Abstract

The role of organic matter in Mississippi Valley-type Pb-Zn deposits has been studied by systematically sampling and characterizing various types of organic matter in the Upper Cambrian Bonneterre formation in lead-zinc mines from the Viburnum Trend and from rocks as far as 20 km away from the Trend. Organic matter that is several kilometers from ore consists of insoluble disseminated kerogen in carbonates. Kerogen from brown dolostones yields mainly n-alkane pyrolysis products up to approximately n-C 20 H 42 , whereas gray and white carbonates that are poorer in organic carbon give much smaller quantities of pyrolysis products. Within meters to centimeters of ore in the Milliken mine, at the south end of the Viburnum Trend, organic matter occurs as solid, partly soluble tacky bitumen and insoluble hard blebs of millimeter to centimeter size. These hydrocarbon materials also yield n-alkane pyrolysis products up to C 20 . In contrast, the solid insoluble organic matter in intimate contact (intergrown) with ore (galena and chalcopyrite) is friable and brittle. Products from pyrolysis-gas chromatography-mass spectrometry of this material are quite different from the kerogen in rocks or the hydrocarbon blebs; they are substituted aromatic molecules such as toluene and methyl naphthalene, rather than n-alkanes.The sulfur content of solid organic matter from the Milliken mine varies and is lowest for tacky material away from ore, intermediate for blebs near ore, and highest for friable material in intimate contact with ore.Pyrolysis-gas chromatography of this sample suite documents the progression of kerogen (far from ore) through solid petroleumlike material (near ore) to degraded organic matter (in contact with ore). The change in the organic matter from n-alkane to a hydrogen poorer aromatic character with a higher sulfur content when associated with sulfide ores, suggests that chemical reactions such as nonbiological (thermochemical) sulfate reduction, which consume hydrogen and produce reactive sulfur, were responsible for organic degradation.

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