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Title: Hydrogen isotope composition of insoluble organic matter from cherts

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1]
  1. California Institute of Technology, Pasadena (USA)

No systematic variation is seen in the D/H ratio of insoluble organic matter present in cherts that were deposited over the last 3.5. B.y. Hydrogen isotope exchange experiments between deuterium-rich acid solutions and acid residues extracted from cherts show that hydrogen, extracted after the chert was outgassed at 350{degree}C, is not affected by the contamination from the chemical treatment of the samples. In two modern cherts (Eocene and Pliocene) having exceptionally low {delta}{sup 18}O values and high carbon contents, hydrogen extracted by pyrolysis at low temperature (200-350{degree}C) is markedly enriched in deuterium ({delta}D values up to +500{per thousand}). Such an enrichment is ascribed to organic products derived from the maturation of kerogen. Provided this hydrogen isotope fractionation is not related to biological activity, a similar effect could have played a role in the maturation of the deuterium-rich organic matter found in the carbonaceous meteorites during an early hydrothermal event.

OSTI ID:
5062163
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 53:2; ISSN 0016-7037
Country of Publication:
United States
Language:
English