On the fate of past gas: What happens to methane released from a bacterially mediated gas hydrate capacitor?
- 9 January 2001
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 2 (1)
- https://doi.org/10.1029/2000gc000131
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- A molecular recorder of methane hydrate destabilizationGeochemistry, Geophysics, Geosystems, 2001
- Massive dissociation of gas hydrate during a Jurassic oceanic anoxic eventNature, 2000
- Formation of gas hydrate from dissolved gas in natural porous mediaMarine Geology, 2000
- The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal MaximumScience, 1999
- Direct measurement of in situ methane quantities in a large gas-hydrate reservoirNature, 1997
- Marine pore-water sulfate profiles indicate in situ methane flux from underlying gas hydrateGeology, 1996
- Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the PaleocenePaleoceanography and Paleoclimatology, 1995
- Late Paleocene to Eocene paleoceanography of the equatorial Pacific Ocean: Stable isotopes recorded at Ocean Drilling Program Site 865, Allison GuyotPaleoceanography and Paleoclimatology, 1995
- Potential distribution of methane hydrates in the world's oceansGlobal Biogeochemical Cycles, 1994
- Pleistocene slope instability of gas hydrate‐laden sediment on the Beaufort sea marginMarine Geotechnology, 1991