Geochemical evidence for seabed fluid flow linked to the subsea permafrost outer border in the South Kara Sea

Driven by rising bottom water temperatures, the thawing of subsea permafrost leads to an increase in fluid flow intensity in shallow marine sediments and results in the emission of methane into the water column. Limiting the release of permafrost-related gas hydrates and permafrost- sequestered meth...

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Bibliographic Details
Published in:Geochemistry
Main Authors: Semenov, Petr, Portnov, Aleksei D, Krylov, Alexey, Egorov, Alexander V, Vanshtein, Boris
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2019
Subjects:
Online Access:https://hdl.handle.net/10037/18472
https://doi.org/10.1016/j.chemer.2019.04.005