Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1977-09

AUTHORS

Hilary Irwin, Charles Curtis, Max Coleman

ABSTRACT

Organic matter is modified by several processes operating at different depths during burial diagenesis: (1) sulphate reduction; (2) fermentation; (3) thermally-induced decarboxylation, and so on. CO2, one common product of each, can be distinguished by its carbon isotope composition: approximately (1) −25‰, (2) +15‰, (3) −20‰ relative to PDB. These values are preserved in diagenetic carbonates of the Upper Jurassic Kimmeridge Clay. Independent corroboration of the relative dominance of each process within specific depth intervals is given by the isotopic composition of incorporated oxygen which is temperature dependent (1) 0 to −2‰, (2) −1.5 to −5‰,(3) −3.5 to −7.0‰. More... »

PAGES

209-213

Journal

TITLE

Nature

ISSUE

5625

VOLUME

269

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/269209a0

DOI

http://dx.doi.org/10.1038/269209a0

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1015093402


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