Abstract
A Gram-negative, pleomorphic, aerobic, haloalkaliphilic archaeon, strain 167-74T, was isolated from commercial rock salt imported into Japan from China. Phylogenetic analysis based on 16S rRNA gene sequence similarities showed that strain 167-74T is closely related to Halostagnicola larsenii XH-48T (98.3 %) and Halostagnicola kamekurae 194-10T (97.2 %). The major polar lipids of the isolate were C20C20 and C20C25 derivatives of phosphatidylglycerol and phosphatidylglycerol phosphate methyl ester. A glycolipid was not detected, in contrast to the two existing, neutrophilic species of the genus Halostagnicola. The DNA G+C content of strain 167-74T was 60.7 mol%. and it gave DNA–DNA reassociation values of 19.5 and 18.8 %, respectively, with Hst. larsenii JCM 13463T and Hst. kamekurae 194-10T. Therefore, strain 167-74T represents a novel species, for which the name Halostagnicola alkaliphila sp. nov. is proposed, with the type strain 167-74T ( = JCM 16592T = CECT 7631T).
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The GenBank/EMBL/DDBJ accession number for the 16S rRNA gene sequence of strain 167-74T is AB533255.
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Two supplementary figures are available with the online version of this paper.
The genus Halostagnicola belonging to the family Halobacteriaceae was first described by Castillo et al. (2006) and, at the time of writing, the genus comprised two species, Halostagnicola larsenii (Castillo et al., 2006) and Halostagnicola kamekurae (Nagaoka et al., 2010). Cells of the type strains of both species are pleomorphic, neutrophilic and strictly aerobic. In this report, we describe an alkaliphilic haloarchaeon, strain 167-74T, isolated from commercial rock salt, that belongs to the genus Halostagnicola.
Strain 167-74T was isolated from a sample of rock salt produced in Hubei Province, China. The rock salt is labelled ‘BEST ancient rock salt’ and is sold in Japan by Hanamasa Co., Ltd. The salt sample (1.0 g) was dissolved in 5 ml sterile 5 % NaCl solution and spread on JCM no. 167 medium agar plates. JCM no. 167 medium contains (l−1) 200 g NaCl, 5.0 g Na2CO3, 0.24 g MgSO4 . 7H2O, 1.0 g KCl, 1.0 g NH4Cl, 5.0 g yeast extract (Difco), 5.0 g Casamino acids (Difco), 1.0 g sodium glutamate, 1.0 g KH2PO4, 0.17 g CaSO4 . 2H2O and 1.0 ml trace metal solution. The trace metal solution contained (l−1) 0.1 g ZnSO4 . 7H2O, 0.03 g MnCl2 . 4H2O, 0.3 g H3BO3, 0.2 g CoCl2 . 6H2O, 0.01 g CuCl2 . 2H2O, 0.02 g NiCl2 . 6H2O and 0.03 g Na2MoO4 . 2H2O (adjusted to pH 3.6 with HCl). All components, except Na2CO3, were dissolved in distilled water and made to 900 ml. The medium was adjusted to pH 6.5 with 40 % KOH, and autoclaved. Sodium carbonate was dissolved in 100 ml distilled water and autoclaved separately. After autoclaving, the two solutions were mixed aseptically. The final pH was 9.0. After incubation of agar plates at 37 °C for 2–4 weeks, various coloured colonies developed. Four colonies were transferred to fresh agar plates, and pure cultures were obtained by plating serial dilutions and repeated transfers on agar plates. Partial 16S rRNA gene sequences of the four isolates were almost the same, and the most alkaliphilic strain, 167-74T, was chosen as a representative for further experiments.
Hst. larsenii JCM 13463T, obtained from the Japan Collection of Microorganisms, and Hst. kamekurae 194-10T, isolated in our previous study (Nagaoka et al., 2010), were used as reference strains.
Colony morphology was observed on agar medium after incubation for 2–3 weeks at 37 °C. Gram-staining was performed according to Dussault (1955). Cell morphology and motility were examined using phase-contrast microscopy (Axiovert 135; Zeiss). Total DNA was extracted by the method of Cline et al. (1989). The 16S rRNA gene was analysed as described previously (Nagaoka et al., 2010). 16S rRNA gene sequences retrieved from the DDBJ (Miyazaki et al., 2003; Pearson & Lipman, 1988) were aligned using clustal_x version 2.0.12 (Larkin et al., 2007). A phylogenetic tree was reconstructed by the neighbour-joining method (Saitou & Nei, 1987) and evaluated by bootstrap sampling, from 1000 replicates (Felsenstein, 1985). Maximum-likelihood analysis was performed with RAxML 7.0.4 using the GTR+Γ model (Stamatakis et al., 2005), and confidence values for the maximum-likelihood tree were obtained by bootstrapping (1000 replicates) using consense in phylip (Felsenstein, 2002). The 16S rRNA gene sequence of strain 167-74T was most similar to those of Hst. larsenii JCM 13463T (98.5 %) and Hst. kamekurae 194-10T (97.2 %). Lower similarities (<94.6 %) were found with sequences from other species of the family Halobacteriaceae with validly published names. The neighbour-joining (Fig. 1) and maximum-likelihood (Supplementary Fig. S1, available in IJSEM Online) trees also supported the conclusion that strain 167-74T was most closely related to members of the genus Halostagnicola.
Phylogenetic tree derived from 16S rRNA gene sequences showing the position of strain 167-74T among related haloarchaea. The tree was reconstructed by the neighbour-joining method. Bootstrap values >600 (from 1000 replicates) are shown. Bar, 1 % sequence divergence.
Total lipids were extracted with chloroform/methanol as described previously (Kamekura, 1993). TLC of polar lipids (Supplementary Fig. S2) suggested that strain 167-74T and the type strains of the other two species of the genus Halostagnicola contained C20C20 and C20C25 archaeol derivatives of phosphatidylglycerol (PG) and phosphatidylglycerol phosphate methyl ester (PGP-Me), as shown by the double spot for PGP-Me. Phospholipids were the same as for the two type strains of the genus Halostagnicola, but no glycolipid spot was detected in strain 167-74T.
Results of physiological characterization are given in the species description, with methods mentioned in the proposed minimal standards for the descriptions of new taxa in the order Halobacteriales (Oren et al., 1997), as described previously (Castillo et al., 2006; Nagaoka et al., 2010). The range and optimal NaCl concentration for growth were determined by using the growth medium containing various concentrations of NaCl (0–30 %, w/v, at intervals of 5 %, w/v). The pH range for growth was assayed from pH 7.0 to 11.0 at intervals of 0.5 pH units in liquid medium with various buffers (glycyl glycine/NaOH, pH 7.0–8.0; glycine/NaOH, pH 8.5–11.0), each at 25 mM. The temperature for growth was determined at 4, 10, 15, 20, 25, 30, 35, 37, 40, 45, 50, 55 and 60 °C in a medium at pH 8.0 with optimal NaCl concentration. Strain 167-74T was capable of growth in the presence of 20–30 % (w/v) NaCl, at pH 8.0–10.0 and at 20–55 °C. Optimal growth of strain 167-74T occurred in 25 % (w/v) NaCl, at pH 9.0 and at 37 °C. Phenotypic testing of the strain used the above optimal growth conditions.
Tests for catalase and oxidase activities and for hydrolysis of starch, gelatin, casein and Tween 80 were performed as described by Gonzalez et al. (1978). Reduction of nitrate was detected by using sulfanilic acid/α-naphthylamine reagent (Smibert & Krieg, 1994). H2S formation was determined by formation of a black sulfide precipitate in medium containing 0.5 % (w/v) sodium subsulfite. Indole production from tryptophan and the utilization of sugars and organic acids were assessed as described by Oren et al. (1997). Antibiotic sensitivity tests were performed by spreading cell suspensions on culture plates and then placing discs impregnated with antibiotics on top (Becton Dickinson). Utilization of single or complex carbon sources was assessed in a modified JCM no. 167 medium (Casamino acids and sodium glutamate omitted; tested under optimal growth conditions) with 0.5 g yeast extract l−1, supplemented with 1.0 % (w/v) test sugar or organic acid.
The G+C content of the total DNA of strain 167-74T, determined by the HPLC method (Tamaoka & Komagata, 1984), was 60.7 mol%. DNA–DNA hybridization between strain 167-74T, Hst. larsenii JCM 13463T and Hst. kamekurae 194-10T was assessed by using the fluorometric method of Ezaki et al. (1989). The relatedness of strain 167-74T to Hst. larsenii JCM 13463T and Hst. kamekurae 194-10T was 19.5 and 18.8 %, respectively. These values are well below the threshold value of 70 % DNA–DNA relatedness generally accepted for the definition of a novel species (Wayne et al., 1987; Stackebrandt & Ebers, 2006).
Detailed results are included in the species description and differences between strain 167-74T, Hst. larsenii JCM 13463T and Hst. kamekurae 194-10T are highlighted in Table 1. On the basis of the data presented, we conclude that strain 167-74T represents a novel species of the genus Halostagnicola, for which we propose the name Halostagnicola alkaliphila sp. nov.
Strains: 1, 167-74T; 2, Hst. larsenii JCM 13463T; 3, Hst. kamekurae 194-10T. Data are from Castillo et al. (2006), Nagaoka et al. (2010) and this study. All strains were positive for reduction of nitrate to nitrite and assimilation of d-galactose, d-glucose, glycerol, maltose, d-mannose, propionate and trehalose. All strains were negative for anaerobic growth in arginine and DMSO, hydrolysis of gelatin and skimmed milk and assimilation of d-sorbitol, succinate and l-malate. All strains were sensitive to bacitracin (10 U), novobiocin (30 mg), anisomycin (50 mg) and pravastatin (50 mg) and resistant to ampicillin (10 mg), chloramphenicol (30 mg), gentamicin (120 mg), kanamycin (30 mg), neomycin (30 mg), penicillin G (10 U), streptomycin (300 mg), tetracycline (30 mg) and vancomycin (30 mg).
Description of Halostagnicola alkaliphila sp. nov.
Halostagnicola alkaliphila [al.ka.li.phi′la. N.L. n. alkali (from Arabic al-qalyi the ashes of saltwort) alkali; N.L. adj. philus -a -um (from Gr. adj. philos -ê -on) friend to, loving; N.L. fem. adj. alkaliphila loving alkaline conditions].
Cells are motile, pleomorphic and rod-shaped (approx. 0.8–1.0×2.0–2.5 µm). Stains Gram-negative. Colonies on agar medium are white/pink and circular, 2–3 mm in diameter. Growth occurs at 20–30 % (w/v) NaCl (optimum, 25 %, w/v), 20–55 °C (optimum, 37 °C) and pH 8.0–10.0 (optimum, pH 8.5–9.0). Cells lyse in water. H2S is not produced from sodium sulfite. Indole is not produced from tryptophan. Nitrate is reduced to nitrite. Nitrite is not reduced and no dinitrogen gas is formed. Anaerobic growth does not occur with DMSO and arginine, but does occur with nitrate. Tests for oxidase activity are positive, but catalase activity is absent. Starch, Tween 80, casein and gelatin are not hydrolysed. Tests positive for urease activity, but negative for β-galactosidase activity. The following substrates are utilized for growth: d-fructose, d-galactose, d-glucose, glycerol, maltose, d-mannose, sucrose, trehalose, d-xylose, pyruvate, propionate, dl-lactate and fumarate. No growth occurs on l-arabinose, cellobiose, citrate, lactose, d-mannitol, ribitol, ribose, raffinose, d-sorbitol, starch, acetate, succinate, l-malate or l-glutamate. Sensitive to anisomycin (50 mg), bacitracin (10 U), erythromycin (15 mg), novobiocin (30 mg), pravastatin (50 mg) and rifampicin (5 mg). Resistant to ampicillin (10 mg), chloramphenicol (30 mg), gentamicin (120 mg), kanamycin (30 mg), nalidixic acid (30 mg), neomycin (30 mg), penicillin G (10 U), streptomycin (300 mg), tetracycline (30 mg) and vancomycin (30 mg). Polar lipids are C20C20 and C20C25 archaeol derivatives of PG and PGP-Me. The G+C content of the type strain is 60.7 mol% (HPLC).
The type strain, strain 167-74T ( = JCM 16592T = CECT 7631T), was isolated from commercial rock salt imported into Japan from Hubei Province, China.