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Geopolymerization threatens the persistence of organic carbon associated with iron in anoxic environments - Nature Communications
Abstract The sequestration of organic carbon (OC) through mineral association in soils and sediments is a crucial process that regulates carbon sink dynamics and the global carbon cycle. However, minerals can participate in both abiotic and biotic OC transformations, altering the persistence of mineral-associated OC under anoxic conditions.
Human Activity Coupled With Climate Change Strengthens the Role of Lakes as an Active Pipe of Dissolved Organic Matter
1 Introduction Lakes are hotspots in carbon transformation and storage, playing a pivotal role in mediating the global carbon cycle and Earth's climate. Lakes process organic carbon at decomposition rates one or two orders of magnitude higher than those observed in soils (Catalán et al., 2016) and contribute to the release of carbon dioxide (CO2) and methane (CH4) into the atmosphere.
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