Abstract
Sources of organic matter in Mesozoic sediments from the DSDP Site 330, Falkland Plateau, have been examined. The lipids of a Cretaceous sample are mixed terrigenous and marine, and those of a Jurassic sample are predominantly marine. Kerogens are predominantly oxidized terrigenous detritus, except from an autochthonous marine sample from the middle Jurassic.
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