IJSEM Faster Access from Outside North America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Abstract Freely available
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via CrossRef
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.
Agricola
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.
Int J Syst Evol Microbiol 57 (2007), 260-264; DOI  10.1099/ijs.0.64633-0
© 2007 International Union of Microbiological Societies

Thermoanaerobacterium aciditolerans sp. nov., a moderate thermoacidophile from a Kamchatka hot spring

I. V. Kublanov1, M. I. Prokofeva1, N. A. Kostrikina1, T. V. Kolganova2, T. P. Tourova1, J. Wiegel3 and E. A. Bonch-Osmolovskaya1

1 Institute of Microbiology, Russian Academy of Sciences, Prospekt 60-Letiya Oktyabrya 7/2, Moscow 117312, Russia
2 Bioengineering Center, Russian Academy of Sciences, Prospect 60-Letiya Oktyabrya 7/1, 117312 Moscow, Russia
3 Department of Microbiology, University of Georgia, Athens, GA, USA

Correspondence
I. V. Kublanov
kublanov.ilya{at}gmail.com


    ABSTRACT
 TOP
 ABSTRACT
 MAIN TEXT
 REFERENCES
 
An anaerobic, moderately thermoacidophilic bacterium, strain 761-119T, was isolated from an acidic hot spring in the Orange Field of the Uzon Caldera (Kamchatka, far-eastern Russia). Cells were spore-forming, Gram-positive rods, possessing one polar flagellum. Growth of strain 761-119T was observed between 37 and 68 °C and in the pH20 °C range 3.2–7.1. No growth was observed within 5 days of incubation at or below 35 °C and at or above 70 °C, as well as at or below pH20 °C 2.8 and at or above pH20 °C 7.5. The optimal temperature and pH20 °C for growth were 55 °C and pH20 °C 5.7, respectively. A wide range of carbohydrates and polysaccharides were fermented, as well as peptides and proteinaceous substrates. The main products of glucose fermentation were acetate, ethanol, lactate, H2 and CO2. The DNA G+C content was 34 (±0.5) mol%. 16S rRNA gene sequence analysis indicated that strain 761-119T belonged to the genus Thermoanaerobacterium. The level of 16S rRNA gene sequence similarity with other Thermoanaerobacterium species was 86.5–97.8 %, with the only moderately acidophilic member of this genus, Thermoanaerobacterium aotearoense, being one of its closest relatives. DNA–DNA hybridization with T. aotearoense showed 33 % relatedness. Thus, morphological (one polar flagellum) and physiological characteristics (lower pH limit of growth at pH20 °C 3.2 compared with T. aotearoense) and 16S rRNA gene sequence analyses revealed that strain 761-119T represents a novel species in the genus Thermoanaerobacterium, for which the name Thermoanaerobacterium aciditolerans sp. nov. is proposed, with the type strain 761-119T (=DSM 16487T=VKM B-2363T).


The GenBank/EMBL/DDBJ accession number for the 16S rRNA gene sequence of strain 761-119T is AY350594.


    MAIN TEXT
 TOP
 ABSTRACT
 MAIN TEXT
 REFERENCES
 
Acidic hot environments are quite common throughout the world and include anthropogenic environments such as mines, coal and coal-refuse piles and self-heated compost heaps, as well as naturally heated volcanic habitats (Brock, 1986Go). Most of the known thermoacidophilic prokaryotes are either aerobic archaea or micro-organisms with different types of anaerobic respiration (Johnson, 1998Go; Wiegel & Canganella, 2001Go). Thermoacidophiles with a fermentative type of metabolism are few in number. Examples are the facultatively anaerobic archaea of the genus Thermoplasma (Segerer et al., 1988Go) and the obligately anaerobic archaea of the genera Acidilobus (Prokofeva et al., 2000Go) and Caldisphaera (Itoh et al., 2003Go). The only anaerobic thermoacidophilic representative among the bacteria is Thermoanaerobacterium aotearoense, a member of the Firmicutes, an obligately anaerobic heterotroph, a moderate thermophile and a moderate acidophile, which was isolated from a hot spring in New Zealand (Liu et al., 1996Go). Molecular and microbial analysis of the diversity of anaerobic thermophiles active at low pH in enrichment cultures obtained from terrestrial and deep-sea sources have revealed the presence of members of the genera Acidilobus, Thermoplasma, Thermoanaerobacter, Thermoanaerobacterium and Thermococcus (Prokofeva et al., 2005Go). Here, we report the detailed characterization of a novel thermoacidophilic bacterium belonging to the genus Thermoanaerobacterium, isolated from one of these enrichment cultures inoculated with water/sediment from the Uzon Caldera in Kamchatka (far-eastern Russia).

For enrichment of thermoacidophilic micro-organisms, the following basal medium was used (g l–1): NH4Cl, 0.33; KCl, 0.33; KH2PO4, 0.33; CaCl2.2H2O, 0.33; MgCl2.6H2O, 0.33; NaCl, 25.0; yeast extract, 0.1; trace elements (Balch et al., 1979Go), 10 ml l–1; vitamins (Wolin et al., 1963Go) 10 ml l–1. Sucrose was added as substrate, at a final concentration of 2 g l–1. The medium was prepared anaerobically and reduced by adding Na2S (600 mg l–1). The medium was dispensed in 10 ml portions in 15 ml Hungate tubes; CO2 was used as the gas phase. The pH of the medium, measured at 20 °C using a pH meter calibrated at 20 °C, was adjusted using anoxic 3 M HCl. The pH and cultivation temperature used were approximately those from the sampling site. From the sample from Orange Field, Uzon Caldera, Kamchatka (coordinates 54° 30.237' N 160° 00.038' E, pH 3.8, 48 °C), an enrichment culture was obtained, growing at 60 °C and pH20 °C 4.0. The dominating micro-organism from this culture was isolated from colonies from the highest positive dilution of the second round of serial dilutions into 1.5 % agar shakes. Isolated colonies were transferred to liquid medium. One of the isolated strains was strain 761-119T, described below.

Cells of strain 761-119T were spore-forming rods, 0.4 µm wide and 3–12 µm long (Fig. 1Goa, b). Cells were motile, with one polar flagellum, and Gram-positive (Fig. 1cGo). The isolate grew over a temperature range of 37–68 °C, with an optimal growth temperature of 55 °C. The pH20 °C range for growth was 3.2–7.1, with an optimum of pH20 °C 5.7. The doubling time under optimal conditions was 1 h. No growth was observed within 5 days of incubation at or below pH20 °C 2.8 or 35 °C and at or above pH20 °C 7.5 or 70 °C. After 2 days of growth at pH20 °C 7.0, a high degree of cell lysis occurred (after abundant growth), but not in medium with pH20 °C below 5.5. Growth of strain 761-119T occurred at NaCl concentrations of 0–3 %. No growth was observed at 4 % NaCl. Isolate 761-119T was able to ferment various mono- and disaccharides including glucose, fructose, xylose, ribose, arabinose, galactose, maltose, sucrose and lactose. It also grew on yeast extract, peptone, sorbitol, starch, xylan, gelatin and albumin. Glycerol, ethanol, pyruvate and citrate did not support growth. Products of glucose fermentation (Bonch-Osmolovskaya & Miroshnichenko, 1994Go) were acetate, ethanol and lactate, at a ratio of 14.5 : 9 : 1, and H2 and CO2 (not quantified). Addition of thiosulfate (2 g l–1) did not stimulate growth significantly; thiosulfate was reduced to molecular sulfur, which was deposited inside the cells. The addition of elemental sulfur (10 g l–1) produced no stimulating effect; only trace amounts of hydrogen sulfide were detected. Sulfate (2 g l–1) supplementation of the medium did not change the growth characteristics noticeably. Sulfate was not reduced; however, sulfite (6 mM) was reduced to hydrogen sulfide and slightly inhibited growth (cell yield was 3.7-fold lower), concomitantly causing a change in cell morphology and in the ratio of fermentation products. The cells became much longer and formed long chains; the formation of ethanol increased 5.5-fold, from approximately 1.55x10–8 to 8.5x10–8 mmol per cell.


Figure 1
View larger version (41K):
[in this window]
[in a new window]

 
Fig. 1. Light and electron micrographs of strain 761-119T. (a) Phase-contrast micrograph of exponentially growing cells. Bar, 10 µm. (b) Electron micrograph of negatively stained (Bonch-Osmolovskaya et al., 1990Go), exponentially growing cells. Bar, 1 µm. (c) Electron micrograph of a thin section (Bonch-Osmolovskaya etal., 1990Go) of exponentially growing cells. Bar, 1 µm.

 
DNA was isolated according to the method of Marmur (1961)Go. The G+C content of the DNA was 34 (±0.5) mol%, as measured by thermal denaturation of the DNA (Marmur & Doty, 1962Go).

The almost complete 16S rRNA gene sequence of strain 761-119T (1441 nt corresponding to nt 11–1469 of Escherichia coli numbering) was determined as described previously (Sokolova et al., 2002Go). Comparison of this 16S rRNA gene sequence against the existing database using the BLAST program (http://www.ncbi.nlm.nih.gov/blast) revealed that strain 761-119T was a member of the large phylum Firmicutes, which includes the so-called low-G+C-content, Gram-positive bacteria. Within this subgroup, strain 761-119T fell within the genus Thermoanaerobacterium in the family Thermoanaerobacteriaceae in the order Thermoanaerobacteriales of the class Clostridia (Garrity et al., 2005Go). The 16S rRNA gene sequence similarity values between strain 761-119T and the type strains of Thermoanaerobacterium species with validly published names were in the range 86.5–97.8 %. The phylogenetic position of isolate 761-119T was revealed by constructing a 16S rRNA gene sequence phylogenetic tree (Fig. 2Go), employing TREECON (Van De Peer & De Wachter, 1994Go) and using Jukes and Cantor corrections (Jukes & Cantor, 1969Go). This analysis showed that the 16S rRNA gene sequence of isolate 761-119T had <97 % similarity with those of all species of the genus Thermoanaerobacterium with one exception – the type strain of the most closely related species T. aotearoense (Liu et al., 1996Go), with 97.8 % sequence similarity. This correlation was also mirrored in a comparison of phenotypic characteristics of isolate 761-119T and species of the genus Thermoanaerobacterium (Table 1Go). Although T. aotearoense and isolate 761-119T used similar growth substrates and were both moderate thermoacidophiles, they differed in that strain 761-119T had one polar flagellum and a lower pH limit of pH20 °C 3.2, while T. aotearoense had peritrichous flagellation and an acidic pH limit for growth of 3.8. DNA–DNA hybridization between strain 761-119T and T. aotearoense was carried out using the method of Marmur (1961)Go and yielded 33 % relatedness, indicating that the two strains belonged to different species. Thus, isolate 761-119T is proposed to represent the type strain of a novel species, for which the name Thermoanaerobacterium aciditolerans sp. nov. is proposed.


Figure 2
View larger version (30K):
[in this window]
[in a new window]

 
Fig. 2. Neighbour-joining tree based on 16S rRNA gene sequences showing the phylogenetic positions of strain 761-119T and representatives of the genus Thermoanaerobacterium. Bootstrap values (expressed as percentages of 1000 replications) are shown at branch points. Bar, 0.05 substitutions per nucleotide position.

 

View this table:
[in this window]
[in a new window]

 
Table 1. Characteristic features of strain 761-119T and Thermoanaerobacterium species

Taxa: 1, T. thermosulfurigenes (data from Lee et al., 1993Go); 2, T. xylanolyticum (Lee et al., 1993Go); 3, T. saccharolyticum (Lee et al., 1993Go); 4, T. zeae (Cann et al., 2001Go); 5, T. polysaccharolyticum (Cann et al., 2001Go); 6, T. aotearoense (Liu et al., 1996Go; this study); 7, strain 761-119T (this study). +, Positive; –, negative; NA, no data available; ND, not determined. All species utilize glucose, galactose and sucrose and form glucose, ethanol, acetate, H2 and CO2.

 
Description of Thermoanaerobacterium aciditolerans sp. nov.
Thermoanaerobacterium aciditolerans (a.ci.di.tol'er.ans. N.L. neut. n. acidum an acid; L. pres. part. tolerans tolerating; N.L. part. adj. aciditolerans acid-tolerating).

Cells are rod-shaped, motile and spore-forming, 0.4 µm in diameter and 3–12 µm long, with Gram-positive cell walls and one flagellum. Obligate anaerobe. Moderate thermophile growing between 37 and 68 °C, with an optimum at 55 °C (no growth within 5 days at or below 35 °C and at or above 70 °C). Moderate acidophile growing in the pH20 °C range 3.2–7.1, with an optimum pH20 °C at 5.7 (no growth at or below pH20 °C 2.8 and at or above pH20 °C 7.5), and at NaCl concentrations of 0–3 % (no growth at 4 % NaCl). Grows by fermentation of glucose, maltose, fructose, sucrose, lactose, xylose, ribose, arabinose, galactose, yeast extract, sorbitol, starch, xylan, gelatin and albumin. Glycerol, ethanol, pyruvate and citrate are not utilized. Fermentation products are acetate, ethanol, lactate, H2 and CO2. Thiosulfate is reduced to S0, which is deposited inside the cells. Sulfite is reduced to sulfide. The DNA G+C content is 34 (±0.5) mol% (thermal denaturation method).

The type strain is 761-119T (=DSM 16487T=VKM B-2363T), isolated from a hydrothermal vent in the Orange Field, Uzon Caldera (Kamchatka, far-eastern Russia).


    ACKNOWLEDGEMENTS
 
This work was supported by the programmes of the Russian Academy of Sciences ‘Molecular and Cell Biology’ and ‘Origin and Evolution of Biosphere’, by RFBR grant # 05-04-48058, as well as by NSF-funded research grant ‘Microbial Observatory Kamchatka, an International Interdisciplinary Research Project’ (NSF MCB-02238407).


    REFERENCES
 TOP
 ABSTRACT
 MAIN TEXT
 REFERENCES
 
Balch, W. E., Fox, G. E., Magrum, G. E., Woese, G. E. & Wolfe, R. S. (1979). Methanogens: reevaluation of a unique biological group. Microbiol Rev 43, 260–296.[Free Full Text]

Bonch-Osmolovskaya, E. A. & Miroshnichenko, M. L. (1994). The influence of molecular hydrogen and elemental sulfur on the metabolism of extremely thermophilic archaea of genus Thermococcus. Microbiology (English translation of Mikrobiologiia) 63, 433–437.

Bonch-Osmolovskaya, E. A., Sokolova, T. G., Kostrikina, N. A. & Zavarzin, G. A. (1990). Desulfurella acetivorans gen. nov., sp. nov. – a new thermophilic sulfur-reducing eubacterium. Arch Microbiol 153, 151–155.[CrossRef]

Brock, T. D. (1986). Notes on the ecology of thermophilic archaebacteria. Syst Appl Microbiol 7, 213–215.

Cann, I. K. O., Stroot, P. G., Mackie, K. R., White, B. A. & Mackie, R. I. (2001). Characterization of two novel saccharolytic, anaerobic thermophiles, Thermoanaerobacterium polysaccharolyticum sp. nov. and Thermoanaerobacterium zeae sp. nov., and emendation of the genus Thermoanaerobacterium. Int J Syst Evol Microbiol 51, 293–302.[Abstract]

Garrity, G. M., Bell, J. A. & Lilburn, T. G. (2005). Taxonomic outline of the prokaryotes. In Bergey's Manual of Systematic Bacteriology, 2nd edn. New York: Springer. http://141.150.157.80/bergeysoutline/main.htm

Itoh, T., Suzuki, K., Sanchez, P. C. & Nakase, T. (2003). Caldisphaera lagunensis gen. nov., sp. nov., a novel thermoacidophilic crenarchaeote isolated from a hot spring at Mt Maquiling, Philippines. Int J Syst Evol Microbiol 53, 1149–1154.[Abstract/Free Full Text]

Johnson, D. B. (1998). Biodiversity and ecology of acidophilic microorganisms. FEMS Microbiol Ecol 27, 307–317.[CrossRef]

Jukes, T. H. & Cantor, C. R. (1969). Evolution of protein molecules. In Mammalian Protein Metabolism, pp. 21–32. Edited by H. N. Munro. New York: Academic Press.

Lee, Y. E., Jain, M. K., Lee, C., Lowe, S. E. & Zeikus, J. G. (1993). Taxonomic distinction of saccharolytic thermophilic anaerobes: description of Thermoanaerobacterium xylanolyticum gen. nov., sp. nov., and Thermoanaerobacterium saccharolyticum gen. nov., sp. nov.; reclassification of Thermoanaerobium brockii, Clostridium thermosulfurogenes, and Clostridium thermohydrosulfuricum E100-69 as Thermoanaerobacter brockii comb. nov., Thermoanaerobacterium thermosulfurigenes comb. nov., and Thermoanaerobacter thermohydrosulfuricus comb. nov., respectively; and transfer of Clostridium thermohydrosulfuricum 39E to Thermoanaerobacter ethanolicus. Int J Syst Bacteriol 43, 41–51.

Liu, S.-Y., Rainey, F. A., Morgan, H. W., Mayer, F. & Wiegel, J. (1996). Thermoanaerobacterium aotearoense sp. nov., a slightly acidophilic, anaerobic thermophile isolated from various hot springs in New Zealand, and emendation of the genus Thermoanaerobacterium. Int J Syst Bacteriol 46, 388–396.[Abstract/Free Full Text]

Marmur, J. (1961). A procedure for the isolation of deoxyribonucleic acid from microorganisms. J Mol Biol 3, 208–218.

Marmur, J. & Doty, P. (1962). Determination of the base composition of deoxyribonucleic acid from its thermal denaturation temperature. J Mol Biol 5, 109–118.[Medline]

Prokofeva, M. I., Miroshnichenko, M. L., Kostrikina, N. A., Chernyh, N. A., Kuznetsov, B. B., Tourova, T. P. & Bonch-Osmolovskaya, E. A. (2000). Acidilobus aceticus gen. nov., sp. nov., a novel anaerobic thermoacidophilic archaeon from continental hot vents in Kamchatka. Int J Syst Evol Microbiol 50, 2001–2008.[Abstract]

Prokofeva, M. I., Kublanov, I. V., Nercessian, O., Tourova, T. P., Kolganova, T. V., Lebedinsky, A. V., Bonch-Osmolovskaya, E. A., Spring, S. & Jeanthon, C. (2005). Cultivated anaerobic acidophilic/acidotolerant thermophiles from terrestrial and deep-sea hydrothermal habitats. Extremophiles 9, 437–448.[CrossRef][Medline]

Segerer, A., Langworthy, T. A. & Stetter, K. O. (1988). Thermoplasma acidophilum and Thermoplasma volcanium sp. nov. from solfatara fields. Syst Appl Microbiol 10, 161–171.

Sokolova, T. G., Kostrikina, N. A., Chernyh, N. A., Tourova, T. P., Kolganova, T. V. & Bonch-Osmolovskaya, E. A. (2002). Carboxydocella thermautotrophica gen. nov., sp. nov., a novel anaerobic, CO-utilizing thermophile from a Kamchatkan hot spring. Int J Syst Evol Microbiol 52, 1961–1967.[Abstract]

Van De Peer, Y. & De Wachter, R. (1994). TREECON for Windows: a software package for the construction and drawing of evolutionary trees for the Microsoft Windows environment. Comput Appl Biosci 10, 569–570.[Free Full Text]

Wiegel, J. & Canganella, F. (2001). Extreme thermophiles. In Encyclopedia of Life Sciences, article 392. Chichester: Wiley. http://www.els.net

Wolin, E. A., Wolin, M. J. & Wolfe, R. S. (1963). Formation of methane by bacterial extracts. J Biol Chem 238, 2882–2888.[Free Full Text]




This article has been cited by other articles:


Home page
Int. J. Syst. Evol. Microbiol.Home page
M. L. Miroshnichenko, T. P. Tourova, T. V. Kolganova, N. A. Kostrikina, N. Chernych, and E. A. Bonch-Osmolovskaya
Ammonifex thiophilus sp. nov., a hyperthermophilic anaerobic bacterium from a Kamchatka hot spring
Int J Syst Evol Microbiol, December 1, 2008; 58(12): 2935 - 2938.
[Abstract] [Full Text] [PDF]


This Article
Right arrow Abstract Freely available
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via CrossRef
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.
Agricola
Right arrow Articles by Kublanov, I. V.
Right arrow Articles by Bonch-Osmolovskaya, E. A.


HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
INT J SYST EVOL MICROBIOL MICROBIOLOGY J GEN VIROL
J MED MICROBIOL ALL SGM JOURNALS