Greenhouse gas release from permafrost found to be influenced by mineral binding processes
A piece of the drilled permafrost core extracted during drilling operations on the New Siberian Islands in the North of eastern Siberia. Credit: Lutz Schirrmeister, Alfred Wegener Institute
About a quarter of the organic carbon contained in ice-rich Arctic permafrost is more difficult for microorganisms to utilize. The reason for this is a strong binding of the organic material originating from dead plant remains to mineral…