Vulcanisaeta Distributa Gen. Nov., Sp. Nov., and Vulcanisaeta Souniana Sp
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International Journal of Systematic and Evolutionary Microbiology (2002), 52, 1097–1104 DOI: 10.1099/ijs.0.02152-0 Vulcanisaeta distributa gen. nov., sp. nov., and Vulcanisaeta souniana sp. nov., novel hyperthermophilic, rod-shaped crenarchaeotes isolated from hot springs in Japan 1 Japan Collection of Takashi Itoh,1 Ken-ichiro Suzuki1† and Takashi Nakase1,2 Microorganisms, RIKEN (The Institute of Physical and Chemical Research), Author for correspondence: Wako-shi, Saitama Takashi Itoh. Tel: j81 48 467 8440. Fax: j81 48 462 4860. 351-0198, Japan e-mail: ito!jcm.riken.go.jp 2 Laboratory of Microbiology, Department Seventeen strains of rod-shaped, heterotrophic, anaerobic, hyperthermophilic of Applied Biology and crenarchaeotes were isolated from several hot spring areas in eastern Japan, Chemistry, Faculty of Applied Bioscience, Tokyo and eight representative strains were characterized further. Cells of these University of Agriculture, strains were straight to slightly curved rods, 04–06 µm in width. Occasionally, Sakuragaoka 1-1-1, cells were branched or bore spherical bodies at the poles. They grew optimally Setagaya-ku, Tokyo 156-8502, Japan at 85–90 SC and at pH 40–45. They utilized yeast extract, peptone, beef extract, Casamino acids, gelatin, starch, maltose and malate as carbon sources and sulfur and thiosulfate as possible electron acceptors. The DNA GMC contents of the novel isolates were 439–462 mol%. The lipids were mainly cyclic and acyclic tetraether core lipids. Phylogenetic analysis of the 16S rDNA sequences revealed that they represented an independent lineage in the family Thermoproteaceae. Moreover, comparison of the 16S rDNA sequences and a DNA–DNA hybridization study showed that they comprised two species, which could also be differentiated by the maximal growth temperature and degrees of NaCl tolerance. Therefore, a new genus, Vulcanisaeta gen. nov., in the family Thermoproteaceae is proposed to accommodate two novel species, Vulcanisaeta distributa sp. nov. and Vulcanisaeta souniana sp. nov. The type species is V. distributa and the type strains are V. distributa IC-017T (l JCM 11212T l DSM 14429T) and V. souniana IC-059T (l JCM 11219T l DSM 14430T). Keywords: Vulcanisaeta distributa, Vulcanisaeta souniana, Thermoproteaceae, hyperthermophilic Archaea INTRODUCTION proteaceae and Thermofilaceae (Burggraf et al., 1997). They are strict or facultative anaerobes that metabolize All the known species within the kingdom Crenar- sulfur and\or thiosulfate and are reported to be chaeota are obligate thermophiles with maximum distributed widely in terrestrial hot springs and marine growth temperatures ranging from 75 to 113 mC geothermal habitats (Huber & Stetter, 2001). Until (Stetter, 1998). Using 16S rRNA\DNA-based phylo- recently, only a few genera and species had been genetic analysis, they can be divided into three major described in the order Thermoproteales (Bonch-Osmo- clusters that correspond to the orders Desulfurococ- lovskaya et al., 1990; Huber et al., 1987; Vo$ lkl et al., cales, Sulfolobales and Thermoproteales (Ludwig & 1993; Zillig et al., 1981, 1983; Zillig, 1989). However, Klenk, 2001; Reysenbach, 2001). At present, all rod- the recent discoveries of two new genera in the family shaped crenarchaeotes are included in the order Thermoproteaceae (Thermocladium and Caldivirga; Thermoproteales, represented by the families Thermo- Itoh et al., 1998a, 1999) and two novel Pyrobaculum species [Pyrobaculum arsenaticum (Huber et al., 2000) ................................................................................................................................................. and Pyrobaculum oguniense (Sako et al., 2001)], as well † Present address: Biological Resource Center, Biotechnology Center, National Institute of Technology and Evaluation, Kazusa-Kamatari, as the detection of several phylotypes related to Kisarazu, Chiba 292-0812, Japan. members of the order Thermoproteales (Barns et al., The DDBJ accession numbers for the 16S rDNA sequences determined in 1994, 1996; Reysenbach et al., 2000; Takai & Hori- this study are AB063630–AB063647, as detailed in Fig. 2. koshi, 1999), suggest that there may be a wider 02152 # 2002 IUMS Printed in Great Britain 1097 T. Itoh, K. Suzuki and T. Nakase diversity of rod-shaped crenarchaeotes in geothermal at atmospheric pressure. Caldivirga maquilingensis JCM habitats. 10307T was cultivated as a reference strain, as described previously (Itoh et al., 1999). In the course of our exploration for novel thermophilic Archaea inhabiting terrestrial geothermal habitats, we Phenotypic and genetic studies. Morphology, growth have isolated a number of thermophilic organisms characteristics, utilization of carbon sources, possible elec- from hot springs in Japan and the Philippines. A tron acceptors, antibiotic sensitivity, lipid composition, preliminary grouping of the rod-shaped isolates by the DNA base composition and DNA–DNA relatedness were ability to grow at 85 mC, DNA base composition and determined as described previously (Itoh et al., 1998a). partial 16S rDNA sequences revealed the existence of Morphology, growth characteristics and utilization of car- another unassigned group belonging to the family bon sources were studied using the medium described above. Thermoproteaceae For electron microscopy, cells were placed on a collodion- , in addition to groups correspond- coated grid, shadowed with platinum\palladium and ex- ing to the genera Caldivirga, Thermocladium and amined with a transmission electron microscope (H-300; Thermoproteus (T. Itoh, K. Suzuki, P. C. Sanchez and Hitachi). Possible electron acceptors were identified using a T. Nakase, unpublished). This paper describes the test medium (Itoh et al., 1998a) under a N# atmosphere. isolation and characterization of a novel group of Growth was estimated by fluorescence intensities after organisms in the family Thermoproteaceae and pro- treatment with NanoOrange dye (Molecular Probes) ac- poses a new genus, Vulcanisaeta gen. nov., including cording to the supplier’s protocol or direct counting using a two novel species, Vulcanisaeta distributa sp. nov. and Petroff-Hauser counting chamber (0n02 mm in depth). A Vulcanisaeta souniana sp. nov. good correlation between the two methods was obtained. 16S rDNA sequencing and phylogenetic analysis were METHODS conducted as reported previously (Itoh et al., 1999). 16S rDNA was amplified with primers A-20F (5h-TCCGGTTG- Isolation procedure. Samples of hot-spring water, mud and ATCCTGCCG-3h, corresponding to positions 8–24 in the soil were collected from several hot spring sites in Japan in Escherichia coli numbering system) and A-1530R (5h-GGA- 1993 and 1994 (Table 1). The samples were transported in GGTGATCCAGCCG-3h, positions 1540–1525). Partial 16S sterile plastic tubes without temperature control and were rDNA sequences were determined with a sequencing primer inoculated within 3 days of sampling into an enrichment A-690R (5h-GGATTTCRCCCCTAC-3h, positions 699– medium described previously (Itoh et al., 1998a) at pH 685). In addition, almost complete 16S rDNA sequences of values ranging from 3n5to6n0. The cultures were incubated five novel isolates and Pyrobaculum organotrophum JCM at 85 mC under N# at atmospheric pressure. After 1 week of 9190T were determined in this study. The 16S rDNA cultivation, cultures yielding predominantly rod-shaped cells sequences were aligned first on the program were purified by the serial dilution technique, as described (Thompson et al., 1997) and edited manually with the aid of previously (Itoh et al., 1998a). the SSU rRNA database (Van de Peer et al., 2000). Culture conditions. The isolates were routinely cultivated in Evolutionary distances were calculated after gaps, ambigu- the salt base solution of the Sulfolobus medium (Brock et al., ous bases and unalignable regions had been eliminated. The " " 1972), containing 0n5 g yeast extract l− ,1n0 mg resazurin l− , phylogenetic tree was constructed by the neighbour-joining −" −" 0n5gNa#S.9H#Ol and 10n0 g sulfur l ,pH4n0–4n5 (adjust- method (Saitou & Nei, 1987) and was evaluated by bootstrap ed at room temperature). N# was used as the gas phase sampling (Felsenstein, 1985). Table 1. Sources of novel isolates ................................................................................................................................................................................................................................................................................................................. Strains identified as Thermoproteus spp. are underlined. All locations are in east Japan (prefectures are shown after commas). The pH of the samples was determined at room temperature. , Not determined. Isolate(s) Location Sample Temperature (mC) pH Date IC-017T, IC-019 Ohwakudani, Kanagawa Water 2n0–2n509\1993 IC-058 Ohwakudani, Kanagawa Soil 85 2n702\1994 IC-051, IC-064 Ohwakudani, Kanagawa Soil 90 1n402\1994 IC-052, IC-065 Ohwakudani, Kanagawa Soil 90 2n102\1994 IC-059T, IC-060, IC-061, IC-062 Sounzan, Kanagawa Water 3n0–3n202\1994 IC-029 Okushiobara, Tochigi Soil 90 1n211\1993 IC-030 Okushiobara, Tochigi Soil 90 3n011\1993 IC-031 Okushiobara, Tochigi Water 75 2n911\1993 IC-032 Okushiobara, Tochigi Water 85 3n411\1993 IC-135 Tamagawa, Akita Water 90 1n611\1994 IC-141 Tamagawa, Akita Water 65 1n811\1994 IC-124 Fukenoyu, Akita Water 90 2n411\1994 IC-136 Gosyokake, Akita Soil 65 2n511\1994 IC-140 Ohnuma, Akita Mud 75 3n311\1994 1098 International Journal of Systematic and Evolutionary