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Applied and Environmental Microbiology, December 2002, p. 6162-6171, Vol. 68, No. 12
0099-2240/02/$04.00+0 DOI: 10.1128/AEM.68.12.6162-6171.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.
Air Force Research LaboratoryMLQL, Tyndall AFB, Florida 32403,1 School of Civil and Environmental Engineering, Cornell University, Ithaca, New York 148532
Received 3 July 2002/ Accepted 24 September 2002
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VC can be oxidized to CO2 under anaerobic conditions in the presence of Fe(III) or humic acids (4, 5), but the microbiology and biochemistry of such anaerobic oxidations have not been investigated. Aerobic bacteria can catalyze the cometabolic oxidation of VC in the presence of monooxygenase inducers such as methane (18), ethane (20), ETH (34), propane (38), propene (15), isoprene (16), toluene (48), and ammonia (56). Bioremediation strategies based on aerobic cometabolism have been examined for VC and other chlorinated ethenes (36, 47), but there are several problems with cometabolic systemselectron donors are required (2), the growth-supporting substrate and the pollutant compete for the same enzymes (15), and reactive toxic metabolites may accumulate and inhibit biodegradation (43, 61).
A few strains of Mycobacterium (25, 26) and Pseudomonas (57, 58) that can grow aerobically on VC as the sole carbon and energy source have been isolated from soil, river water, and activated sludge. Such bacteria are not subject to cometabolic limitations and may play a role in the natural attenuation of VC if they occur in the subsurface at contaminated sites. The origin of VC-assimilating bacteria is unclear, although evolution from strains that grow on ETH seems likely (58). ETH is produced via biosynthesis in plants and soil microorganisms, and aerobic ETH-assimilating bacteria appear to be fairly widespread and easily isolated (10, 23). The VC- and ETH-assimilation pathways in bacteria are not well understood, but there is evidence for an initial monooxygenase attack and the production of VC epoxide (chlorooxirane) (25) and epoxyethane (ethylene oxide) (11), respectively.
While several recent studies (17, 28, 29) have examined the distribution and diversity of anaerobic PCE-TCE-dechlorinating bacteria, similar studies on aerobic VC-assimilating bacteria are lacking, and it is not known whether such bacteria might contribute to the natural attenuation of VC. Evidence from the field (14) suggests that VC can disappear in the aerobic downgradient portions of chlorinated ethene plumes, but whether VC-assimilating bacteria are responsible for the effect is unknown. There is great variation in the kinetic parameters of the few aerobic VC degraders examined thus far, making it difficult to predict the rate and extent of in situ VC oxidation. To address the above issues, we investigated aerobic VC biodegradation in samples from chlorinated-ethene-contaminated sites and examined the phylogeny and kinetic parameters of VC-assimilating strains isolated from the site samples.
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Analytical methods.
VC, ETH, and epoxyethane were analyzed in headspace samples by gas chromatography with flame-ionization detection as described previously (9). For analysis of kinetic data, aqueous concentrations of VC were calculated from total amounts, using a dimensionless Henry's constant of 0.9079 at 20°C (22). For ETH, a Henry's constant of 7.24 at 20°C was estimated by using the technique of Gossett (22). A Hewlett Packard HP 5890 Series II gas chromatograph equipped with a thermal conductivity detector and a 1/8-in.-diameter stainless steel column packed with a 60/80-mesh 5A molecular sieve (Supelco) was used to analyze oxygen in headspace samples (0.5 ml from 160-ml serum bottles). Protein concentrations were routinely measured by a UV absorbance assay based on previously described methods (31, 42). Samples of culture fluid (0.45 ml) were mixed with NaOH (0.15 ml, 10 M) and heated (90°C, 10 min). The samples were cooled, an HCl solution was added (400 µl; 10 M HCl and MSM in a 3:5 ratio), and the tubes were centrifuged (16,000 x g) for 5 min. The absorbance of the supernatants was measured at 230 and 260 nm, and the protein content was calculated in micrograms per milliliter as (183 x A230) - (75.8 x A260). Protein in neutralized lysates was also determined on occasion by using the MicroBCA assay kit (Pierce) as described previously (9). Dry-weight growth yields were determined with 700-ml cultures grown on 100 ml (4,167 µmol) of VC or ETH. Cells were washed in deionized water and then dried at 105°C to a constant weight. The optical density at 600 nm (OD600) was also used to monitor growth in some cases.
Microcosms and enrichment cultures.
Samples of groundwater (50% [vol/vol]), soil (5% [wt/vol]), sediment (5% [wt/vol]), or activated carbon (5% [wt/vol]) were mixed with MSM in 160-ml serum bottles (50-ml or 72-ml [liquid phase]) sealed with Teflon-faced rubber stoppers and aluminum crimp caps. In cases where samples contained solids and groundwater, initial microcosms were set up without the addition of medium. VC was added at 20 to 40 µmol/bottle (0.13 to 0.26 mM aqueous concentration) in the initial microcosms and at 100 to 400 µmol/bottle in later transfers (0.66 to 2.64 mM). The microcosms and enrichments were incubated with the bottles in an inverted position and with shaking at the ambient temperature (20 to 24°C), and active cultures (5% [vol/vol]) were transferred to fresh MSM at intervals. Sterile controls (autoclaved samples in MSM) were set up in accompaniment to the initial microcosms for the monitoring of abiotic losses.
Isolation and identification of VC degraders.
Pure cultures were isolated from the enrichments by spreading dilutions on MSM plates and incubating in desiccators in a 1% (vol/vol) VC-air atmosphere. After incubation at ambient temperature for 1 to 3 months, representative colonies were restreaked on two MSM plates, one of which was reincubated with 1% VC and the other of which was reincubated in air alone. Isolates showing significantly more growth in the presence of VC were investigated further. In some cases, isolations were also done on 1/10-TSA plates both with and without added bovine serum albumin. Utilization of VC was confirmed by reinoculation of isolates into MSM-VC broths and the monitoring of VC consumption (gas chromatography [GC] analysis) and cell growth (OD600 or protein assay). Identification of strains was done by partial sequencing of amplified 16S rDNA (MIDI Labs, Newark, Del.). Phylogenetic analysis was done with ClustalX and TreeView software (see Fig. 1; see legend for details).
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FIG. 1. Phylogeny of VC-assimilating isolates based on partial 16S rRNA gene sequences. Names of VC-degrading isolates from the present study are in boxes. A total of 400 bases were used for analysis after removal of positions containing gaps or ambiguous nucleotides. Bootstrap values from 100 neighbor-joining trees are indicated to the left of the nodes. Branch points with less than 50% bootstrap support were collapsed. The bar represents 3 nucleotide changes per 100 nucleotides. The consensus tree was rooted by using Escherichia coli as the outgroup. GenBank accession numbers are given below each strain.
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Determination of growth rates and growth yields.
VC-grown cells were washed with MSM and inoculated into 50 ml of MSM (OD600 = 0.05, protein = 7 to 11 µg/ml). VC was added at 150 µmol/bottle (1 mM), and the cultures were incubated at 20°C with sampling at intervals for determination of VC and protein concentrations. VC (150 µmol) was added as required. Another set of cultures inoculated with ETH-grown cells was similarly treated, except ETH was provided as the substrate (one addition of 600 µmol/bottle = 0.7 mM). Growth yields were calculated from the linear regression (milligrams of protein produced/mmol of substrate consumed). Maximum specific growth rates were subsequently calculated by fitting an exponential curve to a plot showing protein yield versus time. In this case, protein yield was calculated from substrate depletion data as X0 + Y
S, where X0 is the initial biomass (milligrams of protein), Y is the growth yield (milligrams of protein/millimole of substrate), and
S is the cumulative substrate consumed (millimoles). This method of calculating the growth rate was used due to the availability of more substrate depletion data than protein data and because of the relatively large scatter in the protein measurements for some cultures. The growth yield of strain JS616 was determined by using 3-ml cultures in 10-ml serum bottles. The whole culture was lysed by injecting NaOH (1 ml, 10 M) into the bottle and heating (90°C, 15 min), and then the lysate was neutralized and assayed for protein by measurement of UV absorbance.
VC-ETH utilization kinetics.
VC- or ETH-grown cells were washed in MSM and divided among three 160-ml serum bottles containing 72 ml of MSM each. The cultures were incubated with the bottles inverted at an angle at 20°C and with rotary shaking at 165 rpm, and the headspace gases were sampled at intervals for GC analysis. Estimates of the maximum specific substrate utilization rate (k) and the half-velocity constant (Ks) were obtained from VC or ETH depletion curves. The data were fitted to the Michaelis-Menten model by using the AQUASIM software program, as described previously (9). VC kinetics was determined with cultures pregrown on VC, while ETH kinetics was determined with cultures pregrown on ETH. Protein concentrations were measured at the end of each depletion experiment by lysing the entire contents of each culture bottle, as described previously. Experiments were designed such that biomass increases over the observed depletion curves were negligible (typically < 0.5%).
Oxygen utilization kinetics.
The half-velocity constant with respect to oxygen (Ks[O2]) was determined with 72-ml cultures in triplicate as described above for the VC-ETH kinetics study. After inoculation, the headspace was purged briefly with nitrogen to remove excess oxygen and then 300 µmol of VC or 800 µmol of ETH was added to the culture. Ks(O2) values were estimated using AQUASIM as described above. A zero-oxygen standard was prepared by adding excess sodium sulfite to a 160-ml serum bottle containing 72 ml of distilled water in the presence of cobalt catalyst. The oxygen peak area for the mixture from this bottle, as measured by GC, was defined as corresponding to 0 mg of dissolved oxygen/liter. Oxygen threshold levels (i.e., oxygen uptake levels too low to measure at oxygen concentrations greater than zero) were observed during the study, which required a modification of the Michaelis-Menten model for the AQUASIM program as follows:
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Epoxyethane production assay.
Cells from 50-ml MSM cultures grown to mid-exponential phase on either VC or sodium acetate (20 mM) were washed in KP buffer (K2HPO4, 20 mM [pH 7.0]) and suspended to 0.2 ml with KP buffer in 10-ml serum bottles. The bottles were capped and an epoxypropane solution was added (2.5 mM in 0.8 ml of KP buffer), yielding 1-ml suspensions at an OD600 between 5 and 10 (protein = 0.7 to 2.3 mg/ml). ETH (3 µmol) was added, and the bottles were incubated with shaking (300 rpm) at 20°C. After 10 min of equilibration, 100-µl headspace samples were taken at intervals and analyzed by GC to determine the epoxyethane accumulation rate. At the end of the experiment, protein was assayed and monooxygenase activity was calculated as nanomoles of epoxyethane produced per minute per milligram of protein. In the case of strain JS616, Tween 80 (0.1% [vol/vol]) was added to cultures just before harvesting and was included in the washing buffer to facilitate centrifugation and reduce clumping during the assay.
Bacterial strain accession numbers.
Several of the VC-degrading strains have been deposited with the American Type Culture Collection, with accession numbers as follows: JS60, BAA-494; JS61, BAA-495; JS616, BAA-496; JS617, BAA-497; JS621, BAA-498; and JS614, BAA-499.
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TABLE 1. VC biodegradation in aerobic microcosms and enrichments
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From our survey of sites, it appears that VC-degrading microorganisms are fairly widespread and arise wherever conditions are appropriate for their growth. The presence of chlorinated ethenes is apparently not the sole factor that determines whether VC degraders are present at a site. Other site conditions, such as redox potential, pH, and the presence of other contaminants and nutrients, would be expected to influence the development of VC-degrading microbial populations. The most favorable niches for the growth of VC degraders may be in aerobic areas downgradient of chlorinated ETH plumes, where anaerobic electron donors are depleted and the end products of anaerobic chloroethene metabolism (i.e., VC, ETH, and ethane) accumulate.
Isolation and characterization of bacteria.
Pure cultures of VC-assimilating bacteria were isolated from 15 of the enrichments. All of the isolated strains grew on both VC and ETH as the sole carbon source and were relatively slow growing, requiring 1 to 3 weeks to form colonies on 1/10-TSA plates and 1 to 3 months to form colonies on MSM-VC plates. The optimum temperature and pH for the isolates was determined in two cases (i.e., those of strains JS60 and JS61) to be 30°C and pH 6.0 to 6.5. For the sake of consistency, however, further growth and kinetic experiments with the isolates were performed at 20°C with a pH of 7.0.
On 1/10-TSA plates, colonies of the VC-degrading strains were white, cream, yellow, or orange in color and ranged in form from smooth and circular to raised and irregular. Large- and small-colony variants were produced by pure cultures in several cases, a trait that was particularly noticeable with strain JS614. Strains JS61, JS617, and JS621 did not readily form single colonies on 1/10-TSA or MSM plates, despite growing well in broth medium. The addition of glucose and particularly albumin (as used in mycobacterial media such as Middlebrook 7H9) greatly facilitated colony development with such strains. In liquid culture, all of the isolates except strain JS614 showed some degree of hydrophobic behavior-either clumping or adhering to the walls of serum bottles.
In groundwater enrichments, there was a tendency for less hydrophobic strains (e.g., JS60, JS615, and JS620) related to Mycobacterium rhodesiae (see below) to dominate, while with solid sample types a diverse range of more hydrophobic strains (e.g., JS616, JS617, and JS619) tended to be isolated. The use of groundwater samples in many cases may have biased our survey against the more hydrophobic, possibly surface-associated bacteria at the sampling site. Future sampling efforts should therefore focus on samples of soil or aquifer solids to more fully investigate the diversity of VC-assimilating bacteria. The fact that we could not isolate pure cultures from some enrichments despite repeated attempts also indicates that the biodiversity of aerobic VC degraders is not fully represented by the isolates obtained thus far.
Phylogenetic analysis.
Comparison of partial 16S rDNA sequences from the VC-degrading isolates with sequences from GenBank indicated that with one exception (strain JS614), all of the isolates were Mycobacterium species (Fig. 1). Many of the strains (i.e., TM1, JS60, JS61, JS615, JS618, JS620, and JS621) clustered in a loose group which includes M. rhodesiae, M. sphagni, M. aichiense, M. fortuitum, and M. mucogenicum (44, 52). This group also includes the ETH-degrading strain K1 (34), the trichloroethane-degrading strain TA27 (60), and several polyaromatic hydrocarbon-degrading bacteria (e.g., strains RJGII-135 [46] and SM7.6.1 [21]). Based on analysis of some near-full-length 16S rDNA sequences (1,420 bases), we have tentatively assigned strains TM1, JS60, JS615, and JS620 to M. rhodesiae and strains JS61 and JS618 to M. aichiense.
The strain JS621 partial 16S rDNA sequence (400 bp) was most similar to that of M. mucogenicum (Fig. 1), but comparison of near-full-length sequences (data not shown) revealed a closer relationship to M. rhodesiae (98.2% sequence identity). However, JS621 was slow growing and nonpigmented on plates, in contrast to M. rhodesiae (52), and the other M. rhodesiae-like VC degraders, which grew more rapidly and featured yellow pigmentation. Thus, strain JS621 may represent a novel species of mycobacterium. Based on 16S rDNA analysis, the mycobacterial isolates JS617 and TM2 are most likely to be strains of M. tusciae (51), while JS616 and JS619 are probably strains of M. gadium (8), and M. moriokaense (53), respectively. The 16S rDNA sequence from strain JS614 was most similar to sequences from Nocardioides strains. Analysis of near-full-length 16S rDNA sequences (1,469 bases) indicated that the JS614 gene was 97.4% identical to that of Nocardioides pyridinolyticus, the closest-matching well-established species. Based on these results, it is possible that strain JS614 represents a new Nocardioides species (50).
In two cases, VC-degrading isolates from geographically distant sites had identical partial 16S rDNA sequences (isolates JS60 and JS620 and isolates JS61 and JS618). On the basis of phenotypic differences such as pigmentation and the results of REP-PCR amplification (Fig. 2), which showed all four strains to be distinct, we believe these strains to be independent isolates. The four isolates derived from Moody AFB groundwater (JS621 and three JS621-like strains) had identical partial 16S rDNA sequences and the same colony morphology. Further tests (e.g., REP-PCR assays) are required to determine the relationship between these isolates. The JS621-like strains were isolated from monitoring wells covering the entire length of the VC plume, suggesting that a single VC-degrading strain dominates this site. A similar phenomenon has been observed at Kelly AFB (Texas), where chlorobenzene-degrading bacteria isolated from different groundwater samples were all found to carry identical 16S rDNA genes and degradation pathways (54).
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FIG. 2. Discrimination of closely related VC-degrading mycobacteria by REP-PCR.
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Growth and kinetic parameters.
Five representative strains were selected for more detailed analysis of growth and kinetic parameters with ETH and VC (Table 2). The growth yields and growth rates of the four Mycobacterium strains examined (JS60, JS61, JS616, and JS617) were similar, and all were lower than the values obtained for the Nocardioides strain (JS614). We considered the possibility that the apparent high yields of strain JS614 were due to biases in the lysis or protein quantitation methods used, but alternative protein assays (Micro-BCA) and measurement of dry-weight yields confirmed the initial data. The dry-weight growth yields with JS614 were 20.1 g/mol for VC and 29.4 g/mol for ETH compared to yields with JS60 of 10.8 g/mol for VC and 22.0 g/mol for ETH (averages of two experiments).
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TABLE 2. Growth and kinetic parameters of VC-assimilating bacteria
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The maximum specific growth rates on VC of our mycobacteria were about 5-fold lower than that for Mycobacterium sp. strain L1 (25), 5-fold higher than that for Pseudomonas sp. strain DL1, and 50-fold higher than that for Pseudomonas sp. strain MF1 (58). The comparison with strain L1 may not be entirely appropriate given the higher growth temperature used in that study (30°C), but the comparison with the Pseudomonas strains is appropriate. The more rapid growth of the Mycobacterium strains adds weight to our argument that this group is more likely to be influential in the natural attenuation of VC. The maximum specific growth rate of Nocardioides sp. strain JS614 at 20°C was 15 times higher than that of strain DL1 and 150 times higher than that of strain MF1. Although Nocardioides-type VC degraders appear to be rare based on the results of our site-screening study, they are likely to have a large impact on the natural attenuation of VC where they occur due to their rapid growth and high biomass yields.
In general, the substrate utilization kinetics of the four Mycobacterium strains were more similar to each other than they were to the Nocardioides strain (Table 2). The k values for VC utilization ranged from 9 to 16 nmol/min/mg of protein among the four Mycobacterium strains; however, the corresponding k value for the Nocardioides strain was 43 nmol/min/mg of protein. The k values for ETH were greater than those for VC with the Mycobacterium strains, but the reverse was true with the Nocardioides strain (JS614).
The Ks values of the VC-assimilating strains showed no apparent grouping by phylogeny and were generally similar (ca. 1 µM). The Ks values agreed fairly well with data from other bacteria that grow on VC (58) and were much lower than the Ks values reported for aerobic cometabolic chlorinated-ethene-degrading cultures (3). Ks values for ETH among the Mycobacterium strains were higher than Ks values for VC, suggesting that the enzymes involved have a somewhat greater affinity for VC than for ETH. No such difference in affinity between VC and ETH was apparent for the Nocardioides strain JS614. The low Ks values for VC (and the absence of a measurable VC threshold) suggests that these bacteria are capable of degrading VC to very low levels under appropriate field conditions and are therefore environmentally relevant strains. In terms of kinetic parameters, it appears that it matters very little which species of VC-degrading Mycobacterium resides at a contaminated site but the presence of an organism like Nocardioides JS614 would represent a significantly greater VC oxidation potential.
All five strains examined were able to oxidize ETH to epoxyethane after growth on VC but not after growth on acetate, indicating the presence of an inducible alkene monooxygenase (Table 2). The specific activities measured for epoxyethane production ranged from 7 to 22 nmol/min/mg of protein. The measured activities are lower than the true activity (k value for ETH oxidation; Table 2), probably due to the inhibitory presence of epoxypropane in the cell suspensions. The addition of epoxypropane was required to stop the metabolism of epoxyethane (12) to allow an accumulation rate to be measured, but epoxypropane also partially inhibited ETH oxidation in experiments with strain JS60 (data not shown). In further experiments with JS60 (data not shown), ETH-grown cells also readily metabolized VC, suggesting that the same monooxygenase enzyme is active on VC and ETH and is inducible by both substrates. Alkene monooxygenase activity has also been detected in Mycobacterium sp. strain L1, Pseudomonas sp. strain MF1, and Pseudomonas sp. strain DL1 (25, 57, 58), indicating that monooxygenase-catalyzed epoxidation is common to all VC-assimilating bacteria. The monooxygenase activities calculated in the present study were significantly lower than the corresponding activities reported for Mycobacterium sp. strain L1 (25) and ETH-assimilating mycobacteria (23). This difference is at least partly due to the use of lower incubation temperatures in our experiments (20°C) and the inhibitory effects of epoxypropane.
Oxygen utilization kinetics.
Ks(O2) values were determined for five of the VC-assimilating strains (Table 3). For each strain, the Ks(O2) value for VC was lower than the Ks(O2) value for ETH, similar to the pattern seen with the Ks values for substrate utilization (Table 2). The very low Ks(O2) values measured (0.03 to 0.30 mg/liter) during growth on VC indicate that these five strains can effectively biodegrade VC under conditions of low-oxygen tension similar to those commonly encountered in the subsurface. Although the Ks(O2) values were low, all the strains exhibited oxygen threshold behavior during growth on VC, in which O2 uptake ceased when the O2 concentration dropped below 0.02 to 0.1 mg/liter. The Nocardioides strain (JS614) was the only strain to exhibit any significant oxygen threshold behavior during growth on ETH. It is unlikely that the O2 thresholds observed were analytical artifacts, as in every case elevated oxygen levels in experimental bottles were confirmed by comparison to an identically treated zero-oxygen standard. In addition, the cultures were not limited by lack of VC or ETH at the oxygen threshold point and respiking of oxygen (tested with strain JS616 on VC and strain JS614 on ETH) resulted in further O2 uptake until a threshold was again reached. Thus, cessation of oxygen uptake at the measured threshold value was not a result of substrate depletion or cell death. We cannot explain these observations at present, but they could reflect some properties of the initial monooxygenase in the VC-ETH pathway.
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TABLE 3. Oxygen half-velocity constants of VC-assimilating bacteria
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FIG. 3. Effect of VC starvation on VC degradation. Cultures of JS60 and JS614 were grown on VC in 50-ml MSM broths to mid-exponential phase (OD600 = 0.2 to 0.3; protein = 30 to 70 µg/ml) until the VC (additions of 2 x 150 µmol) was depleted. The cultures were then incubated for 0, 0.5, 1, or 7 days before readdition of VC (150 µmol = 1.0 mM initial aqueous concentration) and monitoring by GC analysis. , no starvation; , 12 h of starvation; , 1 day of starvation; , 1 week of starvation. Data are averages of three replicate cultures; error bars represent standard deviations.
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Testing of ETH degraders for growth on VC.
In light of the recent report describing an ETH-assimilating Pseudomonas strain that could adapt to growth on VC (58), we decided to investigate whether a similar adaptation can occur in gram-positive bacteria. Mycobacterium sp. strain K1 and Corynebacterium sp. strain K3, previously isolated from a consortium grown on ETH (34), were tested for their ability to grow on VC (Fig. 4). Strain K3 did not grow on VC, although cells from the same inoculum grew when ETH was used as the carbon source (data not shown). In contrast, strain K1 readily adapted to growth on VC as the sole carbon source, even after growth on nonselective medium. This finding was unexpected, as the consortium that was the source of strain K1 did not grow on VC (34). It is possible that in the present study, the use of a pure culture or the different experimental conditions permitted the growth of strain K1 on VC. Interestingly, the partial 16S rDNA sequence of strain K1 is similar to those of the M. rhodesiae-like strains we isolated on VC as the sole carbon source (Fig. 1).
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FIG. 4. Testing of ETH-assimilating bacteria for growth on VC as the carbon source. Mycobacterium sp. strain K1 and Corynebacterium sp. strain K3 (34) were grown on 1/10-TSA-1% glucose plates and inoculated into duplicate 50-ml MSM broth volumes at an initial OD600 of 0.10 (protein = 10 to 15 µg/ml). VC was added (150 µmol = 1.0 mM initial aqueous concentration), and the cultures were incubated at 20°C and sampled at intervals to quantify VC and protein. In the case of strain K1, VC was added again (2 x 150 µmol) after the initial amount had been degraded. , VC-strain K1; , protein-strain K1; , VC-strain K3; , protein-strain K3. Data are averages of two replicate cultures.
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Conclusion.
Our findings indicate that the bacterial assimilation of VC is an ecologically significant phenomenon of an importance equal to or greater than that of cometabolic VC degradation. Members of a diverse group of Mycobacterium strains are capable of growth on VC, and these bacteria are indigenous and widely distributed at chlorinated-ethene-contaminated sites. Based on their distribution, growth rates, and kinetic parameters, we believe that Mycobacterium strains are most likely to be responsible for the aerobic natural attenuation of VC that has been observed at many sites. Further characterization of the strains we have isolated will provide a basis for developing molecular methods for detecting VC degraders in the environment and assessing the natural attenuation potential of individual sites. Our VC-assimilating strains may also be useful for enhanced bioremediation by complementing the activities of anaerobic bacteria and providing a mechanism for the complete mineralization of chlorinated ETHs.
N.V.C. was supported by a postdoctoral fellowship from the Oak Ridge Institute for Science and Education (U.S. Department of Energy).
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