Research Article

Gas Seepage along the Edge of the Aquitaine Shelf (France): Origin and Local Fluxes

Table 3

Comparison of gas-bubble fluxes from different settings.

SettingWater depth (m)Gas flux (×103 mol⋅yr−1)Flux measurement techniqueGas originCommentReference

Aquitaine shelf140–18038.2Video recording of gas bubbling through a graduated volumeBiogenicMeasurement for 9 individual streamsThis work
Eastern Mediterranean Sea
(Hydrate site)
1500–1800230–2300Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observationsBiogenicAverage measurement for 20 individual streams[76]
Hakon Mosby MV
(Hydrate site)
12506307ROV observationsBiogenicMeasurement of gas discharge from open faults
and mud volcano
[77]
Makran continental margin
(Hydrate site)
575–287010330Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observationsBiogenicMeasurement from 3 gas flares composed of several streams and extrapolation to all identified flares (>20)[78]
Don-Kuban paleo-fan (Black Sea)
(Hydrate site)
8902000–87000Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observationsBiogenicAverage measurement from ~600 acoustic flares over 106 m2 surface area[79]
Northern summit of Hydrate Ridge
(Hydrate site)
125021900Video recording of gas displacing a fluid through a PVC funnelBiogenicMeasurement for 10 individual streams over 80 m2 surface area[80]
UK Block 15/251671064Gas rate measurementsThermogenicSurveyed area of surface area[81]