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Organic matter in turbidite sediments of the Moroccan Basin appears to be derived primarily from terrigenous sources. Sediments with greater than 0.3 per cent organic carbon also contain a variable component of organic matter produced in the water column at the site of deposition. The organic matter shows evidence of progressive thermal alteration with increasing depth of burial, but even in the deepest sample (1532 m) it is still immature with respect to the degree of thermal alteration required to attain advanced stages of the petroleum hydrocarbon generation process.

Analysis of Organic Matter in Sediment Cores from the Moroccan Basin, Deep Sea Drilling Project Sites 415 and 416