Abstract
Enhanced formation of clay in marine sediments in the lead up to the end-Permian mass extinction likely pulled the Earth back into a hot, high-CO2 state similar to that of the Precambrian.
Original language | English |
---|---|
Pages (from-to) | 756–757 |
Number of pages | 2 |
Journal | Nature Geoscience |
Volume | 15 |
DOIs |
|
Publication status | Published - 3 Oct 2022 |