Marine cold seeps are windows into different depth levels of the submerged geosphere.
Subduction zones and organic-rich passive margins host most of the world's cold seeps. The …

Seafloor methane release due to the thermal dissociation of gas hydrates is pervasive
across the continental margins of the Arctic Ocean. Furthermore, there is increasing …

Methane trapped in marine sediments surrounding continental margins can be driven by
tectonic stress to escape into the oceans. What geological processes control their spatial …

High-resolution 2D seismic data reveal the character and distribution of up to four stacked
bottom simulating reflectors (BSR) within the channel-levee systems of the Danube deep …

Abstract The Pliocene and Pleistocene sediments at lease block Green Canyon 955
(GC955) in the Gulf of Mexico include sand-rich strata with high saturations of gas hydrate; …

The Pliocene cold‐seep carbonate of the Crotone Basin (South Italy) represents a key site
for dimension, outcrop** exposure and quality. These deposits form a large carbonate …

Cold seeps are characterized by high biomass, which is supported by the microbial
oxidation of the available methane by capable microorganisms. The carbon is subsequently …

Marine sediments host large amounts of methane (CH4), which is a potent greenhouse gas.
Quantitative estimates for methane release from marine sediments are scarce, and a poorly …

The interactions of microbial methane generation in fine-grained clay-rich sediments,
methane migration, and gas hydrate accumulation in coarse-grained, sand-rich sediments …

Marine controlled source electromagnetic (CSEM) data have been collected to investigate
methane seep sites and associated gas hydrate deposits at Opouawe Bank on the southern …