At geological time scales, the role of continental erosion in the organic carbon (OC) cycle is determined by the balance between recent OC burial and petrogenic OC oxidation. Evaluating its net effect on the concentration of carbon dioxide and dioxygen in the atmosphere requires the fate of petrogenic OC to be assessed.
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/recycling-graphite-during-himalayan-erosion-geological-stabilization-carbon-crust
[2] http://admin.indiaenvironmentportal.org.in/category/author/valier-galy
[3] http://admin.indiaenvironmentportal.org.in/category/author/olivier-beyssac
[4] http://admin.indiaenvironmentportal.org.in/category/author/christian-france-lanord-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/science
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/himalaya
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/indo-gangetic-plains
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/rivers
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/brahmaputra
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/ganga
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sediment-transport
[12] http://admin.indiaenvironmentportal.org.in/category/thesaurus/carbon-dioxide
[13] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[14] http://admin.indiaenvironmentportal.org.in/category/thesaurus/carbon-sinks
