|
|
||||||||
Biology Department, Portland State University, PO Box 751, Portland, OR 97207-0751, USA
Correspondence
Melissa M. Kendall
kendallm{at}pdx.edu
| ABSTRACT |
|---|
|
|
|---|
Published online ahead of print on 12 August 2005 as DOI 10.1099/ijs.0.63886-0.
The GenBank/EMBL/DDBJ accession numbers for the 16S rRNA gene sequences of strains AK-5T, AK-9 and AK-4 are AY941801, AY941802 and AY663809, respectively.
Graphs showing the effect of environmental factors on the growth rates of strains AK-4, AK-5T and AK-9 are available as supplementary material in IJSEM Online.
| MAIN TEXT |
|---|
|
|
|---|
Methanogens that belong to the family Methanosarcinaceae are characterized as having the broadest substrate range of methanogens; many can grow by reducing CO2 with H2 or by the splitting of acetate and all can grow by dismutating methyl compounds (Kendall & Boone, 2004
). The family Methanosarcinaceae includes eight genera: Methanosarcina, Methanolobus, Methanococcoides, Methanohalobium, Methanohalophilus, Methanosalsum, Methanomethylovorans and Methanimicrococcus. The only described species of Methanimicrococcus, Methanimicrococcus blatticola, is unique among the Methanosarcinaceae because it reduces methylated compounds only in the presence of H2 (Sprenger et al., 2000
).
The genus Methanosarcina currently comprises nine species: Methanosarcina barkeri, Methanosarcina acetivorans, Methanosarcina siciliae, Methanosarcina thermophila, Methanosarcina mazei (=Methanosarcina frisia), Methanosarcina vacuolata, Methanosarcina baltica, Methanosarcina lacustris and Methanosarcina semesiae. The genus Methanosarcina includes slightly halotolerant and slightly halophilic species. Several species were originally isolated from anaerobic sewage sludge digesters (Barker, 1936
; Bryant & Boone, 1987
; Mah & Kuhn, 1984
; Zhilina & Zavarzin, 1987
; Zinder et al., 1985
) and other species of this genus have been isolated from various sediment environments, including marine and estuarine sediments (Elberson & Sowers, 1997
; Lyimo et al., 2000
; Ni & Boone, 1991
; Simankova et al., 2001
; Sowers et al., 1984
; von Klein et al., 2002
). Also, Methanosarcina barkeri strain CM1 has been isolated from sheep rumen (Jarvis et al., 2000
).
The genus Methanococcoides currently contains two species, both from environments with salinity near that of sea water. Methanococcoides methylutens was isolated from submarine canyon sediments that contained large deposits of organic material off the coast of southern California (Sowers & Ferry, 1983
) and Methanococcoides burtonii was obtained from the anoxic hypolimnion of Ace Lake, Antarctica (Franzmann et al., 1992
).
These organisms can dismutate methylamines and methanol for growth but cannot catabolize acetate, dimethylsulfide, H2/CO2 or formate.
We describe three strains of methylotrophic methanogens that have been isolated from the sulfate-reducing zone in the sediments of Skan Bay, Alaska. Strain AK-4 was most closely related to Methanosarcina baltica and an emended description of Methanosarcina baltica is presented incorporating the phenotypic characteristics of this novel strain. Strains AK-5T and AK-9 were most closely related to Methanococcoides burtonii and we propose a novel species, Methanococcoides alaskense, with strain AK-5T (=OCM 775T=DSM 17273T) as the type strain.
Source of inoculum, enrichment and purification
All strains described here were isolated from sediment samples collected from Skan Bay, Alaska (57° N 167° W). Skan Bay lies on the north-west side of Unalaska Island in the Aleutian Island chain. Skan Bay was chosen as the study site because of its accessibility and its similarity (in temperature, pH and salinity) to deep-ocean sediments. Skan Bay is 65 m deep at the sampling site and the temperature of the sediment remains between 1 and 6 °C year-round. The sediments are permanently anoxic below the top centimetre and sulfate is depleted about 45 cm below the sedimentwater interface (Reeburgh, 1980
). Large amounts of organic matter are present, sedimented from diatoms and kelp. The sediment samples were collected with a multi-corer (Ocean Instruments) and samples from various depths (27 cm ranges) were immediately sealed in cans (while excluding air and gas) and stored at 4 °C during transport to the laboratory.
The anaerobic culture techniques of Hungate (1966)
, as modified by Sowers & Noll (1995)
, were used in this study. MSH enrichment medium (Ni & Boone, 1991
) was used as the basal medium for characterization of the strains. The medium was prepared at pH 7·0 with a gas phase mixture of N2 and CO2 (7 : 3). The salinity of the medium was 0·2 M for growth of strain AK-9 and 0·3 M for growth of strains AK-5T and AK-4.
A 1 g sample from the interval taken 3239 cm deep in the sediment was inoculated into MSH enrichment medium (pH 7) containing 20 mM trimethylamine (TMA) as catabolic substrate. Another enrichment culture was inoculated with 1 g sediment collected from the interval 3941 cm deep. Each of these suspensions was mixed, serially diluted and then the serial dilutions were inoculated into MSH enrichment medium with 20 mM TMA. All of the tubes were incubated at 15 °C and the cultures were screened periodically for methanogenesis by analysing a sample of the headspace gas (Maestrojuán & Boone, 1991
). From each of the dilution series, the 103 culture [inoculated with the equivalent of 1 mg (wet weight) sediment] was the enrichment culture of highest dilution that produced methane. These cultures produced detectable methane after 4 weeks incubation and methanogenesis was complete after 16 weeks. No enrichments of higher dilution produced methane, even after 24 weeks of incubation.
Each culture isolated in this way was subjected to a second roll-tube isolation in order to ensure the purity of each strain. The purity of the cultures was checked microscopically and by ensuring that only a single colony type was seen in roll-tube media. Three pure cultures were obtained and named AK-4 (=OCM 774), AK-5T (=OCM 775T) and AK-9 (=OCM 793).
Morphology
Cells in the late-exponential growth phase were fixed directly in culture medium by adding an equal volume of 5 % glutaraldehyde. Cells were fixed for 30 min at 4 °C and then collected by centrifugation. Cells were then fixed for 30 min in cacodylate buffer (pH 7·2) containing 1 % osmium tetroxide. The cells were dehydrated in an ethanol series and embedded in low-viscosity epoxy resin for sectioning. Ultrathin sections were post-stained with uranyl acetate and lead citrate and viewed with a transmission electron microscope (EM-10CA; Zeiss).
Strain AK-4 formed colonies only after 60 days incubation at which time the surface colonies were about 1 mm in diameter, yellow, circular and concave. Cells were 23 µm in diameter, highly irregular coccoids that occurred singly and lacked flagella or pili (Fig. 1
). The cells stained Gram-negative, were autofluorescent and lysed under alkaline conditions or after treatment with SDS, indicating a proteinaceous cell wall.
|
|
|
Each strain grew between 5 and 25 °C, with fastest growth at 2025 °C, but no growth at above 30·6 °C (see Supplementary Figs S1a and S2a in IJSEM Online). As indicated by the square-root equation (Ratkowsky et al., 1983
), strain AK-4 grew optimally at 21 °C, the minimum temperature was 2·3 °C and the maximum temperature was 28·4 °C. Strain AK-5T grew fastest at 23·6 °C, the minimum growth temperature was 2·3 °C and the maximum temperature was 30·6 °C. Strain AK-9 grew optimally at 26·0 °C and the minimum and maximum temperatures for growth were 10·7 and 30·1 °C, respectively. The growth rate of AK-9 was faster than that of AK-5T. Strain AK-4 showed the slowest growth of the three strains. Strains AK-5T, AK-9 and AK-4 grew fastest at Na+ concentrations slightly below that of sea water (0·3 and 0·4 M). Cells grew in the range 0·10·7 M Na+ for strains AK-5T and AK-4 and at 0·10·8 M Na+ for strain AK-9 (see Supplementary Figs S1b and S2b in IJSEM Online). Growth occurred in the pH range 6·37·5 for all three strains, but not at pH 6·0 or 8·0 (see Supplementary Figs S1c and S2c in IJSEM Online).
The catabolic ranges of all strains were determined by adding (in separate tests) 160 mM formate, 40 mM acetate, 40 mM methanol, 25 mM TMA, 5 mM dimethylsulfide or 1 atm H2 to the basal medium for each strain. When a given substrate did not support methanogenesis, possible inhibition was tested by inoculating the culture into culture medium containing that substrate plus 5 mM TMA (on which each strain could grow). The production of methane from cultures with TMA plus another substrate was taken to indicate that the other substrate was not inhibitory.
Each of the three strains grew with TMA as the catabolic substrate. Only strain AK-4 grew on methanol as the catabolic substrate. This is the first report of methyltrophic methanogens that can not grow on methanol, although Methanohalobium evestigatum can grow on low concentrations of methanol (Boone et al., 1993
). None of the strains could catabolize acetate, dimethylsulfide, formate or hydrogen.
All strains grew in MSH medium with TMA as the sole organic substrate. Although the strains did not require growth factors, specific growth rates increased when yeast extract and peptone (0·050·2 % final concentration) were added to the medium.
Phylogenetic analysis
The 16S rRNA gene sequences were determined after extraction of DNA from cell pellets of pure cultures of strains AK-4, AK-5T and AK-9. DNA was extracted by using QIAamp DNA mini kit procedures (Qiagen). DNA for determination of base composition and for DNADNA hybridization experiments was extracted and purified by a modified method of Marmur (1961)
. Cells were lysed hypotonically and the lysate was mixed with chloroform/isoamyl alcohol to denature and remove proteins. DNA was extracted into the aqueous phase and then precipitated by mixing 1 : 1 with cold 95 % (v/v) ethanol. The DNA was spooled onto a glass rod and dissolved into standard saline citrate solution (SSC; 0·15 M NaCl and 0·015 M trisodium citrate, pH 7·0). The 16S rRNA gene was amplified by PCR from genomic DNA by using the archaea-specific primer 4F (5'-TCCGGTTGATCCTGCCRG-3') and the universal primer 1492R (5'-GGTTACCTTGTTACGACTT-3'). Reactions contained 1·5 mM MgCl2, 50 mM KCl, 30 mM Tris/HCl, 12·5 mM dATP, dGTP, dCTP and dTTP, 1 U Taq polymerase (USB Corporation), 20 pmol of each primer and approximately 100 ng DNA. The reactions were incubated under the following conditions: initial denaturation at 94 °C for 5 min, 35 cycles of primer annealing at 50 °C for 30 s, extension at 72 °C for 90 s and denaturing at 94 °C for 30 s; the final extension was at 72 °C for 10 min. PCR products were purified by using an UltraClean PCR Clean-up DNA purification kit (MoBio Laboratories). The purified products from strains AK-4, AK-5T and AK-9 were used as the templates for sequencing. Sequencing reactions were performed with the ABI PRISM Big Dye Terminator Cycle Sequencing kit and an ABI 310 Genetic Analyzer (Applied Biosystems). The almost-complete sequences of both strands were obtained by using the primers 4F (described above), 515F (5'-GTGCCAGCMGCCCGCGGTAA-3'), 765F (5'-TAGATACCCSSGTAGTCC-3' with S=C or G), 906F (5'-GAAACTTAAAKGAATTG-3' with K=G or T), 1100F (5'-GGCAACGAGCGMGACCC-3' with M=A or C), 1492R (described above), 1391R (5'-GACGGGCGGTGTGTRCA-3' with R=A or G), 1098RA (5'-GGGTCTCGCTCGTTSCC-3'), 907R (5'-GTGCCAGCMGCCGCGGTAA-3' with M=A or C) and 609R (5'-TCTACGCATTCACC-3') to produce an overlapping set of sequences that were assembled into one contiguous sequence by using the AutoAssembler Program (Applied Biosystems). The sequences were manually aligned to related sequences of described methanogens obtained from GenBank and to strain FRX-1, a methylotrophic methanogen that we isolated from Lake Fryxell, Antarctica (unpublished data). Only homologous nucleotides were included in the phylogenetic analysis. Secondary structures were used as a guide to ensure correct alignment and that homologous regions were compared. Filters were used to exclude highly variable positions. The phylogenetic relationships were determined by using maximum-likelihood analysis using the HKY-85 model of evolution in PAUP* (Swofford, 2002
). A bootstrap analysis was performed by using 1000 trial replications to provide confidence estimates for tree topologies.
Analysis of the 16S rRNA gene sequences revealed that the sequence of strain AK-4 had a similarity of 99·5 % to that of Methanosarcina baltica. No other 16S rRNA gene sequences of established species showed more than 97 % similarity to that of strain AK-4. The 16S rRNA gene sequences of strains AK-5T and AK-9 were identical and were 99·8 % similar to the sequence of the type strain of Methanococcoides burtonii. An evolutionary tree based on the maximum-likelihood-generated comparison of the 16S rRNA gene sequences is shown in Fig. 4
.
|
The Tm values for strains AK-4, AK-5T and AK-9 were 89·1, 91 and 90 °C, respectively, which correspond to DNA G+C contents of 37·3, 41·9 and 39·5 mol%, respectively.
DNADNA hybridization
DNADNA hybridization values were determined quantitatively with the method described by De Ley et al. (1970)
. The DNA to be tested was diluted to a final concentration of 50 µg ml1 (Huß et al., 1983
) in 1x SSC buffer. DNA was fragmented to 700 bp by sonication (Microson XL 2000; Misonix) for 2 min. The fragment size was verified by electrophoresis and by comparison with a 1 kb ladder (Invitrogen).
DNADNA relatedness between strain AK-4 and Methanosarcina baltica GS1-AT was 88 % and thus strain AK-4 should be classified as a reference strain of Methanosarcina baltica.
DNADNA hybridization tests indicated a DNADNA relatedness value of 55 % between strain AK-5T and its closest relative, Methanococcoides burtonii DSM 6242T. This suggests that strain AK-5T should not be classified as a member of this species if it can be distinguished by phenotypic traits (Wayne et al., 1987
). DNADNA relatedness values of 88 % between strain AK-5T and strain AK-9 suggest that these strains belong together as members of the same species.
Comparisons with related species
On the basis of DNADNA relatedness and 16S rRNA gene sequence analysis, strain AK-4 was assigned as a member of the psychrophilic, methanogenic species Methanosarcina baltica. However, strain AK-4 possesses unique phenotypic properties compared with the Methanosarcina baltica type strain, GS1-AT (Table 1
). Methanosarcina baltica GS1-AT can utilize TMA, methanol and acetate as substrate, but strain AK-4 can only use TMA and methanol. Morphologically, the strains are both highly irregular cocci, but Methanosarcina baltica GS1-AT has flagella and occurs mainly singly or as diploids; strain AK-4 has no flagella and occurs both singly and as pseudosarcinae. The optimum pH for Methanosarcina baltica GS1-AT is 6·5, whereas that for strain AK-4 is 7·2. In addition, strain AK-4 grows over a broader Na+ range, from 0·1 to 0·7 M Na+.
|
Emended description of Methanosarcina baltica von Klein et al. 2002![]()
Methanosarcina baltica (bal'ti.ca. L. n. mare balticum the Baltic Sea; N.L. fem. adj. baltica pertaining to the Baltic Sea).
Cells are irregular cocci with diameters of 1·53 µm and occur singly, in pairs or in tetrads. Cells may be non-motile and lack flagella or cells may exhibit monopolar, monotrichous flagellation. Methanol and methylamines serve as catabolic substrate, with methane as the end product. Some strains may use acetate as catabolic substrate. Dimethylsulfide, formate and H2/CO2 are not used as energy sources. Growth occurs between 22·3 and 28 °C, with an optimum at 25 °C for the type strain. The doubling time is 84 h at 25 °C, 120 h at 9 °C and 167 h at 4 °C. After transfer of cultures, long lag phases lasting 1520 days at 25 °C and 25 days at 49 °C are observed. Growth occurs at 0·10·7 M Na+, with fastest growth occurring at 0·30·4 M Na+ and at pH values between 6·5 and 7·5.
The type strain, GS1-AT (=DSM 14042T=JCM 11281T), was isolated from the anoxic surface layer of the sediment at a depth of 241 m in the Gotland Deep of the Baltic Sea. Strain AK-4 (=OCM 774), isolated from marine sediments at Skan Bay, Alaska, is a reference strain.
Description of Methanococcoides alaskense sp. nov.
Methanococcoides alaskense (a.las'ken.se. N.L. neut. adj. alaskense referring to Skan Bay, Alaska, from where the type strain was isolated).
Irregular cocci 1·52·0 µm in diameter, occurring singly. Non-motile. Pili are present. TMA serves as catabolic substrate with methane as the product. Methanol, acetate, dimethylsulfide, formate and hydrogen are not used as catabolic substrate. TMA serves as sole organic substrate. Fastest growth occurs at 23·6 °C, with salinity between 0·3 and 0·4 M and a pH of 6·37·5.
The type strain, AK-5T (=OCM 775T=DSM 17273T), was isolated from permanently cold, anoxic marine sediments at Skan Bay, Alaska. Strain AK-9 (=OCM 793) is a reference strain.
| ACKNOWLEDGEMENTS |
|---|
| REFERENCES |
|---|
|
|
|---|
Boone, D. R., Whitman, W. B. & Rouvière, P. E. (1993). Diversity and taxonomy of methanogens. In Methanogenesis: Ecology, Physiology, Biochemistry and Genetics, pp. 3580. Edited by J. G. Ferry. New York: Chapman & Hall.
Bryant, M. P. & Boone, D. R. (1987). Emended description of strain MST (DSM 800T), the type strain of Methanosarcina barkeri. Int J Syst Bacteriol 37, 169170.
De Ley, J., Cattoir, H. & Reynaerts, A. (1970). The quantitative measurement of DNA hybridization from renaturation rates. Eur J Biochem 12, 133142.[Medline]
Elberson, M. A. & Sowers, K. R. (1997). Isolation of an aceticlastic strain of Methanosarcina siciliae from marine canyon sediments and emendation of the species description for Methanosarcina siciliae. Int J Syst Bacteriol 47, 12581261.[CrossRef][Medline]
Fiala, G. & Stetter, K. O. (1986). Pyrococcus furiosus sp. nov. represents a novel genus of marine heterotrophic archaebacteria growing optimally at 100 °C. Arch Microbiol 145, 5661.[CrossRef]
Franzmann, P. D., Springer, N., Ludwig, W., Conway de Macario, E. C. & Rohde, M. (1992). A methanogenic Archaeon from Ace Lake, Antarctica: Methanococcoides burtonii sp. nov. Syst Appl Microbiol 15, 573581.
Hungate, R. E. (1966). The Rumen and its Microbes. New York: Academic Press.
Huß, V. A. R., Festl, H. & Schleifer, K. H. (1983). Studies on the spectrophotometric determination of DNA hybridization from renaturation rates. Syst Appl Microbiol 4, 184192.
Jarvis, G. N., Strompl, C., Burgess, D. M., Skillman, L. C., Moore, E. R. B. & Joblin, K. N. (2000). Isolation of identification of ruminal methanogens from grazing cattle. Curr Microbiol 40, 327332.[CrossRef][Medline]
Kendall, M. M. & Boone, D. R. (2004). The Order Methanosarcinales. In The Prokaryotes: an Evolving Electronic Resource for the Microbiological Community. Release 3.17. Edited by M. Dworkin, S. Falkow, E. Rosenberg, K. -H. Schleifer & E. Stackebrandt. New York: Springer. http://link.springer-ny.com/link/service/books/10125/
King, G. M. (1984). Utilization of hydrogen, acetate, and "noncompetitive" substrates by methanogenic bacteria in marine sediments. Geomicrobiol J 3, 275306.
King, G. M., Klug, M. J. & Lovley, D. R. (1983). Metabolism of acetate, methanol, and methylated amines in intertidal sediments of Lowes Cove, Maine. Appl Environ Microbiol 45, 18481853.
Lyimo, T. J., Pol, A., Op den Camp, H. J. M., Harhangi, H. R. & Vogels, G. D. (2000). Methanosarcina semesiae sp. nov., a dimethylsulfide-utilizing methanogen from mangrove sediment. Int J Syst Evol Microbiol 50, 171178.[Abstract]
Maestrojuán, G. M. & Boone, D. R. (1991). Characterization of Methanosarcina barkeri MST and 227, Methanosarcina mazei S-6T, and Methanosarcina vacuolata Z-761T. Int J Syst Bacteriol 41, 267274.[CrossRef]
Mah, R. A. & Kuhn, D. A. (1984). Transfer of the type species of the genus Methanococcus to the genus Methanosarcina, naming it Methanosarcina mazei (Barker 1936
) comb. nov. et emend. and conservation of the genus Methanococcus (Approved Lists 1980) with Methanococcus vannielii (Approved Lists 1980) as the type species. Int J Syst Bacteriol 34, 263265.[CrossRef]
Marmur, J. (1961). A procedure for the isolation of deoxyribonucleic acid from microorganisms. J Mol Biol 3, 208218.
Marmur, J. & Doty, P. A. (1962). Determination of the base composition of deoxyribonucleic acid from its thermal denaturation temperature. J Mol Biol 5, 109118.[Medline]
Ni, S. & Boone, D. R. (1991). Isolation and characterization of a dimethyl sulfide-degrading methanogen, Methanolobus siciliae HI350, from an oil well, characterization of M. siciliae T4/MT, and emendation of M. siciliae. Int J Syst Bacteriol 41, 410416.[CrossRef][Medline]
Oremland, R. S. & Polcin, S. (1982). Methanogenesis and sulfate reduction: competitive and noncompetitive substrates in estuarine sediments. Appl Environ Microbiol 44, 12701276.
Oremland, R. S. & Taylor, B. F. (1978). Sulfate reduction and methanogenesis in marine sediments. Geochim Cosmochim Acta 42, 209214.
Powell, G. E. (1983). Interpreting gas kinetics of batch culture. Biotechnol Lett 5, 437440.[CrossRef]
Ratkowsky, D. A., Lowry, R. K., McMeekin, T. A., Stokes, A. N. & Chandler, R. E. (1983). Model for bacterial culture growth rate throughout the entire biokinetic temperature range. J Bacteriol 154, 12221226.
Reeburgh, W. S. (1980). Anaerobic methane oxidation: rate depth distributions in Skan Bay sediments. Earth Planet Sci Lett 47, 345352.
Simankova, M. V., Parshina, S. N., Tourova, T. P., Kolganova, T. V., Zehnder, A. J. B. & Nozhevnikova, A. N. (2001). Methanosarcina lacustris sp. nov., a new psychrotolerant methanogenic archaeon from anoxic lake sediments. Syst Appl Microbiol 24, 362367.[CrossRef][Medline]
Sly, L. I., Blackall, L. L., Kraat, P. C., Tian-Shen, T. & Sangkhobol, V. (1986). The use of second derivative plots for the determination of mol% guanine plus cytosine of DNA by the thermal denaturation method. J Microbiol Methods 5, 139156.
Sowers, K. R. & Ferry, J. G. (1983). Isolation and characterization of a methylotrophic marine methanogen, Methanococcoides methylutens, gen. nov., sp. nov. Appl Environ Microbiol 45, 684690.
Sowers, K. R. & Noll, K. M. (1995). Techniques for anaerobic growth. In Archaea: a Laboratory Manual, pp. 1547. Edited by K. R. Sowers & H. J. Schreier. Cold Spring Harbor, NY: Cold Spring Harbor Laboratory.
Sowers, K. R., Baron, S. F. & Ferry, J. G. (1984). Methanosarcina acetivorans sp. nov., an acetotrophic methane-producing bacterium isolated from marine sediments. Appl Environ Microbiol 47, 971978.
Sprenger, W. W., van Belzen, M. C., Rosenberg, J., Hackstein, J. H. P. & Keltjens, J. T. (2000). Methanomicrococcus blatticola gen. nov., sp. nov., a methanol- and methylamine-reducing methanogen from the hindgut of the cockroach Periplaneta americana. Int J Syst Evol Microbiol 50, 19891999.[Abstract]
Starr, M. P. & Mandel, M. (1969). DNA base composition and taxonomy of phytopathogenic and other enterobacteria. J Gen Microbiol 56, 113123.[Medline]
Swofford, D. L. (2002). PAUP*: Phylogenetic analysis using parsimony (*and other methods). Sunderland, MA: Sinauer Associates.
von Klein, D., Arab, H., Volker, H. & Thomm, M. (2002). Methanosarcina baltica, sp. nov., a novel methanogen isolated from the Gotland Deep of the Baltic Sea. Extremophiles 6, 103110.[CrossRef][Medline]
Wayne, L. G., Brenner, D. J., Colwell, R. R. & 9 other authors (1987). International Committee on Systematic Bacteriology. Report of the ad hoc committee on reconciliation of approaches to bacterial systematics. Int J Syst Bacteriol 37, 463464.[CrossRef]
Zhilina, T. N. & Zavarzin, G. A. (1987). Methanosarcina vacuolata sp. nov., a vacuolated methanosarcina. Int J Syst Bacteriol 37, 281283.[CrossRef]
Zinder, S. H., Sowers, K. R. & Ferry, J. G. (1985). Methanosarcina thermophila sp. nov., a thermophilic, acetotrophic, methane-producing bacterium. Int J Syst Bacteriol 35, 522523.[CrossRef]
Zwietering, M. H., Jongenburger, I., Rombouts, F. M. & van't Riet, K. (1990). Modeling of the bacterial growth curve. Appl Environ Microbiol 56, 18751881.
This article has been cited by other articles:
![]() |
S. Sakai, H. Imachi, S. Hanada, A. Ohashi, H. Harada, and Y. Kamagata Methanocella paludicola gen. nov., sp. nov., a methane-producing archaeon, the first isolate of the lineage 'Rice Cluster I', and proposal of the new archaeal order Methanocellales ord. nov. Int J Syst Evol Microbiol, April 1, 2008; 58(4): 929 - 936. [Abstract] [Full Text] [PDF] |
||||
![]() |
N. N. Perreault, D. T. Andersen, W. H. Pollard, C. W. Greer, and L. G. Whyte Characterization of the Prokaryotic Diversity in Cold Saline Perennial Springs of the Canadian High Arctic Appl. Envir. Microbiol., March 1, 2007; 73(5): 1532 - 1543. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. M. Kendall, G. D. Wardlaw, C. F. Tang, A. S. Bonin, Y. Liu, and D. L. Valentine Diversity of Archaea in Marine Sediments from Skan Bay, Alaska, Including Cultivated Methanogens, and Description of Methanogenium boonei sp. nov. Appl. Envir. Microbiol., January 1, 2007; 73(2): 407 - 414. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. M. Kendall, Y. Liu, M. Sieprawska-Lupa, K. O. Stetter, W. B. Whitman, and D. R. Boone Methanococcus aeolicus sp. nov., a mesophilic, methanogenic archaeon from shallow and deep marine sediments. Int J Syst Evol Microbiol, July 1, 2006; 56(Pt 7): 1525 - 1529. [Abstract] [Full Text] [PDF] |
||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| INT J SYST EVOL MICROBIOL | MICROBIOLOGY | J GEN VIROL |
| J MED MICROBIOL | ALL SGM JOURNALS | |