Some 56 million years ago, carbon surged into Earth’s atmosphere, raising temperatures by 5°C to 8°C and causing huge wildlife migrations—a scenario that might mirror the world’s future, thanks to global warming. But what triggered this so-called Paleocene-Eocene thermal maximum (PETM) has remained a mystery, until now.
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About the author

Teunis Felter
Teunis Felter has over 20 years experience as an author, editor, and scientist. When not exploring outside, he enjoys reading history, researching genealogy, and civilly discussing politics.