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Applied and Environmental Microbiology, October 2001, p. 4842-4849, Vol. 67, No. 10
Lehrstuhl für Mikrobielle
Ökologie, Universität Konstanz, D-78457
Konstanz,1 and Sektion
Sanierungsforschung, Umweltforschungszentrum Leipzig-Halle GmbH,
D-04318 Leipzig,2 Germany
Received 29 January 2001/Accepted 16 July 2001
Primary features of hydrogen and carbon isotope fractionation
during toluene degradation were studied to evaluate if analysis of
isotope signatures can be used as a tool to monitor biodegradation in
contaminated aquifers. D/H hydrogen isotope fractionation during microbial degradation of toluene was measured by gas chromatography. Per-deuterated toluene-d8 and
nonlabeled toluene were supplied in equal amounts as growth substrates,
and kinetic isotope fractionation was calculated from the shift of the
molar ratios of toluene-d8 and
nondeuterated toluene. The D/H isotope fractionation varied slightly
for sulfate-reducing strain TRM1 (slope of curve [b] =
0099-2240/01/$04.00+0 DOI: 10.1128/AEM.67.10.4842-4849.2001
Copyright © 2001, American Society for Microbiology. All rights reserved.
Stable Hydrogen and Carbon Isotope Fractionation
during Microbial Toluene Degradation: Mechanistic and Environmental
Aspects

1.219), Desulfobacterium cetonicum
(b =
1.196), Thauera aromatica
(b =
0.816), and Geobacter
metallireducens (b =
1.004) and was
greater for the aerobic bacterium Pseudomonas putida
mt-2 (b =
2.667). The D/H isotope fractionation
was 3 orders of magnitude greater than the
13C/12C carbon isotope fractionation reported
previously. Hydrogen isotope fractionation with nonlabeled toluene was
1.7 and 6 times less than isotope fractionation with per-deuterated
toluene-d8 and nonlabeled toluene for
sulfate-reducing strain TRM1 (b =
0.728) and
D. cetonicum (b =
0.198),
respectively. Carbon and hydrogen isotope fractionation during toluene
degradation by D. cetonicum remained constant over a
growth temperature range of 15 to 37°C but varied slightly during
degradation by P. putida mt-2, which showed maximum
hydrogen isotope fractionation at 20°C (b =
4.086) and minimum fractionation at 35°C (b =
2.138). D/H isotope fractionation was observed only if the deuterium
label was located at the methyl group of the toluene molecule which is
the site of the initial enzymatic attack on the substrate by the
bacterial strains investigated in this study. Use of ring-labeled
toluene-d5 in combination with
nondeuterated toluene did not lead to significant D/H isotope fractionation. The activity of the first enzyme in the anaerobic toluene degradation pathway, benzylsuccinate synthase, was measured in
cell extracts of D. cetonicum with an initial activity
of 3.63 mU (mg of protein)
1. The D/H isotope
fractionation (b =
1.580) was 30% greater than that in growth experiments with D. cetonicum. Mass
spectroscopic analysis of the product benzylsuccinate showed that H
atoms abstracted from the toluene molecules by the enzyme were retained
in the same molecules after the product was released. Our findings
revealed that the use of deuterium-labeled toluene was appropriate for studying basic features of D/H isotope fractionation. Similar D/H
fractionation factors for toluene degradation by anaerobic bacteria,
the lack of significant temperature dependence, and the strong
fractionation suggest that analysis of D/H fractionation can be used as
a sensitive tool to assess degradation activities. Identification of
the first enzyme reaction in the pathway as the major fractionating
step provides a basis for linking observed isotope fractionation to
biochemical reactions.
*
Corresponding author. Present address:
Universität Tübingen, Zentrum für Angewandte
Geowissenschaften, Sigwartstr. 10, D-72076 Tübingen, Germany.
Phone: 49-(0)-7071-2976076. Fax: 49-(0)-7071-5059. E-mail:
rainer.meckenstock{at}uni-tuebingen.de.
This paper is publication no. 140 of Deutsche
Forschungsgemeinschaft Priority Program 546 (Geochemical Processes with
Long-Term Effects in Anthropogenically Affected Seepage- and Groundwater).
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