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...
Published in: | Geochemistry |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2019
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/18472 https://doi.org/10.1016/j.chemer.2019.04.005 |