|
Setting | Water depth (m) | Gas flux (×103 mol⋅yr−1) | Flux measurement technique | Gas origin | Comment | Reference |
|
Aquitaine shelf | 140–180 | 38.2 | Video recording of gas bubbling through a graduated volume | Biogenic | Measurement for 9 individual streams | This work |
Eastern Mediterranean Sea (Hydrate site) | 1500–1800 | 230–2300 | Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observations | Biogenic | Average measurement for 20 individual streams | [76] |
Hakon Mosby MV (Hydrate site) | 1250 | 6307 | ROV observations | Biogenic | Measurement of gas discharge from open faults and mud volcano | [77] |
Makran continental margin (Hydrate site) | 575–2870 | 10330 | Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observations | Biogenic | Measurement from 3 gas flares composed of several streams and extrapolation to all identified flares (>20) | [78] |
Don-Kuban paleo-fan (Black Sea) (Hydrate site) | 890 | 2000–87000 | Combination of gas analysis, ship-based hydroacoustic surveys, bubble size modeling, and ROV observations | Biogenic | Average measurement from ~600 acoustic flares over 106 m2 surface area | [79] |
Northern summit of Hydrate Ridge (Hydrate site) | 1250 | 21900 | Video recording of gas displacing a fluid through a PVC funnel | Biogenic | Measurement for 10 individual streams over 80 m2 surface area | [80] |
UK Block 15/25 | 167 | 1064 | Gas rate measurements | Thermogenic | Surveyed area of surface area | [81] |
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