Methanocellales contributes significantly to anthropogenic methane emissions that cause global warming, but few pure cultures for Methanocellales are available to permit subsequent laboratory studies (physiology, biochemistry, etc.).
By combining anaerobic culture and molecular techniques, a novel thermophilic methanogen, strain HZ254T was isolated from a Chinese rice field soil located in Hangzhou, China. The phylogenetic analyses of both the 16S rRNA gene and mcrA gene (encoding the α subunit of methyl-coenzyme M reductase) confirmed its affiliation with Methanocellales, and Methanocella paludicola SANAET was the most closely related species. Cells were non-motile rods, albeit with a flagellum, 1.4–2.8 µm long and by 0.2–0.3 µm in width. They grew at 37–60°C (optimally at 55°C) and salinity of 0–5 g NaCl l−1 (optimally at 0–1 g NaCl l−1). The pH range for growth was 6.4–7.2 (optimum 6.8). Under the optimum growth condition, the doubling time was 6.5–7.8 h, which is the shortest ever observed in Methanocellales. Strain HZ254T utilized H2/CO2 but not formate for growth and methane production. The DNA G+C content of this organism was 52.7 mol%. The sequence identities of 16S rRNA gene and mcrA gene between strain HZ254T and SANAET were 95.0 and 87.5% respectively, and the genome based Average Nucleotide Identity value between them was 74.8%. These two strains differed in phenotypic features with regard to substrate utilization, possession of a flagellum, doubling time (under optimal conditions), NaCl and temperature ranges. Taking account of the phenotypic and phylogenetic characteristics, we propose strain HZ254T as a representative of a novel species, Methanocella conradii sp. nov. The type strain is HZ254T ( = CGMCC 1.5162T = JCM 17849T = DSM 24694T).
Citation: Lü Z, Lu Y (2012) Methanocella conradii sp. nov., a Thermophilic, Obligate Hydrogenotrophic Methanogen, Isolated from Chinese Rice Field Soil. PLoS ONE 7(4): e35279. https://doi.org/10.1371/journal.pone.0035279
Editor: Patrick CY Woo, The University of Hong Kong, China
Received: January 4, 2012; Accepted: March 15, 2012; Published: April 17, 2012
Copyright: © 2012 Lü, Lu. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: The study was supported by the Natural Science Foundation of China (grant no: 40625003; 40830534; www.nsfc.gov.cn) and the Chang Jiang Scholars Program of Chinese Ministry of Education (www.cksp.edu.cn). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
The order Methanocellales, previously recognized as uncultured archaeal group Rice Cluster I (RC-I), plays a key role in methane production from rice field soils , , . Members of Methanocellales are widely distributed in various environments , which further strengthens their roles in global carbon cycling, especially in those microaerophilic environments . However, despite the early detection by molecular techniques in the late 1990s , pure cultures of RC-I were not obtained until recently due to their slow growth and fastidious culture conditions , , . The first axenic culture, a mesophilic hydrogenotrophic methanogen Methanocella paludicola strain SANAET, was isolated under low hydrogen concentrations (<30 Pa) from a Japanese rice field soil , . The second isolate, a thermophilic, hydrogenotrophic methanogen Methanocella arvoryzae strain MRE50T, was purified recently from an enrichment culture which had been established since 2000 , .
Many ecological questions of importance that are difficult to solve by culture-independent methods remain to be answered by pure culture studies of Methanocellales. For example, (1) why are members of Methanocellales more active under low hydrogen partial pressures prevailing in their natural habitats in comparison with other methanogens , ? (2) Why do they become predominant at moderate high temperatures while their natural habitats are often mesophilic , ? (3) How are they able to regulate the expression and translation of their antioxidant machinery thus allowing a presumable adaptation to microaerophilic and even oxic environments , , ? However, despite a successful yet difficult isolation of strain SANAET and MRE50T and their ecological significance, to the best of our knowledge, no subsequent cultivation of them has been reported. In fact, many workers that we know including ourselves have failed to cultivate those strains. Therefore, the available Methanocellales strains remain difficult to cultivate, and more isolates particularly fast-growing ones are needed to push the studies of Methanocellales forward.
Here we report the isolation, physiology and phylogeny of the fastest-growing strain of the order Methanocellales, and propose a new species, Methanocella conradii sp. nov. Its consistency of cultivability is presented as well.
Materials and Methods
Samples and medium
Rice field soil was collected in 2006 from an experimental farm at the China National Rice Research Institute in Hangzhou, China (30°04′37″N, 119°54′37″E). No specific permits were required for the described field studies, as the location is not privately-owned or protected and the field studies did not involve endangered or protected species. Soil sample characteristics and storage were described previously . Soil samples were first inoculated into distilled water (10 g soil plus 10 ml water) for a pre-incubation of up to 100 days. Approximately 5 g pre-incubated soil slurries were inoculated into a modified basal medium , which was prepared by adding 3 ml of trace element solution, 1 ml of tungstate solution, 2 ml of 0.5 M Na2S solution, 1 ml of 1 M bicarbonate solution, and 1 ml each of the three different vitamin solutions into 1 liter of freshwater medium. The freshwater medium contained 0.4 g MgCl2.6H2O, 0.1 g CaCl2.2H2O, 0.1 g NH4Cl, 0.2 g KH2PO4, 0.5 g KCl, 0.3 g L-cysteine-HCl.2H2O, and 0.0005 g resazurin per liter of distilled water. The freshwater medium was autoclaved and cooled under N2 before supplementing with any solutions. The trace element solution was prepared by dissolving 2.000 g FeCl2.4H2O, 0.070 g ZnCl2, 0.100 g MnCl2.4H2O, 0.060 g H3BO3, 0.190 g CoCl2.6H2O, 0.002 g CuCl2.2H2O, 0.024 g NiCl2.6H2O, and 0.036 g Na2MoO4.2H2O into 50 ml of 2 M HCl, then diluting to 1 liter with distilled water. The tungstate solution contained 0.4 g NaOH and 0.007 g Na2WO4.2H2O per liter of distilled water. Vitamin solution 1 contained 0.04 g 4-aminobenzoic acid, 0.01 g D(+)-biotin, 0.01 g DL-α-lipoic acid, 0.1 g calcium-D(+)-pantothenate, 0.1 g vitamin B6, 0.03 g folic acid, 0.05 g nicotinic acid and 0.05 g vitamin B2. The vitamins were dissolved into 1 liter of 50 mM Na-phosphate buffer (pH 7.1). Vitamin solution 2 was consisted of 0.01 g thiamine hydrochloride dissolved in 1 liter of 25 mM Na-phosphate buffer (pH 3.4). Vitamin solution 3 contained 0.05 g vitamin B12 dissolved in 1 liter of distilled water. The vitamin solutions and Na2S solution were filter-sterilized (0.2 µm pore size) with N2 in the headspace. The bicarbonate solution was autoclaved and saturated with CO2. All other solutions were autoclaved with N2 in the headspace.
Enrichments and cultivations
All enrichments and cultivations were performed at 50°C in 100 ml serum bottles under ca. 150 kPa H2/CO2 (80/20, v/v) except that the pre-incubation was under an atmosphere of N2. In the initial several enrichments, 1 g l−1 NaCl was also included in the medium. Unless otherwise mentioned, 1 mM acetate and 0.02% yeast extract was normally included in the standard medium except during the initial several enrichments. Isolation using roll tubes or deep agar was described previously , . After isolation, all incubations were in liquid medium at pH of 6.8 at 55°C, corresponding to a pH of approximately 7.2 at 25°C, under an atmosphere of H2/CO2 (80/20 [v/v]) or N2/CO2 (80/20 [v/v]) without shaking, unless otherwise noted. Substrate utilization and antibiotic (200 mg l−1) and SDS (0, 0.1, 0.5, 1.0, 1.5, 2.0%) susceptibility were performed in 17 ml tubes containing 5 ml medium. Tests for growth temperature, pH and salinity range were carried out in 50 ml vials containing 25 ml medium at 25 to 70°C, pH 6.0 to 8.0, and 0 to 10 g NaCl l−1. The pH was additionally buffered with 10 mM Bicine, which has a pKa of 7.78 at 55°C , and pH values were adjusted at 55°C by adding HCl or NaOH solutions. Growth and substrate utilization were monitored by following the concentration of methane using a gas chromatograph GC-7890A with a thermal conductivity detector (Agilent Technologies). All measurements were performed at least in duplicate, and all incubations were terminated after 1 month unless otherwise mentioned.
Light and electron microcopy
Cell morphology and motility were examined with a phase contrast microscope (Olympus CX41) equipped with a CCD camera (Canon 450D). Phase-contrast micrographs were taken by preparing agar-coated slides for exponential-phase cultures. Colony morphology and fluorescence were visualized by a light microscope (Olympus CX51) equipped with a CDD camera (Olympus DP71) and a fluorescence illumination system (X-cite 120). Cells of strain HZ254T for thin-section electron microscopy were fixed with 2.5% glutaraldehyde overnight, washed with phosphate buffer (pH 7.2, 0.1 M), and post-fixed in 1% osmium tetroxide for 1 h. The fixed cells were washed again with phosphate buffer (pH 7.2, 0.1 M), dehydrated in the serial steps of acetone (30, 50, 70, 80, 90 and 100%), and embedded in Spurr low-viscosity resin. Thin-sections of the cells were made with an ultramicrotome (LEICAUC6i) and stained with uranyl acetate and lead citrate. Transmission electron micrographs were taken by JEM-123O.
PCR amplification, sequencing and phylogenetic analysis
DNA extraction, PCR amplification, terminal restriction fragment length polymorphism (T-RFLP) analysis, cloning and sequencing were performed as previously reported . Sequences were either aligned with RDP's aligner tool using the Ribosomal Database Project (RDP 10)  for 16S rRNA gene or with the Mega 4.0.2 software package  for the deduced McrA amino acid. All sequence alignments were analyzed with the Mega 4.0.2 software package . Distances were calculated using the Jukes-Cantor correction. For phylogenetic analysis, the near full length 16S rRNA gene was amplified using the universal archaeal primer pair Arc21f/1492r . The mcrA gene was amplified with MCRf/MCRr . Phylogenetic trees were produced using the neighbor-joining and maximum-parsimony methods by bootstrap re-sampling analysis with 1000 replicates. 16S rRNA gene and mcrA gene sequences of strain HZ254T have been deposited in GenBank under the accession numbers of JN048683 and JN081865, respectively.
Average Nucleotide Identity
Complete genomes of HZ254T (accession number: CP003243) , SANAET (accession number: AP011532)  and MRE50T (accession number: AM114193)  were used to calculate the ANI (Average Nucleotide Identity) values by the Blast-based method  with the Jspecies package . Please note, although the genome for MRE50T was constructed as a complete metagenome from an enrichment before its isolation , the fact that MRE50T was the only archaeal member in that enrichment includes that its genome was well represented by the metagenome , .
Results and Discussion
Enrichment and isolation
Enrichment of strain HZ254T was directed by both gas and molecular analyses. Measurement of hydrogen consumption and methane formation and T-RFLP analysis based on 16S rRNA genes were performed frequently to monitor the methanogenic activity and the structure of the archaeal and bacterial communities in the enrichment cultures. Cloning and sequencing of the 16S rRNA genes were also conducted occasionally to determine the identity of the predominant archaeal and bacterial groups. Enrichment cultures with neither RC-I as the predominant archaeal group nor significant methanogenic activity were abandoned. The T-RF patterns for the archaeal community along with the successive transfers of the successful enrichments for strain HZ254T are shown in Figure 1. The figure demonstrates that RC-I quickly predominated after just the first transfer from pre-incubated soil slurries, and it exclusively represented the sole archaeal member after at most 13 successive transfers over 338 days, albeit a diverse archaeal community was present during the initial pre-incubation. Therefore, besides the low hydrogen method , our results demonstrate that moderate high temperature remains an effective strategy for enrichment of RC-I methanogens, which is consistent with previous studies that RC-I became predominant upon incubation at 45 to 50°C , . Nevertheless, novel methods are needed to increase the cultivability of RC-I. The combination of the two already effective methods (i.e. by inoculating thermophilic propionate- or acetate-degrading syntrophs into samples incubating at 45 to 55°C with propionate or acetate as substrates) would be an approach worth trying, because it may provide a more selective environment for RC-I. Indeed, in both the Chinese and Italian rice field soils, the predominance of RC-I under syntrophic acetate-degrading conditions was observed at 50°C , .
The analysis was performed using Ar109f/915r primer set and TaqI restriction enzymes . T-RFLP fingerprints were normalized to a total of 100 relative fluorescence units (RFU), and T-RF peaks with RFU less than 1 were discarded. The 254-bp T-RF was affiliated with Methanocellales (RC-I) as determined by cloning and sequencing of 16S rRNA genes, and the T-RF length calculated from the sequence was actually 258-bp (data not shown). All other T-RF peaks could be assigned correspondingly to Methanomicrobiales (Mm), Methanobacteriales (Mb), Methanosarcinaceae (Msr)/Crenarchaeotal group 1.1b (G1.1b), Methanosaetaceae (Msa) and RC-I/Methanomicrobiales (Mm), according to our previous studies in the same soil , , , , respectively. The pre-incubation samples were sampled after 24 hours of incubation, and all other samples were sampled after that methane production ceased and/or hydrogen could not be detected in the headspace. After the 13th transfer, the archaeal community was still frequently monitored by T-RFLP analysis along with subsequent transfers, but the 254-bp was always the sole T-RF product.
Isolation was carried out after the establishment of a stable enrichment culture with RC-I as the sole archaeal group. Deep agar and roll tubes were prepared in an attempt to isolate RC-I colonies. However, colonies formed under standard conditions belonged to bacteria instead of RC-I as screened by 16S rRNA gene sequencing. Therefore, various efforts were made to grow colonies. Firstly, cofactors (e.g. acetate, yeast extract, soil extract, sludge extract and coenzyme M) were supplemented in the medium both individually and in combination. Secondly, agar concentrations of 1.50%, 1.75% and 2.00% were tried. Lastly, antibiotics were included occasionally to eliminate bacteria. The roll tube medium that worked contained 1.50% agar supplemented with 0.05% yeast extract and tryptone and 1 mM acetate. Under these conditions, blue fluorescent colonies of RC-I appeared in several roll tubes after 5 months of incubation, as determined by 16S rRNA gene sequencing. The colonies were picked with Pasteur pipette and further purified by serial dilution in liquid medium supplemented with 200 mg l−1 kanamycin.
The purity of the culture was confirmed by four criteria: (1) the failure to grow in anoxic PYG medium; (2) the failure to detect bacterial 16S rRNA gene using the universal bacterial primer pair 27f (5′-AGAGTTTGA TCMTGGCTCAG-3′) and 907r (5′-CCGTCAATTCMTTTRAGTTT-3′); (3) a homogenous cell morphology by phase contrast microscopy; (4) homogenous 16S rRNA gene sequences of 27 clones (pair-wise sequence similarity >99.9%) obtained using the universal archaeal primer pair Arc21f/1492r. All results indicated that the HZ254T culture was axenic.
Colonies of strain HZ254T were nearly lens-shaped. Both the cells (not shown) and colonies autofluorescenced when excited at 420 nm under an epifluorescence microscope (Figure 2b), which is a characteristic feature of methanogens. Single cells were rod-shaped, 1.4–2.8 µm long and 0.2–0.3 µm wide (Figure 2a). No specific intracytoplasmic structures (intracytoplasmic membranes, inclusion bodies, etc) were found in the cells (Figure 2c). A flagellum was observed after negative staining of the cells (Figure 2d), which was consistent with the presence of a fla gene cluster encoding the flagellum in its genome . Therefore, strain HZ254T is probably motile. However, motility was not observed under our laboratory conditions. Further analyses would be needed to test its motility under different conditions.
(a) Phase contrast micrograph; (b) fluorescence (left) and bright field (right) micrographs of the lens-shaped colony in the same field of view; transmission electron micrograph of (c) a thin section and of (d) negatively stained cells with flagellum; Bars, 10 µm (a); 0.5 mm (b); 500 nm (c); 1 µm (d).
Strain HZ254T utilized H2/CO2 for growth and methane production but not the following tested substrates: 40 mM formate; 20 mM acetate, propionate, lactate or pyruvate; 10 mM methanol, ethanol, 1-propanol, 2-propanol, 1-butanol, 2-butanol or cyclopentanol; and 10 mM methylamine or trimethylamine. Acetate (1 mM) was required as a carbon source for growth. Yeast extract (0.02%) stimulated growth but was not required.
Growth parameters, antibiotic and SDS sensitivity
Growth for strain HZ254T was observed at 37 to 60°C with an optimum at 55°C (Figure S1a). The upper limit of methanogenesis observed in rice soil samples so far is below 60°C , thus our results suggest a potentially new upper boundary (60°C) for methane emission from rice field soils. However, further studies using environmental samples are still needed to confirm this new boundary. The pH range for growth was between pH 6.4 and 7.2, with an optimum around pH 6.8 (Figure S1b). Although a small amount of methane (partial pressure up to 1 kPa) was produced at pH 7.4 over the initial 5 days of incubation, the amount of methane did not increase during a prolonged incubation up to 50 days. The pH remained nearly constant during incubation for most of the treatments. However, at pH 6.8 and 7.2, a slight increase of 0.4 units was observed at the end of the incubation. The strain grew at NaCl concentrations ranging from 0 to 5 g l−1, the optimum growth occurred at 0 to 1 g l−1 (Figure S1c). Under optimal conditions (pH 6.8, 55°C, without NaCl), the doubling time calculated from the methane production rate was 6.5 to 7.8 hours (Figure S1d), which was the shortest so far observed in Methanocellales (Table 1). The maximum specific growth rates calculated from both model fitting and linear regression analyses were consistently around 0.1 h−1 (Figure S1a and S1d). Strain HZ254T could tolerate ampicillin, penicillin-G and kanamycin, but not apramycin, neomycin, rifampicin and chloramphenicol. Cells lysed in 0.5% but not under <0.1% of SDS, and intact cells were hardly seen at 1–2% of SDS when observed by a phase contrast microscope.
Consistency of cultivability
Because of the probable difficulty in cultivation of available Methanocellales species, special focus was paid to assess the cultivable consistency of strain HZ254T. An excellent consistency for cultivating strain HZ254T was judged by three empirical standards: (1) the strain could well survive through successive transfers (seven transfers over more than two years, Table S1); (2) the strain was able to recover from rather long time of storage at 4°C (the maximum storage time allowing recovery was 502 days so far, Table S1); (3) multiple persons within our laboratory could successfully handle the cultivation of the strain. Therefore, strain HZ254T could serve an excellent starting material for laboratory studies of Methanocellales.
GC%, phylogenetic and ANI analyses
The DNA G+C content of strain HZ254T, as determined by genome sequencing, was 52.7 mol% . Strain HZ254T is affiliated with the order Methanocellales, as revealed by the phylogenetic analyses based on the 16S rRNA and mcrA genes (Figure 3 and see Figure S2 and S3 for the detailed alignments). The closest relative of strain HZ254T was M. paludicola SANAET, having gene sequence identities of 95.0% for 16S rRNA gene and 87.5% (nucleotide level) or 94.1% (amino acid level) for the mcrA gene. The corresponding sequence identities between strain HZ254T and M. arvoryzae MRE50T were 92.4–92.5% and 86.5 or 92.0% respectively, and the slight variation for the former values is due to the presence of two slightly different copies of 16S rRNA genes within the genome of strain MRE50T. Moreover, the calculated ANI values among the three strains of Methanocella based on their complete genome sequences were between 69.4 to 74.8%.
The trees were constructed using neighbor-joining method. The McrA tree is based on 155 deduced amino acid positions and Poisson correction. The sequences of Methanopyrus kandleri AV19T, (AE009439; 516778–518289) and (U57340) were used as out groups for rooting the 16S rRNA gene and McrA trees, respectively. The accession number of each reference sequence is shown after the strain name. The coordinates of the sequence were indicated in parenthesis, if it was taken from the complete genome sequence. Bootstrap support (>50% indicated only) was obtained from neighbor-joining (first value) and maximum-parsimony (second value) based on 1000 replicates. The bar represents the number of changes per sequence position.
The collective traits of strain HZ254T with regard to its physiology and phylogeny support it as a member of the order Methanocellales. It shares common phenotypic features with the other two strains (M. arvoryzae MRE50T and M. paludicola SANAET) of Methanocellales, such as the rod-shaped morphology, the growth via hydrogenotrophic methanogenesis and the requirement of acetate as a carbon source. However, they differ in formate utilization, possession of a flagellum, antibiotic susceptibility, temperature range, pH range and salinity range. In addition, the ANI values further distinguish the three strains on the species level, given that they are far below 95 to 96% which is the suggested boundary for species delineation . The comparative characteristics of strain HZ254T, MRE50T and SANAET are listed in Table 1. Interestingly, strain HZ254T seems to be closer to MRE50T than SANAET in major phenotypic traits including temperature range, possession of a flagellum and salinity range, albeit it more resembles SANAET in regard of 16S rRNA and mcrA genes and ANI.
The 16S rRNA gene sequence divergence of 5% between HZ254T and SANAET implies that strain HZ254T could potentially represent a new genus within Methanocellales, given that it is generally considered that a 5 to 7% divergence of 16S rRNA gene sequence is sufficient to delineate different genera . However, the knowledge regarding the physiology of Methanocellales is still quite limited due to the lack of sufficient isolates. In addition, chemotaxonomy ,  and genome-based taxonomy ,  is of importance to further discriminate the taxonomy of the three strains of Methanocellales. Therefore, we decide to propose strain HZ254T as a novel species of the genus Methanocella, Methanocella conradii sp. nov.
Description of Methanocella conradii sp. nov
Methanocella conradii (con.rad'i.i. N.L. gen. masc. n. conradii, named after Ralf Conrad, who has pioneered the studies on RC-I methanogens in environmental samples). Cells are rods and occur singly with a flagellum. Methane is produced exclusively from H2/CO2. Acetate is required for growth and yeast extract can stimulate growth. Growth occurs at 37–60°C (optimum 55°C), at pH 6.4–7.2 (optimum 6.8) and with less than 5 g l−1 of NaCl (optimum 0–1 g l−1). The DNA G+C content is 52.7 mol% determined by genome sequencing. The species was isolated from a rice field soil localized in Hangzhou, China. The type strain is HZ254T ( = CGMCC 1.5162T = JCM 17849T = DSM 24694T).
Effects of (a) temperature, (b) pH and (c) NaCl concentration on growth of M. conradii sp. nov. Specific growth rates at different temperatures were calculated from 2 to 5 replicates by fitting the Gompertz equation , the solid line connects the mean values. Effects of pH and NaCl concentration were estimated by following the cumulative methane partial pressures in headspace, data points represent the averages and standard deviations from duplicate or triplicate samples. (d) Linear regression of the logarithm of sequential methane partial pressures during exponential growth under the optimal conditions (55°C, pH 6.8, 0 g l−1 NaCl), each regression line and equation represents an independent measurement, thus the slope values could be taken as the specific growth rate (μ h−1) and the doubling time (G) was calculated as G = ln (2)/μ.
Alignment of near full length of 16S rRNA genes from 12 species. The numbers after the slash represent the range of the gene length taken for alignment. The alignment was read and printed by Jalview 2.6.1 .
Alignment of deduced McrA amino acid sequences from 12 species. The numbers after the slash represent the range of the amino acid length taken for alignment. The alignment was read and printed by Jalview 2.6.1 .
We thank Lei Cheng and Hui Zhang for their help with anaerobic techniques, William B. Whitman and Sanae Sakai for discussing taxonomy, William B. Whitman and Suzanna L. Bräuer for discussing pH experiment, Jean P. Euzéby for latinization of the species name, and the anonymous reviewers for improving the manuscript.
Conceived and designed the experiments: ZL YHL. Performed the experiments: ZL. Analyzed the data: ZL. Contributed reagents/materials/analysis tools: YHL. Wrote the paper: ZL YHL.
- 1. Conrad R, Erkel C, Liesack W (2006) Rice Cluster I methanogens, an important group of Archaea producing greenhouse gas in soil. Curr Opin Biotech 17: 262–267.R. ConradC. ErkelW. Liesack2006Rice Cluster I methanogens, an important group of Archaea producing greenhouse gas in soil.Curr Opin Biotech17262267
- 2. Erkel C, Kube M, Reinhardt R, Liesack W (2006) Genome of Rice Cluster I archaea - the key methane producers in the rice rhizosphere. Science 313: 370–372.C. ErkelM. KubeR. ReinhardtW. Liesack2006Genome of Rice Cluster I archaea - the key methane producers in the rice rhizosphere.Science313370372
- 3. Lu YH, Conrad R (2005) In situ stable isotope probing of methanogenic archaea in the rice rhizosphere. Science 309: 1088–1090.YH LuR. Conrad2005In situ stable isotope probing of methanogenic archaea in the rice rhizosphere.Science30910881090
- 4. Angel R, Matthies D, Conrad R (2011) Activation of methanogenesis in arid biological soil crusts despite the presence of oxygen. PLoS One 6: e20453.R. AngelD. MatthiesR. Conrad2011Activation of methanogenesis in arid biological soil crusts despite the presence of oxygen.PLoS One6e20453
- 5. Großkopf R, Stubner S, Liesack W (1998) Novel euryarchaeotal lineages detected on rice roots and in the anoxic bulk soil of flooded rice microcosms. Appl Environ Microbiol 64: 4983–4989.R. GroßkopfS. StubnerW. Liesack1998Novel euryarchaeotal lineages detected on rice roots and in the anoxic bulk soil of flooded rice microcosms.Appl Environ Microbiol6449834989
- 6. Erkel C, Kemnitz D, Kube M, Ricke P, Chin KJ, et al. (2005) Retrieval of first genome data for rice cluster I methanogens by a combination of cultivation and molecular techniques. FEMS Microbiol Ecol 53: 187–204.C. ErkelD. KemnitzM. KubeP. RickeKJ Chin2005Retrieval of first genome data for rice cluster I methanogens by a combination of cultivation and molecular techniques.FEMS Microbiol Ecol53187204
- 7. Lueders T, Chin KJ, Conrad R, Friedrich M (2001) Molecular analyses of methyl-coenzyme M reductase alpha-subunit (mcrA) genes in rice field soil and enrichment cultures reveal the methanogenic phenotype of a novel archaeal lineage. Environ Microbiol 3: 194–204.T. LuedersKJ ChinR. ConradM. Friedrich2001Molecular analyses of methyl-coenzyme M reductase alpha-subunit (mcrA) genes in rice field soil and enrichment cultures reveal the methanogenic phenotype of a novel archaeal lineage.Environ Microbiol3194204
- 8. Sizova MV, Panikov NS, Tourova TP, Flanagan PW (2003) Isolation and characterization of oligotrophic acido-tolerant methanogenic consortia from a Sphagnum peat bog. FEMS Microbiol Ecol 45: 301–315.MV SizovaNS PanikovTP TourovaPW Flanagan2003Isolation and characterization of oligotrophic acido-tolerant methanogenic consortia from a Sphagnum peat bog.FEMS Microbiol Ecol45301315
- 9. Sakai S, Imachi H, Sekiguchi Y, Ohashi A, Harada H, et al. (2007) Isolation of key methanogens for global methane emission from rice paddy fields: a novel isolate affiliated with the clone cluster rice cluster I. Appl Environ Microbiol 73: 4326–4331.S. SakaiH. ImachiY. SekiguchiA. OhashiH. Harada2007Isolation of key methanogens for global methane emission from rice paddy fields: a novel isolate affiliated with the clone cluster rice cluster I.Appl Environ Microbiol7343264331
- 10. Sakai S, Imachi H, Hanada S, Ohashi A, Harada H, et al. (2008) 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 58: 929–936.S. SakaiH. ImachiS. HanadaA. OhashiH. Harada2008Methanocella 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 Microbiol58929936
- 11. Sakai S, Conrad R, Liesack W, Imachi H (2010) Methanocella arvoryzae sp nov., a hydrogenotrophic methanogen isolated from rice field soil. Int J Syst Evol Microbiol 60: 2918–2923.S. SakaiR. ConradW. LiesackH. Imachi2010Methanocella arvoryzae sp nov., a hydrogenotrophic methanogen isolated from rice field soil.Int J Syst Evol Microbiol6029182923
- 12. Lu YH, Lueders T, Friedrich MW, Conrad R (2005) Detecting active methanogenic populations on rice roots using stable isotope probing. Environ Microbiol 7: 326–336.YH LuT. LuedersMW FriedrichR. Conrad2005Detecting active methanogenic populations on rice roots using stable isotope probing.Environ Microbiol7326336
- 13. Fey A, Chin KJ, Conrad R (2001) Thermophilic methanogens in rice field soil. Environ Microbiol 3: 295–303.A. FeyKJ ChinR. Conrad2001Thermophilic methanogens in rice field soil.Environ Microbiol3295303
- 14. Peng J, Lü Z, Rui J, Lu Y (2008) Dynamics of the methanogenic archaeal community during plant residue decomposition in an anoxic rice field soil. Appl Environ Microbiol 74: 2894–2901.J. PengZ. LüJ. RuiY. Lu2008Dynamics of the methanogenic archaeal community during plant residue decomposition in an anoxic rice field soil.Appl Environ Microbiol7428942901
- 15. Angel R, Claus P, Conrad R (2011) Methanogenic archaea are globally ubiquitous in aerated soils and become active under wet anoxic conditions. ISME J. R. AngelP. ClausR. Conrad2011Methanogenic archaea are globally ubiquitous in aerated soils and become active under wet anoxic conditions.ISME J
- 16. Widdel F, Bak F (1992) Gram-negative mesophilic sulfate-reducing bacteria. In: Balows A, Trüper HG, Dworkin M, Harder W, Schleifer KH, editors. The Prokaryotes. New York: Springer. pp. 3352–3378.F. WiddelF. Bak1992Gram-negative mesophilic sulfate-reducing bacteria.A. BalowsHG TrüperM. DworkinW. HarderKH SchleiferThe ProkaryotesNew YorkSpringer33523378
- 17. Hungate RE (1969) A roll-tube method for cultivation of strict anaerobes. Methods Microbiol 3B: 117–132.RE Hungate1969A roll-tube method for cultivation of strict anaerobes.Methods Microbiol3B117132
- 18. Fukada H, Takahashi K (1998) Enthalpy and heat capacity changes for the proton dissociation of various buffer components in 0.1 M potassium chloride. Proteins 33: 159–166.H. FukadaK. Takahashi1998Enthalpy and heat capacity changes for the proton dissociation of various buffer components in 0.1 M potassium chloride.Proteins33159166
- 19. Cole JR, Wang Q, Cardenas E, Fish J, Chai B, et al. (2009) The Ribosomal Database Project: improved alignments and new tools for rRNA analysis. Nucleic Acids Res 37: D141–145.JR ColeQ. WangE. CardenasJ. FishB. Chai2009The Ribosomal Database Project: improved alignments and new tools for rRNA analysis.Nucleic Acids Res37D141145
- 20. Tamura K, Dudley J, Nei M, Kumar S (2007) MEGA4: molecular evolutionary genetics analysis (MEGA) software version 4.0. Mol Biol Evol 24: 1596–1599.K. TamuraJ. DudleyM. NeiS. Kumar2007MEGA4: molecular evolutionary genetics analysis (MEGA) software version 4.0.Mol Biol Evol2415961599
- 21. Delong EF (1992) Archaea in coastal marine environments. Proc Natl Acad Sci U S A 89: 5685–5689.EF Delong1992Archaea in coastal marine environments.Proc Natl Acad Sci U S A8956855689
- 22. Springer E, Sachs MS, Woese CR, Boone DR (1995) Partial gene-sequences for the a-subunit of methyl-Coenzyme-M reductase (McrI) as a phylogenetic tool for the family Methanosarcinaceae. Int J Syst Bacteriol 45: 554–559.E. SpringerMS SachsCR WoeseDR Boone1995Partial gene-sequences for the a-subunit of methyl-Coenzyme-M reductase (McrI) as a phylogenetic tool for the family Methanosarcinaceae.Int J Syst Bacteriol45554559
- 23. Lü Z, Lu Y (2012) Complete genome sequence of a thermophilic methanogen Methanocella conradii HZ254 isolated from Chinese rice field soil. J Bacteriol. Z. LüY. Lu2012Complete genome sequence of a thermophilic methanogen Methanocella conradii HZ254 isolated from Chinese rice field soil.J Bacteriol
- 24. Sakai S, Takaki Y, Shimamura S, Sekine M, Tajima T, et al. (2011) Genome sequence of a mesophilic hydrogenotrophic methanogen Methanocella paludicola, the first cultivated representative of the order Methanocellales. PLoS One 6: e22898.S. SakaiY. TakakiS. ShimamuraM. SekineT. Tajima2011Genome sequence of a mesophilic hydrogenotrophic methanogen Methanocella paludicola, the first cultivated representative of the order Methanocellales.PLoS One6e22898
- 25. Goris J, Konstantinidis KT, Klappenbach JA, Coenye T, Vandamme P, et al. (2007) DNA-DNA hybridization values and their relationship to whole-genome sequence similarities. Int J Syst Evol Microbiol 57: 81–91.J. GorisKT KonstantinidisJA KlappenbachT. CoenyeP. Vandamme2007DNA-DNA hybridization values and their relationship to whole-genome sequence similarities.Int J Syst Evol Microbiol578191
- 26. Richter M, Rossello-Mora R (2009) Shifting the genomic gold standard for the prokaryotic species definition. Proc Natl Acad Sci U S A 106: 19126–19131.M. RichterR. Rossello-Mora2009Shifting the genomic gold standard for the prokaryotic species definition.Proc Natl Acad Sci U S A1061912619131
- 27. Rui J, Qiu Q, Lu Y (2011) Syntrophic acetate oxidation under thermophilic methanogenic condition in Chinese paddy field soil. FEMS Microbiol Ecol 77: 264–273.J. RuiQ. QiuY. Lu2011Syntrophic acetate oxidation under thermophilic methanogenic condition in Chinese paddy field soil.FEMS Microbiol Ecol77264273
- 28. Liu F, Conrad R (2010) Thermoanaerobacteriaceae oxidize acetate in methanogenic rice field soil at 50°C. Environ Microbiol 12: 2341–2354.F. LiuR. Conrad2010Thermoanaerobacteriaceae oxidize acetate in methanogenic rice field soil at 50°C.Environ Microbiol1223412354
- 29. Whitman WB, Boone DR, Koga Y, Keswani J (2001) Taxonomy of methanogenic Archaea. The Archaea and the deeply branching and phototrophic bacteria (Bergey's Manual of Systematic Bacteriology, 2nd edn, vol 1) 211–213.WB WhitmanDR BooneY. KogaJ. Keswani2001Taxonomy of methanogenic Archaea.The Archaea and the deeply branching and phototrophic bacteria (Bergey's Manual of Systematic Bacteriology, 2nd edn, vol 1)211213
- 30. Boone DR, Whitman WB (1988) Proposal of minimal standards for describing new taxa of methanogenic bacteria. Int J Syst Bacteriol 38: 212–219.DR BooneWB Whitman1988Proposal of minimal standards for describing new taxa of methanogenic bacteria.Int J Syst Bacteriol38212219
- 31. Koga Y, Nishihara M, Morii H, Akagawa-Matsushita M (1993) Ether polar lipids of methanogenic bacteria: structures, comparative aspects, and biosyntheses. Microbiol Rev 57: 164–182.Y. KogaM. NishiharaH. MoriiM. Akagawa-Matsushita1993Ether polar lipids of methanogenic bacteria: structures, comparative aspects, and biosyntheses.Microbiol Rev57164182
- 32. Konstantinidis KT, Tiedje JM (2005) Towards a genome-based taxonomy for prokaryotes. J Bacteriol 187: 6258–6264.KT KonstantinidisJM Tiedje2005Towards a genome-based taxonomy for prokaryotes.J Bacteriol18762586264
- 33. Konstantinidis KT, Tiedje JM (2007) Prokaryotic taxonomy and phylogeny in the genomic era: advancements and challenges ahead. Curr Opin Microbiol 10: 504–509.KT KonstantinidisJM Tiedje2007Prokaryotic taxonomy and phylogeny in the genomic era: advancements and challenges ahead.Curr Opin Microbiol10504509
- 34. Yuan Y, Conrad R, Lu Y (2009) Responses of methanogenic archaeal community to oxygen exposure in rice field soil. Environ Microbiol Rep 1: 347–354.Y. YuanR. ConradY. Lu2009Responses of methanogenic archaeal community to oxygen exposure in rice field soil.Environ Microbiol Rep1347354
- 35. Wu L, Ma K, Li Q, Ke X, Lu Y (2009) Composition of archaeal community in a paddy field as affected by rice cultivar and N fertilizer. Microbiol Ecol 58: 819–826.L. WuK. MaQ. LiX. KeY. Lu2009Composition of archaeal community in a paddy field as affected by rice cultivar and N fertilizer.Microbiol Ecol58819826
- 36. Yuan Q, Lu Y (2009) Response of methanogenic archaeal community to nitrate addition in rice field soil. Envion Microbiol Rep 1: 362–369.Q. YuanY. Lu2009Response of methanogenic archaeal community to nitrate addition in rice field soil.Envion Microbiol Rep1362369
- 37. Zwietering MH, Jongenburger I, Rombouts FM, van 't Riet K (1990) Modeling of the bacterial growth curve. Appl Environ Microbiol 56: 1875–1881.MH ZwieteringI. JongenburgerFM RomboutsK. van 't Riet1990Modeling of the bacterial growth curve.Appl Environ Microbiol5618751881
- 38. Cole C, Barber JD, Barton GJ (2008) The Jpred 3 secondary structure prediction server. Nucleic Acids Res 36: W197–201.C. ColeJD BarberGJ Barton2008The Jpred 3 secondary structure prediction server.Nucleic Acids Res36W197201