Anaerobic oxidation of methane (AOM) at the thaw front of subsea permafrost
Introduction: Thawing arctic subsea permafrost is a source of organic carbon in deep sediment layers. The permafrost that is at its thermal equilibrium releases biologically produced methane and a deep sulfate-methane transition zone (SMTZ) is formed due to sulfate-rich overlaying marine sediment la...
Main Authors: | , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2016
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/47639/ https://hdl.handle.net/10013/epic.63205144-918a-424f-be34-e6bbd2103862 |