Ti. Eglinton, CARBON ISOTOPIC EVIDENCE FOR THE ORIGIN OF MACROMOLECULAR ALIPHATIC STRUCTURES IN KEROGEN, Organic geochemistry, 21(6-7), 1994, pp. 721-735
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.