Laboratory for Arctic Research, V.I. Ilichov Pacific Oceanological Institute (POI), Far Eastern Branch of the Russian Academy of Sciences, Vladivostok, Russia
Igor Semiletov
Laboratory for Arctic Research, V.I. Ilichov Pacific Oceanological Institute (POI), Far Eastern Branch of the Russian Academy of Sciences, Vladivostok, Russia
Laboratory for Integrated Research of the Arctic System “land-shelf”, National Tomsk State Research University (TSU), Tomsk, Russia
Laboratory of Chemical and Biological Research, Sakhalin State University (SakhSU), Yuzhno-Sakhalinsk, Russia
Natalia Shakhova
Laboratory for Integrated Research of the Arctic System “land-shelf”, National Tomsk State Research University (TSU), Tomsk, Russia
Sadovsky Institute of Geosphere Dynamics (IGD) of the Russian Academy of Sciences, Moscow, Russia
Thawing subsea permafrost in the East Siberian Arctic Seas releases methane, a potent greenhouse gas. Using molecular fossils in sediments, we traced aerobic methane oxidation as a proxy of enhanced methane cycling across the Laptev Sea, including in regions once thought low in emissions. This approach captures long-term patterns of methane cycling over years-decades , overcoming limits of short-term seawater measurements and highlights the importance of the Laptev Sea in Arctic methane cycling.
Thawing subsea permafrost in the East Siberian Arctic Seas releases methane, a potent greenhouse...