Himalayan Pyrite Oxidation Can Outweigh Silicate Weathering, Turning Some Glacier Basins into Net CO2 Sources
hindustantimes.comA new study from IISER Pune reveals that pyrite oxidation in the glaciated upper Indus basin can release more CO2 than silicate weathering absorbs, turning some Himalayan landscapes into net geological carbon sources. Published in Chemical Geology, the research used sulfur and oxygen isotopes to track contributions from pyrite oxidation. While this operates over millions of years and is not comparable to human emissions, it challenges the assumption that mountain weathering always acts as a carbon sink. The findings highlight the complexity of geological carbon cycling, especially in rapidly eroding regions. For those working on carbon markets or climate policy, this is a reminder that natural baselines are not static. The study calls for considering pyrite oxidation in glacier-fed catchments when assessing long-term carbon budgets.
