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-Proteobacteria isolated from a deep-sea hydrothermal system in the Mid-Okinawa Trough
1 Laboratory of Marine Microbiology, Graduate School of Agriculture, Kyoto University, Kyoto 606-8502, Japan
2 Subground Animalcule Retrieval (SUGAR) Project, Frontier Research System for Extremophiles, Japan Agency for Marine–Earth Science and Technology, 2–15 Natsushima-cho, Yokosuka 237-0061, Japan
Correspondence
Satoshi Nakagawa
nakasato{at}kais.kyoto-u.ac.jp
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ABSTRACT |
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 TOP ABSTRACT INTRODUCTIONMETHODSRESULTS AND DISCUSSIONREFERENCES |
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-Proteobacteria, but that they had distant phylogenetic relationships with any species, within the phylogenetic groups, that had validly published names (sequence similarities were less than 91 %). On the basis of the physiological and molecular characteristics of the novel isolates, it is proposed that they should each be classified in a novel genus: Nitratiruptor tergarcus gen. nov., sp. nov., with MI55-1T (=JCM 12459T=DSM 16512T) as the type strain, and Nitratifractor salsuginis gen. nov., sp. nov., with E9I37-1T (=JCM 12458T=DSM 16511T) as the type strain.
The GenBank/EMBL/DDBJ accession numbers for the 16S rRNA gene sequences of strains MI55-1T and E9I37-1T are AB175499 and AB175500, respectively.
Graphs showing growth rates for strains MI55-1T and E9I37-1T at various temperatures, pH values, NaCl concentrations and O2 concentrations are available as supplementary figures in IJSEM Online.
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INTRODUCTION |
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TOPABSTRACTINTRODUCTIONMETHODSRESULTS AND DISCUSSIONREFERENCES |
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-Proteobacteria have been found in a variety of microbial habitats (reviewed by On, 2001
) including the gastrointestinal tracts of animals (Engberg et al., 2000), sulfurous springs (Angert et al., 1998; Rudolph et al., 2001), activated sludge (Snaider et al., 1997), oilfields (Gevertz et al., 2000), an Antarctic Ocean water-column (Bano & Hollibaugh, 2002) and deep-sea cold seep sediments (Li et al., 1998; Inagaki et al., 2002). They metabolize a variety of compounds such as sulfur, iron, arsenate and even man-made pollutants such as tetrachloroethene (Scholz-Muramatsu et al., 1995).
Recently, culture-independent molecular analyses revealed the global predominance of members of the -Proteobacteria in deep-sea hydrothermal environments (Polz & Cavanaugh, 1995; Reysenbach et al., 2000). On the basis of 16S rRNA gene sequences, the members of the -Proteobacteria detected in extreme environments were very diverse and were classified into six subgroups (groups A to G) (Corre et al., 2001; Takai et al., 2003a). Some -proteobacteria were found in episymbiotic association with deep-sea vent metazoans (Haddad et al., 1995; López-García et al., 2002; Goffredi et al., 2004). These researches provided new insights into the ecological roles and phylogenetic diversity of previously unknown extremophiles (Takai et al., 2003a; Campbell et al., 2003).
In terms of physiology, members of the -Proteobacteria have been poorly understood because of their strong resistance to cultivation. There is some evidence for the involvement of these micro-organisms in the biogeochemical sulfur cycle in deep-sea hydrothermal environments (Wirsen et al., 1993; López-García et al., 2003). However, none of these micro-organisms had been cultured until recently. Some members of the -Proteobacteria have now been successfully isolated from deep-sea hydrothermal environments and then characterized (Alain et al., 2002; Miroshnichenko et al., 2002, 2004; Inagaki et al., 2003, 2004; Takai et al., 2003a, 2004, 2005; Nakagawa et al., 2005). Although these isolates have provided some physiological and taxonomic information about deep-sea -proteobacteria, they still represent only a tiny fraction of the phylogenetic diversity revealed by culture-independent analysis. The physiological diversity and ecological significance of these members of the -Proteobacteria remain to be determined. Previously, we reported on the isolation and partial characterization of many -proteobacterial strains, covering nearly all of the previously uncultivated phylogroups (Takai et al., 2003a). Among the isolates, Hydrogenimonas thermophila EP1-55-1%T and Sulfurovum lithotrophicum 42BKTT were recently reported as the first species within -proteobacterial groups A and F, respectively (Takai et al., 2004; Inagaki et al., 2004). In addition to the species, strains MI55-1T and E9I37-1T were also identified as representatives of groups A and F, respectively, but were not described in detail (Takai et al., 2003a). In this paper, we report a detailed characterization and taxonomic study of these strains and propose the new genera Nitratiruptor and Nitratifractor.
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METHODS |
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TOPABSTRACTINTRODUCTIONMETHODSRESULTS AND DISCUSSIONREFERENCES |
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). Samples of two chimney structures called North Big Chimney and Central Big Chimney were collected at the summits of the sulfide mounds in the sediment-hosted back-arc hydrothermal system Iheya North (27° 47' N 126° 53' E), at a depth of approximately 1000 m. The distance between the two sulfide mounds was approximately 50 m. The chimney fraction from North Big Chimney, approximately 10 cm in length and up to 15 cm in width, was subsampled into four sections as previously described (Takai et al., 2001). Likewise, the chimney fraction from Central Big Chimney, approximately 6 cm in length and up to 3 cm in width, was subsampled into three sections. The temperatures of vent fluids from North Big Chimney and Central Big Chimney were 311 and 247 °C, respectively. As a consequence of subseafloor phase-separation (boiling/distillation of hydrothermal fluids), the geochemical composition of the two sets of vent fluids differed (Chiba et al., 2000): the Cl– concentration of the vent fluids from North Big Chimney was similar to that of sea water (511 mM), whereas the vent fluids from Central Big Chimney had a brine-rich composition (864 mM).
Subsamples of the chimney structures were individually suspended in sterilized MJ synthetic sea water (Sako et al., 1996) containing 0·05 % (w/v) sodium sulfide under a N2 atmosphere. The suspended slurries were used to inoculate MMJHS medium (Takai et al., 2003a). MMJHS medium contained 1 g NaHCO3, Na2S2O3.5H2O and NaNO3, 30 g S0 and 10 ml vitamin solution (Balch et al., 1979) per litre MJ synthetic sea water. The medium was prepared under a H2/CO2 (80 : 20) gas phase (300 kPa). The pH of the medium was adjusted to 6·7.
To evaluate the abundance of culturable micro-organisms, a series of serial 1 : 7 dilution experiments were performed at 25, 37, 55, 70 and 85 °C. To obtain pure cultures from the highest positive dilutions, dilution to extinction was carried out at least five times at a temperature identical to that used for the enrichment. Purity was confirmed routinely under a phase-contrast Olympus BX51 microscope and by repeated partial sequencing of the 16S rRNA gene using several PCR primers (Lane, 1991).
Optical and electron microscopy.
Cells were routinely observed with a phase-contrast microscope (BX51; Olympus) equipped with the SPOT RT Slider CCD camera system (Diagnostic Instruments). Negative staining of cells for transmission electron microscopy (JEM-1210 apparatus; JEOL) was achieved as described previously (Zillig et al., 1990).
Measurement of growth.
Growth of the novel isolates was determined using direct cell counts after staining with 4',6-diamidino-2-phenylindole (Porter & Feig, 1980). All of the experiments described below were conducted in duplicate. The cultivation temperatures were 37 and 55 °C for strains E9I37-1T and MI55-1T, unless otherwise noted. To determine temperature, pH and NaCl ranges for growth, cultures of each isolate were grown in 100 ml glass bottles (Schott Glaswerke) containing 20 ml MMJHS medium in a temperature-controlled dry oven and were shaken at 100 r.p.m. in all cases. Temperatures were measured inside control flasks alongside the cultures, as described previously (Sako et al., 2003). When a pH optimum was being determined, the pH of the MMJHS medium was adjusted to various values with 10 mM acetate/acetic acid buffer (pH 4–5), MES (pH 5–6), PIPES (pH 6–7), HEPES (pH 7–7·5) and Tris (pH 8–9·5) at room temperature. If necessary, the pH of the medium was readjusted immediately before inoculation with H2SO4 or NaOH. The pH was found to be stable during the cultivation period. NaCl requirements were determined by using various concentrations of NaCl (0–7 %, w/v) in the medium.
Each isolate was tested for the ability to grow on combinations of a single electron donor and acceptor. MJ synthetic sea water supplemented with 0·1 % (w/v) NaHCO3 and vitamin solution (Balch et al., 1979) was used as the basal medium. In an attempt to examine growth on hydrogen as an electron donor, a H2/CO2 (80 : 20) gas phase (300 kPa) was used. Electron acceptors were provided at final concentrations of 0·1 % (w/v) (Na2S2O3.5H2O and NaNO3), 0·01–0·1 % (w/v) (Na2SO3 and NaNO2), 5 mM (arsenate, arsenite, selenate and selenite), 3 % (w/v) (S0) or 0·09–20 % (v/v) (O2). For testing growth on Na2S2O3.5H2O (0·1 %, w/v), S0 (3 %, w/v) or arsenite and selenite (5 mM) as electron donor, N2/CO2 (80 : 20) was used as the gas phase (300 kPa). NaNO3 (0·1 %, w/v) or O2 (0·09–20 %, v/v) was provided as an electron acceptor; the latter was provided by injecting a defined volume of O2 into the culture bottles as previously described (Nakagawa et al., 2003). The presence or absence of cell growth was determined by microscopic observation.
To clarify the metabolic characteristics of the isolates, gas composition and anion concentrations were monitored during growth. Gas- and ion-chromatography were used as described previously (Nakagawa et al., 2004). Qualitative ammonium determination was done spectrophotometrically using Nessler's reagent on a UV-1600 spectrophotometer (Shimadzu).
In an attempt to examine heterotrophic growth, experiments were conducted using MMJHS medium without NaHCO3 under a gas phase of 100 % H2 (300 kPa). Each of the following potential carbon sources was tested at concentrations of 0·01 and 0·1 % (w/v): L-cystine, L-phenylalanine, L-proline, Casamino acids, D(+)-glucose, lactose, maltose, chitin, starch, cellulose, formate, formaldehyde, formamide, acetate, citrate, pyruvate, propionate, 2-propanol, methanol, tryptone peptone (Difco) and yeast extract (Difco). In addition, to assess the utilization of these organic compounds as an energy source, substrates were added to MMJHS medium under a N2/CO2 (80 : 20) gas phase (300 kPa).
To determine the nitrogen source for growth of the isolates, 0·025 % (w/v) NaNO2, NH4Cl or NaNO3 was added to MMJHS medium lacking all nitrogen sources, under a H2/CO2/O2 (80 : 19·5 : 0·5) gas phase (300 kPa). Likewise, utilization of N2 was examined under a H2/N2/CO2/O2 (60 : 20 : 19·5 : 0·5) gas phase (300 kPa).
Susceptibility to antibiotics (ampicillin, kanamycin, rifampicin, streptomycin and chloramphenicol) was determined using MMJHS medium. Antibiotic concentrations from 50 to 300 µg ml–1 were tested.
Fatty acid methyl ester analysis.
Cellular fatty acid compositions were analysed using cells grown in MMJHS medium under a H2/CO2 (80 : 20) gas phase (300 kPa) at optimum growth temperatures in the late-exponential growth phase. Lyophilized cells (100 mg) were placed in a Teflon-lined, screw-capped tube (Corning) containing 3 ml anhydrous methanolic HCl and heated at 100 °C for 3 h. The extraction and analysis of fatty acid methyl esters were as described previously (Takai et al., 2003b).
Base composition of DNA.
Genomic DNA was prepared as described by Lauerer et al. (1986). The G+C content (mol%) of the genomic DNA was determined by direct analysis of deoxyribonucleotides using HPLC with a DNA-GC kit (Yamasa Shouyu) after digestion of the DNA with nuclease P1 (Tamaoka & Komagata, 1984).
16S rRNA gene sequence analysis.
The 16S rRNA gene was amplified by using a PCR with primers Eubac27F and 1492R (Lane, 1991). The sequence of the 1·5 kb PCR product was directly determined in both strands using a dideoxynucleotide chain-termination method with a DNA sequencer (model 3100; Perkin Elmer/Applied Biosystems). The sequences were aligned with a subset of 16S rRNA gene sequences obtained from DDBJ by the FastAligner utility of ARB software (Ludwig et al., 2004). The resulting alignment was verified against known secondary regions, and only unambiguously aligned nucleotide positions (1105 bases) were used for phylogenetic analyses with PAUP* 4.0 beta 10 (Swofford, 2000). A phylogenetic tree was inferred by using neighbour-joining analysis (Saitou & Nei, 1987) with the Jukes–Cantor correction (Jukes & Cantor, 1969). Bootstrap analysis was done using 100 replicates to provide confidence estimates for tree topologies.
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RESULTS AND DISCUSSION |
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TOPABSTRACTINTRODUCTIONMETHODSRESULTS AND DISCUSSIONREFERENCES |
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Cell morphology
Cells of both strains (MI55-1T and E9I37-1T) were short rods (Fig. 1). Gram staining was negative for both isolates. In both cases, the cells appeared to be non-motile under any cultivation conditions, although strain MI55-1T had bipolar flagella, as shown in Fig. 1(a). Cells occurred singly or in pairs. No sporulation was apparent under any laboratory conditions.
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-Proteobacteria (Table 1). However, strain MI55-1T had relatively narrow temperature, pH and NaCl ranges for growth (Table 1). Strain MI55-1T grew at temperatures in the range 40–57 °C, showing optimum growth at 55 °C. The generation time and maximum cell yield at 55 °C were about 2·5 h and 5·2x109 cells ml–1, respectively. No growth was observed below 37 °C or above 57 °C (see Supplementary Fig. A available in IJSEM Online). Growth occurred between pH 5·4 and 6·9, with optimum growth at about pH 6·4. No growth was detected below pH 4·8 or above pH 7·6 (Supplementary Fig. B). The isolate had an absolute requirement for NaCl for growth, and grew at concentrations in the range 1·5–4·0 % (w/v) NaCl; optimum growth occurred at around 2·5 % NaCl. No growth was observed below 1·0 % NaCl or above 5·0 % NaCl (Supplementary Fig. C).
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or O2 as electron acceptor. Final O2 concentrations from 0·21 to 0·50 % (v/v) supported growth (optimum, 0·40 %, v/v) [see graph (d) available as a supplementary figure in IJSEM Online]. Growth with optimal O2 concentrations and nitrate produced lower cell yields (8·6x107 and 4·5x108 cells ml–1, respectively) than that in MMJHS medium, suggesting that the isolate uses S0 as a sulfur source. The isolate was unable to use any organic compounds as energy or carbon sources. Strain MI55-1T utilized ammonium or nitrate as a nitrogen source but could not utilize molecular nitrogen or nitrite.
During growth of strain MI55-1T, consumption of nitrate and production of N2 were observed (Fig. 2a). The consumption or production of 
, 
or 
was not detected (data not shown). Although the consumption of H2 could not be measured, these results indicated that the isolate utilized H2 as an electron donor and nitrate as an electron acceptor. The accumulation of potential end-products and intermediate products of nitrate reduction, such as nitrite, ammonium, NO and N2O, was not detected. None of the thermophilic members of the -Proteobacteria isolated so far produce N2 as a final product of nitrate reduction (Table 1
). After the exhaustion of nitrate, production of H2S was detected (Fig. 2a). Throughout growth, the consumption or production of 
, 
or 
was not detected (data not shown), suggesting that the isolate reduced S0 with H2. These results suggest that the isolate potentially utilizes S0 as an electron acceptor, although S0 could not serve as a sole electron acceptor to support growth.
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Growth characteristics of strain E9I37-1T
Strain E9I37-1T grew at temperatures in the range 28–40 °C, showing optimum growth at 37 °C. The optimum growth temperature of the isolate was higher than those of other mesophilic -proteobacterial species (Table 1). The generation time and maximum cell yield at 37 °C were about 2·5 h and 1·5x109, respectively. No growth was observed at 25 or 45 °C (Supplementary Fig. A). Growth occurred between pH 5·6 and 7·6, with optimum growth at about pH 7·0. No growth was detected below pH 5·2 or above pH 8·1 (Supplementary Fig. B). The isolate had an absolute requirement for NaCl for growth, and grew at concentrations in the range 1·5–3·5 % (w/v) NaCl, with optimum growth at around 3·0 % NaCl. No growth was observed below 1·0 % NaCl or above 4·0 % NaCl (Supplementary Fig. C).
Strain E9I37-1T represents the first mesophilic and facultatively anaerobic member of the -Proteobacteria reported to grow on molecular hydrogen (Table 1). Strain E9I37-1T utilized H2 as an electron donor and or O2 as an electron acceptor. Final O2 concentrations from 0·09 to 0·55 % (v/v) supported growth (optimum around 0·2 %, v/v) [supplementary graph (d) in IJSEM Online]. Growth at optimal O2 concentrations and with nitrate produced lower cell yields (9·8x107 and 1·2x108 cells ml–1, respectively) than that in MMJHS medium, suggesting that the isolate uses S0 as a sulfur source. The isolate was unable to use any organic compounds as energy or carbon sources. Strain E9I37-1T utilized ammonium or nitrate as a nitrogen source.
During growth of strain E9I37-1T in MMJHS medium, nitrate consumption and N2 production were observed (Fig. 2b). Consumption or production of , , or H2S was not detected (data not shown). These results indicated that the isolate utilized H2 as an electron donor and nitrate as an electron acceptor. The accumulation of potential end-products and intermediate products of nitrate reduction was not detected.
Strain E9I37-1T was sensitive to ampicillin, rifampicin, streptomycin and chloramphenicol (each at 50 µg ml–1), but was insensitive to 
150 µg ml–1 kanamycin (though sensitive at 200 µg ml–1).
Fatty acid and DNA base compositions
Each of the two isolates had a distinctive fatty acid composition (Table 1). The major cellular fatty acids of strain MI55-1T were C18 : 1 (43·6 %), C16 : 0 (31·6 %), 3-OH C14 : 0 (9·9 %), C12 : 0 (8·1 %), C16 : 1 (3·6 %), C18 : 0 (1·6 %) and C14 : 0 (1·6 %). The major cellular fatty acids of strain E9I37-1T were C18 : 1 (42·3 %), C16 : 1 (30·7 %), C16 : 0 (24·3 %), 3-OH C14 : 0 (1·1 %), C14 : 0 (0·9 %) and C18 : 0 (0·7 %). The G+C contents of the genomic DNA of strains MI55-1T and E9I37-1T were found to be 29·6 and 35·5 mol%, respectively, both being lower than those of the closest relatives (described below) (Table 1).
Phylogenetic analyses
Almost-complete 16S rRNA gene sequences from strains MI55-1T and E9I37-1T were determined (1409 and 1439 bp). According to neighbour-joining analysis, strains MI55-1T and E9I37-1T were members of groups A and F, respectively, of the -Proteobacteria (Corre et al., 2001) (Fig. 3). H. thermophila EP1-55-1%T and Sulfurovum lithotrophicum 42BKTT are the only species described to date within each of these phylogroups. The sequences of strains MI55-1T and E9I37-1T were distantly related to those of H. thermophila EP1-55-1%T (90·2 % 16S rRNA gene sequence similarity) and Sulfurovum lithotrophicum 42BKTT (88·5 % similarity), respectively. This low phylogenetic relatedness is below the common index of 16S rRNA gene sequence similarity for differentiation of micro-organisms at the genus level (Gillis et al., 2001).
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-Proteobacteria. Although all of the deep-sea members of the -Proteobacteria isolated so far share the ability to utilize molecular hydrogen and/or sulfur-bearing compounds as energy sources (Table 1), members of each subgroup appear to have consistent physiological characteristics (i.e. group A, facultatively anaerobic thermophiles; group F, facultatively anaerobic mesophiles).
Compared with other members of the -Proteobacteria, strains MI55-1T and E9I37-1T have distinctive physiological, chemotaxonomic and molecular characteristics (Table 1). In addition, 16S rRNA gene sequence comparisons demonstrate that each of the two strains represents a novel genus within the -Proteobacteria. Therefore we propose the names Nitratiruptor tergarcus gen. nov., sp. nov. for strain MI55-1T and Nitratifractor salsuginis gen. nov., sp. nov. for strain E9I37-1T.
Previous reports (Wirsen et al., 1993; Taylor et al., 1999) have classified the -Proteobacteria as microaerobic sulfur-oxidizers. However, new insights (including those in this report) point to their metabolic versatility (Table 1) and therefore to their importance in the cycling of other elements in addition to sulfur. Strains MI55-1T and E9I37-1T were able to utilize hydrogen and nitrate as electron donor and electron acceptor, respectively. Thus, members of the -Proteobacteria probably play a significant role not only in sulfur-cycling, but in hydrogen- and nitrogen-cycling in deep-sea hydrothermal environments.
Description of Nitratiruptor gen. nov.
Nitratiruptor [Ni.tra.ti.rup'tor. N.L. masc. n. nitras, -atis nitrate; L. masc. n. ruptor breaker; N.L. masc. n. Nitratiruptor nitrate-breaker (-reducer)].
Non-motile short rods that stain Gram-negative. Anaerobic to microaerobic. Thermophilic. Strictly chemolithoautotrophic. Able to utilize molecular hydrogen as an electron donor and oxygen or nitrate as electron acceptors. NaCl absolutely required for growth. The G+C content of genomic DNA is about 30 mol%. Major cellular fatty acids are C18 : 1, C16 : 0 and 3-OH C14 : 0. On the basis of the 16S rRNA gene sequence, the genus Nitratiruptor is distantly related to the genus Hydrogenimonas. Members of the genus Nitratiruptor occur in deep-sea hydrothermal fields. The type species is Nitratiruptor tergarcus.
Description of Nitratiruptor tergarcus sp. nov.
Nitratiruptor tergarcus [terg.ar'cus. L. neut. n. tergum back; L. gen. masc. n. arcus (pronounced with long u) of an arc; N.L. gen. n. tergarcus from a black arc (geological term)].
Cells have a mean length of 2·5 µm and a width of approximately 0·8 µm. The temperature range for growth is 40–57 °C (optimum 55 °C). The pH range for growth is 5·4–6·9 (optimum, pH 6·4). NaCl in the concentration range 15–40 g l–l is an absolute growth requirement; optimum growth occurs at 25 g NaCl l–l. Strictly chemolithoautotrophic growth occurs with molecular hydrogen as an electron donor and with oxygen or nitrate as electron acceptor. Nitrate is reduced to N2. Major cellular fatty acids are C18 : 1 (43·6 %), C16 : 0 (31·6 %), 3-OH C14 : 0 (9·9 %) and C12 : 0 (8·1 %). The G+C content of the genomic DNA is 29·6 mol% (HPLC).
The type strain, MI55-1T (=JCM 12459T=DSM 16512T), was isolated from the Iheya North hydrothermal field in the Mid-Okinawa Trough, Japan.
Description of Nitratifractor gen. nov.
Nitratifractor [Ni.tra.ti.frac'tor. N.L. masc. n. nitras, -atis nitrate; L. masc. n. fractor breaker; N.L. masc. n. Nitratifractor nitrate-breaker (-reducer)].
Non-motile short rods that stain Gram-negative. Anaerobic to microaerobic. Mesophilic. Strictly chemolithoautotrophic. Able to utilize molecular hydrogen as an electron donor and oxygen or nitrate as an electron acceptor. NaCl absolutely required for growth. The G+C content of genomic DNA is about 35 mol%. Major cellular fatty acids are C18 : 1, C16 : 1 and C16 : 0. On the basis of the 16S rRNA gene sequence, the genus Nitratifractor is distantly related to the genus Sulfurovum. Members of the genus Nitratifractor occur in deep-sea hydrothermal fields. The type species is Nitratifractor salsuginis.
Description of Nitratifractor salsuginis sp. nov.
Nitratifractor salsuginis (sal.su'gi.nis. L. gen. fem. n. salsuginis from brine).
Cells have a mean length of 2·5 µm and a width of approximately 0·6 µm. The temperature range for growth is 28–40 °C (optimum, 37 °C). The pH range for growth is 5·6–7·6 (optimum, pH 7·0). NaCl in the concentration range 15–35 g l–l is an absolute growth requirement; optimum growth occurs at 30 g NaCl l–l. Strictly chemolithoautotrophic growth occurs with molecular hydrogen as an electron donor and with oxygen or nitrate as an electron acceptor. Nitrate is reduced to N2. Major cellular fatty acids are C18 : 1 (42·3 %), C16 : 1 (30·7 %) and C16 : 0 (24·3 %). The G+C content of genomic DNA is 35·5 mol% (HPLC).
The type strain, E9I37-1T (=JCM 12458T=DSM 16511T), was isolated from the Iheya North hydrothermal field in the Mid-Okinawa Trough, Japan.
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ACKNOWLEDGEMENTS |
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REFERENCES |
|---|
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TOPABSTRACTINTRODUCTIONMETHODSRESULTS AND DISCUSSIONREFERENCES |
|---|
Angert, E. R., Northup, D. E., Reysenbach, A.-L., Peek, A. S., Goebel, B. M. & Pace, N. R. (1998). Molecular phylogenetic analysis of a bacterial community in Sulphur River, Parker Cave, Kentucky. Am Mineral 83, 1583–1592.[Abstract]
Balch, W. E., Fox, G. E., Magrum, L. J., Woese, C. R. & Wolfe, R. S. (1979). Methanogens: reevaluation of a unique biological group. Microbiol Rev 43, 260–296.
Bano, N. & Hollibaugh, J. T. (2002). Phylogenetic composition of bacterioplankton assemblages from the Arctic Ocean. Appl Environ Microbiol 68, 505–518.
Campbell, B. J., Stein, J. L. & Cary, S. C. (2003). Evidence of chemolithoautotrophy in the bacterial community associated with Alvinella pompejana, a hydrothermal vent polychaete. Appl Environ Microbiol 69, 5070–5078.
Chiba, H., Kataoka, S., Ishibashi, J. & Yamanaka, T. (2000). Distribution of hydrothermal vents, fluid chemistry, and phase separation at the Iheya North seafloor hydrothermal system, Mid-Okinawa Trough. Eos Trans AGU Fall Meet Suppl 81, WP86 (Abstract).
Corre, E., Reysenbach, A.-L. & Prieur, D. (2001). Epsilon-proteobacterial diversity from a deep-sea hydrothermal vent on the Mid-Atlantic Ridge. FEMS Microbiol Lett 205, 329–335.[Medline]
Engberg, J., On, S. L., Harrington, C. S. & Gerner-Smidt, P. (2000). Prevalence of Campylobacter, Arcobacter, Helicobacter, and Sutterella spp. in human fecal samples as estimated by a reevaluation of isolation methods for campylobacters. J Clin Microbiol 38, 286–291.
Gevertz, D., Telang, A. J., Voordouw, G. & Jenneman, G. E. (2000). Isolation and characterization of strains CVO and FWKOB, two novel nitrate-reducing, sulfide-oxidizing bacteria isolated from oil field brine. Appl Environ Microbiol 66, 2491–2501.
Gillis, M., Vandamme, P., De Vos, P., Swings, J. & Kersters, K. (2001). Polyphasic taxonomy. In Bergey's Manual of Systematic Bacteriology, 2nd edn, vol. 1, pp. 43–48. Edited by D. R. Boone, R. W. Castenholz & G. M. Garrity. London: Springer.
Goffredi, S. K., Warén, A., Orphan, V. J., Van Dover, C. L. & Vrijenhoek, R. C. (2004). Novel forms of structural integration between microbes and a hydrothermal vent gastropod from the Indian Ocean. Appl Environ Microbiol 70, 3082–3090.
Haddad, A., Camacho, F., Durand, P. & Cary, S. C. (1995). Phylogenetic characterization of the epizootic bacteria associated with the hydrothermal vent polychaete Alvinella pompejana. Appl Environ Microbiol 61, 1679–1687.[Abstract]
Inagaki, F., Sakihama, Y., Inoue, A., Kato, C. & Horikoshi, K. (2002). Molecular phylogenetic analyses of reverse-transcribed bacterial rRNA obtained from deep-sea cold seep sediments. Environ Microbiol 4, 277–286.[CrossRef][Medline]
Inagaki, F., Takai, K., Nealson, K. H. & Horikoshi, K. (2003). Sulfurimonas autotrophica gen. nov., sp. nov., a novel sulfur-oxidizing -proteobacterium isolated from hydrothermal sediments in the mid-Okinawa Trough. Int J Syst Evol Microbiol 53, 1801–1805.
Inagaki, F., Takai, K., Nealson, K. H. & Horikoshi, K. (2004). Sulfurovum lithotrophicum gen. nov., sp. nov., a novel sulfur-oxidizing chemolithoautotroph within the -Proteobacteria isolated from Okinawa Trough hydrothermal sediments. Int J Syst Evol Microbiol 54, 1477–1482.
Jukes, T. H. & Cantor, C. R. (1969). Evolution of protein molecules. In Mammalian Protein Metabolism, pp. 21–132. Edited by H. N. Munro. New York: Academic Press.
Lane, D. J. (1991). 16S/23S rRNA sequencing. In Nucleic Acid Techniques in Bacterial Systematics, pp. 115–175. Edited by E. Stackebrandt & M. Goodfellow. Chichester: Wiley.
Lauerer, G., Kristjansson, J. K., Langworthy, T. A., König, H. & Stetter, K. O. (1986). Methanothermus sociabilis sp. nov., a second species within the Methanothermaceae growing at 97 °C. Syst Appl Microbiol 8, 100–105.
Li, L., Kato, C. & Horikoshi, K. (1998). Bacterial diversity in deep-sea sediments from different depths. Biodivers Conserv 8, 659–677.[CrossRef]
López-García, P., Gaill, F. & Moreira, D. (2002). Wide bacterial diversity associated with tubes of the vent worm Riftia pachyptila. Environ Microbiol 4, 204–215.[CrossRef][Medline]
López-García, P., Duperron, S., Philippot, P., Foriel, J., Susini, J. & Moreira, D. (2003). Bacterial diversity in hydrothermal sediment and epsilonproteobacterial dominance in experimental microcolonizers at Mid-Atlantic Ridge. Environ Microbiol 5, 961–976.[CrossRef][Medline]
Ludwig, W., Strunk, O., Westram, R. & 29 other authors (2004). ARB: a software environment for sequence data. Nucleic Acids Res 32, 1363–1371.
Miroshnichenko, M. L., Kostrikina, N. A., L'Haridon, S., Jeanthon, C., Hippe, H., Stackebrandt, E. & Bonch-Osmolovskaya, E. A. (2002). Nautilia lithotrophica gen. nov., sp. nov., a thermophilic sulfur-reducing -proteobacterium isolated from a deep-sea hydrothermal vent. Int J Syst Evol Microbiol 52, 1299–1304.[Abstract]
Miroshnichenko, M. L., L'Haridon, S., Schumann, P., Spring, S., Bonch-Osmolovskaya, E. A., Jeanthon, C. & Stackebrandt, E. (2004). Caminibacter profundus sp. nov., a novel thermophile of Nautiliales ord. nov. within the class ‘Epsilonproteobacteria’, isolated from a deep-sea hydrothermal vent. Int J Syst Evol Microbiol 54, 41–45.
Nakagawa, S., Takai, K., Horikoshi, K. & Sako, Y. (2003). Persephonella hydrogeniphila sp. nov., a novel thermophilic, hydrogen-oxidizing bacterium from a deep-sea hydrothermal vent chimney. Int J Syst Evol Microbiol 53, 863–869.
Nakagawa, S., Nakamura, S., Inagaki, F., Takai, K., Shirai, N. & Sako, Y. (2004). Hydrogenivirga caldilitoris gen. nov., sp. nov., a novel extremely thermophilic, hydrogen- and sulfur-oxidizing bacterium from a coastal hydrothermal field. Int J Syst Evol Microbiol 54, 2079–2084.
Nakagawa, S., Inagaki, F., Takai, K., Horikoshi, K. & Sako, Y. (2005). Thioreductor micantisoli gen. nov., sp. nov., a novel mesophilic, sulfur-reducing chemolithoautotroph within the -Proteobacteria isolated from hydrothermal sediments in the Mid-Okinawa Trough. Int J Syst Evol Microbiol 55, 599–605.
On, S. L. W. (2001). Taxonomy of Campylobacter, Arcobacter, Helicobacter and related bacteria: current status, future prospects and immediate concerns. J Appl Microbiol 90, 1S–15S.[CrossRef]
Polz, M. F. & Cavanaugh, C. M. (1995). Dominance of one bacterial phylotype at a Mid-Atlantic Ridge hydrothermal vent site. Proc Natl Acad Sci U S A 92, 7232–7236.
Porter, K. G. & Feig, Y. S. (1980). The use of DAPI for identifying and counting microflora. Limnol Oceanogr 25, 943–948.
Reysenbach, A.-L., Longnecker, K. & Kirshtein, J. (2000). Novel bacterial and archaeal lineages from an in situ growth chamber deployed at a Mid-Atlantic Ridge hydrothermal vent. Appl Environ Microbiol 66, 3798–3806.
Rudolph, C., Wanner, G. & Huber, R. (2001). Natural communities of novel Archaea and Bacteria growing in cold sulfurous springs with a string-of-pearls-like morphology. Appl Environ Microbiol 67, 2336–2344.
Saitou, N. & Nei, M. (1987). The neighbor-joining method: a new method for reconstructing phylogenetic trees. Mol Biol Evol 4, 406–425.[Abstract]
Sako, Y., Takai, K., Ishida, Y., Uchida, A. & Katayama, Y. (1996). Rhodothermus obamensis sp. nov., a modern lineage of extremely thermophilic marine bacteria. Int J Syst Bacteriol 46, 1099–1104.
Sako, Y., Nakagawa, S., Takai, K. & Horikoshi, K. (2003). Marinithermus hydrothermalis gen. nov., sp. nov., a strictly aerobic, thermophilic bacterium from a deep-sea hydrothermal vent chimney. Int J Syst Evol Microbiol 53, 59–65.
Scholz-Muramatsu, H., Neumann, A., Meßmer, M., Moore, E. & Diekert, G. (1995). Isolation and characterization of Dehalospirillum multivorans gen. nov., sp. nov., a tetrachloroethene-utilizing, strictly anaerobic bacterium. Arch Microbiol 163, 48–56.[CrossRef]
Snaider, J., Amann, R., Huber, I., Ludwig, W. & Scheifer, K.-H. (1997). Phylogenetic analysis and in situ identification of bacteria in activated sludge. Appl Environ Microbiol 63, 2884–2896.[Abstract]
Swofford, D. L. (2000). PAUP* – Phylogenetic Analysis Using Parsimony and Other Methods, version 4. Sunderland, MA: Sinauer.
Takai, K., Komatsu, T., Ingaki, F. & Horikoshi, K. (2001). Distribution of archaea in a black smoker chimney structure. Appl Environ Microbiol 67, 3618–3629.
Takai, K., Inagaki, F., Nakagawa, S., Hirayama, H., Nunoura, T., Sako, Y., Nealson, K. H. & Horikoshi, K. (2003a). Isolation and phylogenetic diversity of members of previously uncultivated epsilon-Proteobacteria in deep-sea hydrothermal fields. FEMS Microbiol Lett 218, 167–174.[Medline]
Takai, K., Nakagawa, S., Sako, Y. & Horikoshi, K. (2003b). Balnearium lithotrophicum gen. nov., sp. nov., a novel thermophilic, strictly anaerobic, hydrogen-oxidizing chemolithoautotroph isolated from a black smoker chimney in the Suiyo Seamount hydrothermal system. Int J Syst Evol Microbiol 53, 1947–1954.
Takai, K., Nealson, K. H. & Horikoshi, K. (2004). Hydrogenimonas thermophila gen. nov., sp. nov., a novel thermophilic, hydrogen-oxidizing chemolithoautotroph within the -Proteobacteria, isolated from a black smoker in a Central Indian Ridge hydrothermal field. Int J Syst Evol Microbiol 54, 25–32.
Takai, K., Hirayama, H., Nakagawa, T., Suzuki, Y., Nealson, K. H. & Horikoshi, K. (2005). Lebetimonas acidiphila gen. nov., sp. nov., a novel thermophilic, acidophilic, hydrogen-oxidizing chemolithoautotroph within the ‘Epsilonproteobacteria’, isolated from a deep-sea hydrothermal fumarole in the Mariana Arc. Int J Syst Evol Microbiol 55, 183–189.
Tamaoka, J. & Komagata, K. (1984). Determination of DNA base composition by reverse-phase high-performance liquid chromatography. FEMS Microbiol Lett 25, 125–128.
Taylor, C. D., Wirsen, C. O. & Gaill, F. (1999). Rapid microbial production of filamentous sulfur mats at hydrothermal vents. Appl Environ Microbiol 65, 2253–2255.
Wirsen, C. O., Jannasch, H. W. & Molyneaux, S. J. (1993). Chemosynthetic microbial activity at Mid-Atlantic Ridge hydrothermal vent sites. J Geophys Res 98, 9693–9703.
Zillig, W., Holz, I., Janekovic, D. & 7 other authors (1990). Hyperthermus butylicus, a hyperthermophilic sulfur-reducing archaebacterium that ferments peptides. J Bacteriol 172, 3959–3965.
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, H2S production; 
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