Stein, Ruediger; Rullkötter, Jürgen; Kalkreuth, Wolfgang; Welte, Dietrich Hugo (1987): Quantity, provenance, and thermal maturity of organic matter at DSDP Holes 95-612 and 95-613. PANGAEA, https://doi.org/10.1594/PANGAEA.788527, Supplement to: Stein, R et al. (1987): Quantity, provenance, and thermal maturity of organic matter from the New Jersey Continental Margin, Deep Sea Drilling Project Leg 95. In: Poag, CW; Watts, AB; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 95, 651-659, https://doi.org/10.2973/dsdp.proc.95.128.1987
Always quote above citation when using data! You can download the citation in several formats below.
Using methods of analysis from organic geochemistry and organic petrography, we investigated six Pliocene to Maestrichtian samples from DSDP Site 612 and five Pliocene to Eocene samples from DSDP Site 613 for the quantity, type, and thermal maturity of organic matter.
At both sites, organic carbon content is low in the Eocene samples (0.10 to 0.20%) and relatively high in the Pliocene/Miocene samples (0.87 to 1.15%). The Maestrichtian samples from Site 612 contain about 0.6% organic carbon. The organic matter is predominantly terrigenous, as indicated by low hydrogen index values from Rock-Eval pyrolysis and the dominance of long-chain wax alkanes in the extractable hydrocarbons. The organic matter is at a low level of thermal maturity; measured vitrinite reflectance values were between 0.27 and 0.44%.
Median Latitude: 38.795600 * Median Longitude: -72.648800 * South-bound Latitude: 38.771000 * West-bound Longitude: -72.773800 * North-bound Latitude: 38.820200 * East-bound Longitude: -72.523800
Date/Time Start: 1983-08-26T00:00:00 * Date/Time End: 1983-09-17T00:00:00