CARBON ISOTOPIC EVIDENCE FOR THE ORIGIN OF MACROMOLECULAR ALIPHATIC STRUCTURES IN KEROGEN

Authors
Citation
Ti. Eglinton, CARBON ISOTOPIC EVIDENCE FOR THE ORIGIN OF MACROMOLECULAR ALIPHATIC STRUCTURES IN KEROGEN, Organic geochemistry, 21(6-7), 1994, pp. 721-735
Citations number
72
Categorie Soggetti
Geosciences, Interdisciplinary
Journal title
ISSN journal
01466380
Volume
21
Issue
6-7
Year of publication
1994
Pages
721 - 735
Database
ISI
SICI code
0146-6380(1994)21:6-7<721:CIEFTO>2.0.ZU;2-M
Abstract
This study describes compound-specific stable carbon isotopic analyses of aliphatic hydrocarbon products from flash pyrolysis (800-degrees-C , 20 s) of kerogens representing a range of depositional environments (marine, estuarine, lacustrine) and ages (Recent to Ordovician). The c arbon isotopic measurements were obtained, using isotopo-ratio-monitor ing gas chromatography-mass spectrometry (irmGC-MS), for the major ali phatic pyrolysis products (n-hydrocarbons, acyclic isoprenoids and hop anoids). While isotopic compositions of n-hydrocarbons varied substant ially between samples (average values ranged from -35 to -14 parts per thousand), delta-values of n-alkenes and n-alkanes generated from a g iven sample generally ranged over less than +/-3 parts per thousand. T his isotopic uniformity implies a common origin for n-hydrocarbons (pr obably from thermal dissociation of biopolymers), supporting the conce pt of selective preservation of highly resistant aliphatic structures in kerogens. There are notable exceptions to this general relationship , in which either mixed biopolymeric sources (e.g. Guttenberg Fm) or m inor contributions from aliphatic biopolymers (e.g. Monterey) must be inferred. In several cases, average n-hydrocarbon values also closely match the corresponding total organic carbon (TOC) delta-value, indica ting that the n-hydrocarbons in these samples are derived from structu rally important, or at least isotopically representative, constituents of the kerogen. In other samples significant discrepancies were obser ved between the delta-values for these products and deltaC-13(TOC). In these caws the presence of additional components not yielding hydroca rbons on pyrolysis is indicated. Isotopic compositions of isoprenoid h ydrocarbons varied non-systematically relative to those of n-hydrocarb ons, whereas hopanoid hydrocarbons were consistently depleted in C-13 relative to both TOC and n-hydrocarbons, with delta-values as low as - 50 parts per thousand.