Biomethane produced from maize grown on peat emits more CO2 than natural gas
Microbially-enhanced silicate weathering in agricultural soils to remove carbon dioxide
Climate Change and terrigenous inputs decrease the efficiency of the future Arctic Ocean’s biological carbon pump
Climate variability shifts the vertical structure of phytoplankton in the Sargasso Sea
Giant clams modify crystallographic and geochemical pathways of shell formation in response to turbidity
Experimental Warming and Drying Increase the Age of Soil Respired Carbon in Lowland Tropical Forests
Reduced Arctic Ocean CO2 uptake due to coastal permafrost erosion
Elevated CO2 levels promote both carbon and nitrogen cycling in global forests
Long-term flux measurements suggest dynamic emission factors are needed for rewetted peatlands
Alpha-glucans from bacterial necromass indicate an intra-population loop within the marine carbon cycle