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Appl Environ Microbiol, May 1998, p. 1715-1720, Vol. 64, No. 5
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Two New Mycobacterium Strains and Their
Role in Toluene Degradation in a Contaminated Stream
Stephen T.-L.
Tay,1
Harold F.
Hemond,1,*
Martin
F.
Polz,2,
Colleen M.
Cavanaugh,2
Indhira
Dejesus,1 and
Lee R.
Krumholz3
Ralph M. Parsons Laboratory, Department of
Civil and Environmental Engineering, Massachusetts Institute of
Technology, Cambridge, Massachusetts 021391;
Department of Organismic and Evolutionary Biology, Harvard
University, The Biological Laboratories, Cambridge, Massachusetts
021382; and
Department of Botany and
Microbiology, University of Oklahoma, Norman, Oklahoma
730193
Received 2 October 1997/Accepted 6 March 1998
 |
ABSTRACT |
Two toluene-degrading strains, T103 and T104, were isolated from
rock surface biomass in a freshwater stream contaminated with toluene.
The strains exhibit different capacities for degradation of toluene and
other aromatic compounds and have characteristics of the genus
Mycobacterium. Both are aerobic, rod-shaped, gram-positive, nonmotile, and acid-alcohol fast and produce yellow pigments. They have
mainly straight-chain saturated and monounsaturated fatty acids with 10 to 20 carbon atoms and large amounts of tuberculostearic acid that are
typical of mycobacteria. Fatty acid analyses indicate that T103 and
T104 are different mycobacterial strains that are related at the
subspecies level. Their identical 16S rDNA sequences are most similar
to Mycobacterium aurum and Mycobacterium
komossense, and they constitute a new species of fast-growing
mycobacteria. Ecological studies reveal that toluene contamination has
enriched for toluene-degrading bacteria in the epilithic microbial
community. Strains T103 and T104 play only a small role in toluene
degradation in the stream, although they are present in the habitat and
can degrade toluene. Other microorganisms are consequently implicated in the biodegradation.
 |
INTRODUCTION |
In the United States, toluene is
ranked 27th among the top 50 chemical products by production volume,
with 931 million gallons (3.5 × 109 liters) of
toluene manufactured in 1994 (22). Industry uses toluene in
refining gasoline; chemical manufacturing; the manufacture of paints,
lacquers, and adhesives; and some printing and leather-tanning processes. Toluene is usually disposed of as a used solvent. Toluene is
listed as a priority pollutant (46), because contamination of drinking water can pose a potential health hazard. In a 1988 study,
toluene was detected in groundwater, surface water, or soil at 29% of
the hazardous waste sites surveyed; the average amounts detected were
0.2 µM in groundwater, 0.1 µM in surface water, and 77 µg/kg in
soil (46).
Since toluene is ubiquitous in the environment, it is not surprising
that microorganisms capable of degrading toluene have been isolated
from a variety of environments, including polluted topsoils and oil
tanker ballast waters (4, 5, 10, 29, 38, 48, 50). However,
little is known about the role these isolates may play in the
conversion of toluene in the environment. Therefore, studies that
address the response of stream bacteria to effects of anthropogenic
chemical impact are important in enhancing our understanding of the
ecology of contaminant degradation.
This study describes the isolation and characterization of two closely
related toluene-degrading strains of a novel Mycobacterium species from rock surface biofilms in a toluene-contaminated reach of a
small freshwater stream. Ecological data are also presented to assess
the role of these Mycobacterium strains in degrading toluene
in the rock surface biofilms and to determine the impact of toluene
contamination on the stream's microbial community. Earlier studies
showed biodegradation to be the most significant sink for toluene in
this stream (20), and microorganisms attached to stream
sediments and rock surfaces accounted for most of the biodegradative
activity (7).
 |
MATERIALS AND METHODS |
Study site.
The East Drainage Ditch is a small stream in an
industrial area of Wilmington and Woburn, Mass. (7, 20), and
forms part of the Aberjona Watershed, a 90-km2 area 20 km
north of Boston. Toluene in the stream arises from subsurface
contamination below an 80-m-long culvert (11) located 1,600 m upstream from the confluence of the East Drainage Ditch with Halls
Brook. Toluene levels typically range from 0.6 to 4.2 µM in the
streamwater near the source (20). Sampling stations are
upstream 50 m (U50) and 100 m (U100) and downstream 5 m
(D5) and 50 m (D50).
Isolation of bacterial strains.
Rocks were collected in July
1992 from the streambed at station D5. Rock biomass was scraped with
sterile spatulas, serially diluted, and plated onto a mineral salts
(MS) agar medium (35) supplemented with trace elements
(49). The plates were incubated in a desiccator with a
beaker of water (15 ml) previously equilibrated with toluene. The water
was replaced every 2 to 3 days. Toluene was supplied by diffusion from
the beaker in the desiccator that resulted in theoretical
concentrations of approximately 110 µM in the agar based on Henry's
law (36), although the actual concentrations might be
affected by diffusion kinetics and hydrophobic interactions between
toluene and organic constituents of the agar. Plates were monitored
over 7 weeks, during which colonies were picked and restreaked on fresh
plates. Several colonies grew in the presence of toluene, and four
strains, numbered sequentially starting from T101, were selected for
further characterization. Strains T103 and T104 possessed traits
typical of mycobacteria and are described in this paper.
Phenotypic characterization.
Tests for Gram stain, oxidase
activity, catalase activity, carbon source utilization, nitrate
reduction, and acid fastness (Ziehl-Neelsen method) were performed as
previously described (27, 37). Tests for growth on aromatic
compounds were conducted in the same manner as with toluene. Substrates
were supplied by diffusion from a reservoir in the desiccator resulting
in theoretical concentrations in the agar of 10 mg of benzene,
o-xylene, m-xylene, p-xylene, phenol,
or chlorobenzene per liter. Plates were monitored for 4 weeks, and
visible colonies were picked and restreaked on fresh plates that were
further incubated in either the presence or absence of the relevant
substrate.
Toluene biodegradation kinetics.
Rates of toluene
degradation were determined by a headspace gas chromatography method
(7). Cells were grown in 1,100-ml Teflon-stoppered glass
bottles with 600 ml of MS medium initially containing 110 µM toluene.
Toluene levels were monitored daily and replenished when depleted.
After every five toluene feedings, the headspace was flushed with air
to replenish the oxygen. Cells were harvested by centrifugation during
the exponential phase and resuspended in 100 ml of fresh medium.
Kinetic experiments were performed with 60-ml Teflon-stoppered serum
bottles (The West Co., Phoenixville, Pa.) with 19 ml of medium and 0.5 ml of concentrated cell suspension (230 µg of protein/ml for strain T103 and 185 µg of protein/ml for strain T104). Toluene was injected at approximately 1.1, 2.2, 5.4, and 10.9 µM (aqueous concentration). Control experiments were performed with autoclaved cell suspensions. Bottles were shaken in the dark at 20°C on a rotary shaker at 150 rpm
and assayed hourly for toluene. Initial rates of toluene disappearance
were determined to establish Michaelis-Menten kinetic parameters.
Protein was measured with the bicinchoninic acid protein assay (Pierce,
Rockford, Ill.).
Fatty acid analyses.
Cells were grown on Middlebrook 7H10
agar (9) for 7 days at 28°C, harvested, and saponified to
prepare fatty acid methyl esters (33). The analysis was
performed at Microbial ID, Inc. (MIDI, Newark, Del.), by using the MIDI
Microbial Identification System software for identification of fatty
acids. Strains T103 and T104, together with the M. komossense type strain (ATCC 33013), were analyzed in duplicate
and compared with profiles from the Microbial Identification System
(MIS) library (34).
16S rDNA sequencing.
Strains T103 and T104 were cultured in
nutrient broth (Difco Laboratories, Detroit, Mich.) in Teflon-stoppered
serum bottles by shaking at 20°C on a rotary shaker at 150 rpm. Cells
were harvested by centrifugation, and genomic DNA was extracted with a
miniprep (1). The nearly full-length 16S rRNA gene was
amplified from genomic DNA by PCR with forward primer Eubac27F and
reverse primer Universal 1492R (23). All reactions were run
in triplicate under PCR conditions as described elsewhere
(8), and PCR products were purified with the Wizard PCR Prep
(Promega Corp., Madison, Wis.) for automated dye-dideoxy terminator
sequencing at the Michigan State University Sequencing Facility with a
373A DNA sequencing system (Applied Biosystems, Foster City, Calif.).
Sequences for oligonucleotides complementary to the conserved regions
of the eubacterial 16S rRNA gene were kindly provided by Debra J. Lonergan (United States Geological Survey, Reston, Va.); these
oligonucleotides were chosen to prime the sequencing reactions.
Sequencing reaction mixes consisted of 12 pmol of sequencing primer and
50 to 250 ng of PCR template in a total volume of 20 µl of sterile
H2O. The sequences of approximately 1,425 nucleotide bases,
corresponding to the Escherichia coli 16S rDNA sequence from
nucleotides 55 to 1501, were obtained in both directions for the two
strains.
Phylogenetic analyses.
The 16S rDNA secondary structures of
strains T103 and T104 were constructed manually with templates
published in the Ribosomal Database Project (RDP) (25) to
aid in the identification of homologous sequence positions. Sequence
alignments were performed manually in the Genetic Data Environment
(39). All reference sequences and the basic alignment were
obtained from the RDP. Only homologous sites at which the 16S rDNA
sequences of strains T103 and T104 could be aligned unambiguously with
the reference sequences were included in a final data set of 1,165 nucleotides for further analyses. Distance, parsimony, and maximum
likelihood analyses were performed with PHYLIP 3.5 (13),
PAUP 3.1 (42), and fastDNAml (12, 28),
respectively, as described elsewhere (31).
Bacterial counts.
Rock samples were collected from stations
U100, U50, D5, and D50 along the East Drainage Ditch on 7 September
1993. Biomass was scraped with sterile spatulas and suspended in 10 ml
of MS medium, and the resulting cell suspension was successively
diluted to obtain dilutions of 10
2 to 10
7 g
of biomass/ml. Petri dishes containing 1% PTYG agar (3) were inoculated in duplicate with 100 µl of each dilution and incubated at 20°C for 3 weeks. Heterotrophic colonies were counted on
the plates every 3 days, until no new colonies were observed. Since
counts were based on the highest-dilution plates, colony overgrowth on
the plates was not a problem.
Toluene-degrading bacteria were enumerated with MS agar medium
inoculated in duplicate with 100 µl of each dilution, with toluene
supplied as described earlier. Colonies growing on the highest-dilution
plates were picked, transferred to new plates, and incubated in both
the presence and absence of toluene to confirm the abilities of these
isolates to grow with toluene as an energy source.
Toluene levels in the stream.
Duplicate water samples were
collected at stations U100, U50, D5, and D50 on 19 September 1993 with
40-ml vials provided with hollow screw caps and Teflon-coated silicone
septa. Mercuric chloride was added to the samples to a final
concentration of 15 mg/liter. Toluene was measured as described
previously (7).
Nucleotide sequence accession number.
The sequences for
strains T103 and T104 have been deposited in the GenBank database under
accession no. U62889 and U62890. The GenBank accession numbers of the
other sequences used in the analyses are as follows:
Mycobacterium aurum, X55595; Mycobacterium chelonae subsp. abscessus L948, M29559;
Mycobacterium chitae, X55603; Mycobacterium
chlorophenolicus PCP-I, X79094; Mycobacterium diernhoferi SN 1418, X55593; Mycobacterium fortuitum
subsp. fortuitum, X52933; Mycobacterium gilvum,
X55599; Mycobacterium komossense Ko2, X55591;
Mycobacterium neoaurum, M29564; Mycobacterium
sphagni Sph29, X55590; Mycobacterium thermoresistible, X55602; Mycobacterium vaccae, X55601; Mycobacterium
asiaticum N61H, X55604; Mycobacterium avium serovar 1, M29573; Mycobacterium haemophilum, L24800;
Mycobacterium tuberculosis H37/Rv, X52917; Mycobacterium xenopi, X52929; Corynebacterium
xerosis, M59058; Gordona terrae, X79286; Nocardia
otitidiscaviarum, M59056; and Rhodococcus equi, M29574.
Primary literature references for these sequences are available from
the RDP (25).
 |
RESULTS |
Enrichment and isolation.
Two mycobacterial toluene-degrading
strains, T103 and T104, were independently isolated from two yellow
colonies, 1 to 2 mm in diameter, that appeared between 3 and 8 days on
toluene-incubated MS plates inoculated with 10
6 g of
biomass, indicating that these strains were present in the rock surface
biomass at a density of 106 cells/g of biomass. Biomass
scrapings averaged 0.018 g (fresh weight)/cm2 of rock
surface. Both strains grew slowly (relative to other nonmycobacterial
toluene-degrading strains similarly isolated) on solid media when
incubated with toluene. Mycobacterial colonies were not detected on
plates inoculated with higher dilutions of biomass.
Morphological and phenotypic characteristics.
Strains T103 and
T104 had morphologically similar rod-shaped cells when grown on solid
media. Cells were nonmotile, and flagella were not observed under
scanning electron microscopy (data not shown). The strains were
aerobic, gram positive, and acid-alcohol fast (Table
1), which is characteristic of the
mycobacteria (47). Strain T104 differed physiologically from
strain T103 in that T104 could grow on xylenes (Table 1).
Toluene biodegradation kinetics.
Strains T103 and T104 had
maximal toluene consumption rates (Vmax) of
1.0 ± 0.1 and 6.0 ± 1.3 µmol of toluene/mg of protein per
h, respectively; their half-saturation constants
(Ks) were 0.6 ± 0.4 and 3.8 ± 1.9 µM, respectively.
Fatty acid analyses.
Strains T103 and T104 were made up of
mainly straight-chain saturated and monounsaturated fatty acids, as
well as substantial amounts of tuberculostearic acid (Table
2) that are typical of mycobacteria
(16). Fatty acid analyses (34) indicated that T103 and T104 were different strains of a novel
Mycobacterium sp. that was most closely related to M. aurum (similarity indices of 0.31 and 0.24 with strains T103 and
T104, respectively).
16S rDNA sequence analyses.
Strains T103 and T104 possessed
identical 16S rDNA sequences. The secondary structures of the sequences
of T103 and T104 and other fast-growing mycobacteria were identical,
and they contained the shortened stem structure bounded by positions
455 to 477 (E. coli numbering) that typically distinguishes
the fast-growing from the slow-growing mycobacteria (41).
The levels of identity between the T103/T104 sequence and the sequences
of the fast-growing mycobacteria, slow-growing mycobacteria, and other
nonmycobacterial nocardioform bacteria ranged from 96.9 to 99.0%, 96.1 to 97.3%, and 93.0 to 95.7%, respectively. The T103/T104 sequence was
most identical to the sequences of M. aurum (identity,
99.0%) and M. komossense (identity, 98.9%).
Distance and bootstrap analyses confirmed that strains T103 and T104
clustered with fast-growing mycobacteria (Fig.
1). The mycobacteria fell into a closely
related, coherent group, distinct from the other high-G+C gram-positive
bacteria examined. Within the genus, the slow-growing mycobacteria
defined a distinct line of evolutionary descent, while the precise
relationships among the fast-growing species remained unresolved
because of low bootstrap values. Parsimony and maximum likelihood
analyses also showed that strains T103 and T104 belonged with the
fast-growing mycobacteria (data not shown).

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FIG. 1.
Unrooted evolutionary distance tree based on the 16S
rDNA sequences of strains T103 and T104, representative members of the
genus Mycobacterium, and other high-G+C gram-positive
bacteria. Bootstrap values greater than 50% are shown at the nodes.
Bar = 0.01 nucleotide difference per sequence position.
|
|
Bacterial counts and toluene levels.
No toluene was detected
at station U100, although very low levels of toluene (0.04 µM) were
found at station U50. Downstream stations D5 and D50 had high toluene
concentrations of 2.6 and 1.7 µM, respectively, in September 1993 (Fig. 2). The total heterotrophic bacterial plate counts at these stations ranged from 2 × 108 to 7.7 × 108 cells/g of biomass.
Toluene-degrading bacteria were not detected for station U100, where no
toluene was present. The counts of toluene-degrading bacteria for the
other three stations increased with increasing toluene concentration
and comprised 0.03, 1.09, and 0.35% of the total heterotrophic plate
counts at stations U50, D5, and D50, respectively.

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FIG. 2.
Bacterial counts (sampled on 7 September 1993) and
toluene levels (sampled on 19 September 1993) along the East Drainage
Ditch. Error bars represent standard deviations of duplicate samples.
, viable count of heterotrophic bacteria on 1% PTYG
plates incubated at 20°C for up to 4 weeks in the dark. ,
plate count of toluene-degrading bacteria on minimal salts agar with
110 µM toluene. Incubations were performed at 20°C for up to 4 weeks in the dark. , toluene concentration.
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|
 |
DISCUSSION |
Taxonomy and phylogeny.
Although strains T103 and T104 both
degrade toluene and have major characteristics of the genus
Mycobacterium, they exhibit some differences in physiology.
Unlike strain T103, strain T104 is able to grow on the xylenes. Also,
their fatty acid profiles are sufficiently different for them to be
considered different strains of a novel species of fast-growing
mycobacteria. Compared to the slow-growing mycobacteria, many of which
are human and animal pathogens, most of the fast-growing mycobacteria
are common saprophytes in natural habitats (18). They have
been isolated from a diverse array of habitats, are able to survive and
multiply under a wide range of environmental conditions, and can
biotransform a variety of xenobiotic compounds and pollutants,
including polycyclic aromatic hydrocarbons (15) and
groundwater-pollutant mixtures (4). There is a long history
of isolation of mycobacteria that have the capacity to degrade the
aromatic fraction of the oil in contaminated soils (44, 45).
The closest known relative of strains T103 and T104, M. aurum, is a fast-growing species commonly isolated from soils
(47) that is able to metabolize morpholine (6,
26) and vinyl chloride (17). The other closely related
species, M. komossense, is a fast-growing nonpathogenic
species isolated from Sphagnum vegetation of moors in south
Sweden and the Atlantic coastal area of Norway (19). It is
unable to utilize benzoate and benzamide; it is not known if it
possesses the ability to utilize other aromatic hydrocarbons or
xenobiotic compounds. Other closely related species have been found to
degrade a range of aromatic hydrocarbons. M. vaccae is the
only other Mycobacterium species known to grow on toluene.
It also grows on acetone and can degrade acetone, cyclohexane, styrene,
benzene, ethylbenzene, propylbenzene, dioxane, and 1,2-dichloroethylene (4). A Mycobacterium sp. that was closely related
to M. gilvum (14) was isolated from the soil of a
former coal gasification site and is able to degrade the polycyclic
aromatic hydrocarbons phenanthrene, pyrene, and fluoranthene
(2). Overall, their physiological versatility suggests
that the fast-growing mycobacteria should be important in pollutant
biodegradation, and our results point to the possibility that
mycobacteria may be useful in the bioremediation of contaminated
environments.
Biodegradation kinetics.
Toluene contamination of the East
Drainage Ditch appears to selectively enrich for toluene-degrading
bacteria within the epilithic microbial community. Maximal velocities
are somewhat higher than those reported for other aerobic
toluene-degrading bacteria; strain T104 also has a larger
Ks (3.8 µM) than those reported for other toluene-degrading bacterial strains. Pseudomonas sp. strain
T2 had a maximal velocity of 0.30 µmol of toluene/mg of protein per h
(assuming that 50% of a typical cell's dry weight is protein) and a
Ks of 0.48 µM (32). Corresponding
values for a terrestrial strain of Pseudomonas putida, PpF1,
were 0.43 µmol of toluene/mg of protein per h and 0.68 µM,
respectively (32). That Ks values for
strains T103 and T104 lie within the range of toluene concentrations observed in the stream suggests that these strains are adapted to the
ambient level of toluene contamination in the stream. Noncarbon nutrients are unlikely to be limiting in this case, because these are
present in the stream at high levels (43).
In order to assess the role that strains T103 and T104 may play in
toluene biodegradation in intact biofilms, toluene biodegradation rates
for the pure cultures were compared with rates obtained in the
laboratory for rock biofilms from a previous study (7). For
East Drainage Ditch rocks with their natural biofilms under summer
conditions, the rate was observed to be first order for toluene
concentrations up to 2.2 µM and approached zero order for
concentrations greater than 4.3 µM; the Vmax
was 2.0 nmol/cm2 of rock surface per h (7).
Assuming that mass transport is not limiting, the potential
contributions of strains T103 and T104 to toluene biodegradation on the
rock biofilm were estimated according to their cell densities (CD) on
the rock surfaces and their individual kinetic parameters. The CD of
1.8 × 104 cells/cm2 of rock surface was
estimated from plate counts of the mycobacterial isolates
(106 cells/g of biomass) and biomass density (0.018 g of
biomass/cm2 of rock surface). Since the biofilm data were
most reliable for toluene concentrations greater than 4.3 µM
(7), comparisons were performed for toluene concentrations
greater than or equal to 4.3 µM. Assuming a typical cell protein
weight of 0.2 pg (24) and a uniform distribution of
mycobacteria in the biofilm, the relative contributions of strains T103
and T104 to toluene biodegradation by the biofilm can be estimated as
follows:
where
and S is the toluene concentration.
At a toluene concentration of 4.3 µM, strains T103 and T104 are
estimated to account for 0.2 and 0.6%, respectively, of the toluene
biodegradation that occurs on the rock surfaces. These numbers should
be interpreted as upper bounds on the relative contributions of the
pure cultures to toluene degradation in the biofilms; to the extent
that diffusion limitation occurs, these numbers may be lower,
especially in the case of T104. Strain T103, having a
Ks much lower than 4.3 µM, would be less
affected. The low relative contributions suggest that other bacterial
species play a larger role than strains T103 and T104 in toluene
biodegradation on the rock surfaces. Cohen et al. (7) showed
that constantly shaken flasks provided a reasonable microcosm
simulation of the fast-flowing stream. In addition, mass transport of
the substrate to the biofilm surface is not calculated to be a limiting
factor in the turbulent flow regime of this stream, although biofilms themselves are not always free of transport limitation (21). We therefore expect that the results from laboratory microcosms offer a
reasonable estimate of the importance of T103 and T104 to toluene
degradation in the East Drainage Ditch itself.
Microbial ecology.
Toluene levels in the stream do not appear
to have a significant effect on total heterotrophic bacterial counts.
On the other hand, counts of toluene-degrading bacteria in samples from
the contaminated stations are about an order of magnitude higher than those from pristine stations, which suggests that toluene in the contaminated reaches of the stream has caused the epilithic bacterial communities to adapt by selectively enriching for toluene-degrading bacteria. Other studies of freshwater environments (30, 40) also reported viable heterotrophic counts to be unaffected by the
presence of a xenobiotic contaminant, while the numbers of organisms
capable of degrading the contaminant of interest increased by between 2 and 3 orders of magnitude. The increased counts in contaminated reaches
versus uncontaminated reaches of the East Drainage Ditch are not as
high as observed in these other studies, possibly because of greatly
reduced microbial activity at lower temperatures (30). The
East Drainage Ditch study was conducted in the fall when stream
temperatures averaged 11°C. In the other studies, temperatures
averaged 18°C (40) or ranged from 19 to 30°C
(30).
Although strains T103 and T104 were isolated from rock biofilms
collected in July 1992, a 16S rDNA clone with a sequence that is
identical to that of T103 and T104 was recovered independently from DNA
from rock biofilms in July 1993 (43). This detection of the
presence of the Mycobacterium sp. in the stream at different times suggests that this species is a permanent member of the stream's
microbial community. Attempts to isolate the Mycobacterium sp. from the pristine stations were unsuccessful. This, coupled with
the relative ease with which the Mycobacterium sp. strains were isolated from station D5, suggests a greater abundance of this
species in the contaminated reaches of the stream, perhaps as a result
of selection by toluene.
In summary, we describe two closely related toluene-degrading
mycobacterial strains isolated from rock surface biofilms from a
toluene-contaminated freshwater stream. These strains constitute a
novel fast-growing Mycobacterium species and extend our
knowledge of the list of Mycobacterium species that can grow
on toluene. Fast-growing mycobacteria are seen to play an important
role in the environment, as evidenced by increasing discoveries of
members within this group that can degrade a wide range of xenobiotic compounds. Our ecological experiments show a stream response to the
presence of low levels of toluene. This community response appears to
be more complex than the stimulation of a single indigenous toluene-degrading species; other microorganisms that are involved in
toluene degradation must also be present.
 |
ACKNOWLEDGMENTS |
This work was supported by NIEHS Superfund Basic Research Program
grant 5P42ES04675-06 and Office of Naval Research grant N00014-91-J-1489.
We thank Michael Collins for carrying out the kinetics experiment,
Karen Dohrman for performing the fatty acid analysis, Sue Lootens for
performing 16S rDNA sequencing, and Debra Lonergan for advising on
aspects of 16S rDNA sequencing and analyses.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Ralph M. Parsons
Laboratory, Department of Civil and Environmental Engineering,
Massachusetts Institute of Technology, Room 48-311, Cambridge, MA
02139. Phone: (617) 253-1637. Fax: (617) 258-8850. E-mail:
HFHemond{at}mit.edu.
Present address: Massachusetts Institute of Technology, Cambridge,
MA 02139.
 |
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