...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2005
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.738241 https://doi.org/10.1594/PANGAEA.738241 |