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 |
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| Pages (from-to) | 756–757 |
| Number of pages | 2 |
| Journal | Nature Geoscience |
| Volume | 15 |
| Issue number | 10 |
| DOIs |
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| Publication status | Published - 3 Oct 2022 |