Post-glacial climate forcing of surface processes in the Ganges–Brahmaputra river basin and implications for carbon sequestration
Résumé
Climate has been proposed to control both the rate of terrestrial silicate weathering and the export rate of associated sediments and terrestrial organic carbon to river-dominated margins and thus the rate of sequestration of atmospheric CO 2 in the coastal ocean-over glacial interglacial timescales. Focused on the Ganges-Brahmaputra rivers, this study presents records of post-glacial changes in basin-scale Indian summer monsoon intensity and vegetation
Origine : Fichiers produits par l'(les) auteur(s)
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