Function of methylcobalamin: coenzyme M methyltransferase isoenzyme II in Methanosarcina barkeri

Methanosarcina barkeri was recently shown to contain two cytoplasmic isoenzymes of methylcobalamin: coenzyme M methyltransferase (methyltransferase 2). Isoenzyme I predominated in methanol-grown cells and isoenzyme II in acetate-grown cells. It was therefore suggested that isoenzyme I functions in methanogenesis from methanol and isoenzyme II in methanogenesis from acetate. We report here that cells of M. barkeri grown on trimethylamine, H₂/CO₂, or acetate contain mainly isoenzyme II. These cells were found to have in common that they can catalyze the formation of methane from trimethylamine and H₂, whereas only acetate-grown cells can mediate the formation of methane from acetate. Methanol-grown cells, which contained only low concentrations of isoenzyme II, were unable to mediate the formation of methane from both trimethylamine and acetate. These and other results suggest that isoenzyme II (i) is employed for methane formation from trimethylamine rather than from acetate, (ii) is constitutively expressed rather than trimethylamine-induced, and (iii) is repressed by methanol. The constitutive expression of isoenzyme II in acetate-grown M. barkeri can explain its presence in these cells. The N-terminal amino acid sequences of isoenzyme I and isoenzyme II were analyzed and found to be only 55% similar.Abbreviations H-S-CoM coenzyme M or 2-mercaptoethane-sulfonate - CH₃-S-CoM methyl-coenzyme M or 2(methylthio)-ethanesulfonate - [Co] cobalamin - CH₃-[Co] methylcobalamin - H₄MPT tetrahydromethanopterin - CH₃-H₄MPT N ⁵-methyltetrahydromethanopterin - MT₁ methyltransferase 1 or methanol: 5-hydroxybenzimidazolyl cobamide methyltransferase - MT₂ methyltransferase 2 or methylcobalamin: coenzyme M methyltransferase - Mops morpholinopropanesulfonate - 1 U = 1 mol/min     

Methanopyrus kandleri,gen. and sp. nov. represents a novel group of hyperthermophilic methanogens,growing at 110°C

A novel group of hyperthermophilic rod-shaped motile methanogens was isolated from a hydrothermally heated deep sea sediment (Guaymas Basin, Gulf of California) and from a shallow marine hydrothermal system (Kolbeinsey ridge, Iceland). The grew between 84 and 110°C (opt: 98°C) and from 0.2% to 4% NaCl (opt. 2%) and pH 5.5 to 7 (opt: 6.5). The isolates were obligate chemolithoautotrophes using H₂/CO₂ as energy and carbon sources. In the presence of sulfur, H₂S was formed and cells tended to lyse. The cell wall consisted of a new type of pseudomurein containing ornithin in addition to lysine and no N-acetylglucosamine. The pseudomurein layer was covered by a detergent-sensitive protein surface layer. The core lipid consisted exclusively of phytanyl diether. The GC content of the DNA was 60 mol%. By 16S rRNA comparisons the new organisms were not related to any of the three methanogenic lineages. Based on the physiological and molecular properties of the new isolates, we describe here a new genus, which we name Methanopyrus (the methane fire). The type species is Methanopyrus kandleri (type strain: AV19; DSM 6324).This paper is dedicated to Otto Kandler on the occasion of his 70th birthday     

Sequence of the 16S rRNA gene from the thermoacidophilic archaebacteriumSulfolobus solfataricus and its evolutionary implications

Summary The sequence of the small-subunit rRNA from the thermoacidophilic archaebacteriumSulfolobus solfataricus has been determined and compared with its counterparts from halophilic and methanogenic archaebacteria, eukaryotes, and eubacteria. TheS. solfataricus sequence is specifically related to those of the other archaebacteria, to the exclusion of the eukaryotic and eubacterial sequences, when examined either by evolutionary distance matrix analyses or by the criterion of minimum change (maximum parsimony). The archaebacterial 16S rRNA sequences all conform to a common secondary structure, with theS. solfataricus structure containing a higher proportion of canonical base pairs and fewer helical irregularities than the rRNAs from the mesophilic archaebacteria.S. solfataricus is unusual in that its 16S rRNA-23S rRNA intergenic spacer lacks a tRNA gene.     

Isolation and characterization of Methanocorpusculum parvum,gen. nov., spec. nov., a new tungsten requiring,coccoid methanogen

A new mesophilic, monotrichously flagellated methane-producing coccus of 1m in diameter was isolated from an anaerobic sour whey digester, originally inoculated with sewage sludge. Growth and methane production were observed with H₂/CO₂, formate and — less effectively — with 2-propanol/CO₂. The isolate grew at temperatures between 15° C and 45° C with the optimum at around 37° C. Acetate, yeast extract and tungstate were required in the medium. Clarified rumen fluid stimulated growth.The DNA of the new methanogen has a G+C content of 48.5 mol%. Comparative 16 S rRNA oligonucleotide cataloguing allows to define the new isolate as a member of a new genus of the order Methanomicrobiales. Further evidence for this is provided by the antigenic crossreactivity with anti-S probes and by metabolic features.Because of its small size the new methanogen is named Methanocorpusculum parvum.This work was supported by a grant of the Deutsche Forschungsgemeinschaft DFG to J. W. and E. S. Immunologic studies were supported in part by grants No. DE-FGO2-84 R 13197 from the U.S. Department of Energy, and No. 261.81/82 from the North Atlantic Treaty Organization (NATO)     

Retrieval of first genome data for rice cluster I methanogens by a combination of cultivation and molecular techniques

We report first insights into a representative genome of rice cluster I (RC-I), a major group of as-yet uncultured methanogens. The starting point of our study was the methanogenic consortium MRE50 that had been stably maintained for 3 years by consecutive transfers to fresh medium and anaerobic incubation at 50 degrees C. Process-oriented measurements provided evidence for hydrogenotrophic CO(2)-reducing methanogenesis. Assessment of the diversity of consortium MRE50 suggested members of the families Thermoanaerobacteriaceae and Clostridiaceae to constitute the major bacterial component, while the archaeal population was represented entirely by RC-I. The RC-I population amounted to more than 50% of total cells, as concluded from fluorescence in situ hybridization using specific probes for either Bacteria or Archaea. The high enrichment status of RC-I prompted construction of a large insert fosmid library from consortium MRE50. Comparative sequence analysis of internal transcribed spacer (ITS) regions revealed that three different RC-I rrn operon variants were present in the fosmid library. Three, approximately 40-kb genomic fragments, each representative for one of the three different rrn operon variants, were recovered and sequenced. Computational analysis of the sequence data resulted in two major findings: (i) consortium MRE50 most likely harbours only a single RC-I genotype, which is characterized by multiple rrn operon copies; (ii) seven genes were identified to possess a strong phylogenetic signal (eIF2a, dnaG, priA, pcrA, gatD, gatE, and a gene encoding a putative RNA-binding protein). Trees exemplarily computed for the deduced amino acid sequences of eIF2a, dnaG, and priA corroborated a specific phylogenetic association of RC-I with the Methanosarcinales.     

The immune response to Lactococcus lactis: Implications for its use as a vaccine delivery vehicle

Abstract The development of hydrogenotrophic bacteria in the rumen of lambs was investigated by culture and labeling experiments. ¹⁴CO₂ and ¹³CO₂ incorporation by the rumen microflora of a 24-h-old lamb showed that while there was no labeled methane, double-labeled acetate was formed indicating the presence of hydrogen-dependent acetogenesis. In vitro counts from rumen fluid of 20-h-old lambs confirmed an extensive colonization of acetogenic bacteria while methanogens were absent. Methanogens appeared in the rumen of 30-h-old lambs, and as they developed there was a proportional decrease in the numbers of acetogens, indicating a competition for hydrogen between these two groups. Hydrogen-utilizing sulfate-reducing bacteria, which were established by the 3rd day after birth, did not seem to be affected by this competition.     

Intralineage diversity of archaebacterial ribosomes: A dichotomy of ribosome features separates sulfur-dependent archaebacteria and methanococcaceae from other archaebacterial taxa

Summary The aggregate masses and relative protein contents of eubacterial and archaebacterial ribosomes have been estimated from the buoyant densities of the ribosomal subunits and the anhydrous weights of the rRNA species. In contrast to the situation in eubacteria, archaebacterial ribosomes fall into two size classes that differ only in the relative abundances of their protein moieties. One class comprises eubacterial-sized particles (2.3-megadalton (Mdal) monomer; 1.5-Mdal and 0.8-Mdal large and small subunits, respectively) having a eubacterial composition of roughly one-third protein and two-thirds RNA. The other class comprises ribosomes heavier than those of eubacteria (3-Mdal monomer; 1.8-Mdal and 1.2-Mdal subunits) and having the same protein/RNA ratio as eukaryotic ribosomes (55% and 50% protein for the small and large subunits, respectively). Eubacterialsized ribosomes are harbored by extreme halophiles and all methanogens but the Methanococcaceae. Ribosomes heavier than those of eubacteria are found in the Methanococcaceae and all sulfur-dependent thermophiles. The data indicate that a change in ribosome structure occurred within the methanogen branch; therefore, although ribosome composition is distributed in archaebacteria, its distribution does not break them into two separate kingdoms: The Methanococcaceae and Methanobacteriaceae are related to each other far more closely than either is to the sulfur-dependent thermophiles, and the root of the archaebacterial tree definitely does not lie betweenMethanobacterium andMethanococcus. We surmise that ribosomes larger than those of eubacteria represent a more rudimentary organelle structure that became fixed owing to nonparallel evolution of the translational machinery in archaebacteria.     

Rumen methanogens: a review

The Methanogens are a diverse group of organisms found in anaerobic environments such as anaerobic sludge digester, wet wood of trees, sewage, rumen, black mud, black sea sediments, etc which utilize carbon dioxide and hydrogen and produce methane. They are nutritionally fastidious anaerobes with the redox potential below −300 mV and usually grow at pH range of 6.0–8.0 [1]. Substrates utilized for growth and methane production include hydrogen, formate, methanol, methylamine, acetate, etc. They metabolize only restricted range of substrates and are poorly characterized with respect to other metabolic, biochemical and molecular properties.     

新疆低阶煤本源生物甲烷转化中微生物群落组成及变化

【目的】探究新疆低阶煤生物甲烷转化过程微生物群落组成及多样性。【方法】采用厌氧培养方法和末端限制性片段长度多态性技术(Terminal restriction fragment length polymorphism,T-RFLP)分析新疆低阶煤本源微生物对甲烷转化及有机酸含量的影响,分析新疆哈密大南湖长焰煤生物甲烷转化过程中微生物群落动态变化。【结果】研究表明长焰煤和褐煤对本源微生物产甲烷影响较小,随着低阶煤生物甲烷转化时间的延长,甲烷产量呈上升趋势,转化60 d后长焰煤甲烷产量高达10.28 m L/g,挥发性有机酸(VFA)浓度则最低;微生物多样性指数变化不明显,不同转化时间微生物主要类群为放线菌门(Actinobacteria),拟杆菌门(Bacteroidetes),厚壁菌门(Firmicutes),变形菌门(Proteobacteria);甲烷菌的群落结构相对于细菌较简单,在整个低阶煤生物转化产甲烷过程中共有古菌类群为甲烷八叠球菌属(Methanosarcina)、甲烷盐菌属(Methanohalobium)、甲烷叶菌属(Methanolobus)、甲烷食甲基菌属(Methanomethylovorans),它们是构成群落结构的基本菌群。【结论】低阶煤生物甲烷转化过程微生物群落具有丰富的多样性,且不同时期多样性有较大差异。甲烷菌群落结构相对于细菌较简单,共有类群明显。