Diversity and enrichment of nitrite-dependent anaerobic methane oxidizing bacteria from wastewater sludge

Recently discovered microorganisms affiliated to the bacterial phylum NC10, named "Candidatus Methylomirabilis oxyfera", perform nitrite-dependent anaerobic methane oxidation. These microorganisms could be important players in a novel way of anaerobic wastewater treatment where ammonium and residual dissolved methane might be removed at the expense of nitrate or nitrite. To find suitable inocula for reactor startup, ten selected wastewater treatment plants (WWTPs) located in The Netherlands were screened for the endogenous presence of M. oxyfera using molecular diagnostic methods. We could identify NC10 bacteria with 98% similarity to M. oxyfera in nine out of ten WWTPs tested. Sludge from one selected WWTP was used to start a new enrichment culture of NC10 bacteria. This enrichment was monitored using specific pmoA primers and M. oxyfera cells were visualized with fluorescence oligonucleotide probes. After 112 days, the enrichment consumed up to 0.4 mM NO(2)(-) per day. The results of this study show that appropriate sources of biomass, enrichment strategies, and diagnostic tools existed to start and monitor pilot scale tests for the implementation of nitrite-dependent methane oxidation in wastewater treatment at ambient temperature.     

自然生境中亚硝酸盐型厌氧甲烷氧化细菌研究进展

随着功能微生物介导的亚硝酸盐型厌氧甲烷氧化(nitrite-dependent anaerobic methane oxidation,N-DAMO)过程被发现,人们对自然界的碳氮循环有了全新的认识,该过程成为自然生态系统中温室气体甲烷的汇,同时还是氮污染的消减途径。本文系统介绍了N-DAMO过程反应机理以及参与该过程的亚硝酸盐型厌氧甲烷氧化细菌(Candidatus Methylomirabilis oxyfera)的生理生化特征,并对研究该功能菌的分子微生物方法进行了汇总。通过对不同自然生境中该细菌的研究报道进行总结分析,揭示各生境中年均降水量、年均温度、所处不同自然区等大尺度宏观环境因子及碳源、氮源、pH和氧气含量等生存因子对其群落结构的潜在影响,最后在展望中提出此功能菌在未来可深入研究的方向,期望能厘清厌氧甲烷氧化过程及其功能菌在碳、氮循环中的生态学功能。     

Non-linear dynamics of carbon and hydrogen isotopic signatures based on a biological kinetic model of nitrite-dependent methane oxidation by “Candidatus Methylomirabilis oxyfera”

System dynamics of nitrite-dependent anaerobic methane oxidation (N-DAMO) in a “Candidatus Methylomirabilis oxyfera” culture are described using a mathematical model based on chemical kinetics, microbial growth dynamics and equations for ¹³C and ²H isotopic fractionation. Experimental data for the N-DAMO model were taken from Rasigraf et al. (2012), who studied N-DAMO in a batch culture of “Ca. M. oxyfera” started at two different conditions with varying methane, nitrite and biomass concentrations. In the model, instead of using concentrations of each isotopologue (¹²C and ¹³C, ¹H and ²H), total concentrations and respective isotope ratios were considered as variables. The empirical Monod equations, which included methane and nitrite as two rate-limiting substrates, a threshold methane concentration CH _4min below which there was no biomass growth, and the same kinetic coefficients for the separate batch experiments, fitted the experimental data much better than apparent first-order kinetics that required rather different kinetic coefficients for the two experiments. Non-linear dynamics of ¹³C and ²H isotopic signatures were obtained based on the N-DAMO model. It was shown that rate limitation by methane or nitrite concentrations significantly affected the dynamics of carbon and hydrogen isotopic signatures. Fractionation rate increased at higher initial biomass concentration. The non-linear N-DAMO model satisfactorily described experimental data presented in the two-dimensional plot of hydrogen versus carbon stable isotopic signatures.     

稻田土壤亚硝酸盐型甲烷厌氧氧化菌群落结构的时空特征

稻田是温室气体甲烷的重要排放源之一,对全球气候变化具有重要影响.由隶属于NC10门的Candidatus Methylomirabilis oxyfera(M.oxyfera)-like细菌介导的亚硝酸盐型甲烷厌氧氧化是控制稻田甲烷排放的新途径.目前,有关此类微生物群落在稻田土壤中的时空分布特征及其环境影响因素尚不明确...     

Ultrastructure of the denitrifying methanotroph "Candidatus Methylomirabilis oxyfera," a novel polygon-shaped bacterium

"Candidatus Methylomirabilis oxyfera" is a newly discovered denitrifying methanotroph that is unrelated to previously known methanotrophs. This bacterium is a member of the NC10 phylum and couples methane oxidation to denitrification through a newly discovered intra-aerobic pathway. In the present study, we report the first ultrastructural study of "Ca. Methylomirabilis oxyfera" using scanning electron microscopy, transmission electron microscopy, and electron tomography in combination with different sample preparation methods. We observed that "Ca. Methylomirabilis oxyfera" cells possess an atypical polygonal shape that is distinct from other bacterial shapes described so far. Also, an additional layer was observed as the outermost sheath, which might represent a (glyco)protein surface layer. Further, intracytoplasmic membranes, which are a common feature among proteobacterial methanotrophs, were never observed under the current growth conditions. Our results indicate that "Ca. Methylomirabilis oxyfera" is ultrastructurally distinct from other bacteria by its atypical cell shape and from the classical proteobacterial methanotrophs by its apparent lack of intracytoplasmic membranes.     

A new intra-aerobic metabolism in the nitrite-dependent anaerobic methane-oxidizing bacterium Candidatus 'Methylomirabilis oxyfera'

Biological methane oxidation proceeds either through aerobic or anaerobic pathways. The newly discovered bacterium Candidatus 'Methylomirabilis oxyfera' challenges this dichotomy. This bacterium performs anaerobic methane oxidation coupled to denitrification, but does so in a peculiar way. Instead of scavenging oxygen from the environment, like the aerobic methanotrophs, or driving methane oxidation by reverse methanogenesis, like the methanogenic archaea in sulfate-reducing systems, it produces its own supply of oxygen by metabolizing nitrite via nitric oxide into oxygen and dinitrogen gas. The intracellularly produced oxygen is then used for the oxidation of methane by the classical aerobic methane oxidation pathway involving methane mono-oxygenase. The present mini-review summarizes the current knowledge about this process and the micro-organism responsible for it.     

pmoA Primers for detection of anaerobic methanotrophs

Published pmoA primers do not match the pmoA sequence of "Candidatus Methylomirabilis oxyfera," a bacterium that performs nitrite-dependent anaerobic methane oxidation. Therefore, new pmoA primers for the detection of "Ca. Methylomirabilis oxyfera"-like methanotrophs were developed and successfully tested on freshwater samples from different habitats. These primers expand existing molecular tools for the study of methanotrophs in the environment.     

Existence of Novel Phylotypes of Nitrite-Dependent Anaerobic Methane-Oxidizing Bacteria in Surface and Subsurface Sediments of the South China Sea

Nitrite-dependent anaerobic methane oxidation (n-damo) is a recently discovered new microbial process performed by the Candidatus Methylomirabilis oxyfera with an unusual intra-aerobic pathway, but there is no report about n-damo bacteria in marine environments. M. oxyfera-like sequences were successfully retrieved for the first time from both surface and subsurface ocean sediments of the South China Sea (SCS) using both 16S rRNA and pmoA genes as biomarkers and PCR amplification in this study. The majority of M. oxyfera-like 16S rRNA gene-based PCR amplified sequences from the SCS sediments formed a new group distinctively different from those detected in freshwater habitats and the information is consistent phylogenetically with those obtained from the pmoA gene. This study showed the existence of n-damo in ocean sediments and suggests that marine sediments harbor n-damo phylotypes different from those in the freshwater. This finding here expands our understanding on the distribution of n-damo bacteria to marine ecosystem and implies their potential contribution to the marine C and N cycling.     

Gene expression analysis of the mechanism of inhibition of Desulfovibrio vulgaris Hildenborough by nitrate-reducing, sulfide-oxidizing bacteria

Sulfate-reducing bacteria (SRB) are inhibited by nitrate-reducing, sulfide-oxidizing bacteria (NR-SOB) in the presence of nitrate. This inhibition has been attributed either to an increase in redox potential or to production of nitrite by the NR-SOB. Nitrite specifically inhibits the final step in the sulfate reduction pathway. When the NR-SOB Thiomicrospira sp. strain CVO was added to mid-log phase cultures of the SRB Desulfovibrio vulgaris Hildenborough in the presence of nitrate, sulfate reduction was inhibited. Strain CVO reduced nitrate and oxidized sulfide, with transient production of nitrite. Sulfate reduction by D. vulgaris resumed once nitrite was depleted. A DNA macroarray with open reading frames encoding enzymes involved in energy metabolism of D. vulgaris was used to study the effects of NR-SOB on gene expression. Shortly following addition of strain CVO, D. vulgaris genes for cytochrome c nitrite reductase and hybrid cluster proteins Hcp1 and Hcp2 were upregulated. Genes for sulfate reduction enzymes, except those for dissimilatory sulfite reductase, were downregulated. Genes for the membrane-bound electron transferring complexes QmoABC and DsrMKJOP were downregulated and unaffected, respectively, whereas direct addition of nitrite downregulated both operons. Overall the gene expression response of D. vulgaris upon exposure to strain CVO and nitrate resembled that observed upon direct addition of nitrite, indicating that inhibition of SRB is primarily due to nitrite production by NR-SOB.     

Ammonium and Nitrite Inhibition of Methane Oxidation by Methylobacter albus BG8 and Methylosinus trichosporium OB3b at Low Methane Concentrations

Methane oxidation by pure cultures of the methanotrophs Methylobacter albus BG8 and Methylosinus trichosporium OB3b was inhibited by ammonium choride and sodium nitrite relative to that in cultures assayed in either nitrate-containing or nitrate-free medium. M. albus was generally more sensitive to ammonium and nitrite than M. trichosporium. Both species produced nitrite from ammonium; the concentrations of nitrite produced increased with increasing methane concentrations in the culture headspaces. Inhibition of methane oxidation by nitrite was inversely proportional to headspace methane concentrations, with only minimal effects observed at concentrations of>500 ppm in the presence of 250 μM nitrite. Inhibition increased with increasing ammonium at methane concentrations of 100 ppm. In the presence of 500 μM ammonium, inhibition increased initially with increasing methane concentrations from 1.7 to 100 ppm; the extent of inhibition decreased with methane concentrations of > 100 ppm. The results of this study provide new insights that explain some of the previously observed interactions among ammonium, nitrite, methane, and methane oxidation in soils and aquatic systems.     

Distribution of putative denitrifying methane oxidizing bacteria in sediment of a freshwater lake, Lake Biwa

Methane oxidation coupled to denitrification is mediated by 'Candidatus Methylomirabilis oxyfera', which belongs to the candidate phylum NC10. The distribution of putative denitrifying methane-oxidizing bacteria related to "M. oxyfera" was investigated in a freshwater lake, Lake Biwa, Japan. In the surface layer of the sediment from a profundal site, a phylotype closely related to "M. oxyfera" was most frequently detected among NC10 bacteria in PCR analysis of the 16S rRNA gene. In the sediment, sequences related to "M. oxyfera" were also detected in a pmoA gene library. The presence of NC10 bacteria was also confirmed by catalyzed reporter deposition fluorescence in situ hybridization (CARD-FISH). Denaturing gradient gel electrophoresis (DGGE) and quantitative real-time PCR indicated that the abundance of the "M. oxyfera"-related phylotype was higher in the upper layers of the profundal sediment. The horizontal distribution of the putative methanotrophs in lake sediment was also analyzed by DGGE, which revealed that their occurrence was restricted to deep water areas. These results agreed with those in a previous study of another freshwater lake, and suggested that the upper layer of the profundal sediments is the main habitat for denitrifying methanotrophs.     

Model of the molecular basis for hydroxylamine oxidation and nitrous oxide production in methanotrophic bacteria

Many methane-oxidizing bacteria (MOB) have been shown to aerobically oxidize ammonia and hydroxylamine (NH(2)OH) to produce nitrite and nitrous oxide (N(2)O). Genome sequences of alphaproteobacterial, gammaproteobacterial, and verrucomicrobial methanotrophs revealed the presence of haoAB, cytL, cytS, nirS or nirK, and norCB genes that may be responsible for N(2)O production, and additional haoAB genes were sequenced from two strains of Methylomicrobium album. The haoAB genes of M. album ATCC 33003 were inducible by ammonia and NH(2)OH, similar to haoAB induction by ammonia in Methylococcus capsulatus Bath. Increased expression of genes encoding nitric oxide reductase (cNOR; norCB) was measured upon exposure of M. capsulatus Bath to NaNO(2) and NO-releasing sodium nitroprusside. Only incubations of M. capsulatus Bath with methane, ammonia, and nitrite produced N(2)O. The data suggest a possible pathway of nitrite reduction to NO by reversely operating NH(2)OH oxidoreductase and NO reduction to N(2)O by cNOR independently or in conjunction with ammonia-induced enzymes (i.e. HAO or cytochrome c'-β). Results of this study show that MOB likely have diverse mechanisms for nitrogen oxide metabolism and detoxification of NH(2)OH that involve conventional and unconventional enzymes.     

Anaerobic methane oxidation potential and bacteria in freshwater lakes: Seasonal changes and the influence of trophic status

Nitrite-dependent anaerobic methane oxidation (n-damo), mainly carried out by n-damo bacteria, is an important pathway for mitigating methane emission from freshwater lakes. Although n-damo bacteria have been detected in a variety of freshwater lakes, their potential and distribution, and associated environmental factors, remain unclear. Therefore, the current study investigated the potential and distribution of anaerobic methanotrophs in sediments from Erhai Lake and Dianchi Lake, two adjacent freshwater lakes in the Yunnan Plateau with different trophic status. Both lakes showed active anaerobic methane oxidation potential and harbored a high density of n-damo bacteria. Based on the n-damo pmoA gene, sediment n-damo bacterial communities mainly consisted of Candidatus Methylomirabils oxyfera and Candidatus Methylomirabils sinica, as well as novel n-damo organisms. Sediment anaerobic methane oxidation potential and the n-damo bacterial community showed notable differences among seasons and between lakes. The environmental variables associated with lake trophic status (e.g. total nitrogen, ammonia nitrogen, nitrate nitrogen, and total organic carbon) might have significant impacts on the anaerobic methane oxidation potential, as well as the abundance and community structure of n-damo bacteria. Therefore, trophic status could determine the n-damo process in freshwater lake sediment.     

Methamphetamine Alters the Normal Progression by Inducing Cell Cycle Arrest in Astrocytes

Methamphetamine (MA) is a potent psychostimulant with a high addictive capacity, which induces many deleterious effects on the brain. Chronic MA abuse leads to cognitive dysfunction and motor impairment. MA affects many cells in the brain, but the effects on astrocytes of repeated MA exposure is not well understood. In this report, we used Gene chip array to analyze the changes in the gene expression profile of primary human astrocytes treated with MA for 3 days. Range of genes were found to be differentially regulated, with a large number of genes significantly downregulated, including NEK2, TTK, TOP2A, and CCNE2. Gene ontology and pathway analysis showed a highly significant clustering of genes involved in cell cycle progression and DNA replication. Further pathway analysis showed that the genes downregulated by multiple MA treatment were critical for G2/M phase progression and G1/S transition. Cell cycle analysis of SVG astrocytes showed a significant reduction in the percentage of cell in the G2/M phase with a concomitant increase in G1 percentage. This was consistent with the gene array and validation data, which showed that repeated MA treatment downregulated the genes associated with cell cycle regulation. This is a novel finding, which explains the effect of MA treatment on astrocytes and has clear implication in neuroinflammation among the drug abusers.     

Methane formation and oxidation by prokaryotes

The review deals with systematization and generalization of new information concerning the phylogenetic and functional diversity of prokaryotes involved in the methane cycle. Methane is mostly produced by methanogenic archaea, which are responsible for the terminal stage of organic matter decomposition in a number of anoxic ecotopes. Although phylogeny, physiology, and biochemistry of methanogens have been extensively studied, important discoveries were made recently. Thus, members of deep phylogenetic lineages within the Euryarchaeota phylum (Methanomassiliicoccales, “Candidatus Methanofastidiosa,” “Methanonatronarchaeia”) and even outside it (“Ca. Verstraetearchaeota” and “Ca. Bathyarchaeota”) were reported to carry out methyl-reducing methanogenesis. Moreover, evidence was obtained on aerobic methane production by marine heterotrophic bacteria, which demethylate polysaccharide esters of methylphosphonic acid. Methanotrophic microorganisms oxidize methane both aerobically and anaerobically, decreasing significantly the release of this greenhouse gas into the atmosphere. In the presence of oxygen methane is oxidized by methanotrophic members of Alpha- and Gammaproteobacteria, as well as by Verrucomicrobia. Methanotrophic gammaproteobacteria have been recently revealed in hypoxic and even anoxic environments, where they probably oxidize methane either in a trophic consortium with oxygenic phototrophs and/or methylotrophs or using electron acceptors other than oxygen. Anaerobic methane oxidation has been known for a long time. Sulfat- and nitrate-dependent anaerobic methane oxidation carried out by the ANME archaea via reverse methanogenesis are the best studied processes. While metal-dependent anaerobic methane oxidation is considered possible, the mechanisms and agents responsible for this process have not been reliably identified. Intracellular oxygen production during nitrite-dependent anaerobic methane oxidation was shown for bacteria “Ca. Methylomirabilis oxyfera.” These findings stimulate interest in the processes and microorganisms of the methane cycle.