Claypool, George E; Milkov, Alexei V; Lee, Young-Joo; Torres, Marta E; Borowski, Walter S; Tomaru, Hitoshi (2006): Carbon and deuterium isotopes and C ratios in gas hydrates of ODP Leg 204 sites. PANGAEA, https://doi.org/10.1594/PANGAEA.774729, Supplement to: Claypool, GE et al. (2006): Microbial methane generation and gas transport in shallow sediments of an accretionary complex, southern Hydrate Ridge (ODP Leg 204), offshore Oregon, USA. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-52, https://doi.org/10.2973/odp.proc.sr.204.113.2006
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Sediments at the southern summit of Hydrate Ridge display two distinct modes of gas hydrate occurrence. The dominant mode is associated with active venting of gas exsolved from the accretionary prism and leads to high concentrations (15%-40% of pore space) of gas hydrate in seafloor or near-surface sediments at and around the topographic summit of southern Hydrate Ridge. These near-surface gas hydrates are mainly composed of previously buried microbial methane but also contain a significant (10%-15%) component of thermogenic hydrocarbons and are overprinted with microbial methane currently being generated in shallow sediments. Focused migration pathways with high gas saturation (>65%) abutting the base of gas hydrate stability create phase equilibrium conditions that permit the flow of a gas phase through the gas hydrate stability zone. Gas seepage at the summit supports rapid growth of gas hydrates and vigorous anaerobic methane oxidation.
The other mode of gas hydrate occurs in slope basins and on the saddle north of the southern summit and consists of lower average concentrations (0.5%-5%) at greater depths (30-200 meters below seafloor [mbsf]) resulting from the buildup of in situ-generated dissolved microbial methane that reaches saturation levels with respect to gas hydrate stability at 30-50 mbsf. Net rates of sulfate reduction in the slope basin and ridge saddle sites estimated from curve fitting of concentration gradients are 2-4 mmol/m**3/yr, and integrated net rates are 20-50 mmol/m**2/yr. Modeled microbial methane production rates are initially 1.5 mmol/m**3/yr in sediments just beneath the sulfate reduction zone but rapidly decrease to rates of <0.1 mmol/m**3/yr at depths >100 mbsf. Integrated net rates of methane production in sediments away from the southern summit of Hydrate Ridge are 25-80 mmol/m**2/yr. Anaerobic methane oxidation is minor or absent in cored sediments away from the summit of southern Hydrate Ridge.
Ethane-enriched Structure I gas hydrate solids are buried more rapidly than ethane-depleted dissolved gas in the pore water because of advection from compaction. With subsidence beneath the gas hydrate stability zone, the ethane (mainly of low-temperature thermogenic origin) is released back to the dissolved gas-free gas phases and produces a discontinuous decrease in the C1/C2 vs. depth trend. These ethane fractionation effects may be useful to recognize and estimate levels of gas hydrate occurrence in marine sediments.
Median Latitude: 44.576105 * Median Longitude: -125.127166 * South-bound Latitude: 44.568430 * West-bound Longitude: -125.152500 * North-bound Latitude: 44.586300 * East-bound Longitude: -125.073930
Date/Time Start: 2002-07-13T01:00:00 * Date/Time End: 2002-09-01T00:00:00
204-1244B * Latitude: 44.586160 * Longitude: -125.119860 * Date/Time Start: 2002-07-13T01:00:00 * Date/Time End: 2002-07-13T12:45:00 * Elevation: -896.0 m * Penetration: 54.1 m * Recovery: 56.85 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 54.1 m cored; 0 m drilled; 105.1 % recovery
204-1244C * Latitude: 44.586300 * Longitude: -125.119830 * Date/Time Start: 2002-07-13T12:45:00 * Date/Time End: 2002-07-16T05:30:00 * Elevation: -895.1 m * Penetration: 333.5 m * Recovery: 315.5 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 39 cores; 332 m cored; 1.5 m drilled; 95 % recovery
204-1244E * Latitude: 44.586180 * Longitude: -125.119530 * Date/Time Start: 2002-08-18T23:00:00 * Date/Time End: 2002-08-22T01:45:00 * Elevation: -893.3 m * Penetration: 250 m * Recovery: 137.73 m * Location: North Pacific Ocean * Campaign: Leg204 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 19 cores; 135.8 m cored; 114.2 m drilled; 101.4 % recovery
Datasets listed in this Collection
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T2) Carbon isotope composition of methane and carbon dioxide in void gas of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774717
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T3) Isotope composition of C2-C5 hydrocarbons in void gas of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774718
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T4) Deuterium composition of methane in void gas of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774719
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T5) Carbon isotope composition of methane and carbon dioxide in PCS gas of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774720
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T6) Carbon isotope composition of methane and carbon dioxide in hydrate-bound gas of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774724
- Claypool, GE; Milkov, AV; Lee, Y-J et al. (2006): (Table T7) Isotope composition of dissolved inorganic carbon from interstitial waters of ODP Leg 204 sites. https://doi.org/10.1594/PANGAEA.774725