(Table 1) Molecular and carbon-isotopic compositions of void gas from DSDP Leg 96

• Main Authors: Pflaum, Ronald C, Brooks, James M, Cox, H Benjamin, Kennicutt, Mahlon C, Sheu, Der-Duen
• Format: Dataset
• Language: English
• Published: PANGAEA 1986
• Subjects: 96-618; 96-619; 96-620; 96-621; Carbon dioxide; Deep Sea Drilling Project; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Elevation of event; Ethane; Event label; Gas chromatograph Carle Model 800; Gas chromatograph Hewlett-Packard 571OA; Glomar Challenger; Gulf of Mexico; Gulf of Mexico/BASIN; Gulf of Mexico/FAN; Latitude of event; Leg96; Longitude of event; Mass spectrometer Nuclide RMS 60; Methane; Methane/ethane ratio; Sample code/label; δ13C; Orca
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.788218; https://doi.org/10.1594/PANGAEA.788218

Molecular and isotopic compositions of void gases from Sites 618 and 619 were determined. The gases were predominantly methane with the C1/C2 ratios averaging 4,000 and 26,000 at Sites 618 and 619, respectively. The delta13C-C1 values at Site 618 were nearly constant, ranging from - 70.1 to - 73.7 per mil. delta13C-CH1 values for Site 619 between 76 and 178 meters sub-bottom ranged from - 94.8 to - 70.8 per mil, becoming progressively heavier with depth. The molecular and isotopic compositions at both sites are characteristic of biogenic methane. Small spheres (~ 1-2 mm diameter) of gas hydrates were observed in the Orca Basin between 20 and 40 m sub-bottom and were often associated with sandy sections. The hydrate was predominantly methane with a delta13-C1 of - 7 per mil and trace amounts of ethane, propane, and carbon dioxide. The isotopic value for the methane was similar to that of the nearest gas pocket, indicating that hydrate was formed from predominantly biogenic methane without isotopic fractionation.