|
|
||||||||
nba
1,2
1 Laboratory of Microbiology, Wageningen University, Dreijenplein 10, 6703 HB Wageningen, The Netherlands
2 Department of Environmental Engineering, Istanbul Technical University, 34469 Maslak, Istanbul, Turkey
3 Department of Marine Biogeochemistry and Toxicology, Royal Netherlands Institute for Sea Research, PO Box 59, 1790 AB Den Burg (Texel), The Netherlands
Correspondence
Melike Balk
Melike.Balk{at}wur.nl
| ABSTRACT |
|---|
|
|
|---|
The GenBank/EMBL/DDBJ accession number for the 16S rRNA gene sequence of strain HB1T is DQ146482.
| MAIN TEXT |
|---|
|
|
|---|
Although the Deltaproteobacteria is not a large assemblage of genera, its members show considerable morphological and physiological diversity (Rabus et al., 2006
). Members of the family Desulfobacteraceae in the order Desulfobacterales are widely distributed in freshwater, marine, hypersaline and oil- or hydrocarbon-polluted sediments (Bak & Widdel, 1986
; Brysch et al., 1987
; Szewzyk & Pfennig, 1987
; Gogotova & Vainstein, 1989
; Schnell et al., 1989
; Rees & Patel, 2001
; Cravo-Laureau et al., 2004
; Kjeldsen et al., 2007
). These bacteria are anaerobic, mesophilic, Gram-negative, oval to coccoid, slightly curved or rod-shaped and grow optimally at 20–35 °C. A wide variety of substrates including alcohols, fatty acids and aromatic and aliphatic compounds can be utilized by this group of organisms (Kuever et al., 2005
). Members of the family Desulfobacteraceae play an important role in the degradation of volatile fatty acids in anaerobic bioreactors treating sulfate-rich wastewaters, such as those from paper mills, tanneries or the food oil industry (Oude Elferink et al., 1994
; Colleran et al., 1995
; Roest et al., 2005
). Acetate and butyrate are important intermediates in the anaerobic degradation of wastewaters. Some bacteria in the family Desulfobacteraceae are able to oxidize butyrate either incompletely to acetate or completely to carbon dioxide with concomitant reduction of sulfate to sulfide (Stieb & Schink, 1989
; Platen et al., 1990
; Brandt et al., 1999
).
The microbial community of an upflow anaerobic sludge blanket (UASB) reactor treating paper-mill wastewater (Industriewater, Eerbeek, The Netherlands) was investigated. In this reactor, both sulfate reduction and methanogenesis have been found to be important (Oude Elferink et al., 1998
). In a previous study, the dominant micro-organisms present in the anaerobic paper-mill wastewater treatment system were assessed by molecular techniques (Roest et al. 2005
). As it was not clear from these earlier molecular studies which bacteria were involved in butyrate degradation with sulfate, in the present study, particular attention was paid to bacteria that are able to degrade butyrate with sulfate. Here, we report the taxonomic characterization of strain HB1T, which was isolated from granular sludge of the full-scale mesophilic UASB reactor at Eerbeek. Detailed characteristics of the granular sludge were described previously by Oude Elferink et al. (1998)
. About 10 ml granular sludge was disintegrated by a Potter homogenizer (Tamson). Serial dilutions of the homogenized sample were prepared in a bicarbonate-buffered anaerobic medium containing sodium butyrate and sodium sulfate. Bacterial growth was evident at a dilution of 10–8 of the incubation at 37 °C within 30 days.
Dilution series were made in a basal bicarbonate-buffered medium containing 10 mM sodium butyrate with 20 mM sodium sulfate. The basal liquid culture medium contained (g l–1 unless indicated): NaCl (7), NaHCO3 (4), Na2SO4 (2.8), MgCl2 . 6H2O (1.2), KCl (0.5), NH4Cl (0.3), KH2PO4 (0.2), CaCl2 (0.15), Na2S . 7–9H2O (0.3), yeast extract (0.02), selenite/tungstate solution (1 ml l–1) (Widdel & Bak, 1992
) and a trace element solution (1 ml l–1) containing (mg l–1 unless indicated): FeCl2 . 4H2O (1500), CoCl2 . 2H2O (190), MnCl2 . 4H2O (100), ZnCl2 (70), H3BO3 (62), Na2MoO4 . 2H2O (36), NiCl2 . 6H2O (24), CuCl2 . 2H2O (17), EDTA (500) and 37 % HCl (7 ml l–1). In addition, vitamins were added from a concentrated stock solution according to Stams et al. (1983)
. The cultures were grown routinely in 117 ml serum vials with butyl rubber stoppers and aluminium crimp seals. The vials contained 50 ml basal medium and a gas phase of 1.7 bar N2/CO2 or H2/CO2 (80/20 %, v/v). Concentrated stock solutions of substrates were prepared anoxically, sterilized by filtration and added to the medium to final concentrations of 5–20 mM. Besides the substrates, vitamins, CaCl2, NaHCO3 and Na2S . 7–9H2O were added from stock solutions after sterilization of the medium. The pH of the medium was 7. Unless stated otherwise, all cultivations were carried out at 30 °C.
For isolation, the enriched culture was incubated in the presence of butyrate by using the soft-agar dilution method. This procedure was applied in 117 ml serum vials. Colonies, which were visible after 1 month of incubation, were picked with a sterile needle and subcultured in liquid medium containing butyrate and sulfate. The colonies were about 1 mm in diameter, lens-shaped and brownish. Serial agar and liquid dilutions were repeated until a pure culture was obtained.
Microscope observations were performed with a Leica DC250 photomicroscope. Cells of strain HB1T were oval to rod-shaped, 1–1.3 µm wide and 2.6–3.5 µm long, depending on the growth phase (Fig. 1
). The cells stained Gram-negative (Murray et al., 1994
). The cells were non-spore-forming and occurred singly, in pairs or in long chains.
|
Temperature limits for growth were determined by culture incubation from 10 to 65 °C in the basal medium. The pH limits for growth were determined in the same medium adjusted to pH values between 5 and 9 by changing the CO2 content of the gas phase. The dependence of growth on NaCl concentration was determined in basal medium containing NaCl at concentrations ranging from 0 to 40 g l–1. Under optimal conditions, the doubling time of the isolate in media with butyrate and sulfate was about 130 h (µmax=0.0037 h–1) and the final cell density (OD600) was about 0.38.
Strain HB1T was mesophilic. Growth occurred between 15 and 37 °C, with an optimum growth temperature of 28–30 °C. Growth was possible at pH 6.5–8.0, with an optimum at pH 7.0. Growth was observed in 0–15 g NaCl l–1, with an optimum around 5 g NaCl l–1.
The G+C content of the DNA was determined by using standard HPLC analysis (Mesbah et al., 1989
) at the Deutsche Sammlung von Mikroorganismen und Zellkulturen GmbH (Braunschweig, Germany). Genomic DNA was isolated according to the procedure of Cashion et al. (1977)
.
Organic compounds were measured by HPLC as described previously by Stams et al., (1993)
. Gases and alcohols were measured by gas chromatography (Balk et al., 2003
; Henstra & Stams, 2004
) and thiosulfate, nitrate and sulfate were analysed by an HPLC system equipped with an Ionpac AS9-SC column and an ED 40 electrochemical detector (Dionex) (Scholten & Stams, 1995
). Sulfide was analysed by the method of Trüper & Schlegel (1964)
.
Strain HB1T used the following substrates as electron donors and carbon sources (tested at 20 mM, unless indicated): H2/acetate (1.7 bar/2 mM), formate, ethanol (5 mM), propionate, 1-propanol (5 mM), 1-butanol (5 mM), 2,3-butandiol (5 mM), fumarate, succinate, butyrate (10 mM), crotonate, catechol (0.5 mM), phenol (1 mM), benzoate (3 mM), 4-hydroxybenzoate (3 mM), palmitate (5 mM) and stearate (2 mM). Growth on ethanol, propionate, crotonate and benzoate was much faster than on butyrate. Growth on pyruvate and crotonate was possible without an electron acceptor. The strain was not able to grow on H2/CO2, methanol, acetone, lactate, malate, glucose or fructose. Slight growth was observed on acetate in the presence of sulfate. A maximum 2 mM acetate was utilized by strain HB1T during 3 weeks of incubation and acetate was not fully oxidized, even after longer incubations. Aromatic compounds including catechol, phenol, benzoate and 4-hydroxybenzoate were oxidized completely by strain HB1T.
Sulfate (20 mM) and thiosulfate (20 mM) were used as electron acceptors, but nitrate (10 mM), sulfite (5 mM) and elemental sulfur (0.5 g l–1) were not. Thiosulfate and sulfite were not disproportionated.
Butyrate was oxidized completely by strain HB1T. After 28 days of incubation in the presence of sulfate, no acetate was detected, and the molar ratio of the butyrate oxidized (7.2 mmol) to sulfide formed (16.0 mmol) of 1 : 2.23 was close to the expected theoretical values for the complete oxidation of butyrate according to the following reaction:
|
|
|
|
Based on morphological and physiological differences from members of the class Deltaproteobacteria, it is proposed that strain HB1T represents a novel species in a new genus. Characteristics that differentiate strain HB1T from phylogenetically related species are given in Table 2
; other detailed characteristics determined are given in the species description below.
|
Description of Desulfatirhabdium gen. nov.
Desulfatirhabdium (De.sul.fa'ti.rhab'di.um. L. pref. de- from; N.L. masc. n. sulfas -atis sulfate; Gr. neut. n. rhabdium a little rod; N.L. neut. n. Desulfatirhabdium a sulfate-reducing small rod).
Cells are anaerobic, Gram-negative, non-spore-forming and oval to rod-shaped. Thiosulfate and sulfate are reduced to sulfide. Volatile fatty acids are oxidized completely. Predominant cellular fatty acids are iso-C15 : 0, anteiso-C15 : 0, C16 : 0 and C14 : 0. Phylogenetically, the genus belongs to the family Desulfobacteraceae in the class Deltaproteobacteria. The type species is Desulfatirhabdium butyrativorans.
Description of Desulfatirhabdium butyrativorans sp. nov.
Desulfatirhabdium butyrativorans (bu.ty.ra.ti.vo'rans. N.L. n. butyras -atis butyrate; L. part. adj. vorans devouring; N.L. part. adj. butyrativorans butyrate-devouring).
Displays the following properties in addition to those described for the genus. Cells are 1–1.3x2.6–3.5 µm. Colonies are brownish, lens-shaped in the agar after about 1 month of incubation. Growth occurs at 15–37 °C (optimum 28–30 °C) and pH 6.5–8.0 (optimum pH 7.0). Growth occurs at NaCl concentrations of 0–15 g NaCl l–1, with an optimum at 5 g NaCl l–1. Sulfate and thiosulfate are used as electron acceptors. In the presence of an electron acceptor, growth occurs on H2/acetate (1.7 bar/2 mM), formate (20 mM), ethanol (5 mM), pyruvate (20 mM), propionate (20 mM), propanol (5 mM), 1-butanol (5 mM), 2,3-butandiol (5 mM), fumarate (20 mM), succinate (20 mM), 1-butyrate (10 mM), crotonate (20 mM), catechol (0.5 mM), phenol (1 mM), benzoate (3 mM), 4-hydroxybenzoate (3 mM), palmitate (5 mM) and stearate (2 mM). Only slight growth is observed on acetate. Fermentative growth occurs on pyruvate and crotonate. Not able to grow on H2/CO2, methanol, acetone, lactate, malate, glucose or fructose. β-Hydroxy fatty acids are present in the range of C14 : 0 to C18 : 0, of which C16 : 0 was the most abundant. The DNA G+C content of the type strain is 55.1 mol%.
The type strain, HB1T (=DSM 18734T =JCM 14470T), was isolated from a UASB reactor treating paper-mill wastewater operated at 37 °C with butyrate as the energy source.
| ACKNOWLEDGEMENTS |
|---|
| REFERENCES |
|---|
|
|
|---|
Balk, M., Weijma, J., Friedrich, M. W. & Stams, A. J. M. (2003). Methanol utilization by a novel thermophilic homoacetogenic bacterium, Moorella mulderi sp. nov., isolated from a bioreactor. Arch Microbiol 179, 315–320.[Medline]
Blumenberg, M., Krüger, M., Nauhaus, K., Talbot, H. M., Oppermann, B. I., Seifert, R., Pape, T. & Michaelis, W. (2006). Biosynthesis of hopanoids by sulfate-reducing bacteria (genus Desulfovibrio). Environ Microbiol 8, 1220–1227.[CrossRef][Medline]
Brandt, K. K., Patel, B. K. C. & Ingvorsen, K. (1999). Desulfocella halophila gen. nov., sp. nov., a halophilic, fatty-acid-oxidizing, sulfate-reducing bacterium isolated from sediments of the Great Salt Lake. Int J Syst Bacteriol 49, 193–200.
Brysch, K., Schneider, C., Fuchs, G. & Widdel, F. (1987). Lithoautotrophic growth of sulfate-reducing bacteria, and description of Desulfobacterium autotrophicum. Arch Microbiol 148, 264–274.[CrossRef]
Campbell, L. L. & Postgate, J. R. (1965). Classification of the spore-forming sulfate-reducing bacteria. Bacteriol Rev 29, 359–363.
Canfield, D. E., Jorgensen, B. B., Fossing, H., Glud, R., Gundersen, J., Ramsing, N. B., Thamdrup, B., Hansen, J. W., Nielsen, L. P. & Hall, P. O. (1993). Pathways of organic carbon oxidation in three continental margin sediments. Mar Geol 113, 27–40.[CrossRef][Medline]
Cashion, P., Holder-Franklin, M. A., McCully, J. & Franklin, M. (1977). A rapid method for the base ratio determination of bacterial DNA. Anal Biochem 81, 461–466.[CrossRef][Medline]
Colleran, E., Finnegan, S. & Lens, P. (1995). Anaerobic treatment of sulfate-containing waste streams. Antonie van Leeuwenhoek 67, 29–46.[CrossRef][Medline]
Cravo-Laureau, C., Matheron, R., Joulian, C., Cayol, J. L. & Hirschler-Réa, A. (2004). Desulfatibacillum alkenivorans sp. nov., a novel n-alkene-degrading, sulfate-reducing bacterium, and emended description of the genus Desulfatibacillum. Int J Syst Evol Microbiol 54, 1639–1642.
Glud, R. N., Risgaard-Petersen, N., Thamdrup, B., Fossing, H. & Rysgaard, S. (2000). Benthic carbon mineralization in a high-Arctic sound (Young Sound, NE Greenland). Mar Ecol Prog Ser 206, 59–71.[CrossRef]
Gogotova, G. I. & Vainstein, M. B. (1989). Description of sulfate-reducing bacterium Desulfobacterium macestii sp. nov. capable of autotrophic growth. Mikrobiologiia 58, 76–80 (in Russian).
Henry, E. A., Devereux, R., Maki, J. S., Gilmour, C. C., Woese, C. R., Mandelco, L., Schauder, R., Remsen, C. C. & Mitchell, R. (1994). Characterization of a new thermophilic sulfate-reducing bacterium Thermodesulfovibrio yellowstonii, gen. nov. and sp. nov.: its phylogenetic relationship to Thermodesulfobacterium commune and their origins deep within the bacterial domain. Arch Microbiol 161, 62–69.[Medline]
Henstra, A. M. & Stams, A. J. M. (2004). Novel physiological features of Carboxydothermus hydrogenoformans and Thermoterrabacterium ferrireducens. Appl Environ Microbiol 70, 7236–7240.
Jørgensen, B. B. (1982). Mineralization of organic matter in the sea bed – the role of sulfate reduction. Nature 296, 643–645.[CrossRef]
Kjeldsen, K. U., Loy, A., Jakobsen, T. F., Thomsen, T. R., Wagner, M. & Ingvorsen, K. (2007). Diversity of sulfate-reducing bacteria from an extreme hypersaline sediment, Great Salt Lake (Utah). FEMS Microbiol Ecol 60, 287–298.[CrossRef][Medline]
Kohring, L. L., Ringelberg, D. B., Devereux, R., Stahl, D. A., Mittelman, M. W. & White, D. C. (1994). Comparison of phylogenetic relationships based on phospholipid fatty acid profiles and ribosomal RNA sequence similarities among dissimilatory sulfate-reducing bacteria. FEMS Microbiol Lett 119, 303–308.[CrossRef][Medline]
Kostka, J. E., Thamdrup, B., Glud, R. N. & Canfield, D. E. (1999). Rates and pathways of carbon oxidation in permanently cold Arctic sediments. Mar Ecol Prog Ser 180, 7–21.
Kuever, J., Rainey, F. A. & Widdel, F. (2005). Family I. Desulfobacteraceae fam. nov. In Bergey's Manual of Systematic Bacteriology, 2nd edn, vol. 2, part C, pp. 959–960. Edited by D. J. Brenner, N. R. Krieg, J. T. Staley & G. M. Garrity. New York: Springer.
Lane, D. J. (1991). 16S/23S rRNA sequencing. In Nucleic Acid Techniques in Bacterial Systematics, pp. 115–175. Edited by E. Stackebrandt & M. Goodfellow. Chichester: Wiley.
Ludwig, W., Strunk, O., Westram, R., Richter, L., Meier, H., Yadhukumar, Buchner, A., Lai, T., Steppi, S., Jobb, G. & other authors (2004). ARB: a software environment for sequence data. Nucleic Acids Res 32, 1363–1371.
Mesbah, M., Premachandran, U. & Whitman, W. B. (1989). Precise measurement of the G+C content of deoxyribonucleic acid by high-performance liquid chromatography. Int J Syst Bacteriol 39, 159–167.
Mori, K., Kim, H., Kakegawa, T. & Hanada, S. (2003). A novel lineage of sulfate-reducing microorganisms: Thermodesulfobiaceae fam. nov., Thermodesulfobium narugense, gen. nov., sp. nov., a new thermophilic isolate from a hot spring. Extremophiles 7, 283–290.[CrossRef][Medline]
Moussard, H., L'Haridon, S., Tindall, B. J., Banta, A., Schumann, P., Stackebrandt, E., Reysenbach, A.-L. & Jeanthon, C. (2004). Thermodesulfatator indicus gen. nov., sp. nov., a novel thermophilic chemolithoautotrophic sulfate-reducing bacterium isolated from the Central Indian Ridge. Int J Syst Evol Microbiol 54, 227–233.
Murray, R. G. E., Doetsch, R. N. & Robinow, C. F. (1994). Determinative and cytological light microscopy. In Methods of General and Molecular Biology, pp. 21–41. Edited by P. Gerhardt, R. G. E. Murray, W. A. Wood & N. R. Krieg. Washington, DC: American Society for Microbiology.
Oude Elferink, S. J. W. H., Lens, P. N. L., Dijkema, C. & Stams, A. J. M. (1994). Sulfate reduction in methanogenic bioreactors. FEMS Microbiol Lett 142, 237–241.[CrossRef]
Oude Elferink, S. J. W. H., Boschker, H. T. S. & Stams, A. J. M. (1998). Identification of sulfate reducers and Syntrophobacter sp. in anaerobic granular sludge by fatty acid biomarkers and 16S rRNA probing. Geomicrobiol J 15, 3–17.
Platen, H., Temmes, A. & Schink, B. (1990). Anaerobic degradation of acetone by Desulfococcus biacutus sp. nov. Arch Microbiol 154, 355–361.[CrossRef][Medline]
Rabus, R., Hansen, T. A. & Widdel, F. (2006). Dissimilatory sulfate- and sulfur-reducing prokaryotes. In The Prokaryotes. A Handbook on the Biology of Bacteria, 3rd edn, vol. 2, pp 659–768. Edited by M. Dworkin, S. Falkow, E. Rosenberg, K. H. Schleifer & E. Stackebrandt. New York: Springer.
Rees, G. N. & Patel, B. K. (2001). Desulforegula conservatrix gen. nov., sp. nov., a long-chain fatty acid-oxidizing, sulfate-reducing bacterium isolated from sediments of a freshwater lake. Int J Syst Evol Microbiol 51, 1911–1916.[Abstract]
Roest, K., Heilig, H. G., Smidt, H., de Vos, W. M., Stams, A. J. & Akkermans, A. D. (2005). Community analysis of a full-scale anaerobic bioreactor treating paper mill wastewater. Syst Appl Microbiol 28, 175–185.[CrossRef][Medline]
Rysgaard, S., Thamdrup, B., Risgaard-Petersen, N., Fossing, H., Berg, P., Christensen, P. B. & Dalsgaard, T. (1998). Seasonal carbon and nutrient mineralization in a high-Arctic coastal marine sediment, Young Sound, Northeast Greenland. Mar Ecol Prog Ser 175, 261–276.
Schnell, S., Bak, F. & Pfennig, N. (1989). Anaerobic degradation of aniline and dihydroxybenzenes by newly isolated sulfate-reducing bacteria and description of Desulfobacterium anilini. Arch Microbiol 152, 556–563.[CrossRef][Medline]
Scholten, J. C. & Stams, A. J. M. (1995). The effect of sulfate and nitrate on methane formation in a freshwater sediment. Antonie van Leeuwenhoek 68, 309–315.[CrossRef][Medline]
Stams, A. J. M., Veenhuis, M., Weenk, G. H. & Hansen, T. A. (1983). Occurrence of polyglucose as a storage polymer in Desulfovibrio species and Desulfobulbus propionicus. Arch Microbiol 136, 54–59.[CrossRef]
Stams, A. J. M., van Dijk, J. B., Dijkema, C. & Plugge, C. M. (1993). Growth of syntrophic propionate-oxidizing bacteria with fumarate in the absence of methanogenic bacteria. Appl Environ Microbiol 59, 1114–1119.
Stieb, M. & Schink, B. (1989). Anaerobic degradation of isobutyrate by methanogenic enrichment cultures and by a Desulfococcus multivorans strain. Arch Microbiol 151, 126–132.[CrossRef]
Szewzyk, R. & Pfennig, N. (1987). Complete oxidation of catechol by strictly anaerobic sulfate-reducing Desulfobacterium catecholicum sp. nov. Arch Microbiol 147, 163–168.[CrossRef]
Thamdrup, B. & Canfield, D. E. (1996). Pathways of carbon oxidation in continental margin sediments of central Chile. Limnol Oceanogr 41, 1629–1650.[Medline]
Trüper, H. G. & Schlegel, H. G. (1964). Sulphur metabolism in Thiorhodaceae. I. Quantitative measurements on growing cells of Chromatium okenii. Antonie van Leeuwenhoek 30, 225–238.[CrossRef][Medline]
Widdel, F. (1980). Anaerober Abbau von Fettsäuren und Benzoesäure durch neu Isolierte Arten Sulfat-reduzierender Bakterien. PhD thesis, Göttingen University, Germany (in German).
Widdel, F. & Bak, F. (1992). Gram-negative mesophilic sulfate-reducing bacteria. In The Prokaryotes, 2nd edn., vol. 4, pp. 3352–3378. Edited by A. Balows, H. G. Trüper, M. Dworkin, W. Harder & K. H. Schleifer. New York: Springer.
Zeikus, J. G., Dawson, M. A., Thompson, T. E., Ingvorsen, K. & Hatchikian, E. C. (1983). Microbial ecology of volcanic sulfidogenesis: isolation and characterization of Thermodesulfobacterium commune gen. nov. and sp. nov. J Gen Microbiol 129, 1159–1169.
Zoetendal, E. G., Akkermans, A. D. L. & de Vos, W. M. (1998). Temperature gradient gel electrophoresis from human fecal samples reveals stable and host-specific communities of bacteria. Appl Environ Microbiol 64, 3854–3859.
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| INT J SYST EVOL MICROBIOL | MICROBIOLOGY | J GEN VIROL |
| J MED MICROBIOL | ALL SGM JOURNALS | |