1996 Volume 30 Issue 1 Pages 35-45
Insoluble macromolecules (kerogen) were isolated from 7 marine and 10 lacustrine sediment samples and subjected to alkaline KMnO4 oxidation, followed by analysis of organic acids in the oxidation products. The major compounds consist of aliphatic C4-C15α, ω-dicarboxylic acids, n-C7-C28 monocarboxylic acids and benzene mono-to-polycarboxylic acids. The α, ω-dicarboxylic acids from lacustrine kerogens have a maximum at C8 or C9. Whereas those from marine ones show a shoulder in this carbon range, have a maximum at C4 and decrease with increasing carbon number. This difference in the relative abundance of C4 and C8, C9 α, ω-dicarboxylic acids may be due to different precursory materials in the different environments. This result is in accordance with our previous findindg, suggesting strongly that a portion of the chemical structures of kerogens from marine and lake environments is generally different from each other. A mathematical expression was proposed to visualize the feature of molecular distribution of α, ω- dicarboxylic acids from kerogens. In addition, it is shown by both alkaline CuO oxidation and KMnO4 experiments that polymerized structure of polyhydroxy acids can be one of the precursors for α, ω-dicarboxylic acids from kerogens.