M&E Papers in Press. Published online on March 23, 2012 doi:10.1264/jsme2.ME11357

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2 Revised ME11357

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4 Isolation and Characterization of Novel Sulfate-Reducing Bacterium Capable of

5 Anaerobic Degradation of p-Xylene

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* 7 YURIKO HIGASHIOKA, HISAYA KOJIMA , AND MANABU FUKUI

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9 The Institute of Low Temperature Science, Hokkaido University, Nishi 8, Kita 19,

10 Kita-ku, Sapporo, Hokkaido 060-0819, Japan

11 Proofs

12 (Received December 21, 2011-Accepted February 2, 2012)

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14 Running headline: p-Xylene-Degrading Sulfate Reducer

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16 * Corresponding author. E-mail: [email protected]; Tel:

17 +81-11-706-5460;Advance Fax: +81-11-706-5460.

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19

20

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 22 A novel strain of p-xylene-degrading sulfate reducer was isolated in pure culture.

23 Strain PP31 was obtained from a p-xylene-degrading enrichment culture established

24 from polluted marine sediment. Analyses of the 16S rRNA gene and two functional

25 genes involved in sulfate respiration and anaerobic degradation of aromatic compounds

26 revealed that the isolate was closely related to members of the genus Desulfosarcina.

27 Strain PP31 was capable of growing on p-xylene under sulfate-reducing conditions, and

28 the ratio of generated sulfide and consumed p-xylene suggested complete oxidation by

29 the novel isolate. The strain could not grow on benzene, toluene, ethylbenzene,

30 m-xylene o-xylene, or n-hexane as an electron donor. Strain PP31 is the first isolated

31 bacterium that degrades p-xylene anaerobically, and will be useful to understanding the

32 mechanism of anaerobic degradation of p-xylene. Proofs

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34 Key words: Sulfate-reducing , p-xylene,View anaerobic biodegradation

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Advance

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 36 Due to its relatively high toxicity and water solubility, p-xylene is considered a

37 noteworthy organic pollutant. It is a monoaromatic compound refractory to biological

38 degradation, particularly under anoxic conditions. It has been demonstrated that

39 enrichment cultures can anaerobically degrade p-xylene under nitrate- or

40 sulfate-reducing conditions (12, 14). These studies indicated that complete oxidation of

41 p-xylene can be coupled with the reduction of nitrate to N2 or of sulfate to sulfide.

42 These enrichment cultures are overwhelmingly dominated by specific bacterial

43 phylotypes, suggesting that these bacteria are responsible for the anaerobic degradation

44 of p-xylene. Despite repeated trials with these cultures, a bacterium that can

45 anaerobically degrade of p-xylene has not yet been isolated in pure culture. In contrast,

46 the other isomers of xylene have been shown to be degrProofsaded by pure cultures of

47 sulfate-reducing bacteria (4, 11).

48 The above-mentioned p-xylene-degradingView sulfate-reducing culture was dominated by a

49 specific organism related to the genus Desulfosarcina, which includes strains capable of

50 degrading toluene and/or o-xylene. Impurity in this enrichment culture was shown in

51 another study, by shifts in the community structure induced when the substrate was

52 changed,Advance and by the isolation of another strain from it (5). In the present study, the

53 dominant organism in the enrichment culture was successfully isolated in pure culture

54 by applying a modified isolation technique. The obtained strain was characterized in

55 detail; this novel sulfate reducer could anaerobically degrade p-xylene without the

56 assistance of other bacteria.

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58 Materials and methods

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 59

60 Maintenance of p-xylene-degrading enrichment culture

61 A p-xylene-degrading sulfate-reducing enrichment culture was previously established

62 using marine sediments from Shuaiba, Kuwait as the inoculum (13). The enrichment

63 culture was maintained in our laboratory by periodic transfer to fresh medium. The

64 basal medium used was identical to that used in the previous study. It contained the

–1 65 following constituents (L ): 20.0 g NaCl; 4 g Na2SO4; 0.2 g KH2PO4; 0.25 g NH4Cl;

66 3.0 g MgCl2·6H2O; 0.5 g KCl; 0.15 g CaCl2·2H2O; 1 mL trace element solution; 1 mL

67 selenite-tungstate solution; 1 mL vitamin mixture solution; 1 mL vitamin B12 solution;

68 30 mL of 1 M NaHCO3 solution; and 1.5 mL of 1 M Na2S solution (18). This

69 bicarbonate-buffered defined medium was also used forProofs all culture experiments

70 performed in the present study unless specified otherwise. As the sole electron donor to

71 sustain growth, 2% (v/v) p-xylene solutionView prepared in 2,2,4,4,6,8,8-heptamethylnonane

72 to reduce the toxic effects was added to the basal medium (14). The volumetric ratio of

73 diluted p-xylene solution to basal medium was 1:25. An aliquot (1% of the volume of

74 fresh medium) of grown enrichment culture was inoculated using a N2-flushed sterilized

75 syringeAdvance into freshly prepared medium. As an additional reductant, sodium dithionite was

76 added to the fresh medium prior to each inoculation. The culture bottles were incubated

77 at 28°C in the dark. They were manually shaken several times a week. Growth was

78 monitored by turbidity and dissolved sulfide concentration in the aqueous phase,

79 determined as described previously (1).

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81 Isolation of a novel sulfate-reducing bacterium

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 82 The p-xylene-degrading enrichment culture was subjected to agar shake dilution (18)

83 with some modification, with p-xylene as the sole substrate for growth. First, the usual

84 agar shake dilution was performed using basal medium containing no water-soluble

85 organic substrate. After solidification of the medium, a small glass tube (internal

86 diameter, 1 mm; length, 40 mm) was stuck to the surface of solidified medium in each

87 agar shake tube (Fig. 1). Each small tube contained a droplet of 2%-diluted (v/v)

88 p-xylene solution, which was held in the tube by capillarity. The headspace of the agar

89 shake tubes was filled with the N2/CO2 (80:20 [v/v]) mixture, and the tubes were

90 incubated at 28°C. After 5 months, an isolated colony was picked and inoculated into

91 fresh medium containing 5 mmol L-1 acetate. The purity of the resulting culture was

92 confirmed by the experiments described below. The isolateProofs was designated as strain

93 PP31.

94 View

95 Physiological characterization of the isolated strain PP31

96 The physiological characterization of strain PP31 was performed at 28°C. The

97 utilization of electron donors in the presence of sulfate was tested by monitoring the

98 growthAdvance in media, each containing one of the following substrates (concentrations in

99 mmol L-1 unless otherwise stated): propionate (5), succinate (5), formate (5), fumarate

100 (10), pyruvate (10), n-butyrate (5), lactate (20), acetate (10), benzoate (1), glucose (10),

101 ethanol (5), phenol (0.5), and yeast extract (0.5 g L-1). For the test hydrocarbon

102 utilization, toluene, benzene, o-xylene, m-xylene, p-xylene, ethylbenzene, and n-hexane

103 were diluted to 2% (v/v) in 2,2,4,4,6,8,8-heptamethylnonane. Each solution was added

104 to 25-fold volume of basal medium. In the H2 utilization test, the headspace of the

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 105 culture bottle was filled with H2:N2:CO2 (50:40:10 by volume, total pressure=200 kPa).

106 The utilization of electron acceptors was tested using sulfate-free basal medium

107 containing 5 mmol L-1 propionate as an electron donor. The electron acceptors tested

108 were thiosulfate (10 mmol L-1), nitrate (10), and sulfite (5). Growth under fermentative

109 conditions was also tested with sulfate-free basal medium, using fumarate or lactate as

110 substrates. The optimum growth temperature was determined by incubation at 8

111 different temperatures ranging from 13 to 42°C, using the basal medium supplemented

112 with 10 mmol L-1 fumarate.

113 All culture experiments performed to allow physiological characterization were

114 followed by denaturing gradient gel electrophoresis (DGGE) analysis to verify the

115 identity and purity of the cells grown under various conditions.Proofs Cells were harvested

116 from growth-positive cultures using centrifugation and washed with phosphate-buffered

117 saline. From the collected cells, partial fragmentsView of the 16S rRNA gene were directly

118 amplified using the primer pair GC341F/533r (10, 12). DGGE was performed as

119 described previously (5).

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121 AnaerobicAdvance degradation of p-xylene by PP31

122 Portions (1.2 mL) of the pure culture of strain PP31 grown on 2% p-xylene were

123 inoculated into bottles containing 115 mL of the fresh medium and 5 mL p-xylene

124 solution of various concentrations. To investigate the effect of p-xylene concentration

125 on the strain, solutions of various concentrations (0, 0.2, 0.5, 1, 2, 4, 6, 8, 10, and 15%

126 in v/v) were prepared by diluting p-xylene with 2,2,4,4,6,8,8-heptamethylnonane.

127 During incubation at 28°C, the sulfide concentration of each bottle was continually

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 128 monitored as a readily measurable indicator of p-xylene degradation. The concentration

129 of p-xylene in the carrier phase was investigated by a gas chromatography system

130 (GC-2014; Shimadzu, Kyoto, Japan) equipped with a flame ionization detector. The

131 hydrophobic phase directly taken from the cultures was diluted with acetone, and then

132 mixed with a known amount of ethylbenzene as an internal standard. Hydrocarbons in

133 the diluted solution were separated by DB-5MS column (J & W Scientific, Flosom, CA,

134 USA; length, 30 m; internal diameter, 0.25 mm). The oven temperature program for

135 analysis was begun at 50°C for 10 min, proceeded at the rate of 5°C min–1 to 250°C,

136 and held for 60 min. The injector and detector temperatures were both set at 250°C.

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138 Phylogenetic analysis and G+C content determination Proofs

139 The total DNA of strain PP31 was extracted using the method described previously

140 (19). From the extracted genomic DNA,View fragments of nearly the full length of the 16S

141 rRNA gene were amplified with primers 27f and 1492r (10). Amplification was initiated

142 with 1 min of denaturation at 94°C. Each thermal cycle consisted of the following steps;

143 30 s denaturation at 94°C, 30 s annealing at 55°C, and 60 s elongation at 72°C.

144 Twenty-threeAdvance cycles were carried out, followed by an additional extension of 10 min at

145 72°C. To confirm the purity of the culture, partial fragments of the 16S rRNA gene were

146 also amplified using three universal PCR primer pairs, 27f/533r, 515f/1492r, and

147 341f/907r (10, 12).

148 Phylogenetic analyses were also performed on two functional genes, dsrA and bamA,

149 which are involved in sulfate respiration and anaerobic degradation of aromatic

150 compounds, respectively. Fragments of the dsrA gene that encoded the alpha subunit of

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 151 dissimilatory sulfite reductase were amplified using primers DSR1Fdeg (7) and

152 DSR1334R (16). The PCR steps were as follows: initial denaturation for 3 min at 94°C;

153 30 cycles of denaturation (40 s at 94°C), annealing (40 s at 54°C), and extension (120 s

154 at 72°C); and a final extension for 8 min at 72°C. Fragments of the bamA gene that

155 encoded 6-oxocyclohex-1-ene-1-carbonyl-coenzyme A hydrolase were amplified using

156 the primer pair BamA-SP9/BamA-ASP1 (8). The PCR steps were as follows: initial

157 denaturation for 10 min at 94°C; 35 cycles of denaturation (30 s at 94°C), annealing (45

158 s at 60°C), extension (1 min at 72°C), and a final extension for 10 min at 72°C. For

159 analysis of the bamA gene, one of the closest relatives of PP31 was also sequenced as a

160 reference. An actively growing culture of Desulfosarcina variabilis DSM 2060T was

161 obtained from Deutsche Sammlung von Mikroorganismen undProofs Zelkulturen (DSMZ) and

162 analyzed using a method identical to that used for strain PP31.

163 The PCR products were treated with ExoSViewAP-IT (USB, Cleveland, OH, USA) and

164 then used as templates for direct sequencing. The sequences of the PCR products were

165 determined by cycle sequencing using a dye terminator (BigDye Terminator v3.1 Cycle

166 Sequencing Kit; Applied Biosystems, Foster City, CA, USA).

167 The Advancenucleotide sequence of the 16S rRNA gene and amino acid sequences deduced

168 from the nucleotide sequences of the dsrA and bamA genes were aligned with reference

169 sequences from the public database using the ClustalX program (17). The phylogenetic

170 tree was constructed by the neighbor-joining method using MEGA software version 3.1

171 (9). Bootstrap analysis was performed for 500 replicates.

172 Genomic DNA for G+C content determination was extracted with the AquaPure

173 genomic DNA isolation kit (Bio-Rad, Hercules, CA, USA). The extracted DNA was

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 174 digested with P1 nuclease using a commercially available kit (Yamasa GC kit; Yamasa

175 Shoyu, Choshi, Japan) according to the manufacturer’s instructions. The resulting

176 mixture of deoxyribonucleosides was analyzed with a high-performance liquid

177 chromatography system equipped with an ODS column (YMC-Pack ODS-AQ; YMC,

178 Kyoto, Japan) and a UV detector (SPD-20A; Shimadzu, Kyoto, Japan). The G+C

179 content was determined by using an equimolar mixture of four deoxyribonucleosides

180 supplied in the kit as the quantitative standard.

181

182 Nucleotide sequence accession numbers

183 The nucleotide sequences obtained in this study have been assigned

184 DDBJ/EMBL/GenBank accession numbers AB610146-AB610148Proofs (16S rRNA, dsrA,

185 and bamA genes of strain PP31) and AB610408 (bamA gene sequence of D. variabilis).

186 View

187 Results

188 Isolation of a novel sulfate-reducing bacterium, strain PP31

189 As a result of agar shake dilution, with p-xylene as the sole substrate, well-isolated

190 coloniesAdvance were obtained from the deep agar tube. A culture originating from one of these

191 colonies was subjected to further experiments to check its purity. First, genomic DNA

192 was extracted from cells in the culture for analysis of the 16S rRNA gene. The PCR

193 product obtained with primer pair 27f/1492r was fully sequenced without ambiguity. It

194 perfectly matched the sequence of the DGGE band pXy-K-13 (13), thus corresponding

195 to the dominant organism in the original enrichment culture. All PCR products obtained

196 using three universal primer pairs were also sequenced without ambiguity and resulting

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 197 sequences were consistent with that obtained with the 27f/1492r primer pair.

198 The previous study on enrichment indicated that the organism corresponding to DGGE

199 band pXy-K-13 was readily outcompeted by other bacteria in the presence of aqueous

200 substrates (5). To confirm the absence of bacterial contaminants, the culture obtained in

201 this study was transferred to medium containing various electron donors or acceptors

202 including those less selective. As described below, no contaminating organism was

203 detected in these experiments. Based on these results, it was concluded that the

204 dominant bacterium in the enrichment culture was isolated in pure culture, and

205 designated as strain PP31.

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207 Degradation of p-xylene by strain PP31 Proofs

208 The pure culture of strain PP31 was transferred to medium not supplemented with any

209 water-soluble substrate but containing p-xylene.View With 2% p -xylene in the carrier phase,

210 growth of the strain was consistently observed when successively transferred to the

211 same p-xylene-containing medium. The effect of p-xylene concentration on the

212 degradation activity of PP31 was investigated using various concentrations of p-xylene.

213 The resultingAdvance changes in the sulfide concentration are shown in Fig. 2. These cultures

214 used p-xylene as the sole electron donor and sulfate as the sole electron accepter;

215 therefore, an increase in sulfide indicated oxidative degradation of p-xylene coupled

216 with sulfate reduction. Continuous sulfide production was observed in cultures at

217 p-xylene concentrations of 8% or lower (Fig. 2). In these cultures, turbidity, indicating

218 bacterial growth, was also observed. Degradation of p-xylene was confirmed by direct

219 measurement of its concentration in the carrier phase. p-Xylene was quantified for

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 220 cultures of 5 selected concentrations, and a decrease in p-xylene concentration was

221 consistently observed (Fig. 3). With 0.2 and 0.5% concentrations, p-xylene was depleted

222 until day 334. Total amounts of sulfide in these cultures on day 334 were compared to

223 the amounts of consumed p-xylene. The calculated molar ratios of generated sulfide and

224 consumed p-xylene were 5.3 and 5.0, respectively. These values are comparable to the

225 theoretically expected value of 5.25, calculated assuming complete oxidation of

2- 226 p-xylene coupled with sulfate reduction to sulfide, as follows: C6H4(CH3)2+5.25SO4 →

2- 227 8CO2+5.25S +5H2O.

228

229 Phylogenetic and physiological characteristics of strain PP31

230 Phylogenetic analysis based on the nearly full-length 16SProofs rRNA gene sequence

231 indicated that strain PP31 belongs to the class (Fig. 4). It is most

232 closely related to members of the genusView Desulfosarcina shown in the tree, with

233 sequence identity of 98%. The relatedness of PP31 to Desulfosarcina was also

234 supported by analyses of functional genes (Fig. 5). The sequence of the bamA gene in D.

235 variabilis was not available in the public database and was therefore determined in the

236 presentAdvance study. The nucleotide sequence obtained was similar to that of Desulfosarcina

237 ovata, and the amino acid sequence deduced was identical to that of D. ovata. These

238 sequences were also closely related to that of Desulfosarcina cetonica; however, strain

239 PP31 was distinct from these species.

240 Genomic G+C content of strain PP31 was determined to be 54.8%, which is higher

241 than those of Desulfosarcina variabilis and Desulfosarcina ovata (51%), but lower than

242 Desulfosarcina cetonica (59%).

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 243 In the presence of sulfate, cell growth was observed in cultures containing the

244 following substrates: acetate, propionate, succinate, pyruvate, formate, fumarate,

245 n-butyrate, benzoate, and yeast extract. Autotrophic growth on hydrogen was also

246 observed. No cell growth was observed in basal medium containing any of the

247 following substrates: lactate, phenol, ethanol, and glucose. Similarly, no growth was

248 observed in the cultures with hydrocarbons other than p-xylene. As for an electron

249 acceptor alternative to sulfate, growth was observed with thiosulfate, but not with

250 nitrate or sulfite. In sulfate-free medium without an alternative electron acceptor,

251 fumarate supported the growth of strain PP31, but lactate did not. The growth of strain

252 PP31 was observed over the temperature range of 20-37°C, with the optimum of 28°C.

253 As part of the purity check, growth-positive cultures inProofs these experiments were

254 subjected to DGGE. In all cases, only a single band at the same position as the inoculum

255 was observed (supplemental material), indicaViewting successful isolation of the dominant

256 organism in the original enrichment culture.

257

258 Discussion

259 Benzene,Advance toluene, ethylbenzene, and three isomers of xylene are often collectively

260 referred to as BTEX. Among the BTEX compounds, only p-xylene has not yet been

261 demonstrated to be anaerobically degraded by the activity of a single organism. To our

262 knowledge, strain PP31 is the first isolated bacterium that degrades p-xylene

263 anaerobically.

264 To reveal the biodegradation mechanism of hazardous materials, it is important to

265 obtain pure cultures of organisms that have the ability to catabolize the target materials.

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 266 Although the importance of anaerobic processes has been widely recognized,

267 difficulties in the cultivation and isolation of anaerobes have hindered advances in the

268 study of the anaerobic biodegradation of pollutants. In recent years, exhaustive analyses

269 of genomes and proteomes using advanced techniques have been applied to pure culture

270 of strict anaerobes capable of degrading hydrocarbons (2, 3). In this context, the

271 development of a pure culture of strain PP31 potentially has great importance in the

272 field of bioremediation.

273 It is likely that the isolated strain PP31 belongs to the genus Desulfosarcina. Members

274 of the genus Desulfosarcina are sulfate-reducing bacteria capable of degrading a variety

275 of complex organic substances. In this genus, three species with valid published names

276 are known, two of which, D. ovata and D. cetonica, are Proofsable to use toluene as an

277 electron donor; the former can also degrade o-xylene. In addition, another

278 toluene-degrading bacterium, related to theseView species, has been recently isolated (6). In

279 contrast to these close relatives, strain PP31 utilized p-xylene as an electron donor to

280 sustain growth but was not able to use other BTEX compounds including o-xylene and

281 toluene. Comparative analysis of these bacteria with different functions may be an

282 effectiveAdvance approach to understand the mechanism of anaerobic degradation of

283 monoaromatic hydrocarbons coupled with sulfate reduction or other types of anaerobic

284 respiration.

285

286 Acknowledgements

287 This study was supported by grants from the Ministry of Education, Culture, Sports,

288 Science and Technology, Japan (22370005), and from the Institute for Fermentation,

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 289 Osaka, to Fukui. We thank Shinya Sato and Takato Matsui for their assistance with the

290 quantification of p-xylene and G+C content determination, respectively.

291

292 References

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294 precipitated sulfides in cultures of sulfate-reducing bacteria. J. Microbiol. Methods

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305 metallireducensAdvance. Mol. Cell. Proteomics 8:2159-69.

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316 6. Higashioka, Y., H. Kojima, and M. Fukui. 2011. Temperature-dependent differences

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320 7. Klein, M., M. Friedrich, A.J. Roger, P. Hugenholtz, S. Fishbain, H. Abicht, L.L.

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323 183:6028–6035.

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326 M. Boll. 2008. 6-Oxocyclohex-1-ene-1-carbonyl-coenzyme A hydrolases from

327 obligately anaerobic bacteria: characterization and identification of its gene as a

328 functionalAdvance marker for aromatic compounds degrading anaerobes. Environ. Microbiol.

329 10:547–1556.

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331 9. Kumar, S., K. Tamura, and M. Nei. 2004. MEGA3: Integrated software for molecular

332 evolutionary genetics analysis and sequence alignment. Briefings Bioinf. 5:150–163.

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334 10. Lane, D.J. 1991. 16S/23S rRNA sequencing, p. 115–175. In E. Stackebrandt, and M.

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337 11. Morasch, B., B. Schink, C.C. Tebbe, and R.U. Meckenstock. 2004. Degradation of

338 o-xylene and m-xylene by a novel sulfatereducer belonging to the genus

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341 12. Muyzer, G., A. Teske, C.O. Wirsen, and H.W. Jannasch. 1995. Phylogenetic

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349 14. Rabus, R., R. Nordhaus, W. Ludwig, and F. Widdel. 1993. Complete oxidation of

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353 15. Rotaru, A.E., C. Probian, H. Wilkes, and J. Harder. 2009. Highly enriched

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357 16. Santillano, D., A. Boetius, and A. Ramette. 2010. Improved dsrA-based terminal

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361 17. Thompson, J.D., T.J. Gibson, F. Plewniak, F. Jeanmougin, and D.G. Higgins. 1997.

362 The Clustal_X windows interface: flexible strategies for multiple sequence alignment

363 aided by quality analysis tools. Nucleic. Acids. Res. 25:4876–4882.

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365 18. Widdel, F., and F. Bak. 1992. Gram-negative mesophilic sulfatereducing bacteria, p.

366 3352–3378. In A. Balows, H.G. Truper, M. Dworkin, W. Harder, and K.H. Schleifer

367 (ed.), The prokaryotes, 2nd ed., vol. IV. Springer-Verlag, New York. 368 Proofs 369 19. Wilson, K. 1990. Miniprep of bacterial genomic DNA, p. 2.4.1–2.4.2. In F.M. 370 Ausubel, R. Brent, R.E. Kingston, D.D.View Moore, J.G. Seidmann, J.A. Smith, and K. 371 Struhl (ed.), Short Protocols in Molecular Biology, 2nd ed., Wiley, New York.

372

373 Advance

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 374 Figure legends

375

376 Fig. 1. Schematic illustration of method used to isolate p-xylene-degrading sulfate

377 reducer.

378

379 Fig. 2. Changes in sulfide concentration in culture of PP31 incubated in the presence of

380 various concentrations of p-xylene in the carrier phase. *, 0%; ▵, 0.2%; ○, 0.5%; □,

381 1%; ‘, 2%; ▲, 4%; ●, 6%; ■, 8%; ‹, 10%; +, 15%; ×, abiotic control with 2%

382 p-xylene. 383 Proofs 384 Fig. 3. Changes in p-xylene concentrations in carrier phase in cultures of strain PP31. 385 The experiment was started on day 0 withView 0.2, 0.5, 1, 2, and 4% p-xylene. 386

387 Fig. 4. Phylogenetic position of strain PP31 within the family ,

388 based on 16S rRNA gene sequence analysis. Desulfovibrio desulfuricans is included as 389 an outgroup.Advance The tree was constructed with the neighbor-joining method using 1256 390 positions. Genetic distances were calculated using the Kimura 2-parameter model.

391 Numbers on nodes represent percentage values of 1,000 bootstrap resampling (values

392 larger than 50 are shown).

393

394 Fig. 5. Phylogenetic position of strain PP31 based on partial sequences of dsrA gene (A)

395 and bamA gene (B). These neighbor-joining trees were constructed with amino acid

396 sequences deduced from nucleotide sequences (218 and 83 amino acid positions were

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology 397 used for DsrA and BamA, respectively). Numbers on nodes are percentage values of

398 1,000 bootstrap resampling (values larger than 50 are shown). Genetic distances were

399 calculated with the Poisson correction

400

Proofs View

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology Proofs View

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Fig.1

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology Proofs

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology Proofs Fig.3

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology

Fig.4

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology

Proofs Fig.5

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Copyright 2012 by the Japanese Society of Microbial Ecology / the Japanese Society of Soil Microbiology