Rock weathering tells a new story: more erosion does not always mean more carbon consumption
Peer-Reviewed Publication
Updates every hour. Last Updated: 22-Oct-2026 16:16 ET (22-Oct-2026 20:16 GMT/UTC)
Rock weathering is an important process regulating atmospheric CO2 concentrations and long-term climate evolution, yet how enhanced erosion affects rock weathering and its carbon effects remains poorly understood. Focusing on the Lancang River basin on the southeastern margin of the Tibetan Plateau, the authors quantitatively reveal the differential responses of silicate, carbonate, and sulfide weathering to changes in erosion. The results show that, as erosion intensifies, silicate weathering rates decrease while sulfide oxidation rates increase, causing weathering in the basin to tend toward a net carbon source. The related findings have now been published in Science China Earth Sciences.
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