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Aerobic methanotrophic bacteria are capable of utilizing methane as their sole energy source. They are commonly found at the oxic/anoxic interfaces of environments such as wetlands, aquatic sediments, and landfills, where they feed on methane produced in anoxic zones of these environments. Until recently, all known species of aerobic methanotrophs belonged to the phylum Proteobacteria, in the classes Gammaproteobacteria and Alphaproteobacteria. However, in 2007-2008 three research groups independently described the isolation of thermoacidophilic methanotrophs that represented a distinct lineage within the bacterial phylum Verrucomicrobia. Isolates were obtained from geothermal areas in Italy, New Zealand and Russia. They are by far the most acidophilic methanotrophs known, with a lower growth limit below pH 1. Here we summarize the properties of these novel methanotrophic Verrucomicrobia, compare them with the proteobacterial methanotrophs, propose a unified taxonomic framework for them and speculate on their potential environmental significance. New genomic and physiological data are combined with existing information to allow detailed comparison of the three strains. We propose the new genus Methylacidiphilum to encompass all three newly discovered bacteria.

Aerobic methanotrophic bacteria consume methane as it diffuses away from methanogenic zones of soil and sediment. They act as a biofilter to reduce methane emissions to the atmosphere, and they are therefore targets in strategies to combat global climate change. No cultured methanotroph grows optimally below pH 5, but some environments with active methane cycles are very acidic. Here we describe an extremely acidophilic methanotroph that grows optimally at pH 2.0-2.5. Unlike the known methanotrophs, it does not belong to the phylum Proteobacteria but rather to the Verrucomicrobia, a widespread and diverse bacterial phylum that primarily comprises uncultivated species with unknown genotypes. Analysis of its draft genome detected genes encoding particulate methane monooxygenase that were homologous to genes found in methanotrophic proteobacteria. However, known genetic modules for methanol and formaldehyde oxidation were incomplete or missing, suggesting that the bacterium uses some novel methylotrophic pathways. Phylogenetic analysis of its three pmoA genes (encoding a subunit of particulate methane monooxygenase) placed them into a distinct cluster from proteobacterial homologues. This indicates an ancient divergence of Verrucomicrobia and Proteobacteria methanotrophs rather than a recent horizontal gene transfer of methanotrophic ability. The findings show that methanotrophy in the Bacteria is more taxonomically, ecologically and genetically diverse than previously thought, and that previous studies have failed to assess the full diversity of methanotrophs in acidic environments.

Samples from diverse upland soils that oxidize atmospheric methane were characterized with regard to methane oxidation activity and the community composition of methanotrophic bacteria (MB). MB were identified on the basis of the detection and comparative sequence analysis of the pmoA gene, which encodes a subunit of particulate methane monooxygenase. MB commonly detected in soils were closely related to Methylocaldum spp., Methylosinus spp., Methylocystis spp., or the "forest sequence cluster" (USC ␣), which has previously been detected in upland soils and is related to pmoA sequences of type II MB (Alphaproteobacteria). As well, a novel group of sequences distantly related (<75% derived amino acid identity) to those of known type I MB (Gammaproteobacteria) was often detected. This novel "upland soil cluster ␥" (USC ␥) was significantly more likely to be detected in soils with pH values of greater than 6.0 than in more acidic soils. To identify active MB, four selected soils were incubated with 13 CH 4 at low mixing ratios (<50 ppm of volume), and extracted methylated phospholipid fatty acids (PLFAs) were analyzed by gas chromatography-online combustion isotope ratio mass spectrometry. Incorporation of 13 C into PLFAs characteristic for methanotrophic Gammaproteobacteria was observed in all soils in which USC ␥ sequences were detected, suggesting that the bacteria possessing these sequences were active methanotrophs. A pattern of labeled PLFAs typical for methanotrophic Alphaproteobacteria was obtained for a sample in which only USC ␣ sequences were detected. The data indicate that different MB are present and active in different soils that oxidize atmospheric methane.Methane (CH 4 ) is present in the atmosphere at a mixing ratio of about 1.7 ppm of volume (ppmv). An estimated 30 Tg of CH 4 from the atmosphere year Ϫ1 is oxidized by aerobic methanotrophic bacteria (MB) in upland soils, accounting for about 6% of the global atmospheric CH 4 sink (21, 31). Bender and Conrad (2) suggested that MB active in upland soils are specialized oligotrophs adapted to the trace level of atmospheric CH 4 and possess a methane monooxygenase (MMO) with a higher substrate affinity than that of cultivated MB. It was later demonstrated that the application of single-reactant Michaelis-Menten kinetics to MMO is not always appropriate and that the apparent affinity for CH 4 varies depending on the cultivation conditions (13). Nevertheless, recent studies indicate that MB in at least some soils that oxidize atmospheric CH 4 are indeed taxonomically distinct from known MB (28).The 13 recognized genera of MB are divided into two groups, type I (further divided into types I and X) and type II. These differ in phylogenetic affiliation (Gammaproteobacteria versus Alphaproteobacteria) and in diverse biochemical characteristics (21). Identification of MB in soils is often performed by the cultivation-independent detection of a fragment of pmoA, a gene encoding the active-site subunit of particulate MMO (22,26,30,35,38). This marker gene is ...

Over 200 years ago Alexander von Humboldt (1808) observed that plant and animal diversity peaks at tropical latitudes and decreases toward the poles, a trend he attributed to more favorable temperatures in the tropics. Studies to date suggest that this temperature-diversity gradient is weak or nonexistent for Bacteria and Archaea. To test the impacts of temperature as well as pH on bacterial and archaeal diversity, we performed pyrotag sequencing of 16S rRNA genes retrieved from 165 soil, sediment and biomat samples of 36 geothermal areas in Canada and New Zealand, covering a temperature range of 7.5-99 1C and a pH range of 1.8-9.0. This represents the widest ranges of temperature and pH yet examined in a single microbial diversity study. Species richness and diversity indices were strongly correlated to temperature, with R 2 values up to 0.62 for neutralalkaline springs. The distributions were unimodal, with peak diversity at 24 1C and decreasing diversity at higher and lower temperature extremes. There was also a significant pH effect on diversity; however, in contrast to previous studies of soil microbial diversity, pH explained less of the variability (13-20%) than temperature in the geothermal samples. No correlation was observed between diversity values and latitude from the equator, and we therefore infer a direct temperature effect in our data set. These results demonstrate that temperature exerts a strong control on microbial diversity when considered over most of the temperature range within which life is possible.

All aerobic methanotrophic bacteria described to date are unable to grow on substrates containing carboncarbon bonds. Here we demonstrate that members of the recently discovered genus Methylocella are an exception to this. These bacteria are able to use as their sole energy source the one-carbon compounds methane and methanol, as well as the multicarbon compounds acetate, pyruvate, succinate, malate, and ethanol. To conclusively verify facultative growth, acetate and methane were used as model substrates in growth experiments with the type strain Methylocella silvestris BL2. Quantitative real-time PCR targeting the mmoX gene, which encodes a subunit of soluble methane monooxygenase, showed that copies of this gene increased in parallel with cell counts during growth on either acetate or methane as the sole substrate. This verified that cells possessing the genetic basis of methane oxidation grew on acetate as well as methane. Cloning of 16S rRNA genes and fluorescence in situ hybridization with strain-specific and genus-specific oligonucleotide probes detected no contaminants in cultures. The growth rate and carbon conversion efficiency were higher on acetate than on methane, and when both substrates were provided in excess, acetate was preferably used and methane oxidation was shut down. Our data demonstrate that not all methanotrophic bacteria are limited to growing on one-carbon compounds. This could have major implications for understanding the factors controlling methane fluxes in the environment.Aerobic methanotrophic bacteria occupy a key position in the global methane cycle. In aerobic interfaces of flooded soils and wetlands their activity limits potential methane efflux to the atmosphere, and in well-aerated upland soils they consume atmospheric methane directly (8, 25). The 11 described genera of methanotrophic bacteria include species with diverse environmental tolerances and biochemical properties, but one trait considered common to all is the inability to grow on substrates containing carbon-carbon bonds (5,18,20). Growth is limited to methane, methanol, and in some cases formate, formaldehyde, and methylamines (5). Experiments with 14 C-labeled substrates have shown that small amounts of some organic acids can also be assimilated during exponential growth on one-carbon substrates. However, this accounts for at most 5 to 10% of the total C assimilation, no energy is gained, and no growth occurs on these compounds alone (18).Recently, the new methanotrophic species Methylocella palustris (13, 14), Methylocella silvestris (17), and Methylocella tundrae (9) were isolated from acidic peat, forest, and tundra soils, respectively. Together with Methylocapsa acidiphila (12), these species form a distinct taxonomic cluster of acidophilic, methanotrophic bacteria. These belong to the Alphaproteobacteria (type II methanotrophs) but are not monophyletic with the previously known type II methanotrophs of the genera Methylosinus and Methylocystis. Instead, Methylocella species are closely related to the nonmeth...

BackgroundThe phylum Verrucomicrobia is a widespread but poorly characterized bacterial clade. Although cultivation-independent approaches detect representatives of this phylum in a wide range of environments, including soils, seawater, hot springs and human gastrointestinal tract, only few have been isolated in pure culture. We have recently reported cultivation and initial characterization of an extremely acidophilic methanotrophic member of the Verrucomicrobia, strain V4, isolated from the Hell's Gate geothermal area in New Zealand. Similar organisms were independently isolated from geothermal systems in Italy and Russia.ResultsWe report the complete genome sequence of strain V4, the first one from a representative of the Verrucomicrobia. Isolate V4, initially named "Methylokorus infernorum" (and recently renamed Methylacidiphilum infernorum) is an autotrophic bacterium with a streamlined genome of ~2.3 Mbp that encodes simple signal transduction pathways and has a limited potential for regulation of gene expression. Central metabolism of M. infernorum was reconstructed almost completely and revealed highly interconnected pathways of autotrophic central metabolism and modifications of C1-utilization pathways compared to other known methylotrophs. The M. infernorum genome does not encode tubulin, which was previously discovered in bacteria of the genus Prosthecobacter, or close homologs of any other signature eukaryotic proteins. Phylogenetic analysis of ribosomal proteins and RNA polymerase subunits unequivocally supports grouping Planctomycetes, Verrucomicrobia and Chlamydiae into a single clade, the PVC superphylum, despite dramatically different gene content in members of these three groups. Comparative-genomic analysis suggests that evolution of the M. infernorum lineage involved extensive horizontal gene exchange with a variety of bacteria. The genome of M. infernorum shows apparent adaptations for existence under extremely acidic conditions including a major upward shift in the isoelectric points of proteins.ConclusionThe results of genome analysis of M. infernorum support the monophyly of the PVC superphylum. M. infernorum possesses a streamlined genome but seems to have acquired numerous genes including those for enzymes of methylotrophic pathways via horizontal gene transfer, in particular, from Proteobacteria.ReviewersThis article was reviewed by John A. Fuerst, Ludmila Chistoserdova, and Radhey S. Gupta.

The activity and abundance of methanotrophic bacteria were measured in an acidic and a neutral forest soil. The soils exhibited high uptake rates (>30 microg CH4 m(-2) h(-1)) of atmospheric CH4 at all measurement times throughout the vegetation period. The abundances of various phylogenetic groups of methanotrophs, including some uncultured putative ones, were measured using real-time polymerase chain reaction assays. Each assay specifically targeted the pmoA gene or mmoX gene of a particular group of methanotrophs, or the amoA gene of ammonia-oxidizing bacteria. As yet uncultured methanotrophs of a group previously named 'forest soil cluster' or 'USC alpha' were numerically dominant in the acidic soil, while cultured but taxonomically uncharacterized methanotrophs of a group 'Cluster I' were dominant in the neutral soil. Each group was detected in numbers equivalent to about 10(6) pmoA gene copies per gram dry weight of soil and comprised >90% of the detectable methanotrophic bacteria in the respective soil. As the numbers of ammonia-oxidizing bacteria were similar but not higher, they could not have accounted for the observed CH4 uptake rates due to their low cell-specific CH4 oxidation activity. Based on CH4 flux and bacterial abundance data, estimated cell-specific CH4 oxidation rates of the detected methanotrophic bacteria were 540-800 x 10(-18) mol cell(-1) h(-1), which is high compared with literature values of cultured methanotrophic bacteria. These estimated cell-specific CH4 oxidation rates are sufficiently high to allow not only maintenance but even growth on atmospheric CH4 alone. Transcripts of mRNA of the pmoA gene were detected in the acidic soil, demonstrating that USC alpha methanotrophs expressed pmoA under ambient methane mixing ratios. On the other hand, pmoA transcripts of Cluster I or of other methanotrophic groups were not detectable. Our study suggests that USC alpha and Cluster I methanotrophs are adapted to the low concentration of methane in forest soils by possessing high cell-specific CH4 oxidation activities.