Abstract
During the Paleocene-Eocene Thermal Maximum (PETM), rapid release of isotopically light C to the ocean-atmosphere system elevated the greenhouse effect and warmed temperatures by 5-7 °C for 10
Original language | English |
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Pages (from-to) | 192-206 |
Journal | Earth and Planetary Science Letters |
Volume | 258 |
DOIs | |
Publication status | Published - 2007 |