Abstract
The middle Paleocene through early Eocene long‐term gradual warming was
superimposed by several transient warming events, such as the Paleocene‐Eocene
Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM2). Both events
show evidence for extreme global warming associated with a major injection of carbon
into the ocean‐atmosphere system, but the mechanisms of carbon injection
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