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Applied and Environmental Microbiology, January 1999, p. 251-259, Vol. 65, No. 1
Department of Microbiology, University of
Washington, Seattle, Washington 98195-7274
Received 16 June 1998/Accepted 19 October 1998
Two strains of bacteria were isolated from creosote-contaminated
Puget Sound sediment based on their ability to utilize naphthalene as a
sole carbon and energy source. When incubated with a polycyclic aromatic hydrocarbon (PAH) compound in artificial seawater, each strain
also degraded 2-methylnaphthalene and 1-methylnaphthalene; in addition,
one strain, NAG-2N-113, degraded 2,6-dimethylnaphthalene and
phenanthrene. Acenaphthene was not degraded when it was used as a sole
carbon source but was degraded by both strains when it was incubated
with a mixture of seven other PAHs. Degenerate primers and the PCR were
used to isolate a portion of a naphthalene dioxygenase iron-sulfur
protein (ISP) gene from each of the strains. A phylogenetic analysis of
PAH dioxygenase ISP deduced amino acid sequences showed that the genes
isolated in this study were distantly related to the genes encoding
naphthalene dioxygenases of Pseudomonas and
Burkholderia strains. Despite the differences in PAH
degradation phenotype between the new strains, the dioxygenase ISP
deduced amino acid fragments of these organisms were 97.6% identical. 16S ribosomal DNA-based phylogenetic analysis placed these bacteria in
the gamma-3 subgroup of the Proteobacteria, most closely
related to members of the genus Oceanospirillum. However,
morphologic, physiologic, and genotypic differences between the new
strains and the oceanospirilla justify the creation of a novel genus
and species, Neptunomonas naphthovorans. The type strain of
N. naphthovorans is strain NAG-2N-126.
As a group, the bacteria are
well-known for their metabolic diversity. One consequence of this
diversity is the fact that many biohazardous or persistent
anthropogenic chemical compounds are degraded by microbial activities.
One group of compounds that are generally both biohazardous and stable
are the polycyclic aromatic hydrocarbons (PAHs). PAHs are composed of
fused aromatic rings in linear, angular, or cluster arrangements and
are produced during the pyrolysis of organic material (1).
Although some PAHs are toxic, carcinogenic, or teratogenic, a variety
of bacteria can degrade certain PAHs completely to CO2 and
metabolic intermediates, en route gaining energy and carbon for cell growth.
Naphthalene, which is composed of two fused aromatic rings, has long
been used in enrichment cultures to isolate PAH-catabolizing bacteria
from soils and freshwater. Naphthalene-degrading bacteria commonly
isolated from terrestrial environments include Pseudomonas and Burkholderia strains. In addition, naphthalene-degrading
Pseudomonas, Comamonas, Acinetobacter,
and Sphingomonas strains have been isolated from soil
enrichment cultures by using other PAHs (29, 45). A
well-studied example of naphthalene catabolism is the naphthalene degradation (nah) pathway of Pseudomonas putida
NCIB 9816-4 and G7 (reviewed in reference 44). In
these Pseudomonas strains, 16 nah genes are
organized into two operons that encode enzymes specific to naphthalene
catabolism. A positive transcriptional regulator of the nah
genes, nahR, is encoded by a separate gene. NahR is
activated by salicylate, an intermediate in naphthalene degradation.
Four of the nah genes, nahAa, nahAb,
nahAc, and nahAd, encode components of the
naphthalene ring-hydroxylating dioxygenase, which catalyzes the
incorporation of both atoms of molecular oxygen into adjacent positions
of an aromatic ring, the first step in naphthalene catabolism. Since
naphthalene-degrading Pseudomonas strains are abundant in
PAH-contaminated terrestrial and freshwater sites (36),
studies of these bacteria in the laboratory may yield information that
is relevant to the dominant PAH degradation events at these sites.
In contrast, although naphthalene-degrading Pseudomonas
(9, 42) and Sphingomonas (10, 45)
strains have been enriched for and isolated from marine sediments, it
is not clear that PAH-catabolizing Pseudomonas,
Burkholderia, Comamonas, or
Sphingomonas strains are abundant in the marine environment.
In fact, the few studies that have focused on isolating numerically
important PAH-degrading bacteria from marine sites, both polluted and
nonpolluted, have identified members of completely different genera,
including the genera Cycloclasticus, Vibrio, and
Pseudalteromonas (11, 12, 20). All of these
bacteria are obligately marine; thus, it seems possible that a
significant portion of the PAH degradation that occurs in marine
environments is degradation by obligately marine microorganisms.
Importantly, little is known about how any of the obligately marine
bacteria catabolize PAHs, such as naphthalene.
To understand more about PAH-degrading bacteria in marine ecosystems,
Geiselbrecht et al. (11) assembled a collection of naphthalene- and phenanthrene-degrading bacteria from Eagle Harbor, a
coal tar creosote-contaminated Environmental Protection Agency (EPA)
superfund site in Puget Sound. These bacteria were identified as
Cycloclasticus, Vibrio, and
Pseudalteromonas species. The Vibrio isolate that
was obtained represents a new species, "Vibrio
cyclotrophicus" (21). Two other strains of
PAH-degrading bacteria isolated from Eagle Harbor, strains NAG-2N-126
and NAG-2N-113, did not belong to the genera mentioned above. The
purpose of this study was to describe the isolation of these two
strains, characterize their PAH degradation properties, and place them
into a meaningful taxonomic and phylogenetic framework.
(Part of this work was presented at the 96th General Meeting of the
American Society for Microbiology, New Orleans, La., May 1996.)
Media.
Strains NAG-2N-126 and NAG-2N-113, as well as control
Oceanospirillum strains, were grown in artificial seawater
solution ONR7a (5) supplemented with an appropriate carbon
source, in marine medium 2216 (Difco Laboratories, Detroit, Mich.), or
in peptone-succinate-salt (PSS) medium (22).
Sediment sampling and strain isolation.
Eagle Harbor
sediments were obtained on 17 September 1993 at global positioning
system coordinates 47°37.29', 122°30.25' and a depth of 15.5 m. The ambient sediment temperature was 16°C. Samples were obtained
with a boxcore device from the University of Washington's R.V.
Clifford Barnes. Sediment subcores were obtained by using
sterile modified 60-ml syringes; the subcores were stored at 4°C
until they were processed (within 24 h). Five milliliters of
surficial sediment, representing approximately the top 1 cm, was
diluted in 5 ml of ONR7a (a 1:2 dilution). After vigorous vortexing,
this preparation was diluted 1:200; 100 µl of the resulting 10-ml
1:200 dilution was spread plated onto an ONR7a plate solidified with
0.8% agarose. After the plates were dried, they were inverted, and
naphthalene crystals were placed in each lid. Naphthalene was the sole
carbon and energy source in the plates. The plates were incubated,
inverted and wrapped in Parafilm, at 15°C for approximately 4 weeks.
The resulting colonies were picked and inoculated into ONR7a containing
naphthalene crystals as the sole carbon source at a concentration of
approximately 1 mg ml PAH degradation experiments.
PAH degradation experiments
involved growing cultures with individual PAHs and monitoring the
disappearance of the PAH with a gas chromatograph equipped with a flame
ionization detector. Experiments were conducted in triplicate in 20-ml
Balch tubes with Teflon-lined stoppers. PAHs (5 ppm of naphthalene, 5 ppm of 1-methylnaphthalene, 5 ppm of 2-methylnaphthalene, 5 ppm of biphenyl, 1 ppm of acenaphthene, 1 ppm of fluorene, 1 ppm of
phenanthrene, 0.5 ppm of 2,6-dimethylnaphthalene) were delivered to the
tubes in methylene chloride, and the methylene chloride was removed by
evaporation. Five milliliters of ONR7a was added to each tube. The
tubes were vortexed for 30 s and shaken for several days to allow
the PAH to reach maximum solubility. The PAH concentrations in these
experiments were near or below the saturation concentration of each PAH
in seawater (25, 26).
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Polycyclic Aromatic Hydrocarbon Degradation by a New Marine
Bacterium, Neptunomonas naphthovorans gen. nov., sp.
nov.
and
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ABSTRACT
Top
Abstract
Introduction
Materials and methods
Results
Discussion
References
![]()
INTRODUCTION
Top
Abstract
Introduction
Materials and methods
Results
Discussion
References
![]()
MATERIALS AND METHODS
Top
Abstract
Introduction
Materials and methods
Results
Discussion
References
1. Purity was verified by
restreaking colonies onto ONR7a-agarose-naphthalene plates.
Dioxygenase ISP sequencing and phylogenetic analysis. DNA was isolated by using an Instagene kit (Bio-Rad, Hercules, Calif.) and late-exponential-phase cells grown in marine medium 2216. Naphthalene dioxygenase iron-sulfur protein (ISP) gene fragments were amplified by using PCR and the following two degenerate primers: pPAH-F (GGYAAYGCNAAAGAATTCGTNTGYWSHTAYCAYGGITGGG; [Pseudomonas putida G7 nahAc [38] amino acid positions 93 to 107) and pPAH-NR700 (CCAGAATTCNGTNGTRTTHGCATCRATSGGRTKCCA; P. putida G7 nahAc amino acid positions 316 to 327). The following PCR program was used: 35 cycles consisting of 1 min at 94°C (initial denaturation at 96°C), 1.5 min at 42°C, and 3 min at 72°C. The last step of the last cycle was continued for 7 min. Salts and free nucleotides were removed from the PCR product by using Ultrafree-MC filter units (Millipore, Bedford, Mass.), and the PCR product was then digested with EcoRI, isolated by agarose gel electrophoresis, and purified by using glass wool spin columns. The purified product was cloned into pBluescript II KS+ (Stratagene, La Jolla, Calif.) by using standard techniques (35). Dioxygenase genes were sequenced with a Taq DyeDeoxy terminator cycle sequencing kit (Applied Biosystems, Foster City, Calif.) and primers T3 and T7.
The following dioxygenase ISP sequences (GenBank accession numbers are given in parentheses) were retrieved from GenBank: P. putida G7 nahAc (M83947), Burkholderia sp. strain DNT dntAc (U62430), Pseudomonas aeruginosa PaK1 pahAc (D84146), P. putida JS42 ntdAc (U49504), P. putida F1 todC1 (J04996), Burkholderia cepacia LB400 bphA1 (M86348), P. putida KKS102 bphA1 (D17319), Comamonas testosteroni bphA1 (U47637), Rhodococcus sp. strain RHA1 bphA1 (D32142), Rhodococcus sp. strain M5 bpdB (U27591), Cycloclasticus pugetii PS-1 xylC1 (AF092998), and Cycloclasticus sp. strain 1P-32 nahAc (AF053737). The data set was aligned by using Pileup, which was obtained from the PHYLIP package, version 3.2 (8); PHYLIP was accessed through the Genetics Computer Group (13). The aligned data set was analyzed by performing a heuristic parsimony analysis with PAUP, version 3.0s (40). The data set was resampled 100 times by using a random sequence addition. The deduced amino acid alignments used for this analysis can be obtained in a variety of formats via the World Wide Web at the following URL: http://weber.u.washington.edu/~staley.16S rDNA sequencing and phylogenetic analysis. 16S rRNA genes were amplified by PCR by using universal primers and the following program: 32 cycles consisting of 1.5 min at 94°C, 1 min at 42°C, and 4 min at 72°C. The last step of the last cycle was continued for 10 min (19). The 16S ribosomal DNA (rDNA) PCR product was cloned and sequenced by using the protocol described above for naphthalene dioxygenase genes, except that the PCR product was cloned into the NotI site in pBluescript II KS+. 16S rDNA fragments (Escherichia coli nucleotides 28 to 1491 [2]) were sequenced by using 16S rDNA-specific sequencing primers (5).
The 16S rDNA sequence of strain NAG-2N-126 was examined with the Ribosomal Database Project (RDP) SIMILARITY_RANK program (24), which suggested that this strain is related to the genus Oceanospirillum. Representative sequences of members of the gamma-3 subgroup of the class Proteobacteria, which were used in the phylogenetic analyses, were obtained from the RDP or from GenBank. 16S rDNA sequences were initially aligned with similar sequences by using the RDP version 5.0 ALIGN_SEQUENCE program. The aligned sequences were imported into SeqApp (15), and manual adjustments were made to the aligned data set. The NAG-2N-126 16S rDNA sequence was projected onto the Oceanospirillum linum 16S rRNA secondary structure model (18) to check for correct alignment of homologous nucleotides. The data set was initially analyzed with PAUP, version 3.0s (40). The single most-parsimonious tree produced by a heuristic analysis was used to determine the transition-to-transversion ratio by using the MacClade 3.05 State Changes and Stasis command (27). The resulting ratio, 1.05, was specified in maximum-likelihood and neighbor-joining analyses. The programs used in the neighbor-joining analysis, NEIGHBOR and SEQBOOT, were obtained from the PHYLIP package (8). The fastDNAml program was obtained from the RDP (7, 31). The tree shown in Fig. 3 was constructed by using the TREEVIEW program (32). The 16S rDNA alignment used for these analyses can be obtained in a variety of formats via the World Wide Web at the following URL: http://weber.u.washington.edu/~staley.Microscopy. Late-exponential-phase cells of strain NAG-2N-126 grown on marine medium 2216 were concentrated by centrifugation and resuspension in 0.1 volume of half-strength ONR7a. Cells were pipetted onto Formvar-coated 200-mesh copper grids and allowed to settle for 10 min. Excess liquid was blotted from each preparation, and the cells were stained with 1.0% phosphotungstic acid. Cells were viewed with a JEOL transmission electron microscope at 60 kV.
Phenotypic tests. The pHs and salinities which allowed growth were examined in ONR7a broth supplemented with 0.1% peptone. For pH determinations, media were prepared with alternative buffers at concentrations of 25 mM near their pKa values. The following buffers were used: 2-(N-morpholino)ethanesulfonic acid (MES), pH 5.5; N-(2-acetamido)-2-aminoethanesulfonic acid (ACES), pH 6.5; 3-[N-tris(hydroxymethyl)methylamino]-2-hydroxypropanesulfonic acid (TAPSO), pH 7.6; tris(hydroxymethyl)methylaminopropanesulfonic acid (TAPS), pH 8.5; and 2-(N-cyclohexylamino)-ethanesulfonic acid (CHES), pH 9.5. Salinities were adjusted by varying the concentrations of the inorganic salts in ONR7a (the NH4Cl, Na2HPO4, FeCl2, and TAPSO concentrations were not varied). The salinities tested were 0.35, 1.05, 1.75, 3.5, 7.0, and 10.5%. Cultures were incubated at 24°C with shaking and were observed daily for 5 days. The temperature range for growth was determined on solid marine medium 2216 which was preincubated at the appropriate temperature for 2 h prior to inoculation. The temperatures tested included 4, 15, 24, 30, 37, and 42°C.
Gram stain reactions were determined by the method of Manafi and Kneifel (28). Routine phenotypic tests, including tests to determine catalase and oxidase activities, reduction of possible electron acceptors, and production of extracellular enzymes, were conducted as described previously (14). Nitrate reduction assays were performed with 0.1 and 0.01% NaNO3. Tween 80 was used for the lipase test. Poly-
-hydroxybutyrate inclusions were
visualized with Sudan black and were verified by purification and
spectral analysis. Luminescence was tested by growing strains on solid marine medium 2216 supplemented with 3% glycerol.
For the carbon source utilization tests, late-exponential-phase cells
were added to ONR7a containing the carbon source of interest at a
concentration of 0.1% in microtiter wells. Growth was monitored by
measuring the increase in turbidity at 600 nm with an automated
microplate reader (model EL311sx; BIO-TEK, Winooski, Vt.) and Delta
Soft II software (BioMetallics, Princeton, N.J.) after 2, 4, and 7 days
of incubation at room temperature. Growth was defined as two or more
cell doublings more than the negative control, which contained no
carbon source. Each test was carried out in triplicate. Under these
conditions, O. linum ATCC 11336 was not able to use any of
the carbon sources tested as a sole carbon and energy source, a result
that is consistent with other reports (22).
Carbohydrate acidification and fermentation tests were performed as
described previously (14) in PSS medium. Tests were conducted in triplicate, and O. linum was used as a negative
control. Tubes were observed daily for 2 weeks and were considered
positive if they became acidic at any time during the incubation
period. The fermentation tubes contained 0.15% agar, were inoculated
at approximately 42°C, and were covered with 2 to 3 mm of mineral oil. In most instances, growth occurred mostly near the surfaces of the
fermentation tubes; nevertheless, such tubes were considered positive.
Antibiotic resistance determination. Resistance to antibiotics was determined in microtiter wells containing marine medium 2216 and serially diluted antibiotics. The sensitivity level of an antibiotic was defined as the concentration at which the antibiotic reduced the level of growth to less than one-half the level of growth without an antibiotic. Turbidities were determined after 2 days with the microplate reader. The antibiotics tested were chloramphenicol, kanamycin, ampicillin, and streptomycin.
Determination of G+C content of DNA. The guanine-plus-cytosine content of genomic DNA was determined by the thermal denaturation method (14). E. coli and O. linum were used as reference organisms.
Nucleotide sequence accession numbers. The Neptunomonas naphthovorans NAG-2N-126 16S rDNA sequence has been deposited in the GenBank database under accession no. AF053734. The naphthalene dioxygenase ISP sequences of NAG-2N-126 and NAG-2N-113 have been deposited in the GenBank database under accession no. AF053736 and AF053735, respectively.
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RESULTS |
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Isolation of strains. Both NAG-2N-126 and NAG-2N-113 were obtained as part of a direct plating effort to compare the effectiveness of plate counts and the effectiveness of a most-probable-number (MPN) approach for enumeration of PAH-degrading bacteria. Since the sediments used were diluted prior to plating (final dilution, 1:20,000), isolation of these bacteria indicates that they were relatively numerous in Eagle Harbor, which is a highly contaminated EPA superfund site (3). It is important to note that creosote was visible as a free contaminant in these sediments. The two isolates were obtained from the same sediment boxcore sample but different plates.
PAH degradation experiments.
Both strains were tested for the
ability to degrade individual PAHs which are common in creosote and
other petroleum products (30) (Table
1). Consistent with the results of
sole-carbon-source tests, strains NAG-2N-126 and NAG-2N-113 degraded
naphthalene and 2-methylnaphthalene; NAG-2N-113 also degraded 1 ppm of
phenanthrene and 0.5 ppm of 2,6-dimethylnaphthalene. Interestingly,
1-methylnaphthalene was degraded by both strains, although the strains
did not grow with 1-methylnaphthalene as a sole carbon source. The
other PAHs that were tested were not significantly transformed in the
single-PAH experiments.
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Dioxygenase ISP sequence analysis. A low-stringency Southern hybridization experiment performed with the P. putida G7 nahAb, nahAc, and nahAd genes indicated that the new strains contained genes homologous to the genes that encode some of the prototypical naphthalene dioxygenase components (data not shown). Southern hybridization experiments performed with other dioxygenase probes representing the biphenyl and monoaromatic dioxygenase families, however, failed to reveal the presence of other dioxygenases in the new strains. Since Southern hybridization has limited power to recognize novel dioxygenase genes, we could not conclude from these experiments that the new strains only contain a single PAH dioxygenase.
Degenerate PCR primers were designed with the intent of amplifying approximately one-half of the nahAc gene, which encodes the naphthalene dioxygenase ISP. Degeneracies were introduced to allow binding to genes with high or low guanine-plus-cytosine contents. Using these primers and the PCR, we amplified and sequenced 630 bp (corresponding to 210 deduced amino acids) of a PAH dioxygenase large-subunit gene from NAG-2N-126 and NAG-2N-113. When deduced amino acid sequences were used, pairwise comparisons showed that the dioxygenases from NAG-2N-126 and NAG-2N-113 are 97.6% identical. The most closely related amino acid sequence, the P. aeruginosa PaK1 pahAc sequence (42), is 66% identical to the amino acid sequences of the dioxygenases from NAG-2N-126 and NAG-2N-113. The DNA guanine-plus-cytosine contents of the dioxygenase gene fragments from NAG-2N-126 and NAG-2N-113 were 42 and 40 mol%, respectively, indicating that these strains had not obtained these genes through a recent horizontal gene transfer event from bacteria with higher guanine-plus-cytosine contents. A parsimony analysis produced the dendrogram shown in Fig. 2. This tree shows that the putative dioxygenases from the new strains, together with naphthalene dioxygenases from Pseudomonas strains, nitroaromatic dioxygenases from Pseudomonas and Burkholderia strains, and a putative naphthalene dioxygenase from a Cycloclasticus strain, form a monophyletic cluster that does not include the biphenyl and monoaromatic dioxygenases.
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Genotypic analyses.
Nearly complete (approximately 1,470 bp)
16S rDNA sequences of strains NAG-2N-126 and NAG-2N-113 were
found to be identical. The NAG-2N-126 16S rDNA sequence was
compared to sequences representing the RDP's
Oceanospirillum assemblage and other members of the gamma-3
subgroup of the Proteobacteria (Table
2). Based on nucleotide identity alone,
strain NAG-2N-126 is clearly affiliated with the oceanospirilla.
The 16S rDNA sequence of NAG-2N-126 differs by 6.9% from the most
closely related sequence, the sequence of Oceanospirillum multiglobiferum.
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Colony and cell morphology. On solid PSS medium, NAG-2N-126 and NAG-2N-113 formed white, circular, convex colonies that had entire edges and were 3 mm in diameter. On solid marine medium 2216, both strains formed colonies similar to the colonies on PSS medium, except that the colonies were beige or light brown. When grown on solid marine medium 2216 containing naphthalene, both strains produced a diffusible brown pigment reminiscent of pigments produced by certain Oceanospirillum spp. when they are grown with aromatic amino acids (22, 23). Strain NAG-2N-113 produced a brilliant violet pigment when it was grown on solid marine medium 2216 supplemented with 3% glycerol.
NAG-2N-126 and NAG-2N-113 were examined by phase-contrast microscopy. Typical cells of each strain were straight rods, and very few cells were motile. The cells often clumped together, and India ink staining showed that a capsule was produced. Typical cells were 2 to 3 µm long and 0.7 to 0.9 µm in diameter. Electron microscopy of strain NAG-2N-126 showed that some cells had a single polar flagellum (Fig. 4).
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Phenotypic characteristics.
Strains NAG-2N-126 and NAG-2N-113
produced similar results in all tests. Both strains grew at pH values
between 6.5 and 8.5 (optimum pH, 7.5) at salinities ranging from 1.75 to 7.0% (50 to 200% seawater). The temperature range for growth was 4 to 24°C. Temperatures below 4°C were not tested. Both strains
were negative for DNase, amylase, gelatinase, and lipase
activities; however, a phosphatase was produced. Nitrate was not
reduced, nor was cysteine reduced to H2S; however, selenite
was reduced. The strains were gram negative, catalase and oxidase
positive, and ampicillin resistant (sensitivity level, 78 µg/ml).
Both strains produced poly-
-hydroxybutyrate granules. Neither strain
was luminescent under the conditions tested.
-hydroxybutyrate, glutarate,
p-hydroxybenzoate, L-serine, and
D-glucuronate. Strain NAG-2N-113 used naphthalene,
2-methylnaphthalene, phenanthrene, D-glucose,
D-fructose, glycerol, mannitol, D-arabitol, L-glutamate, L-proline, DL-alanine,
succinate, acetate, citrate, pyruvate, L-serine, and
DL-lactate. The following compounds were not used as sole
carbon sources by either strain: 2,6-dimethylnaphthalene, 1-methylnaphthalene, biphenyl, acenaphthene, fluorene,
L-arabinose, D-ribose,
D-xylose, L-rhamnose, D-galactose,
D-mannose, D-trehalose, D-melibiose, D-sucrose, D-lactose,
D-maltose, D-raffinose, dextran sulfate, sorbitol, adonitol,
methyl-D-glucopyranoside, ethanol, i-propanol,
glycine, L-leucine, L-ornithine,
L-arginine, tyrosine, gluconate, fumarate,
D-galacturonate, DL-malate, malonate,
propionate, DL-asparagine,
L-hyroxyproline, N-acetylglucosamine,
butyrate, valerate, adenine, D-glucosamine, caproate,
tartrate, erythritol, quinate, and methanol. Strain NAG-2N-113
was not tested with D-gluconate or
p-hydroxybenzoate.
Both strains fermented sucrose, D-glucose,
D-mannose, L-arabinose,
D-fructose, D-galactose, and mannitol. Only
NAG-2N-126 fermented D-lactose and D-xylose.
Neither strain fermented L-fucose, sorbitol, or dulcitol.
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DISCUSSION |
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Strains NAG-2N-126 and NAG-2N-113 were isolated from coal tar creosote-contaminated marine sediment from Eagle Harbor, Washington. Since the sediment was diluted 20,000-fold prior to plating, the bacteria were probably present at concentrations greater than 2 × 104 cells/ml of sediment. It is interesting that even though these bacteria were relatively numerous, they were not isolated from high-dilution PAH-MPN tubes that were inoculated with sediment from the same boxcore (11). Instead, Cycloclasticus, Vibrio, and Pseudalteromonas strains were isolated by the PAH-MPN protocol. This result reinforces a paradigm of environmental microbiology, that different isolation strategies can result in the isolation of different bacteria with the same physiological characteristic of interest. Thus, an integrated approach to bacterial isolation is recommended. Although the two strains were isolated from a dilute sediment sample, sequences related to the NAG-2N-126 or NAG-2N-113 sequence were not recovered from a 16S rDNA clonal library which was prepared from Eagle Harbor sediment (17). This result is not surprising since the direct microbial counts in sediment from the site exceeded the apparent concentration of strain NAG-2N-126 or NAG-2N-113 by several orders of magnitude (11).
PAH catabolism studies showed that strains NAG-2N-126 and NAG-2N-113 each degraded naphthalene and 2-methylnaphthalene with concomitant growth. In addition, each strain significantly transformed 1-methylnaphthalene, although neither strain used this compound as a sole carbon and energy source. A possible explanation for this is that the initial PAH degradation enzymes of the strains transform 1-methylnaphthalene, causing removal of the PAH; however, one or more enzymes downstream in the catabolic pathway fails to recognize the transformed 1-methylnaphthalene, resulting in dead end products. This could cause unfavorable kinetics for complete 1-methylnaphthalene removal.
Interestingly, there were differences in the PAH degradation profiles of strains NAG-2N-126 and NAG-2N-113, despite the high level of similarity of the putative naphthalene dioxygenase large subunits (level of amino acid identity, 97.6%). Strain NAG-2N-126 could not degrade phenanthrene, but strain NAG-2N-113 not only transformed phenanthrene but grew with phenanthrene as a sole carbon and energy source. In addition, strain NAG-2N-113 transformed 2,6-dimethylnaphthalene. This observation may be similar to the scenario described by Erickson and Mondello (6) for B. cepacia LB400 and "Pseudomonas pseudoalcaligenes" KF707. Very few amino acid differences in the biphenyl dioxygenase large subunits of these strains (level of amino acid identity, 95.6%) resulted in dramatically different abilities to degrade polychlorinated biphenyl. By changing the amino acids by site-directed mutagenesis and documenting changes in polychlorinated biphenyl degradation patterns, Erikson and Mondello showed that the catabolic differences were due to a few key amino acids. Alternatively, strain NAG-2N-113 may contain more than one dioxygenase, which results in the degradation of a wider range of aromatic substrates. Elucidation of the basis for the difference in phenanthrene and 2,6-dimethylnaphthalene catabolism by strains NAG-2N-126 and NAG-2N-113 will require a functional analysis of the dioxygenases of these organisms.
Although there were differences in the ability to degrade single PAHs, NAG-2N-126 and NAG-2N-113 produced similar results when they were incubated with a mixture of eight PAHs. Interestingly, both strains degraded acenaphthene only when they were incubated with other PAHs, even though the cells used in the single-PAH experiments were induced with naphthalene. Perhaps naphthalene or other PAHs are required to keep the PAH degradation enzymes induced. The PAH mixture experiments were important since PAHs are typically found as complex mixtures in the environment, such as creosote-contaminated sites, which contain 150 to 200 distinct aromatic compounds (30).
A phylogenetic analysis based on deduced amino acids encoded by putative PAH dioxygenase ISP genes of strains NAG-2N-126 and NAG-2N-113 indicated that the PAH dioxygenases are related to naphthalene dioxygenases (Fig. 2). This result is not surprising since these bacteria were isolated by using naphthalene and since PAH catabolism experiments indicated that they degrade naphthalenes but not a broad range of PAHs. Other dioxygenases in the naphthalene dioxygenase phylogenetic cluster include prototypical Pseudomonas naphthalene dioxygenases (38, 42), Burkholderia nitroaromatic dioxygenases (33, 39), and a putative dioxygenase from Cycloclasticus spp. (12). All of the dioxygenases in this group that have been characterized transform naphthalene, and some also degrade phenanthrene (37). Strains NAG-2N-126 and NAG-2N-113 also produce indigo from indole, another characteristic of the naphthalene dioxygenase family. Since the cloned dioxygenases of strains NAG-2N-126 and NAG-2N-113 are most similar to naphthalene dioxygenases and the aromatic substrates of the new strains are similar to the aromatic substrates of naphthalene dioxygenases, this suggests that the cloned genes encode functional dioxygenases; however, further study will be required to show this.
The isolation of naphthalene degradation genes from the new marine strains suggests that their naphthalene degradation system is similar to the prototypical Pseudomonas nah pathway. Members of the genus Cycloclasticus, another marine PAH-degrading genus, have also been shown to contain genes homologous to known PAH degradation genes of terrestrial bacteria. The Cycloclasticus xylC1 and xylC2 genes, which were first isolated from an Alaskan strain, "Cycloclasticus oligotrophus" RB1 (43), have recently been shown to be present in Cycloclasticus strains from Puget Sound and the Gulf of Mexico (12). The xylC1 and xylC2 genes encode enzymes that are related to the biphenyl dioxygenase large and small subunits, respectively. A second dioxygenase ISP gene related to the naphthalene dioxygenases has also recently been isolated from Cycloclasticus strains (12). Thus, at least some marine bacteria have PAH degradation systems that involve components homologous to components of the prototypical PAH degradation pathways.
However, while there are recognizable similarities between putative PAH degradation genes of obligately marine bacteria and known PAH-degrading dioxygenase ISP genes, the levels of homology are relatively low. For instance, the xylC1 and xylC2 genes of "C. oligotrophus" RB1 are 65.7 and 63.3% identical to "P. pseudoalcaligenes" KF707 bphA1 and bphA2. However, the corresponding ferredoxin and ferredoxin reductase genes, which are presumably required for dioxygenase activity, are not located near the xylC genes, as they are in most known PAH catabolic systems (43). Furthermore, naphthalene type dioxygenase ISP genes retrieved from Puget Sound and the Gulf of Mexico Cycloclasticus strains exhibit only 45.3% amino acid identity with their closest relative, P. aeruginosa PaK1 pahAc (12). Thus, the study of obligately marine bacteria has greatly expanded the known diversity of ISP sequences. Further study of the PAH catabolic systems of the obligately marine bacteria may reveal significant differences in gene organization and regulation, if not differences in the biochemical pathways for PAH catabolism, compared to the prototypical PAH degradation systems.
Phylogenetic analyses in which the nearly complete 16S rDNA sequence of
strain NAG-2N-126 was used clearly indicated that this strain is
related to members of the genus Oceanospirillum in the
gamma-3 subgroup of the Proteobacteria. However, the 16S rDNA sequence of the new strain was not closely related to any known
sequence (levels of identity,
93.1%). Accordingly, strain NAG-2N-126
was not monophyletic with the members of the genus Oceanospirillum, including O. linum, O. maris, O. beijerinckii, and O. multiglobiferum, and on a purely phylogenetic basis it is not
clear that the new strains should be included in the genus Oceanospirillum. The taxonomy of the bacteria in the
Oceanospirillum genetic cluster is complicated. Although
both "O. kriegii" and "O. jannaschii"
were originally placed in the genus Oceanospirillum, they
are not recognized members of the genus (23, 34). In addition, it has been suggested that O. japonicum should be
excluded from the genus Oceanospirillum based on low levels
of similarity to the other Oceanospirillum spp. as
determined by rRNA hybridization and multilocus enzyme electrophoresis
experiments (34). Our phylogenetic placement of O. japonicum further suggests that it should be excluded from the
genus Oceanospirillum.
Consistent with their phylogenetic placement, strains NAG-2N-126 and
NAG-2N-113 share many phenotypic properties with
Oceanospirillum spp. (Table
3). However, there are some major
phenotypic differences between strains NAG-2N-126 and NAG-2N-113 and
Oceanospirillum spp., suggesting that the new strains do not
belong to the genus Oceanospirillum. Morphologically,
strains NAG-2N-126 and NAG-2N-113 are rod shaped and have only a single
polar flagellum; Oceanospirillum spp. are helical and have
bipolar tufts of flagella (22, 23). Physiologically, the
Puget Sound strains utilize carbohydrates, both in the presence and in
the absence of oxygen, and produce acid in both cases.
Oceanospirillum spp. fail to utilize carbohydrates and are
obligately aerobic. In addition, strains NAG-2N-126 and NAG-2N-113
generally have a broader nutritional profile than the oceanospirilla
have.
|
Other genera that are phylogenetically similar to the new strains are
the genera Balneatrix (4) and
Marinobacterium (16). Although we were not able
to obtain the 16S rDNA sequence of Balneatrix alpica, this
bacterium is obviously not highly related to strains NAG-2N-126 and
NAG-2N-113 by virtue of its ability to reduce nitrate, its high DNA G+C
content, and its inability to grow in media containing more than 1%
NaCl. The genus Marinobacterium is obligately aerobic, has a
high DNA G+C content, and does not produce poly-
-hydroxybutyrate. Other phenotypic differences between the new strains and their relatives are summarized in Table 3. The phylogenetic and phenotypic differences between strains NAG-2N-126 and NAG-2N-113 and their closest
relatives justify the creation of a novel genus and species, Neptunomonas naphthovorans.
Description of Neptunomonas gen. nov. Neptunomonas (Nep.tu.no.mo'nas. Rom. myth. Neptune, the Roman god of the sea; Gr.n. monas, unit; M.L. n. Neptunomonas, Neptune's bacterium.) Gram-negative rod-shaped bacteria that belong to the gamma-3 subgroup of the Proteobacteria based on phylogenetic analyses of 16S rRNA genes. Cells of the type species are approximately 0.7 to 0.9 by 2.0 to 3.0 µm and are motile by means of a single polar flagellum. Facultatively aerobic. Oxidase and catalase positive. May utilize amino acids, carbohydrates, organic acids, sugar alcohols, and some PAHs as sole carbon and energy sources. Cells require sodium ions for growth.
The DNA G+C content is 46 mol%. The type and only species of the genus is Neptunomonas naphthovorans.Description of Neptunomonas naphthovorans sp. nov.
Neptunomonas naphthovorans (naph.tho.vo'rans. Chem. n.
naphthalene, a white crystalline hydrocarbon
[C10H8]; L. masc. vorus, devouring; L. part. naphthovorans, naphthalene devouring).
Rod-shaped bacteria that are motile by means of a single polar
flagellum. Growth occurs in defined media containing ammonium salts as
a nitrogen source. Facultatively aerobic. Marine; requires at least 50% seawater salinity for growth. Catalase and oxidase positive. Uses
some amino acids, carbohydrates, organic acids, and sugar alcohols, as
well as certain PAHs, for growth. Nitrate is not reduced. Colonies are
small, convex, and entire and produce a brown diffusible pigment when
the organism is grown on rich media supplemented with naphthalene. The
temperature range is
4 to 24°C. The DNA G+C content is 46 mol%.
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ACKNOWLEDGMENTS |
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This research was supported by grants N00014-91-J-1792 and N00014-91-J-1578 from the Office of Naval Research University Research Initiative in Bioremediation to the University of Washington under the auspices of the Marine Bioremediation Program. Additional support was provided by National Institutes of Health Biotechnology Fellowship GM-0837-05 to B.P.H. and by Sigma Xi Grants-in-Aid of Research to B.P.H. We also thank the National Oceanic and Atmospheric Administration's Sanctuaries and Reserves Division for continuing support of B.P.H.
We thank members of the University of Washington's Marine Bioremediation Program for useful discussions concerning this work. We also thank Jeanne Poindexter for hands-on help with the electron microscopy. In addition, we thank Rob Sanford and Joanne Chee-Sanford for help with gas chromatography. We thank John Gosink for plentiful advice concerning phylogenetic analyses. Finally, we thank Matthew Stoecker for critically evaluating the manuscript.
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FOOTNOTES |
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* Corresponding author. Mailing address: Department of Microbiology, University of Washington, Box 357242, Seattle, WA 98195-7274. Phone: (206) 543-6646. Fax: (206) 543-8297. E-mail: brianh{at}u.washington.edu.
Present address: Immunex Corporation, Bothell, WA 98021-3900.
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