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• W2076243370 endingPage "945" @default.
• W2076243370 startingPage "943" @default.
• W2076243370 abstract "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. Here, we report a multiscale (nanometer to micrometer) structural characterization of petrogenic OC in the Himalayan system. We show that graphitic carbon is preserved and buried in marine sediments, while the less graphitized forms are oxidized during fluvial transport. Radiocarbon dating indicates that 30 to 50% of the carbon initially present in the Himalayan rocks is conserved during the erosion cycle. Graphitization during metamorphism thus stabilizes carbon in the crust over geological time scales." @default.
• W2076243370 created "2016-06-24" @default.
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• W2076243370 date "2008-11-07" @default.
• W2076243370 modified "2023-10-14" @default.
• W2076243370 title "Recycling of Graphite During Himalayan Erosion: A Geological Stabilization of Carbon in the Crust" @default.
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• W2076243370 doi "https://doi.org/10.1126/science.1161408" @default.
• W2076243370 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/18988852" @default.
• W2076243370 hasPublicationYear "2008" @default.
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