Glacial retreat converts exposed landscapes from net carbon sinks to sources

Abstract Retreat of continental ice sheets exposes comminuted sediment in disequilibrium with non-glacial conditions. Weathering of this sediment may create climate feedbacks by altering exchange of greenhouse gases between atmosphere and landscapes. Here we show in a partially deglaciated watershed...

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Bibliographic Details
Main Authors: A. J. Pain, J. B. Martin, E. E. Martin, J. T. Salinas-Reyes, C. Bennett
Format: Article
Language:English
Published: Nature Portfolio 2025-05-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02404-z
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