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Open AccessLong-term organic carbon preservation enhanced by iron and manganese
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 ...
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Open AccessCarboxyl-richness controls organic carbon preservation during coprecipitation with iron (oxyhydr)oxides in the natural environment
The coprecipitation of organic carbon with iron minerals is important for its preservation in soils and sediments, but the mechanisms for carbon-iron interactions and thus the controls on organic carbon cyclin...
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Ecological variables for deep-ocean monitoring must include microbiota and meiofauna for effective conservation
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Open AccessInfluence of hydro-climatic factors on future coastal land susceptibility to erosion in Bangladesh: a geospatial modelling approach
This study envisaged the likely impacts of future hydro-climatic changes on the susceptibility of coastal land to erosion through the development of raster-based geographical information system (GIS) model cal...
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Open AccessHydrothermal activity, functional diversity and chemoautotrophy are major drivers of seafloor carbon cycling
Hydrothermal vents are highly dynamic ecosystems and are unusually energy rich in the deep-sea. In situ hydrothermal-based productivity combined with sinking photosynthetic organic matter in a soft-sediment setti...
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Open AccessThe long-term fate of permafrost peatlands under rapid climate warming
Permafrost peatlands contain globally important amounts of soil organic carbon, owing to cold conditions which suppress anaerobic decomposition. However, climate warming and permafrost thaw threaten the stabil...