The F1FO ATP synthase genes in Methanosarcina acetivorans are dispensable for growth and ATP synthesis

There is a long-standing discussion in the literature, based on biochemical and genomic data, whether some archaeal species may have two structurally and functionally distinct ATP synthases in one cell: the archaeal A₁A_O together with the bacterial F₁F_O ATP synthase. To address a potential role of the bacterial F₁F_O ATP synthase, we have exchanged the F₁F_O ATPase gene cluster in Methanosarcina acetivorans against a puromycin resistance cassette. Interestingly, the mutant was able to grow with no difference in growth kinetics to the wild type, and cellular ATP contents were identical in the wild type and the mutant. These data demonstrate that the F₁F_O ATP synthase is dispensable for the growth of M. acetivorans .     

Methane formation from methanol and molecular hydrogen by protoplasts of new methanogenic isolates and inhibition by dicyckohexylcarbodiimide

Protoplasts have been prepared by pronase treatment of cells of two as yet unidentified methanogenic species, strains Gö1 and AJ2. The rate in which these protoplasts formed methane from methanol and molecular hydrogen amounted to 55% (strain Gö1) or 18% (strain AJ2) of the rate of whole cells. Cell extracts, however, had lost most of the activity, and the rate was only 3.6% of the one of whole cells. Methanogenesis by protoplasts from the above mentioned substrates was inhibited by dicyclohexylcarbodiimide, and this inhibition could be abolished by the protonophore tetrachlorosalicylanilide.     

Using thermodynamics to obtain geochemical information from genomes

Thermodynamic characterization of the relative stabilities of chemical compounds is a pillar of conceptual models in various fields of geosciences. Analogous models applied to genomes can yield new information about the relationship between genomes and their geochemical environments. In this perspective article, we present a chemical and thermodynamic analysis of prokaryotic lineages that have been the target of previous phylogenomic studies of evolutionary adaptation to varying redox conditions. The thermodynamic model development begins by quantifying the effects of hydrogen activity (aH₂) and temperature on the relative stabilities of organic compounds with different carbon oxidation state. When applied to proteins instead of metabolites, the same techniques can be used to identify combinations of aH₂ and temperature at which reference proteomes for Class I or Class II methanogens are relatively stable. The calculated aH₂ values are compatible with reported measurements for habitats of methanogens ranging from highly reducing submarine hydrothermal systems to less reducing environments including methanogenic sediments. In contrast to the transition between the two classes of methanogenic archaea, that between basal and terrestrial groups of Thaumarchaeota (denoting the origin of ammonia-oxidizing archaea) occurs at a less-reducing redox boundary. These examples reveal the consequences of energy minimization driving evolution and show how geochemical calculations involving biomolecules can be used to quantify and better understand the coevolution of the geosphere and biosphere.     

Dominance of Methanomicrobium phylotype in methanogen population present in Murrah buffaloes (Bubalus bubalis)

Aims:  To study the diversity of rumen methanogens in Murrah buffaloes ( Bubalus bubalis ) from North India by using 16S rRNA gene libraries obtained from the pooled rumen content from four animals and using suitable software analysis.
Methods and Results:  Genomic DNA was isolated and PCR was set up by using specific primers. Amplified product was cloned into a suitable vector and the positive clones were selected on the basis of blue–white screening and sequenced. The resulting nucleotide sequences were arranged in the phylogenetic tree. A total of 108 clones were examined, revealing 17 different 16S rRNA gene sequences or phylotypes. Of the 17 phylotypes, 15 (102 of 108 clones) belonged to the genus Methanomicrobium , indicating that the genus Methanomicrobium is the most dominant component of methanogen populations in Murrah buffaloes ( Bubalus bubalis ) from North India. The largest group of clones (102 clones) was more than 98% similar to Methanomicrobium mobile . BLAST analysis of the rumen contents from individual animals also revealed 17 different phylotypes with a range of 3–10 phylotypes per animal.
Conclusion:  Methanomicrobium phylotype is the most dominant phylotype of methanogens present in Murrah buffaloes ( Bubalus bubalis ).
Significance and Impact of the Study:  Effective strategies can be made to inhibit the growth of Methanomicrobium phylotype to reduce the methane emission from rumen contents and thus help in preventing global warming.     

Isolation of methanogens from Arabian sea sediments and their salt tolerance

Abstract Sea sediments in tropical regions have been less studied for methanogenesis and methanogens present therein. Three species of methanogens viz. Methanobacterium bryantii, Methanococcus voltae and Methanosarcina barkeri were isolated from Arabian sea sediments collected near the west coast of India. Maximum methane was formed by M. voltae at 3.0% (w/v) NaCl and other two methanogens at 0.06% (w/v) NaCl. M. bryantii and M. barkeri tolerated 2.5 and 3.0% (w/v) NaCl respectively due to which these methanogens must have survived in salt conditions of the sea sediments.     

Analysis of the methane production in thermophilic anaerobic reactors: use of autofluorescence microscopy

Methanogenic activity in thermophilic, anaerobic reactors was determined by comparing the amount of methane generated in single- and two-stage systems with the size of the methanogenic population, as determined by microscopy. The methanogenic activities were 2.71 × 10^–9 ml methane cell^–1 d^–1 and 1.10 × 10^–9 ml methane cell^–1 d^–1 for 10 and 4 days of the hydraulic retention time (HRT), in the single-stage system. In the two-stage system, 7.49 × 10^–9 ml methane cell^–1 d^–1 in the acidogenic reactor and 1.56 × 10^–9 ml methane cell^–1 d^–1 in the methanogenic reactor for 4 days of the HRT. A high correlation was evident between the methane production and methanogenic population [0.1354 ln(x) – 2.1375](R ² 0.8619).     

In situ stimulation of bacterial sulfate reduction in sulfate-limited freshwater lake sediments

Abstract By adding sulfate in the form of solid gypsum, it was possible to transform in situ a predominantly methanogenic sediment ecosystem into a sulfate-reducing one. The concentrations of sulfate, sulfide, methane, acetate, propionate, soluble iron, and manganese were determined in the porewater before and after the transition. Although sulfate was no longer limiting, acetate and propionate continued to accumulate and reached much higher concentrations than under sulfate-limited conditions. Metabolic activities of fermenting bacteria and of sulfate reducers, which belong to the group that incompletely oxidizes organic material, might be responsible for the increased production of volatile fatty acids. The elevated concentrations of soluble Fe(II)²⁺ and Mn(II)²⁺ observed in the porewater stem from iron and manganese compounds which may be reduced chemically by hydrogen sulfide and other microbially produced reducing agents or directly through increased activities of the iron and manganese reducing bacteria. In the horizon with high sulfate-reducing activities the methane concentrations in the porewater were lower than in non-stimulated sediment regions. The shape of the concentration depth profile indicates methane consumption through sulfate reducing processes. The in situ experiment demonstrates the response of a natural microbial ecosystem to fluctuations in the environmental conditions.