Detection of methane and quantification of methanogenic archaea in faeces from young broiler chickens using real-time PCR

AIMS: To detect the presence of methanogens in the faeces of broiler chicks during the first 2 weeks of age. METHODS AND RESULTS: Chicken faecal samples from 120 broiler chicks were incubated for methane gas formation and methanogenic archaea were analysed using real-time PCR. The copy number of the order Methanobacteriales 16S rDNA gene in chicken faeces when the broilers were 3-12 days of age, litter and house flies collected in the bird house ranged from 4.19 to 5.51 log(10) g(-1) wet weight. The number of positive methane culture tubes increased from 25% to 100% as the birds aged. CONCLUSIONS: Methanogens were successfully detected in faecal samples from 3- to 12-day-old broilers, as well as litter and house flies using real-time PCR. The copy number of methanogenic 16S rDNA gene in these samples was also similar to the number observed in litter and house flies. SIGNIFICANCE AND IMPACT OF THE STUDY: The same methanogens consistently appeared in chicken faeces a few days after birth. Detection of the methanogenic bacteria in litter and house flies implicated them as potential environmental sources for methanogen colonization in broiler chicks.     

Succession of methanogenic archaea in rice straw incorporated into a Japanese rice field: estimation by PCR-DGGE and sequence analyses

The succession and phylogenetic profiles of methanogenic archaeal communities associated with rice straw decomposition in rice-field soil were studied by polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE) analysis followed by 16S rDNA sequencing. Nylon bags containing either leaf sheaths or blades were buried in the plowed layer of a Japanese rice field under drained conditions during the off-crop season and under flooded conditions after transplanting. In addition, rice straw samples that had been buried in the rice field under drained conditions during the off-crop season were temporarily removed during spring plowing and then re-buried in the same rice field under flooded conditions at transplanting. Populations of methanogenic archaea were examined by amplification of the 16S rRNA genes in the DNA extracted from the rice straw samples. No PCR product was produced for samples of leaf sheath or blade prior to burial or after burial under drained conditions, indicating that the methanogen population was very small during decomposition of rice straw under oxic conditions. Many common bands were observed in rice straw samples of leaf sheath and blade during decomposition of rice straw under flooded conditions. Cluster analysis based on DGGE patterns divided methanogenic archaeal communities into two groups before and after the mid-season drainage. Sequence analysis of DGGE bands that were commonly present were closely related to Methanomicrobiales and Rice cluster I. Methanomicrobiales, Rice cluster I and Methanosarcinales were major members before the mid-season drainage, whereas the DGGE bands that characterized methanogenic archaeal communities after the mid-season drainage were closely related to Methanomicrobiales. These results indicate that mid-season drainage affected the methanogenic archaeal communities irrespective of their location on rice straw (sheath and blade) and the previous history of decomposition during the off-crop season.     

Ecophysiology of syntrophic communities that degrade saturated and unsaturated long-chain fatty acids

Syntrophic relationships are the key for biodegradation in methanogenic environments. We review the ecological and physiological features of syntrophic communities involved in the degradation of saturated and unsaturated long-chain fatty acids (LCFA), as well as their potential application to convert lipids/fats containing waste to biogas. Presently, about 14 species have been described with the ability to grow on fatty acids in syntrophy with methanogens, all belonging to the families Syntrophomonadaceae and Syntrophaceae . The principle pathway of LCFA degradation is through β-oxidation, but the initial steps in the conversion of unsaturated LCFA are unclear. Communities enriched on unsaturated LCFA also degrade saturated LCFA, but the opposite generally is not the case. For efficient methane formation, the physical and inhibitory effects of LCFA on methanogenesis need to be considered. LCFA adsorbs strongly to biomass, which causes encapsulation of active syntrophic communities and hampers diffusion of substrate and products in and out of the biomass. Quantification of archaea by real-time PCR analysis suggests that potential LCFA inhibitory effect towards methanogens might be reversible. Rather, the conversion of adsorbed LCFA in batch assays was shown to result in a significant increase of archaeal cell numbers in anaerobic sludge samples.     

获取有机物厌氧降解产甲烷过程中关键功能类群——互营细菌培养物

互营代谢是微生物之间的重要种间互作关系之一,参与互营代谢的微生物广泛存在于土壤、淡水和海水沉积物、厌氧消化反应器、动物肠道和极端环境中(如地下油藏),在有机物厌氧降解转化为二氧化碳和甲烷的过程中发挥着关键性的作用。研究互营细菌的物质代谢和能量传递的分子机制,对认识缺氧环境中的元素生物地球化学循环具有重要意义,也为解决全球能源危机、缓解气候变暖提供理论指导。但是,互营细菌生长缓慢、对氧气敏感,其分离培养的难度大。本文主要回顾了互营细菌的分离策略及其生理生化特征,展望了互营细菌分离培养的发展趋势,并指出以高通量筛选与定向分离相结合的方法,获得具有特定生理生态学功能的互营细菌,是互营微生物资源和分类学研究的发展方向。     

Monitoring growth of the methanogenic archaea Methanobacterium formicicum using an electronic nose

Growth of the methanogenic archaea, Methanobacterium formicicum, in pure culture was monitored by analysing samples from the gas phase with an array of chemical gas sensors (an `electronic nose'). Analyses of the methane and protein formation rates were used as independent parameters of growth, and the data obtained from the electronic nose were evaluated using principal component analysis (PCA). We found that different growth phases can be distinguished with the electronic nose followed by PCA evaluation. The fast response of the sensors in combination with the high correlations with other parameters measuring growth show that the electronic nose can be a useful tool to rapidly determine methanogenic growth.     

Rumen microbial diversity in Svalbard reindeer, with particular emphasis on methanogenic archaea

Ruminal methanogens, bacteria and ciliate protozoa of Svalbard reindeer grazing natural pastures in October (late fall) and April (late winter) were investigated using molecular-based approaches. The appetite of the Svalbard reindeer peaks in August (summer) and is at its lowest in March (winter). Microbial numbers, quantified by real-time PCR, did not change significantly between October and April, when food intakes are at similar levels, although the numbers of methanogens tended to be higher in October ( P =0.074), and ciliate numbers tended to be higher in April ( P= 0.055). Similarly, no change was detected in the bacterial and protozoal population composition by rRNA gene-based denaturing gradient gel electrophoresis analysis. Dominant methanogens were identified using a 16S rRNA gene library (97 clones) prepared from pooled PCR products from reindeer on October pasture ( n =5). Eleven of the 22 distinct operational taxonomic units (OTUs) generated exhibited a high degree of sequence similarity to methanogens affiliated with Methanobacteriales (eight OTUs), Methanomicrobiales (one OTU) and Methanosarcinales (two OTUs). The remaining 11 OTUs (53% of the clones) were associated with a cluster of uncultivated ruminal archaea. This study has provided important insights into the rumen microbiome of a high-arctic herbivorous animal living under harsh nutritional conditions, and evidence suggesting that host type affects the population size of ruminal methanogens.     

Pathways of energy conservation in methanogenic archaea

Methanogenic archaea are strictly anaerobic organisms that derive their metabolic energy from the conversion of a restricted number of substrates to methane. H₂+CO₂ and formate are converted to CH₄ via the CO₂-reducing pathway, while methanol and methylamines are metabolized by the methylotrophic pathway. A limited number of methanogenic organisms utilize acetate by the aceticlastic pathway. Redox reactions involved in these processes are partly catalyzed by membrane-bound enzyme systems that generate or, in the case of endergonic reactions, use electrochemical ion gradients. The H₂:heterodisulfide oxidoreductase, the F₄₂₀H₂:heterodisulfide oxidoreductase and the CO:heterodisulfide oxidoreductase, are novel systems that generate a proton motive force by redox-potential-driven H⁺ translocation. The methyltetrahydromethanopterin:coenzyme M methyltransferase is a unique, reversible sodium ion pump that couples methyl transfer with the transport of Na⁺ across the cytoplasmic membrane. Formylmethanofuran dehydrogenase is a reversible ion pump that catalyzes formylation and deformylation, of methanofuran. In summary, the pathways are coupled to the generation of an electrochemical sodium ion gradient and an electrochemical proton gradient. Both ion gradients are used directly for ATP synthesis via membrane integral ATP synthases. The function of the above-mentioned systems and their components in the metabolism of methanogens are described in detail.Abbreviations DCCD N,N dicyclohexylcarbodiimide - F ₄₂₀ (N-l-Lactyl--l-glutamyl)-l-glutamic acid phosphodiester of 7,8 didemethyl-8-hydroxy-5-deazariboflavin-5-phosphate - H ₄MPT Tetrahydromethanopterin - HS-CoM 2-Mercaptoethanesulfonate - HS-HTP 7-Mercaptoheptanoyl-O-phospho-l-threonine - MF Methanofuran - Ms Methanosarcina - Mc Methanococcus - Mb Methanobacterium - SF 6847 3,5-Di-tert-butyl-4-hydroxybenzylidene-malononitrile - Electrochemical sodium ion gradient - Electrochemical proton gradient     

产甲烷古菌中CRISPR簇的研究

【目的】通过对51个产甲烷古菌基因组中成簇的规律间隔短回文重复序列(Clustered regularly interspaced short palindromic repeats,CRISPR)的组成和来源进行研究,推测产甲烷古菌与环境中其他微生物的物质交换和相互作用,在基因组水平上阐述产甲烷古菌之间的遗传差异。【方法】利用CRISPRdb和CRISPRFinder,找出产甲烷古菌基因组中所有潜在的CRISPR簇。对CRISPR簇的基本组成部分进行分析:利用BLASTCLUST对重复序列(Repeat)进行分类;分别将间隔序列(Spacer)与Refseq病毒基因组、Refseq质粒基因组和Refseq产甲烷古菌基因组进行比对,从而获得间隔序列的物种来源和功能信息的注释。【结果】在51个产甲烷古菌中共找到了196个CRISPR簇,这些CRISPR簇中包含了总共4 355条间隔序列。在这些产甲烷古菌中,CRISPR簇的分布是不均匀的,且每个物种的间隔序列数量与其CRISPR簇数量是不成正比的。在对重复序列进行分类之后,发现Mclu1是分布最广且最具代表性的一类重复序列。在4 355条间隔序列中有388条具有物种注释信息,266条具有功能注释信息。从CRISPR簇间隔序列的来源来看,产甲烷古菌曾受到来自Poxiviridae、Siphoviridae以及Myoviridae属病毒的攻击,并且产甲烷古菌之间存在比较广泛的遗传物质交换。【结论】产甲烷古菌基因组中的CRISPR簇在组成和来源上存在较大的差异,这些差异与它们的生存环境有较大的关系。从CRISPR簇的角度阐述了产甲烷古菌之间基因组序列的差异。     

Simulating the contribution of coaggregation to interspecies hydrogen fluxes in syntrophic methanogenic consortia

A simple model (termed the syntrophy model) for simulating the contribution of coaggregation to interspecies hydrogen fluxes between syntrophic bacteria and methanogenic archaea is described. We applied it to analyzing partially aggregated syntrophic cocultures with various substrates, revealing that large fractions of hydrogen molecules were fluxed in aggregates.     

Biogeochemistry of methane and methanogenic archaea in permafrost

This study summarizes the findings of our research on the genesis of methane, its content and distribution in permafrost horizons of different age and origin. Supported by reliable data from a broad geographical sweep, these findings confirm the presence of methane in permanently frozen fine-grained sediments. In contrast to the omnipresence of carbon dioxide in permafrost, methane-containing horizons (up to 40.0 mL kg(-1)) alternate with strata free of methane. Discrete methane-containing horizons representing over tens of thousands of years are indicative of the absence of methane diffusion through the frozen layers. Along with the isotopic composition of CH(4) carbon (delta(13)C -64 per thousand to -99 per thousand), this confirms its biological origin and points to in situ formation of this biogenic gas. Using (14)C-labeled substrates, the possibility of methane formation within permafrost was experimentally shown, as confirmed by delta(13)C values. Extremely low values (near -99 per thousand) indicate that the process of CH(4) formation is accompanied by the substantial fractionation of carbon isotopes. For the first time, cultures of methane-forming archaea, Methanosarcina mazei strain JL01 VKM B-2370, Methanobacterium sp. strain M2 VKM B-2371 and Methanobacterium sp. strain MK4 VKM B-2440 from permafrost, were isolated and described.     

Phylogenetic diversity of methanogenic archaea in swine waste storage pits

Total DNA was isolated from swine feces and a swine waste storage pit and used as templates for PCR amplification of archaeal 16 rDNA using specific primers. Only the sample from the center of the waste pit produced a PCR product. DNA sequence analyses of random clones demonstrated a variety of methanogenic archaea. Six groups of sequences were identified, including those similar to Methanobrevibacter sp., Methanocorpusculum sp., and Methanoculleus sp. Three groups of sequences represented unidentified organisms. These data suggest that swine waste storage pits may represent an untapped source of novel methanogenic archaea.     

Fermentation of isoleucine and arginine by pure and syntrophic cultures of Clostridium sporogenes

Abstract The fermentation of isoleucine, arginine and isoleucine + arginine by pure and syntrophic cultures of Clostridium sporogenes was investigated. Growth of C. sporogenes on isoleucine, if any, was poor, but some isoleucine was fermented to 2-methylbutyrate and hydrogen. In syntrophic cultures with Methanobacterium formicicum or Methanosarcina barkeri growth was better, and isoleucine was completely fermented, the hydrogen being used for methane production. Pure cultures of C. sporogenes grew on arginine and produced 5-aminovalerate, ornithine and acetate. The reducing equivalents for 5-aminovalerate production from intermediarily formed proline were provided by oxidative conversion of arginine to acetate and by oxidative metabolism of some amino acids present in the yeast extract. However, when isoleucine was available together with arginine in syntrophic cultures of C. sporogenes and M. formicicum , the reducing equivalents for arginine fermentation came mainly from the oxidation of isoleucine (Stickland reaction), and the hydrogen produced in excess served for the reduction of CO₂ to methane.     

The microbiological basis of process control in methanogenic fermentation of soluble wastes

The essential requirement for anaerobic digestion of industrial wastes is that the process should operate reliably at high performance. In the digestion of dilute, soluble wastes it is necessary to retain the active biomass within the digester at short liquid retention times for the process to be economically feasible and this is reflected in digester design. Performance of digesters can only be assessed by interpretation of measurable parameters such as pH₂, E_h, pH, volatile fatty acid concentrations, temperature, gas production, biomass content and feed rate and composition. The effects of changes in these parameters on the microbiology of methanogenic digestion and the application of this knowledge in control of the process is discussed.     

Cultivation of syntrophic anaerobic bacteria in membrane-separated culture devices

A dialysis culture device was used for growth of syntrophic fatty acid-oxidizing and ethanol-oxidizing anaerobic bacteria. A pure culture of the fatty acid oxidizer Clostridium bryantii was grown inside dialysis tubing which was surrounded by a pure culture of Desulfovibrio vulgaris. The same apparatus was used for the syntrophic cultivation of Pelobacter acetylenicus and Acetobacterium woodii with ethanol as substrate. In both cases, substrate degradation and product formation were about half as fast as with the homogeneously mixed control cultures. In the compartment of the hydrogen producer, the concentration of free hydrogen during syntrophic ethanol degradation was about 10 times as high as in that of the hydrogen utilizer, whereas the homogeneously mixed culture exhibited an intermediate hydrogen partial pressure.     

Microdistribution of sulfate-reducing bacteria in sediments of a hypertrophic lake and their response to the addition of organic matter

To clarify the ecological significance of the association of sulfate-reducing bacteria (SRB) with sediment particle size, SRB utilizing lactate (l-SRB), propionate (p-SRB) and acetate (a-SRB) were examined with different sizes of sediment particles in a hypertrophic freshwater lake using the anaerobic plate count method. The numbers ofl-SRB anda-SRB were 10⁴–10⁵ colony forming units (CFU) per ml in the 0–3 cm layer and 10²–10³ CFU ml⁻¹ in the 10–13 cm layer while the numbers ofp-SRB were one or two orders lower than those ofl-SRB anda-SRB. A sediment suspension was fractionated into four fractions (<1, 1–10, 10–94 and >94 μm). The highest proportions ofl-SRB anda-SRB were found in the 10–94 μm fraction: 66–97% forl-SRB and 53–98% fora-SRB. The highest proportion ofp-SRB was found in the >94 μm fraction (70–74%). These results indicate that most SRB were associated with sediment particles. One isolate from an acetate-utilizing enrichment culture was similar toDesulfotomaculum acetoxidans, a spore-forming sulfate-reducing bacterium. When lactate and sulfate were added to sediment samples,l-SRB anda-SRB in the <10 μm-fraction grew more rapidly than those in whole sediment for the first 2 days. This result suggests that nutrients uptake by free-living and small particle-associated (<10 μm) SRB is higher than that by SRB associated with larger particles.     

Distribution of cytochromes in methanogenic bacteria

Abstract Various methanogenic bacteria belonging to the orders Methanobacteriales, Methanococcales , and Methanomicrobiales were examined for the presence of cytochromes. Those methanogens which are capable of growing only on H ₂+ CO ₂ or formate were found to lack cytochromes. However, membrane-bound cytochromes were detected in species able to utilize methanol, methylamines or acetate.