Open access
Oct 2026
Depressed chemical weathering inhibited climate stabilization after the end-Permian biocrisis.
The Permian-Triassic transition (∼252 million years ago) marks the most severe mass extinction in Earth's history, followed by a protracted interval of environmental instability and delayed biological recovery. Although elevated atmospheric carbon dioxide (CO2) from extensive volcanism is widely invoked, the role of co...
Guang-Yi Wei, Fei-Fei Zhang, Hua Zhang et al.
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