作者: Miriam Römer , Heiko Sahling , Thomas Pape , André Bahr , Tomas Feseker
DOI: 10.1016/J.MARGEO.2012.07.005
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摘要: Abstract We investigated gas bubble emissions at the Don–Kuban paleo-fan in northeastern Black Sea regarding their geological setting, quantities as well spatial and temporal variabilities during three ship expeditions between 2007 2011. About 600 bubble-induced hydroacoustic anomalies water column (flares) originating from seafloor above hydrate stability zone (GHSZ) ~ 700 m depth were found. At about 890 m a hydrocarbon seep area named “Kerch area” was newly discovered within GHSZ. propose locally domed sediments (“mounds”) ultra-high resolution bathymetric mapping with an autonomous underwater vehicle (AUV) to result accumulation shallow depths. In situ measurements indicated spatially limited temperature elevations sediment likely induced by upward fluid flow which may confine local GHSZ few meters below seafloor. As result, bubbles are suspected migrate into near-surface escape through small-scale faults. Hydroacoustic surveys revealed that several flares originated of 1 km2 size. The highest flare disappeared 350 m depth, suggesting released methane remains column. A flux estimate, combining data visual quantifications dives remotely operated (ROV) results ship-based analysis 2 87 × 106 mol CH4 yr− 1 escaped Kerch area. Our show finding represents so far underestimated type seep, has be considered budget calculations.