Dataset - B2FIND

(Table 1) Pressure upon recovery of sediment and gas samples at the Batumi se...

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(Figure 5) Pore-water concentration of chloride in sediment core GeoB11913 fr...

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Hydrate abundances at the high-flux Batumi seep area in the southeastern Blac...

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...

Mineralogical and stable isotope analyses of carbonates from the eastern Blac...

Authigenic carbonates associated with cold seeps provide valuable archives of changes in the long-term seepage activity. To investigate the role of shallow-buried hydrates on...

Gas analysis of sediment cores from the Batumi seep area

Detailed knowledge of the extent of post-genetic modifications affecting shallow submarine hydrocarbons fueled from the deep subsurface is fundamental for evaluating source and...

Pore-water concentration of chloride in sediment cores and equilibrium temper...

Vodyanitskii mud volcano is located at a depth of about 2070 m in the Sorokin Trough, Black sea. It is a 500-m wide and 20-m high cone surrounded by a depression, which is...

Swath sonar multibeam EM120 bathymetry during METEOR cruise M72/3 with links ...

Multibeam data were collected during R/V Meteor cruise M72/3 leading to easterly Black Sea. Multibeam sonar system was Kongsberg Simrad EM-120. Data are unprocessed and may...

(Table 1) Mean grain sizes and standard deviations of gas hydrate samples

Methane hydrates are present in marine seep systems and occur within the gas hydrate stability zone. Very little is known about their crystallite sizes and size distributions...