Nature, Published online: 17 June 2026; doi:10. 1038/s41586-026-10664-8 Permafrost thaw on the Qinghai–Tibet Plateau increases rock-weathering rates while reducing river CO2 emissions, suggesting geological carbon fluxes may eventually outpace thaw-driven emissions.
Source: [Nature](https://www.nature.com/articles/s41586-026-10664-8)