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1 Japan Collection of Microorganisms, RIKEN BioResource Center, 2-1 Hirosawa, Wako, Saitama 351-0198, Japan
2 Graduate School of Life Sciences, Toyo University, 1-1-1 Izumino, Itakura, Oura, Gunma 374-0193, Japan
3 Faculty of Life Sciences, Toyo University, 1-1-1 Izumino, Itakura, Oura, Gunma 374-0193, Japan
Correspondence
Takashi Itoh
ito{at}jcm.riken.jp
| ABSTRACT |
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| MAIN TEXT |
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Here, we describe the isolation and phenotypic and phylogenetic characterization of a novel moderately thermophilic and acidophilic archaeon, IC-189T, isolated from a solfataric field in Hakone, Kanagawa, Japan. Its physiological and morphological features resemble those of the aforementioned Thermoplasmatales species; however, its 16S rRNA gene sequence, its DNA G+C content and some of its physiological features warrant a taxonomic status within a novel genus in this order.
A soil sample (60 °C, pH 1.4) was collected from a solfataric field in Ohwaku-dani (Hakone, Kanagawa Prefecture, Japan) on 19 July 2002 and brought back to our laboratory in a sterile, hermetically sealed, plastic tube on the same day. In an attempt to isolate various micro-organisms by using a single culture medium, a soil suspension was diluted serially and each dilution was distributed in multiple wells and cultivated (as in the most-probable number method). Approximately 1 g (wet weight) soil sample was suspended in 10 ml Sulfolobus medium (pH 2.5; Brock et al., 1972
) and 102-, 103-, and 104-fold dilutions in the same medium were distributed in wells of PCR plates (96 wells for each dilution, 100 µl per well), sealed with caps and incubated at 55 °C for 2 weeks. Microbial growth was observed in 70 wells at the 104-fold dilution. Growth in the wells could be divided roughly into four cultural types: 47 wells showed a predominance of relatively large coccoid cells (approx. 3–5 µm in diameter); four wells contained numerous small cocci (<1 µm in diameter); 18 wells contained coexisting large and small cocci; and one well contained only rod-shaped cells. One of the cultures dominated by small cocci was further diluted serially (1 : 10) and each dilution was divided equally into 10 tubes and cultivated. This step was repeated for one growth-positive culture at the highest dilution. Then, the serial dilution (1 : 10)/cultivation method was repeated twice to obtain a pure culture, which was designated IC-189T and studied further (as described below). On the other hand, the strain that comprised large cocci and the strain that comprised rod-shaped cells were identified as a Picrophilus species and an actinobacterium, respectively, on the basis of 16S rRNA gene sequences (data not shown). After strain IC-189T had been purified, it was cultivated routinely at 60 °C in a modified Thermoplasma medium (JCM medium no. 180, but with the pH adjusted to 3.0). The purity of the strain was confirmed routinely by microscopic examination and repeated partial sequencing of the 16S rRNA gene using several primers. In addition, no 16S rRNA gene fragments were PCR-amplified with bacteria-specific primers (Namwong et al., 2005
), Nanoarchaeota-specific primers (Hohn et al., 2002
) or Sulfolobales-specific primers (T. Itoh, unpublished data). Unless otherwise indicated, the modified Thermoplasma medium was used for the phenotypic characterization of strain IC-189T.
Cells of strain IC-189T were mostly irregular cocci and sometimes showed lobe- and club-shaped forms (Fig. 1
). Despite the cultural type observed in the PCR plate wells, cells grown in the modified Thermoplasma medium (and even in the Sulfolobus medium) were dominated by cocci 1–3 µm in diameter; larger (up to 8 µm) and smaller (around 0.8 µm) cocci were frequently observed (Fig. 1
). Most cells occurred singly, but some were accompanied by budding daughter cells or were catenated like beads on a string (Fig. 1c
). No motile cells were observed. Under a light microscope, some large cells seemed to have inclusion bodies (Fig. 1b
). The cells showed moderate natural fluorescence when examined under a fluorescence microscope (BX51; Olympus) (excitation, 330–385 nm; absorption, 420 nm). Platinum–palladium-shadowed cells, prepared and observed under a transmission electron microscope as described previously (Itoh et al., 1998
), revealed pili (one or a few per cell) (Fig. 1d
). To prepare thin sections, cells were fixed with 2.5 % glutaraldehyde at 4 °C for 2 h; this was followed by post-fixation with 2 % OsO4 in 0.1 M cacodylate buffer at 4 °C for 2 h. After dehydration with increasing ethanol concentrations, the cells were embedded in epoxy resin. Ultrathin sections were stained with uranyl acetate and lead acetate and then examined under a transmission electron microscope (JEM-1230; JEOL). The cells apparently lacked cell walls and were each surrounded by a single, thin layer approximately 10 nm thick (Fig. 1e
). This cell-envelope width is comparable to those of the cell wall-less genera Thermoplasma and Ferroplasma. On a plate medium solidified with 0.8 % (w/v) Phytagel (Sigma), strain IC-189T produced colourless, small (<1.5 mm in diameter), flat or slightly umbonate colonies with a fried-egg appearance (Fig. 1f
).
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To evaluate utilization of carbon and energy sources, the modified Thermoplasma medium (pH 3.0) was altered further as follows: yeast extract concentration was reduced to 0.005 %, and glucose was replaced by each of the test substrates. Strain IC-189T utilized glucose and mannose, but not arabinose, fructose, galactose, lactose, maltose, D-ribose, sucrose, xylose, starch, glycogen (at 0.5 %), acetate, butyrate, citrate, formate, fumarate, L-lactate, malate, propionate, pyruvate, succinate, methanol, ethanol, formamide, methylamine, trimethylamine, gelatin (at 0.2 %), beef extract, peptone, malt extract or tryptone (at 0.05 %). Glutamate supported weak growth, but none of the other 19 amino acids supported growth (at 0.2 %). The strain also grew on yeast extract as the sole source of carbon and energy. The addition of FeSO4 . 7H2O (0.5 %) to the medium was inhibitory to growth. The strain tolerated the presence of NaCl at concentrations up to 2.5 %, but not at 3.0 %. Growth was inhibited by the addition of erythromycin, novobiocin and rifampicin in the early exponential phase, but not by the addition of ampicillin, chloramphenicol, kanamycin, oleandomycin, penicillin, streptomycin or vancomycin (all at 100 µg ml–1).
TLC analysis of the lipid fraction, extracted as described previously (Itoh et al., 1998
), detected a large amount of tetraether core lipids, including at least three acyclic or cyclic moieties. Diether core lipid was not detected. On a thin-layer chromatogram of the quinone fraction (Itoh et al., 1985
), a single band that corresponded to a menaquinone moiety was detected. HPLC analysis revealed that it contained MK-7 as a major component.
The G+C content of the genomic DNA was 56.1 mol%, as determined by the HPLC method of Tamaoka (1994)
. The almost-complete 16S rRNA gene was PCR -amplified with primers A-20F and A-1530R and then sequenced as described previously (Itoh et al., 2002
). The G+C content of the 1434 positions determined was 57.9 mol%. In a Southern hybridization study performed with a labelled 16S rRNA gene of strain IC-189T, a single band was detected from total DNA sample digested with BglII, EcoRV or BstXII, indicating that there was a single copy of the 16S rRNA gene in the genomic DNA (data not shown). A BLAST search of the 16S rRNA gene sequence of strain IC-189T revealed that, of the archaeal orders, it was related most closely to the order Thermoplasmatales (Reysenbach, 2001
). Therefore the sequence was aligned with those of the previously described Thermoplasmatales species by using the CLUSTAL_X program (Thompson et al., 1997
). However, strain IC-189T was found to be related only distantly to thoese Thermoplasmatales species: the levels of sequence similarity with respect to the two Picrophilus species were 91.0 %, this being followed by 90.9 % for T. acidophilum, 90.8 % for T. volcanium and 86.2 % for F. acidiphilum. Therefore, the sequence was compared again with a dataset that included several uncultured clones belonging to the order Thermoplasmatales in GenBank. After the removal of ambiguous bases and unreliable alignment sections, 1349 base positions were compared and a phylogenetic tree (Fig. 2
) was reconstructed by using the neighbour-joining method (Saitou & Nei, 1987
). Strain IC-189T was also shown to be related distantly to these clones, with 90.2–92.8 % sequence similarity, but it showed some affinity (73 % bootstrap support) with clones isolated from acid mine drainage and related habitats; these clones are known as the alphabet (A to E) plasma groups (Baker & Banfield, 2003
).
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Cells are pleomorphic, predominantly comprising irregular cocci that range from 1.0 to 3.0 µm in diameter. Cells lack a cell wall and are surrounded by a thin membrane (approx. 10 nm thick). Buds (daughter cells) are sometimes associated with cells. Pili are present. Non-motile. On solid medium, small colourless colonies with a fried-egg appearance are formed. Strictly aerobic. Acidophilic and moderately thermophilic. Heterotrophic, requiring yeast extract for growth. Growth is inhibited by erythromycin, novobiocin and rifampicin (at 100 µg ml–1). Lipids predominantly comprise tetraethers; MK-7 is the major respiratory quinone. The DNA G+C content is 56 mol%. Phylogenetically, the genus represents an independent lineage within the order Thermoplasmatales. Inhabits geothermal terrestrial habitats. The genus is monospecific, at present, and the type species is Thermogymnomonas acidicola.
Description of Thermogymnomonas acidicola sp. nov.
Thermogymnomonas acidicola (a.ci.di'co.la. N.L. neut. n. acidum an acid; L. suff. -cola from L. n. incola an inhabitant; N.L. n. acidicola an inhabitant of an acidic environment).
Morphology and growth properties are as described for the genus. Growth occurs at temperatures in the range 38–68 °C (optimum, 60 °C) and at pH 1.8–4.0 (optimum, pH 3.0). Yeast extract, as well as glucose and mannose (in the presence of yeast extract), serve as carbon and energy sources. NaCl is tolerated at concentrations up to 2.5 %. The DNA G+C content DNA is 56.1 mol%.
The type strain, IC-189T (=JCM 13583T=DSM 18835T), was isolated from a sample of solfataric soil collected from Ohwaku-dani, Hakone, Japan.
| ACKNOWLEDGEMENTS |
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