Sulfate-driven anaerobic oxidation of methane (SD-AOM) controls methane release from
marine sediments to the ocean. A variety of authigenic precipitates within sediments has …

Sediments at marine cold seep areas provide potential archives of past fluid flow, which
allow insights into the evolution of past methane seepage activities. However, signals for …

Sulfate-driven anaerobic oxidation of methane (SD-AOM) and organoclastic sulfate
reduction (OSR) are the two processes that consume sulfate in methane-rich marine …

Methane seeps are widespread on the seafloor in continental margins. However, the
responses of methane flux and diagenetic processes at cold seeps to drastic environmental …

Microbially-mediated methane, S and Fe cycling in the sediments can largely reduce the flux
of methane from the ocean to the atmosphere. Compared to a large number of records …

In this paper, the QS-1 sediments (3.64 m long; at 1500 m water depth) collected from the
Qiongdongnan Basin were used to analyze the relationship between sedimentary …

Release of methane from the seafloor throughout the world's oceans and the
biogeochemical processes involved may have significant effects on the marine sedimentary …

Microbially mediated anaebic oxidation of methane (AOM) coupled with sulfate consumption
within the sulfate methane transition zone (SMTZ) in marine sediments is a widely recorded …

Sulfate-driven anaerobic oxidation of methane (SD-AOM) supports chemosynthesis-based
communities and limits the release of methane from marine sediments. Formation of …

Large amounts of methane are stored along continental margins in the form of methane
hydrate. Methane hydrate is sensitive to environmental change, resulting in the release of …