Calcium isotopic evidence for secondary carbonate precipitation in a large river catchment, Southeastern Tibetan Plateau
Peer-Reviewed Publication
Updates every hour. Last Updated: 17-Apr-2026 03:16 ET (17-Apr-2026 07:16 GMT/UTC)
Calcium (Ca) plays a fundamental role in carbonate weathering and the global carbon cycle. Carbonate weathering contributes approximately 80% of the dissolved Ca flux delivered from global rivers to the oceans. Therefore, it is crucial to elucidate the geochemical behavior of Ca isotopes during carbonate weathering. The research group led by Prof. Han Guilin at the China University of Geosciences (Beijing) integrated multi-isotope datasets (including Li-K-Fe-Zn) to investigate the geochemical behavior of Ca isotopes in river water and suspended sediments of the Lancang River during carbonate weathering. This work provides new insights into the global C-Ca cycle. The related findings have now been published in Science China Earth Sciences in 2025.
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