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Long-term organic carbon preservation enhanced by iron and manganese - Nature

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Long-term organic carbon preservation enhanced by iron and manganese - Nature

The balance between degradation and preservation of sedimentary organic carbon (OC) is important for global carbon and oxygen cycles1. The relative importance of different mechanisms and environmental conditions contributing to marine sedimentary OC preservation, however, remains unclear2–8. Simple organic molecules can be geopolymerized into recalcitrant forms by means of the Maillard reaction5, although reaction kinetics at marine sedimentary temperatures are thought to be slow9,10.

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Long-term organic carbon preservation enhanced by iron and manganese - Nature

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Long-term organic carbon preservation enhanced by iron and manganese - Nature

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