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Applied and Environmental Microbiology, November 1999, p. 5169-5172, Vol. 65, No. 11
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Reductive Dehalogenation and Conversion of
2-Chlorophenol to 3-Chlorobenzoate in a Methanogenic Sediment
Community: Implications for Predicting the Environmental Fate of
Chlorinated Pollutants
Jennifer G.
Becker,*
David A.
Stahl, and
Bruce E.
Rittmann
Department of Civil Engineering, Northwestern
University, Evanston, Illinois 60208
Received 17 May 1999/Accepted 31 August 1999
 |
ABSTRACT |
Biotransformation of 2-chlorophenol by a methanogenic sediment
community resulted in the transient accumulation of phenol and
benzoate. 3-Chlorobenzoate was a more persistent product of 2-chlorophenol metabolism. The anaerobic biotransformation of phenol to
benzoate presumably occurred via para-carboxylation and
dehydroxylation reactions, which may also explain the observed conversion of 2-chlorophenol to 3-chlorobenzoate.
 |
TEXT |
Anaerobic biotransformation of a
wide variety of aromatic compounds initially involves the formation of
a carboxyl group on the aromatic nucleus, e.g., via a carboxylation
reaction (6). An anaerobic isolate (21) and a
coculture (9) that are able to carboxylate phenol have been
characterized. Other aromatics that undergo anaerobic carboxylation
include simple polyaromatic hydrocarbons (22), aniline
(8), o-cresol (2), and
m-cresol (12). However, under anaerobic
conditions, biotransformation of most halogenated aromatic compounds is
typically initiated by reductive dehalogenation (14). In
fact, it appears that removal of the halogen substituent must occur
before anaerobic cleavage of the aromatic nucleus is feasible
(19). Indeed, in nearly all previous studies, anaerobic
transformation of 2-chlorophenol (2-CP) by mixed cultures occurred
solely via reductive dehalogenation to phenol (e.g., see references
4 and 15). The pathway by which
phenol is biodegraded in mixed cultures under methanogenic conditions
has been examined in a number of investigations (e.g., see references
16 and 18). The results of these
recent studies indicate that 4-hydroxybenzoate is formed via
para-carboxylation of phenol and subsequently dehydroxylated
to yield benzoate, which undergoes ring cleavage and ultimately is mineralized.
However, in some cases, more than one pathway may be possible for the
biotransformation of aromatic compounds in mixed anaerobic cultures.
Which pathway is operative may determine whether or not the parent
compound is ultimately mineralized. For example, Londry and Fedorak
(12) examined the biotransformation of m-cresol in a methanogenic consortium. Biotransformation of m-cresol
initially proceeded via para-carboxylation to yield
4-hydroxy-2-methylbenzoic acid. Metabolism of this intermediate
appeared to be the rate-limiting step in the biotransformation of
m-cresol. 4-Hydroxy-2-methylbenzoate predominantly underwent
demethylation to yield 4-hydroxybenzoic acid, which was ultimately
converted to acetate via reductive dehydroxylation to benzoate and
subsequent ring cleavage. However, "premature" reductive
dehydroxylation of 4-hydroxy-2-methylbenzoate produced a minor
metabolite, 2-methylbenzoate, which persisted.
The existence of two m-cresol biotransformation pathways,
one leading to mineralization of the parent compound and the other resulting in the production of a persistent substituted benzoate, points to the importance of understanding biotransformation pathways. This information is necessary for predicting the fate of organic pollutants in the environment and for designing bioremediation strategies and wastewater treatment processes. In this paper, we report
that in mixed anaerobic cultures, in addition to undergoing the
expected pathway of reductive dehalogenation to phenol and ultimate
mineralization, transformation of 2-CP may initially involve the
formation of a carboxyl group analogous to the anaerobic biotransformation of nonhalogenated aromatic compounds.
Establishment of cultures.
Strict anaerobic and aseptic
techniques were used throughout the experiments. Experiments were
performed with batch reactors consisting of 160-ml or 2-liter glass
vessels with serum bottle closures. The glass vessels were sealed with
thick black butyl septa and aluminum crimp caps. All of the reactors
had the same ratio of headspace volume to slurry-phase volume (3:5,
vol/vol). The slurry phase was composed of sediment and anaerobic
medium (1:9, vol/vol). The anaerobic sediment inoculum was collected from a depth of 100 m at a site located approximately 16 km east of Fox Point, Wisconsin, in Lake Michigan by using a box corer, transferred to canning jars, and stored at 4°C for approximately three months until used. The techniques used for medium preparation, culture handling, and sampling were based on previously described methods (13). The anaerobic medium used for this study has
been previously described (5) and was prepared by combining
separate sterile, anoxic solutions of salts, bicarbonate buffer, and
reducing agents with the remaining medium components. The sediment
inoculum was added to the glass vessels inside an anaerobic glove box
(85% N2-10% CO2-5% H2; Coy
Laboratories, Ann Arbor, Mich.), and the bicarbonate buffer was
equilibrated with 30% CO2-70% N2. 2-CP was
added to a final concentration of 200 µM. One 2-liter reactor and two
160-ml viable reactors were prepared in this manner. In the interest of
brevity, only the results obtained with the duplicate 160-ml reactors
are presented here. Except where noted, the results obtained with the
2-liter reactor were similar. A 2-liter sterile control was prepared in
the same manner as the viable reactors, except that the sediment
inoculum was autoclaved for 1 h on each of three consecutive days
before being combined with sterile medium and 2-CP. The reactors were
incubated statically at 30°C.
Analysis of aromatic compounds.
The reactors were continuously
shaken on a platform shaker (100 rpm) during sampling events.
Slurry-phase samples were taken by using deoxygenated and sterile
disposable syringes, filtered (0.45-µm pore size; Gelman Acrodisc),
and either analyzed immediately or frozen (
20°C) prior to analysis.
The aqueous concentrations of 2-CP and its aromatic metabolites were
determined by using a reversed-phase high-performance liquid
chromatography system (Hitachi, Ltd., Tokyo, Japan) equipped with a
computer interface and D-7000 HSM software (Hitachi). Separations were
performed by using a mobile phase of methanol-water-acetic acid
(60:38:2, vol/vol) at a flow rate of 1.0 ml/min and a C18
column (4.7 mm by 235 mm) (Partisil 5 ODS-3; Whatman International
Ltd.). Detection was by UV absorbance with a diode array detector
(Hitachi, model L-4500) operated at 280 nm. Linear calibration factors
were determined from external standards, which were injected along with
each sample set. Identification of aromatic metabolites of 2-CP
biotransformation was based on comparison of their retention times and
UV spectra (250 to 380 nm) with those of authentic compounds.
2-CP fate.
Complete removal of 2-CP was observed in the viable
reactors within 50 days, as shown for the duplicate 160-ml reactors in Fig. 1A. The concentration of 2-CP in the
2-liter sterile control remained nearly constant during this period,
which indicates that transformation of 2-CP in the viable reactors was
due to biological activity. Whenever 2-CP was no longer detectable in
the sediment slurry reactors, it was replenished.

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FIG. 1.
Anaerobic biotransformation of 2-CP in the sediment
community (A) and corresponding production of phenol (B), benzoate (C),
and 3-CB (D). Squares represent the average concentrations in duplicate
160-ml batch slurry reactors. Error bars represent 1 standard
deviation. Circles represent the concentration of 2-CP in a single
2-liter sterile control.
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|
Transformation of 2-CP in the sediment slurry reactors resulted in the
production of several aromatic metabolites, including
phenol and
benzoate (Fig.
1B and C). Substantial amounts of a
third metabolite,
which had a significantly longer retention time
than phenol or
benzoate, were also detected in the sediment slurry
reactors. On the
basis of its retention time and absorbance spectrum,
the unknown
metabolite was identified as 3-chlorobenzoate (3-CB).
The
concentrations of 3-CB in the duplicate 160-ml reactors are
shown in
Fig.
1D.
The formation of these aromatic metabolites was not limited to the
2-CP-degrading sediment slurries described here. Significant
amounts of
phenol, benzoate, and 3-CB were also detected in previous
studies
involving 2-CP-degrading slurry reactors that were inoculated
with
anaerobic sediment collected from the Lake Michigan site
at various
times over a period of two years (
1). In addition,
trace
amounts of a compound with the same retention time and absorbance
spectrum as 3-chloro-4-hydroxybenzoate were sporadically detected
in
the previously studied 2-CP-degrading sediment slurries. None
of these
aromatic metabolites were ever detected in sterile
controls.
The concentrations of phenol, benzoate, and 3-CB followed similar
patterns in all of the sediment slurry reactors. In each
case, phenol
production occurred concomitantly with the removal
of the first
addition of 2-CP (Fig.
1B). The decline in phenol
concentrations was
accompanied by the production of benzoate (Fig.
1C). As shown in Fig.
1D, by the time benzoate was no longer detectable
in the slurries, some
3-CB had been formed in each of the reactors.
Significant production of
3-CB coincided with the biotransformation
of the second (160-ml
reactors [Fig.
1D]) or third (2-liter reactor
[data not shown])
addition of 2-CP.
All of the 2-CP transformed in the duplicate 160-ml reactors within the
first 3 weeks of incubation was converted to phenol.
This indicates
that, initially, all of the 2-CP transformed in
the reactors underwent
reductive dehalogenation. The concomitant
removal of phenol and
production of benzoate in the three reactors
suggest that the phenol
produced by reductive dehalogenation was
subsequently biotransformed to
benzoate, presumably via sequential
carboxylation and dehydroxylation
reactions. However, the detection
of 3-CB in all three reactors by day
63 (Fig.
1D) indicates that
transformation of 2-CP via a second pathway
also occurred. The
amount of 2-CP transformed via this alternative
pathway was significant.
The maximum molar ratios of 3-CB accumulated
to cumulative 2-CP
degraded exceeded 20% in the duplicate 160-ml
reactors.
The presence of 3-CB or an alternative 2-CP biotransformation pathway
may have decreased the overall rate of 2-CP transformation
in some of
the reactors. High concentrations of 3-CB persisted
in the 160-ml
reactors for approximately 60 to 70 days (Fig.
1D).
As shown in Fig.
1A, during this period, the biotransformation
of 2-CP via reductive
dehalogenation or an alternative pathway
was severely reduced in the
duplicate 160-ml reactors. It is not
known whether reductive
dehalogenation of 2-CP continued after
63 days in the 160-ml reactors
because no phenol was detected
in these systems after 49 days (Fig.
1B), and the 3-CB levels
did not increase significantly after 63 days
(Fig.
1D).
On the other hand, although 3-CB persisted for over 50 days in the
2-liter reactor, the rate of 2-CP transformation was not
significantly
diminished for an extended period of time (data
not shown), as was
observed in the 160-ml reactors. Furthermore,
low levels of phenol were
sporadically detected during periods
of increasing 3-CB concentrations
in the 2-liter reactor (data
not shown), which suggests that
simultaneous biotransformation
of 2-CP to 3-CB and reductive
dehalogenation of 2-CP were
feasible.
Removal of 3-CB was observed approximately two to three months after it
was produced in the 2-CP-degrading reactors, as illustrated
in Fig.
1D.
No aromatic metabolites of 3-CB biotransformation
were detected in the
2-liter and duplicate 160-ml 2-CP-degrading
reactors. However, in a
parallel study, benzoate accumulated transiently
in dilutions of
methanogenic 3-CB-degrading reactors that were
inoculated with sediment
obtained from the same site in Lake Michigan
(
1). Therefore,
it is likely that 3-CB was biotransformed in
the 2-CP-degrading
sediment slurry reactors via reductive dehalogenation
to benzoate.
Presumably, benzoate-degrading populations that had
already been
established within the 2-CP-degrading community rapidly
consumed
benzoate produced from the reductive dehalogenation of
3-CB and
prevented it from
accumulating.
The initial biotransformation of 2-CP via reductive dehalogenation in
the sediment slurry reactors was expected on the basis
of results of
numerous previous studies (e.g., see references
4
and
15). The biotransformation of 2-CP to 3-CB has
not
been observed frequently. However, a methanogenic consortium that
was enriched on phenol and proteose peptone for several years
produced
3-CB from 2-CP when the monochlorophenol was added in
equimolar amounts
with phenol (
3). The phenol-degrading consortium
also
carboxylated other
ortho-substituted phenolic compounds in
the presence of phenol and the growth substrate, but unlike the
methanogenic sediment community evaluated in this study, it did
not
mediate reductive dehalogenation of 2-CP or biotransformation
of 3-CB.
The proposed pathways for 2-CP biotransformation in the sediment slurry
reactors are shown in Fig.
2. Reductive
dehalogenation
of 2-CP to phenol, followed by carboxylation of phenol
to 4-hydroxybenzoate
and subsequent dehydroxylation to benzoate, is
shown on the left
side of Fig.
2. 4-Hydroxybenzoate was the only
aromatic metabolite
that was not detected (UV,
A280) in this pathway. However,
4-hydroxybenzoate
has also been undetectable in several other studies
involving
the anaerobic biotransformation of phenol to benzoate (e.g.,
see
reference
20).
Biologically mediated reactions that could lead to the production of
3-CB from 2-CP in the sediment slurry reactors are shown
on the right
side of Fig.
2. In this sequence of reactions, 2-CP
is
para-carboxylated to produce 3-chloro-4-hydroxybenzoate,
which
is subsequently dehydroxylated to yield 3-CB. Several
observations
support this proposed pathway. First, the analogous
reactions
of carboxylation of phenol to 4-hydroxybenzoate and
dehydroxylation
of 4-hydroxybenzoate to benzoate occurred in the
sediment slurry
reactors. Second, trace amounts of a compound with the
same retention
time and absorbance spectrum as
3-chloro-4-hydroxybenzoate, which
is an intermediate in the proposed
pathway, were detected sporadically
in previously studied
2-CP-degrading slurry reactors that were
inoculated with sediment
obtained from the same Lake Michigan
site (
1). Finally, in
previous studies conducted by other researchers
(
16,
17),
monofluorophenols were added as phenol analogs to
anaerobic
phenol-degrading enrichments in order to elucidate the
phenol
biodegradation pathway. In these studies, 2-fluorophenol
was
transformed to 3-fluorobenzoate, 2-fluorobenzoate was produced
from
3-fluorophenol, and 4-fluorophenol was not transformed.
para-Carboxylation
followed by dehydroxylation can explain
the production of the
monofluorobenzoates from 2- and 3-fluorophenol
but cannot occur
with 4-fluorophenol because the
para
position is blocked by the
fluorine substitute. The biotransformation
reactions involving
the monofluorophenols (
16,
17) and 2-CP
(
3) in phenol-degrading
enrichments demonstrate that
carboxylation and subsequent dehydroxylation
of a monohalogenated
phenol are feasible in other anaerobic
communities.
The transformation of 2-CP to 3-CB in the sediment slurry reactors may
involve cometabolic reactions. Several observations
are consistent with
this hypothesis. First, carboxylation and
dehydroxylation of phenol to
benzoate in an anaerobic coculture
that contains the
Clostridium-like strain 6 and the gram-positive
strain 7 (
9) are cometabolic reactions (
10). Furthermore,
an enzyme that mediates decarboxylation of 4-hydroxybenzoate and
the
reverse phenol carboxylase activity in
Clostridium
hydroxybenzoicum,
which was isolated from a
2,4-dichlorophenol-degrading freshwater
sediment enrichment, also acts
on other hydroxylated aromatic
compounds (
7).
3,4-Dihydroxybenzoate, 3-fluoro-4-hydroxybenzoate,
and
3-methoxy-4-hydroxybenzoate (vanillate) are decarboxylated
by this
enzyme. Similarly, the strain 6 reversible 4-hydroxybenzoate
decarboxylase also catalyzes the carboxylation of catechol to
3,4-dihydroxybenzoate (
11). Thus, the populations that
participate
in the transformation of phenol and the production of
benzoate
in the sediment slurry reactors could also conceivably mediate
cometabolic transformation of 2-CP to 3-CB. In other words, the
production of 3-CB from 2-CP might have been the result of nonspecific,
"premature" carboxylation and dehydroxylation
reactions.
The results of this study reveal a potential limitation of using
anaerobic microbial communities to remove chlorinated phenols.
That is,
transformation of 2-CP to another chlorinated compound
is not
acceptable from a treatment standpoint if that chlorinated
product is
not further degraded. Although the 2-CP-degrading community
examined in
this study eventually removed 3-CB, this property
is not shared by all
anaerobic 2-CP-degrading communities (e.g.,
see reference
15). Furthermore, some of the evidence obtained
in
this study suggests that 3-CB production may be correlated
with reduced
2-CP biotransformation rates. However, the extent
to which this
transformation occurs in natural and engineered
anaerobic environments
and the factors that determine whether
2-CP is transformed via
reductive dehalogenation or an initial
carboxylation reaction are not
yet
known.
 |
ACKNOWLEDGMENTS |
This research was supported by U.S. Environmental Protection Agency
grant R823351.
We thank Gina Berardesco for obtaining the sediment samples and Brian
Wrenn for thoughtful comments on the manuscript.
 |
FOOTNOTES |
*
Corresponding author. Present address: Department of
Civil and Environmental Engineering, Lehigh University, 13 E. Packer Ave., Bethlehem, PA 18015-3176. Phone: (610) 758-3543. Fax: (610) 758-6405. E-mail: jgb4{at}lehigh.edu.
 |
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Applied and Environmental Microbiology, November 1999, p. 5169-5172, Vol. 65, No. 11
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
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