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• W2891451637 abstract "Abstract Geophysical data from the South Kara Sea reveal U-shaped erosional structures buried beneath the 50–250 m deep seafloor of the continental shelf across an area of ~32 000 km 2 . These structures are interpreted as thermokarst, formed in ancient yedoma terrains during Quaternary interglacial periods. Based on comparison to modern yedoma terrains, we suggest that these thermokarst features could have stored approximately 0.5 to 8 Gt carbon during past climate warmings. In the deeper parts of the South Kara Sea (>220 m water depth) the paleo thermokarst structures lie within the present day gas hydrate stability zone, with low bottom water temperatures −1.8 o C) keeping the gas hydrate system in equilibrium. These thermokarst structures and their carbon reservoirs remain stable beneath a Quaternary sediment blanket, yet are potentially sensitive to future Arctic climate changes." @default.
• W2891451637 created "2018-09-27" @default.
• W2891451637 creator A5008117177 @default.
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• W2891451637 date "2018-09-25" @default.
• W2891451637 modified "2023-10-10" @default.
• W2891451637 title "Shallow carbon storage in ancient buried thermokarst in the South Kara Sea" @default.
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• W2891451637 doi "https://doi.org/10.1038/s41598-018-32826-z" @default.
• W2891451637 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/6156565" @default.
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