Isolation and characterization of a thermophilic acetotrophic strain of Methanothrix

An enrichment culture which converted acetate to methane at 60°C was obtained from a thermophilic anaerobic bioreactor. The predominant morphotype in the enrichment was a sheathed gas-vacuolated rod with marked resemblence to the mesophile Methanothrix soehngenii. This organism was isolated using vancomycin treatments and serial dilutions and was named Methanothrix sp. strain CALS-1. Strain CALS-1 grew as filaments typically 2–5 cells long, and cultures showed opalescent turbidity rather than macroscopic clumps. The cells were enclosed in a striated subunit-type sheath and there were distinct cross-walls between the cells, similar to M. soehngenii. The gas vesicles in cells were typically 70 nm in diameter and up to 0.5 m long, and were collapsed by pressures over 3 atm (ca. 300 kPa). Stationary-phase cells tended to have a higher vesicle content than did growing cells, and occasionally bands of cells were seen floating at the top of the liquid in stationary-phase cultures. Acetate was the only substrate of those tested which was used for methanogenesis by strain CALS-1, and acetate was decarboxylated by the aceticlastic reaction. The optimum temperature for growth of strain CALS-1 was near 60°C (doubling time=24–26 h), with no growth occurring at 70°C and 37°C. The optimum pH value for growth was near 6.5 in bicarbonate/CO₂ buffered medium and no growth occurred at pH 5.5 or pH 8.4. No growth was obtained below pH 7 when the medium was buffered with 20 mM phosphate. Strain CALS-1 grew in a chemically defined medium and required biotin. Sulfide concentrations over 1 mM were inhibitory to the culture, and growth was more rapid with 1 mM 2-mercaptoethane sulfonate (coenzyme M) or 1 mM titanium citrate as an accessory reductant than with 1 mM cysteine. It is likely that strain CALS-1 represents a new species in the genus Methanothrix.     

Isolation and characterization of a thermophilic Methanobacterium able to use formate,the strain FTF

A thermophilic anaerobic which produced methane from formate and H₂ and CO₂ was isolated from a bench-scale digester treating a mixture of solid wastes at 55°C, after enrichment cultures on sodium acetate. The cells were slightly crooked rods occurring singly or in filaments. The bacterium was not motile, and stained Gram positive. Colonies appearing after 1 week of incubation were white with filamentous edges and 1 mm in diameter. The organism used H₂:CO₂ or formate as an energy source. Yeast extract was not required but stimulated growth significantly. Casamino acids were stimulatory and could serve as a nitrogen source. Cysteine was used as a sulfur source. The optimum pH for growth was 7.5. Growth occurred from 35 to 70°C with an optimum at 55°C. The deoxyribonucleic acid base composition was 49.2 mol% guanine plus cytosine. Though this isolate conforms to Methanobacterium thermoformicium, its proper assignment awaits further studies. It has been deposited in the Deutsche Sammlung von Mikroorganismen as strain DSM 3012.This work was supported in part by the Conseil Régional Nord/Pas-de-Calais     

Incorporation of [methyl-3H]thymidine by obligate and facultative anaerobic bacteria when grown under defined culture conditions

Abstract Incorporation of [ methyl -³H]thymidine into bacterial DNA was determined for a range of axenic anaerobic bacterial cultures: fermentative heterotrophs, sulphate-reducing bacteria, purple sulphur bacteria, acetogens and methanogens. Anaerobically growing Bacillus sp. and the obligate aerobe Thiobacillus ferrooxidans were also investigated. Actively growing cultures of sulphate-reducing bacteria belonging to the genera Desulfovibrio, Desulfotomaculum, Desulfobacter, Desulfobotulus and Desulfobulbus , purple sulphur bacteria ( Chromatium vinosum OP2 and Thiocapsa roseopersicina OP1), methanogens ( Methanococcus GS16 and Methanosarcina barkeri ) and an acetogen ( Acetobacterium woodii ) did not incorporate [ methyl -³H]thymidine into DNA. The only obligate anaerobes in which thymidine incorporation into DNA could be unequivocally demonstrated were members of the genus Clostridium . Anaerobically growing Bacillus sp. also incorporated thymidine. These data demonstrate that pure culture representatives of major groups of anaerobic bacteria involved in the terminal oxidation of organic carbon and anoxygenic phototrophs within sediments are unable to incorporate [ methyl -³H]thymidine into DNA, although some obligate and facultative anaerobes can. Variability in thymidine incorporation amongst pure culture isolates indicates that unless existing techniques can be calibrated to take this into consideration then productivity estimates in both aerobic and anaerobic environments may be greatly underestimated using the [ methyl -³H]thymidine technique.     

Phytanyl-glycerol ethers and squalenes in the archaebacteriumMethanobacterium thermoautotrophicum

Summary The lipids of a thermophilic chemolithotroph,Metbanobacterium thermoautotropbicum, have been analyzed by chromatographic techniques and identified by infrared spectrometry and combined gas chromatography-mass spectrometry. Of the total chloroform soluble lipids 79% and 21% are polar and non-polar lipids, respectively. The major components of the polar lipids are dialkyl ethers of glycerol or its derivatives. The nature of the glycerol ether alkyl groups was found to be that of the saturated tetraisoprenoid hydrocarbon phytane. The non-polar lipids of the chloroform soluble fraction consist principally of three series of C₂₀, C₂₅ and C₃₀ acyclic isoprenoid hydrocarbons, the major components being squalene and a continuous range of hydrosqualene derivatives, from dihydrosqualene up to and including decahydrosqualene. These data establish thatM. tbermoautotropbicum contains predominantly non-sapo-nifiable lipids as doHalobacterium, Halococcus, Sulfolobus andTbermoplasma. In particular, the composition of the chloroform soluble lipids ofM. tbermoautotropbicum is quite similar to that ofHalobacterium cutirubrum. The results strongly support the recent proposal, based on 16S rRNA sequence homologies, that the extreme halophiles and methanogens share a common ancestor. In addition, it is pointed out that the occurrence of phytane and related polyisoprenoid compounds in ancient sediments can no longer be considered unequivocally as indicative of past photosynthetic activity. Finally, speculations are made concerning the possible role of and evolutionary significance of the presence of squalene and hydrosqualenes in these organisms. To our knowledge this is the first report of squalene and hydrosqualenes in a strictly anaerobic microorganism.To either of whom reprint requests should be sent.     

A re-appraisal of the diversity of the methanogens associated with the rumen ciliates

The diversity of methanogenic archaea associated with different species of ciliated protozoa in the rumen was analysed. Partial fragments of archaeal SSU rRNA genes were amplified from DNA isolated from single cells from the rumen protozoal species Metadinium medium, Entodinium furca, Ophryoscolex caudatus and Diplodinium dentatum. Sequence analysis of these fragments indicated that although all of the new isolates clustered with sequences previously described for methanogens, there was a difference in the relative distribution of sequences detected here as compared to that of previous work. In addition, many of the novel sequences, although clearly of archaeal origin have relatively low identity to the sequences in database which are most closely related to them.     

Production of C<Subscript>35</Subscript> isoprenoids depends on H<Subscript>2</Subscript> availability during cultivation of the hyperthermophile<Emphasis Type="Italic"> Methanococcus jannaschii</Emphasis>

A series of five progressively saturated C₃₅ isoprenoids has been identified in cell-free extracts of the deep-sea methanogen Methanococcus jannaschii. Production and relative abundance of the isoprenoids were dependent on culture conditions; significant production occurred in a 16-l fermentor (12-l working volume) and a 2.5-l fermentor (2-l working volume) but could not be duplicated in serum bottles. Several factors were investigated and shown not to account for the different production levels, including medium composition, pH, and temperature. However, the interphase mass transfer rate was shown to significantly affect the production of C₃₅ isoprenoids in a fermentor. The structures of the novel isoprenoids were confirmed by hydrogenation reactions and mass spectra of the isoprenoids. Indirect evidence based on genomics and mass spectrometry data implicates head-to-head condensation of farnesyl pyrophosphate (C₁₅) with geranylgeranyl pyrophosphate (C₂₀) as the mechanism for C₃₅ synthesis.Communicated by J. WiegelB.P. Manquin and J.A. Morgan contributed equally to this work.     

A simplified method for the cultivation of extreme anaerobic Archaea based on the use of sodium sulfite as reducing agent

The extreme sensitivity of many Archaea to oxygen is a major obstacle for their cultivation in the laboratory and the development of archaeal genetic exchange systems. The technique of Balch and Wolfe (1976) is suitable for the cultivation of anaerobic Archaea but involves time-consuming procedures such as the use of air locks and glove boxes. We describe here a procedure for the cultivation of anaerobic Archaea that is more convenient and faster and allows the preparation of liquid media without the use of an anaerobic chamber. When the reducing agent sodium sulfide (Na₂S) was replaced by sodium sulfite (Na₂SO₃), anaerobic media could be prepared without protection from oxygen outside an anaerobic chamber. Exchange of the headspace of serum bottles by appropriate gases was sufficient to maintain anaerobic conditions in the culture media. Organisms that were unable to utilize sulfite as a source for cellular sulfur were supplemented with hydrogen sulfide. H₂S was simply added to the headspace of serum bottles by a syringe. The use of H₂S as a source for sulfur minimized the precipitation of cations by sulfide. Representatives of 12 genera of anaerobic Archaea studied here were able to grow in media prepared by this procedure. For the extremely oxygen-sensitive organism Methanococcus thermolithotrophicus, we show that plates could be prepared outside an anaerobic chamber when sulfite was used as reducing agent. The application of this method may faciliate the cultivation and handling of extreme anaerobic Archaea considerably. Received: January 4, 2000 / Accepted: April 5, 2000     

A mathematical model for the kinetics of Methanobacterium bryantii M.o.H. considering hydrogen thresholds

We develop a kinetic model that builds on the foundation of classic Monod kinetics, but incorporates new phenomena such as substrate thresholds and survival mode observed in experiments with the H2-oxidizing methanogen Methanobacterium bryantii M.o.H. We apply our model to the experimental data presented in our companion paper on H2 thresholds. The model accurately describes H2 consumption, CH4 generation, biomass growth, substrate thresholds, and survival state during batch experiments. Methane formation stops when its Gibbs free energy is equal zero, although this does not interrupt H2 oxidation. The thermodynamic threshold for H2 oxidation occurs when the free energy for oxidizing H2 and transferring electrons to biomass is no longer negative, at approximately 0.4 nM. This threshold is not controlled by the Gibbs free energy equation of methanogenesis from H2 + HCO3- as we show in our companion paper. Beyond this threshold, the microorganisms shift to a low-maintenance metabolism called "the survival state" in response to extended H2 starvation; adding the starvation response as another new feature of the kinetic model. A kinetic threshold (or S (min)), a natural feature of the Monod kinetics, is also captured by the model at H2 concentration of around approximately 2,400 nM. S (min) is the minimum substrate concentration to maintain steady-state biomass concentration. Our model will be useful for interpreting threshold results and designing new studies to understand thresholds and their ecological implications.     

Effect of different acetate:propionate ratios on the methanogenic community during thermophilic anaerobic digestion in batch experiments

The present study investigated the metabolism of different acetate:propionate ratios (0.25, 0.33, 0.5, 1.0, 2.0, 3.0, 4.0) in equimolar carbon concentration during an anaerobic decomposition process under defined laboratory conditions and evaluated the engaged methanogenic community. Significant differences on a metabolic level (gas production, gas composition, volatile fatty acid (VFA) concentration) were observed between acetate:propionate ratios ≤1 and ≥2. Generally ratios ≥2 resulted in a faster methane production and VFA decomposition compared to ratios ≤1. Regarding the composition of the methanogenic community as well as the abundance of Methanosarcinales these differences were not reflected in an appropriate manner when DNA based methods (dHPLC and qPCR) were applied. However, by a culture based approach these differences could be documented showing a significant difference in the number of cultivable methanogens between initial acetate:propionate ratios ≤1 and ≥2.     

闽江口芦苇沼泽湿地土壤产甲烷菌群落结构的垂直分布

应用PCR-RFLP技术及测序分析对闽江口芦苇湿地土壤产甲烷菌群落结构的垂直分布特征进行了研究。在构建的6个克隆文库中,每个克隆文库随机挑选100个克隆进行菌落PCR验证,共得到591个阳性克隆。PCR产物经限制性内切酶MspⅠ进行RFLP分析后得到37个不同的分类操作单元(OTUs)。对37个克隆子进行了序列测定,与GenBank数据库中的序列进行比对,最近相似性在91%—99%之间。RFLP分析和系统发育分析表明,闽江口芦苇湿地土壤中产甲烷菌群落包括3大类群:甲烷杆菌目(Methanobacteriales)、甲烷微菌目(Methanomirobiales)和甲烷八叠球菌目(Methanosarcinales)。不同土壤深度中产甲烷菌群落的分布呈现出不同的特征。土壤表层(0—10 cm)优势产甲烷菌类群为Methanoregula,约占76%;10—20 cm土层主要的产甲烷菌类群为Methanolinea和Methanoregula,分别约占23%和29%;20—30cm土层优势的产甲烷菌类群为Methanolinea,约占66%。Shannon指数(H’)和Simpson多样性指教(D)表明,10—20cm土层产甲烷菌多样性高于土壤表层(0—10 cm)和20—30 cm土层。37个测序OTUs中有26个OTUs属于不可培养的产甲烷菌序列,表明闽江口芦苇湿地土壤中存在大量不可培养的产甲烷菌。