Pape, Thomas; Bahr, André; Klapp, Stephan A; Abegg, Friedrich; Bohrmann, Gerhard (2011): Hydrate abundances at the high-flux Batumi seep area in the southeastern Black Sea. PANGAEA, https://doi.org/10.1594/PANGAEA.763866, Supplement to: Pape, T et al. (2011): High-intensity gas seepage causes rafting of shallow gas hydrates in the southeastern Black Sea. Earth and Planetary Science Letters, 307, 35-46, https://doi.org/10.1016/j.epsl.2011.04.030
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Submarine gas hydrates are a major global reservoir of the potent greenhouse gas methane. Since current assessments of worldwide hydrate-bound carbon vary by one order of magnitude, new technical efforts are required for improved and accurate hydrate quantifications. Here we present hydrate abundances determined for surface sediments at the high-flux Batumi seep area in the southeastern Black Sea at 840 m water depth using state-of-the art autoclave technology. Pressure sediment cores of up to 2.65 m in length were recovered with an autoclave piston corer backed by conventional gravity cores. Quantitative core degassing yielded volumetric gas/bulk sediment ratios of up to 20.3 proving hydrate presence. The cores represented late glacial to Holocene hemipelagic sediments with the shallowest hydrates found at 90 cmbsf. Calculated methane concentrations in the different cores surpassed methane equilibrium concentrations in the two lowermost lithological Black Sea units sampled. The results indicated hydrate fractions of 5.2% of pore volume in the sapropelic Unit 2 and mean values of 21% pore volume in the lacustrine Unit 3. We calculate that the studied area of ~ 0.5 km**2 currently contains about 11.3 kt of methane bound in shallow hydrates. Episodic detachment and rafting of such hydrates is suggested by a rugged seafloor topography along with variable thicknesses in lithologies. We propose that sealing by hydrate precipitation in coarse-grained deposits and gas accumulation beneath induces detachment of hydrate/sediment chunks. Floating hydrates will rapidly transport methane into shallower waters and potentially to the sea-atmosphere boundary. In contrast, persistent in situ dissociation of shallow hydrates appears unlikely in the near future as deep water warming by about 1.6 °C and/or decrease in hydrostatic pressure corresponding to a sea level drop of about 130 m would be required. Because hydrate detachment should be primarily controlled by internal factors in this area and in similar hydrated settings, it serves as source of methane in shallow waters and the atmosphere which is mainly decoupled from external forcing.
Median Latitude: 41.957927 * Median Longitude: 41.290267 * South-bound Latitude: 41.956833 * West-bound Longitude: 41.287833 * North-bound Latitude: 41.959117 * East-bound Longitude: 41.292417
Date/Time Start: 2007-03-19T18:44:00 * Date/Time End: 2007-04-11T13:09:00
Batumi_seep_Backscatter_area * Latitude: 41.958150 * Longitude: 41.291030 * Location: Batumi seep area * Method/Device: Multiple investigations (MULT) * Comment: Backscatter area 1,172,500 m**3
Batumi_seep_sampled_area * Latitude: 41.958150 * Longitude: 41.291030 * Location: Batumi seep area * Method/Device: Multiple investigations (MULT) * Comment: Sampled area 569,835 m**
Datasets listed in this publication series
- Pape, T; Bahr, A; Klapp, SA et al. (2011): (Table 2) Specifics of pressure cores recovered with the DAPC. https://doi.org/10.1594/PANGAEA.763856
- Pape, T; Bahr, A; Klapp, SA et al. (2011): (Table 3) Total methane volume (VCH4t) in the individual core, nominal methane in situ concentrations (nCCH4U3), and concentrations of hydrate-bound methane (CCH4hbU3) in Unit 3, as well as contents of gas hydrates in Units 2 and 3. https://doi.org/10.1594/PANGAEA.763857
- Pape, T; Bahr, A; Klapp, SA et al. (2011): (Table 4) Amounts of hydrate-bound and overall C1 to C3-hydrocarbons stored in Batumi seep area surface sediments. https://doi.org/10.1594/PANGAEA.763860
- Pape, T; Bahr, A; Klapp, SA et al. (2011): (Table 5) Unit-specific lengths (LsUx), pore fluid volumes (VpfUx), pore fluid masses (mpfUx), and methane masses (mCH4Ux) calculated for pressure cores from the Batumi seep area. https://doi.org/10.1594/PANGAEA.763862