Published: 2026-06-17

NEWS
A new study published in Nature study shows that rock weathering increasingly counteracts river CO₂ emissions as permafrost degrades. The study has been carried out by a collaborative team of researchers from Umeå University, Sweden, and East China Normal University.

Text: Anna-Lena Lindskog

Thawing permafrost is often viewed as a growing source of greenhouse gases as climate warming releases ancient carbon stored in frozen soils. But a new study published in the journal Nature reveals a more complex picture. As permafrost thaws, rivers may also develop an overlooked capacity to remove carbon dioxide (CO₂) through intensified rock weathering. Researchers found that warming and permafrost degradation expose reactive minerals and increase water–rock interactions, accelerating chemical weathering processes that consume CO₂. In some river catchments, this geological carbon uptake partially or even fully offset river CO₂ emissions.

The international research team investigated 50 rivers across the Qinghai–Tibet Plateau, Earth’s largest high-altitude cryosphere outside the polar regions, to understand how thawing permafrost reshapes carbon cycling. By combining measurements of river CO₂ emissions, dissolved carbon, isotopic tracers and geochemical modelling, the researchers found evidence that thawing landscapes intensify chemical weathering, transferring carbon into dissolved inorganic forms while consuming atmospheric CO₂.

Carbon uptake can even exceed emissions
“We found that river CO₂ emissions decline while carbon uptake through rock weathering increases as permafrost cover decreases,” said Liwei Zhang, biogeochemist at East China Normal University. “In some catchments where permafrost has become patchier, weathering-driven carbon uptake was large enough to offset or even exceed river CO₂ emissions.”

Across the study region, the team estimated that carbon uptake from rock weathering offsets roughly 35 percent of river CO₂ emissions on average. In regions with continuous permafrost, the offset was relatively small. However, in landscapes with discontinuous or isolated permafrost, weathering-driven carbon uptake sometimes exceeded 100 percent of river CO₂ emissions, suggesting that geological carbon uptake can rival biological carbon release.

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