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Title: Changes in kerogen composition across an oxidation front in map turbidites as revealed by pyrolysis GC-MS

Conference ·
OSTI ID:539021

We have studied four Madeira Abyssal Plain (MAP) TOC rich turbidites for the influence of post depositional oxidation on organic matter composition. Kerogens were isolated and studied by pyrolysis-GC-MS analysis. This showed that the kerogen of the oxidized part of the turbidite is chemically significantly different from the unoxidized part. The relative amount of saturated and unsaturated n-alkanes has increased substantially (e.g. increase from 39 to 62%), at the cost of the isoprenoid alkanes and alkylated thiophenes (e.g. decrease from 16 to 6%, 8 to 3% respectively). In addition, large differences in the internal distributions of the various compound groups of the pyrolysates were observed. For example, prist-1-ene and 1,2,3,4-tetramethylbenzene were markedly decreased in the pyrolysates of the oxidized part of the turbidites. These results strongly support the selective preservation of high molecular weight aliphatic biopolymeric substances under oxidative conditions.

OSTI ID:
539021
Report Number(s):
CONF-960807-; TRN: 97:004029-0089
Resource Relation:
Conference: 212. national meeting of the American Chemical Society (ACS), Orlando, FL (United States), 25-30 Aug 1996; Other Information: PBD: 1996; Related Information: Is Part Of 212th ACS national meeting; PB: 1830 p.
Country of Publication:
United States
Language:
English

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