H. Wilkes et al., Anaerobic degradation and carbon isotopic fractionation of alkylbenzenes in crude oil by sulphate-reducing bacteria, ORG GEOCHEM, 31(1), 2000, pp. 101-115
A mesophilic enrichment culture of sulphate-reducing bacteria isolated from
the water phase of a North Sea oil tank using oil from the same tank as so
le source of carbon and energy specifically depletes certain CL-CS alkylben
zenes in crude oil during growth. The enrichment culture grows on oils of d
ifferent origin and composition resulting in similar patterns of alkylbenze
ne depletion. Two pure cultures of sulphate-reducing bacteria, strain oXyS1
and mXyS1 which were isolated on o-xylene and m-xylene, respectively, also
grow on crude oil. Strain oXyS1 preferentially depletes o-xylene and o-eth
yltoluene while strain mXyS1 preferentially depletes In-xylene and m-ethylt
oluene. Roth strains also utilize toluene. The degradative patterns of the
pure cultures are complementary and their combination results in the degrad
ative pattern of the enrichment culture. During growth of the enrichment cu
lture and the pure strains on crude oil alkylated benzoic acids were the ma
in metabolic products, which were isolated from the water phases of the inc
ubation experiments. The patterns of alkylated benzoic acids produced by th
e pure cultures are again complementary with respect to the pattern observe
d for the enrichment culture. The spectrum of alkylated benzoic acids sugge
sts that partial oxidation of alkylbenzenes, which do not support growth, t
akes place resulting in the formation of dead-end metabolites. Alkylphenyls
uccinic and fumaric acids were produced in trace amounts only. The portion
of alkylbenzenes remaining in crude oil becomes enriched in C-13 during gro
wth of bacteria. From the data obtained in this study it can be estimated t
hat the carbon isotopic fractionation of the initial reaction of alkylbenze
ne degradation by the present bacteria is between -26 and -33 parts per tho
usand. We suggest that the variability in alkylbenzene concentrations and t
heir carbon isotopic signature together with the occurrence of alkylated be
nzoic acids may be used as a specific indicator of initial biodegradation o
f crude oils and fossil fuel products by sulphate-reducing bacteria in vari
ous environments. (C) 2000 Elsevier Science Ltd. All rights reserved.