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1 School of Earth and Environmental Sciences and Research Institute of Oceanography, Seoul National University, San 56-1 Shillim-dong, Kwanak-gu, Seoul 151-742, Republic of Korea
2 South Sea Institute/Korea Ocean Research and Development Institute (KORDI), 391 Jang mok-ri, Jangmok-myon, Geoje 656-830, Republic of Korea
Correspondence
Byung Cheol Cho
bccho{at}snu.ac.kr
| ABSTRACT |
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Details of the whole-cell fatty acid compositions of strain CL-MP28T and related Oceanobacillus species are available in a supplementary table in IJSEM Online.
Present address: Marine Environmental Research Department, KORDI, Ansan 426-744, Republic of Korea ![]()
| MAIN TEXT |
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In this study, a novel strain, CL-MP28T, was isolated from the surface of a sediment core sample collected at depth of 2247 m in the Ulleung Basin of the East Sea, Korea. The sediment slurry was spread on a plate containing marine agar 2216 (Difco) and incubated at 20 °C for 2 weeks. Strain CL-MP28T was isolated on the plate and subsequently purified on marine agar 2216 at 30 °C four times. The strain was maintained at 80 °C both on marine agar 2216 at 4 °C and in marine broth 2216 (Difco) supplemented with 30 % (v/v) glycerol.
The 16S rRNA gene was amplified from a single colony by a PCR with Taq DNA polymerase (Bioneer) and primers 27F and 1492R (Lane, 1991
). The PCR product was purified using an AccuPrep PCR purification kit (Bioneer). Sequencing of the 16S rRNA gene was performed with an Applied Biosystems automatic sequencer (ABI3730XL) at Macrogen Corp. (Seoul, Korea). An almost-complete 16S rRNA gene sequence (1354 bp) of strain CL-MP28T was obtained. This sequence was compared with those available in GenBank by using BLASTN (Altschul et al., 1990
) searches. The sequence of strain CL-MP28T was manually aligned with those of the type strains of the three Oceanobacillus species and with those of the type species of other genera in the family Bacillaceae, obtained from GenBank and the Ribosomal Database Project (Cole et al., 2003
) databases using known 16S rRNA secondary structure information. Phylogenetic trees were obtained by using the neighbour-joining (Saitou & Nei, 1987
), maximum-parsimony (Fitch, 1971
) and maximum-likelihood (Felsenstein, 1981
) methods. An evolutionary distance matrix for the neighbour-joining method was generated according to the model of Jukes & Cantor (1969)
. The robustness of the tree topologies was assessed by using bootstrap analyses based on 1000 replications (for the neighbour-joining and maximum-parsimony methods) or 100 replications (for the maximum-likelihood method). Alignment analyses were carried out using the jPHYDIT program (Jeon et al., 2005
), and phylogenetic analysis were carried out using MEGA3 (Kumar et al., 2004
) and PAUP* 4.0 (Swofford, 1998
). Likelihood parameters were estimated by means of the hierarchical ratio tests in MODELTEST, version 3.04 (Posada & Crandall, 1998
). The sequence similarities indicated that the closest relatives of strain CL-MP28T were O. iheyensis JCM 11309T (95.96 %) and O. oncorhynchi R-2T (95.48 %). Phylogenetic analyses based on the 16S rRNA gene sequence showed that strain CL-MP28T formed a robust cluster with species of the genus Oceanobacillus (Fig. 1
). Thus, it is clear that our isolate belongs to the genus Oceanobacillus. However, the low levels of similarity (95.096.0 %) between the 16S rRNA gene sequence of the novel isolate and those of previously described species of the genus Oceanobacillus indicated that strain CL-MP28T represents a novel species of the genus (Stackebrandt & Goebel, 1994
; Rosselló-Mora & Amann, 2001
). The relatedness of the genomic DNA was determined by means of dot-blot hybridization. Probe DNA labelling was performed using a nick translation kit (Roche), and hybridization and detection were done using the DIG labelling and detection kit (Roche) according to the manufacturer's instruction. The level of DNADNA relatedness between strain CL-MP28T and O. iheyensis KCTC 3954T was 24.7 %, while that for O. oncorhynchi R-2T was 17.5 %. These values are below the currently accepted limit for DNA relatedness (70 %) for the phylogenetic definition of a species (Stackebrandt & Goebel, 1994
) and therefore provide evidence that our isolate (CL-MP28T) represents a novel species of the genus Oceanobacillus. The DNA G+C content was determined by HPLC analysis (Tamaoka & Komagata, 1984
) at the Korean Culture Center of Microorganisms (Seoul, Korea) and was found to be 40.2 mol%.
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-galactosidase and gelatinase) (Table 1
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7c, C18 : 1
9t and/or C18 : 1
12t), the relatively low optimal NaCl concentration for growth and the lack of growth at temperatures below 15 °C of strain CL-MP28T differentiate it from O. picturae KCTC 3821T.
Some phenotypic characteristics of strain CL-MP28T, e.g. acid production from amygdalin and a relatively low optimal NaCl concentration for growth, clearly distinguish the novel isolate from previously described species of the genus Oceanobacillus. Furthermore, the DNADNA relatedness data supported our suggestion that strain CL-MP28T should be classified within a novel species within the genus Oceanobacillus (Stackebrandt & Goebel, 1994
). In conclusion, phylogenetic analyses based on 16S rRNA gene sequences, DNADNA relatedness and physiological and chemotaxonomic features suggest that strain CL-MP28T represents a novel species of the genus Oceanobacillus, for which the name Oceanobacillus profundus sp. nov. is proposed.
Description of Oceanobacillus profundus sp. nov.
Oceanobacillus profundus (pro.fun'dus. L. masc. adj. profundus from the deep).
Cells are Gram-positive, peritrichously flagellated, straight rods that are approximately 0.20.4x0.82 µm in size and produce ellipsoidal spores terminally positioned within swollen sporangia. Colonies are circular and creamy white in colour. Obligately aerobic or facultatively alkaliphilic. Grows at 1542 °C (optimum 35 °C) and pH 6.59.5 (optimum pH 7.58.5). Catalase- and oxidase-positive. The NaCl range for growth is 014 % (w/v) at pH 7.5 (optimum 13 %). Nitrate reductase,
-galactosidase (ONPG) and DNase activities are present and hydrolysis of gelatin, aesculin, casein and Tweens 40 and 60 is demonstrated. Indole production, urease and hydrolysis of Tween 80 are absent. Acids are produced from glycerol, D-xylose, D-glucose, D-fructose, D-mannose, mannitol, N-acetylglucosamine, amygdalin, maltose, lactose, D-trehalose and D-turanose, but not from D-arabinose, galactose, L-rhamnose, myo-inositol, D-melibiose, glycogen or L-fucose. The DNA G+C content is 40.2 mol%. The major fatty acids are anteiso-C15 : 0 (64.9 %), anteiso-C17 : 0 (11.9 %), iso-C16 : 0 (7.7 %), iso-C14 : 0 (5.6 %), iso-C15 : 0 (3.8 %) and C16 : 0 (2.5 %). The major isoprenoid quinone is MK-7.
The type strain, CL-MP28T (=KCCM 42318T=DSM 18246T), was isolated from the surface of a sediment core sample collected at a depth of 2247 m in the Ulleung Basin of the East Sea, Korea.
| ACKNOWLEDGEMENTS |
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