Abstract
Low- and high-molecular-weight organic sulphur compounds were analyzed in a selected number of samples of the Permian Kupferschiefer (Poland). Their significant presence in these mature samples supports the hypothesis that during deposition, and shortly thereafter, labile organic sulphur compounds must have been very abundant. This assumption has led to a new model for metal accumulation, based on a slow and gradual release of sulphur from these labile organic sulphur compounds during increasing diagenesis.
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