A Novel Freshwater to Marine Evolutionary Transition Revealed within Methylophilaceae Bacteria from the Arctic Ocean.

Bacteria inhabiting polar oceans, particularly the Arctic Ocean, are less studied than those at lower latitudes. Discovering bacterial adaptations to Arctic Ocean conditions is essential for understanding responses to the accelerated environmental changes occurring in the North. The Methylophilaceae are emerging as a model for investigating the genomic basis of habitat adaptation, because related lineages are widely distributed across both freshwater and marine ecosystems. Here, we investigated Methylophilaceae diversity in the salinity-stratified surface waters of the Canada Basin, Arctic Ocean. In addition to a diversity of marine OM43 lineages, we report on the genomic characteristics and evolution of a previously undescribed Methylophilaceae clade (BS01) common to polar surface waters yet related to freshwater sediment Methylotenera species. BS01 is restricted to the lower-salinity surface waters, while OM43 is found throughout the halocline. An acidic proteome supports a marine lifestyle for BS01, but gene content shows increased metabolic versatility compared to OM43 and evidence for ongoing genome-streamlining. Phylogenetic reconstruction shows that BS01 colonized the pelagic ocean independently of OM43 via convergent evolution. Salinity adaptation and differences in one-carbon and nitrogen metabolism may play a role in niche differentiation between BS01 and OM43. In particular, urea utilization by BS01 is predicted to provide an ecological advantage over OM43 given the limited amount of inorganic nitrogen in the Canada Basin. These observations provide further evidence that the Arctic Ocean is inhabited by distinct bacterial groups and that at least one group (BS01) evolved via a freshwater to marine environmental transition. IMPORTANCE Global warming is profoundly influencing the Arctic Ocean. Rapid ice melt and increased freshwater input is increasing ocean stratification, driving shifts in nutrient availability and the primary production that supports marine food webs. Determining bacterial responses to Arctic Ocean change is challenging because of limited knowledge on the specific adaptations of Arctic Ocean bacteria. In this study, we investigated the diversity and genomic adaptations of a globally distributed group of marine bacteria, the Methylophilaceae, in the surface waters of the Arctic Ocean. We discovered a novel lineage of marine Methylophilaceae inhabiting the Arctic Ocean whose evolutionary origin involved a freshwater to marine environmental transition. Crossing the salinity barrier is thought to rarely occur in bacterial evolution. However, given the ongoing freshening of the Arctic Ocean, our results suggest that these relative newcomers to the ocean microbiome increase in abundance and, therefore, ecological significance in a near-future Arctic Ocean.

Methylotenera oryzisoli sp. nov., a lanthanide-dependent methylotrophic bacteria isolated from rice field soil.

A new lanthanide (Ln3+)-dependent methanol-utilizing bacterial strain, La3113T, was isolated from rice field soil and its taxonomic position was investigated using polyphasic approaches. The strain was aerobic, Gram-stain-negative, strongly motile, catalase-positive and cytochrome oxidase-positive. It could neither catalyse the hydrolysis of urea nor reduce nitrate to nitrite. Growth was observed within a temperature range of 10-40 °C and a pH range of 6-8, with optimum growth at 28 °C and pH 7. Methylamine was utilized as the single source of energy, carbon and nitrogen, and it was oxidized by methylamine dehydrogenase. C16 : 1 ω7c, C16 : 1 ω6c and C16 : 0 were the dominant cellular fatty acids. Its draft genome (2.67 Mbp and 44.9 mol% G+C content) encodes genes including three Ln3+-dependent methanol dehydrogenase (XoxF-type MDH) genes, those for formaldehyde assimilation (ribulose monophosphate pathway), formate dehydrogenases and methylamine dehydrogenases, but not Ca2+-dependent MDH (MxaFI-MDH), which characterizes the species as a Ln3+-dependent methylotroph. The 16S rRNA gene sequence showed that strain La3113T belongs to the genus Methylotenera and is closely related to Methylotenera mobilis JLW8T (98.29 % identity). The digital DNA-DNA hybridization (dDDH) values (less than 30 %) and average nucleotide identity (ANI) values (less than 85 %) between genomes of strain La3113T and related type strains were lower than the thresholds for species delineation (70 % for dDDH and 95-96 % for ANI). On the basis of these polyphasic approaches, we propose a novel Methylotenera species, Methylotenera oryzisoli sp. nov. (type strain La3113T=NBRC 111954T=DSM 103219T).

Pseudomethylobacillus aquaticus gen. nov., sp. nov., a new member of the family Methylophilaceae isolated from an artificial reservoir.

A bacterial strain, designated H-5T, was isolated from an artificial reservoir in Taiwan and characterized using a polyphasic taxonomic approach. Cells of strain H-5T were Gram-stain-negative, aerobic, motile by means of a single polar flagellum, rod-shaped, covered by large capsules and formed white colonies. Growth occurred at 15-30 °C (optimum, 25 °C), at pH 6-8 (optimum, pH 7) and with 0-0.5 % NaCl (optimum, 0 %). Phylogenetic analyses based on the 16S rRNA gene, the methanol dehydrogenase gene and the coding sequences of 92 protein clusters indicated that strain H-5T was affiliated with genera in the family Methylophilaceae in the class Betaproteobacteria. Strain H-5T was most closely related to Methylobacillus methanolivorans ZT with a 95.0 % 16S rRNA gene sequence similarity. Strain H-5T showed less than 73.7 % average nucleotide identity and less than 23.6 % digital DNA-DNA hybridization identity compared to the strains of related genera within the family Methylophilaceae. The predominant fatty acids were summed feature 3 (C16 : 1ω7c and/or C16 : 1ω6c) and C16 : 0. The major isoprenoid quinone was Q-8 and the DNA G+C content was 58.3 mol%. The major polar lipids were phosphatidylethanolamine, phosphatidylglycerol, one uncharacterized aminophospholipid, one uncharacterized phospholipid and one uncharacterized lipid. On the basis of the genotypic and phenotypic data presented here, strain H-5T represents a novel species of a new genus in the family Methylophilaceae, for which the name Pseudomethylobacillus aquaticus gen. nov., sp. nov. is proposed. The type strain is H-5T (=BCRC 81154T=KCTC 62865T).

Evolution in action: habitat transition from sediment to the pelagial leads to genome streamlining in Methylophilaceae.

The most abundant aquatic microbes are small in cell and genome size. Genome-streamlining theory predicts gene loss caused by evolutionary selection driven by environmental factors, favouring superior competitors for limiting resources. However, evolutionary histories of such abundant, genome-streamlined microbes remain largely unknown. Here we reconstruct the series of steps in the evolution of some of the most abundant genome-streamlined microbes in freshwaters ("Ca. Methylopumilus") and oceans (marine lineage OM43). A broad genomic spectrum is visible in the family Methylophilaceae (Betaproteobacteria), from sediment microbes with medium-sized genomes (2-3 Mbp genome size), an occasionally blooming pelagic intermediate (1.7 Mbp), and the most reduced pelagic forms (1.3 Mbp). We show that a habitat transition from freshwater sediment to the relatively oligotrophic pelagial was accompanied by progressive gene loss and adaptive gains. Gene loss has mainly affected functions not necessarily required or advantageous in the pelagial or is encoded by redundant pathways. Likewise, we identified genes providing adaptations to oligotrophic conditions that have been transmitted horizontally from pelagic freshwater microbes. Remarkably, the secondary transition from the pelagial of lakes to the oceans required only slight modifications, i.e., adaptations to higher salinity, gained via horizontal gene transfer from indigenous microbes. Our study provides first genomic evidence of genome reduction taking place during habitat transitions. In this regard, the family Methylophilaceae is an exceptional model for tracing the evolutionary history of genome streamlining as such a collection of evolutionarily related microbes from different habitats is rare in the microbial world.

Methylotrophs and Methylotroph Populations for Chloromethane Degradation.

Chloromethane is a halogenated volatile organic compound, produced in large quantities by terrestrial vegetation. After its release to the troposphere and transport to the stratosphere, its photolysis contributes to the degradation of stratospheric ozone. A better knowledge of chloromethane sources (production) and sinks (degradation) is a prerequisite to estimate its atmospheric budget in the context of global warming. The degradation of chloromethane by methylotrophic communities in terrestrial environments is a major underestimated chloromethane sink. Methylotrophs isolated from soils, marine environments and more recently from the phyllosphere have been grown under laboratory conditions using chloromethane as the sole carbon source. In addition to anaerobes that degrade chloromethane, the majority of cultivated strains were isolated in aerobiosis for their ability to use chloromethane as sole carbon and energy source. Among those, the Proteobacterium Methylobacterium (recently reclassified as Methylorubrum) harbours the only characterisized 'chloromethane utilization' (cmu) pathway, so far. This pathway is not representative of chloromethane-utilizing populations in the environment as cmu genes are rare in metagenomes. Recently, combined 'omics' biological approaches with chloromethane carbon and hydrogen stable isotope fractionation measurements in microcosms, indicated that microorganisms in soils and the phyllosphere (plant aerial parts) represent major sinks of chloromethane in contrast to more recently recognized microbe-inhabited environments, such as clouds. Cultivated chloromethane-degraders lacking the cmu genes display a singular isotope fractionation signature of chloromethane. Moreover, 13CH3Cl labelling of active methylotrophic communities by stable isotope probing in soils identify taxa that differ from the taxa known for chloromethane degradation. These observations suggest that new biomarkers for detecting active microbial chloromethane-utilizers in the environment are needed to assess the contribution of microorganisms to the global chloromethane cycle.

Isolation and genomic characterization of Novimethylophilus kurashikiensis gen. nov. sp. nov., a new lanthanide-dependent methylotrophic species of Methylophilaceae.

Recently, it has been found that two types of methanol dehydrogenases (MDHs) exist in Gram-negative bacterial methylotrophs, calcium-dependent MxaFI-MDH and lanthanide-dependent XoxF-MDH and the latter is more widespread in bacterial genomes. We aimed to isolate and characterize lanthanide-dependent methylotrophs. The growth of strain La2-4T on methanol, which was isolated from rice rhizosphere soil, was strictly lanthanide dependent. Its 16S rRNA gene sequence showed only 93.4% identity to that of Methylophilus luteus MimT , and the name Novimethylophilus kurashikiensis gen. nov. sp. nov. is proposed. Its draft genome (ca. 3.69 Mbp, G + C content 56.1 mol%) encodes 3579 putative CDSs and 84 tRNAs. The genome harbors five xoxFs but no mxaFI. XoxF4 was the major MDH in the cells grown on methanol and methylamine, evidenced by protein identification and quantitative PCR analysis. Methylamine dehydrogenase gene was absent in the La2-4T genome, while genes for the glutamate-mediated methylamine utilization pathway were detected. The genome also harbors those for the tetrahydromethanopterin and ribulose monophosphate pathways. Additionally, as known species, isolates of Burkholderia ambifaria, Cupriavidus necator and Dyadobacter endophyticus exhibited lanthanide dependent growth on methanol. Thus, lanthanide can be used as an essential growth factor for methylotrophic bacteria that do not harbor MxaFI-MDH.

Microbial megacities fueled by methane oxidation in a mineral spring cave.

Massive biofilms have been discovered in the cave of an iodine-rich former medicinal spring in southern Germany. The biofilms completely cover the walls and ceilings of the cave, giving rise to speculations about their metabolism. Here we report on first insights into the structure and function of the biofilm microbiota, combining geochemical, imaging and molecular analytics. Stable isotope analysis indicated that thermogenic methane emerging into the cave served as an important driver of biofilm formation. The undisturbed cavern atmosphere contained up to 3000 p.p.m. methane and was microoxic. A high abundance and diversity of aerobic methanotrophs primarily within the Methylococcales (Gammaproteobacteria) and methylotrophic Methylophilaceae (Betaproteobacteria) were found in the biofilms, along with a surprising diversity of associated heterotrophic bacteria. The highest methane oxidation potentials were measured for submerged biofilms on the cavern wall. Highly organized globular structures of the biofilm matrix were revealed by fluorescent lectin staining. We propose that the extracellular matrix served not only as an electron sink for nutrient-limited biofilm methylotrophs but potentially also as a diffusive barrier against volatilized iodine species. Possible links between carbon and iodine cycling in this peculiar habitat are discussed.

Comprehensive Genomic Analyses of the OM43 Clade, Including a Novel Species from the Red Sea, Indicate Ecotype Differentiation among Marine Methylotrophs.

The OM43 clade within the family Methylophilaceae of Betaproteobacteria represents a group of methylotrophs that play important roles in the metabolism of C1 compounds in marine environments and other aquatic environments around the globe. Using dilution-to-extinction cultivation techniques, we successfully isolated a novel species of this clade (here designated MBRS-H7) from the ultraoligotrophic open ocean waters of the central Red Sea. Phylogenomic analyses indicate that MBRS-H7 is a novel species that forms a distinct cluster together with isolate KB13 from Hawaii (Hawaii-Red Sea [H-RS] cluster) that is separate from the cluster represented by strain HTCC2181 (from the Oregon coast). Phylogenetic analyses using the robust 16S-23S internal transcribed spacer revealed a potential ecotype separation of the marine OM43 clade members, which was further confirmed by metagenomic fragment recruitment analyses that showed trends of higher abundance in low-chlorophyll and/or high-temperature provinces for the H-RS cluster but a preference for colder, highly productive waters for the HTCC2181 cluster. This potential environmentally driven niche differentiation is also reflected in the metabolic gene inventories, which in the case of the H-RS cluster include those conferring resistance to high levels of UV irradiation, temperature, and salinity. Interestingly, we also found different energy conservation modules between these OM43 subclades, namely, the existence of the NADH:quinone oxidoreductase complex I (NUO) system in the H-RS cluster and the nonhomologous NADH:quinone oxidoreductase (NQR) system in the HTCC2181 cluster, which might have implications for their overall energetic yields.

Emended Description of Methylovorus glucosotrophus Govorukhina and Trotsenko 1991.

Phylogeneticanalysis based,on comparison of the 16S rRNA gene sequences in combination with comparative analysis of physiological, biochemical, and chemotaxonomic characteristics and DNA-DNA hybridization revealed that "Methylobacillusfructoseoxidans" 34 (VKM B-1609 = DSM 5897 and-Methylov- orus glucosotrophus 6B 1T (ATCC 49758T = DSM 6874T = VKM B- 1745T = NCIMB 13222 ) belong to the same Methylovorus species. Extended description of the limited facultative methylotroph Methylovorus gluco- sotrophus is proposed, which includes the fructose-utilizing strain 34. Emended description of Methylovorus glucosotrophus is provided.

The ecology of pelagic freshwater methylotrophs assessed by a high-resolution monitoring and isolation campaign.

Methylotrophic planktonic bacteria fulfill a particular role in the carbon cycle of lakes via the turnover of single-carbon compounds. We studied two planktonic freshwater lineages (LD28 and PRD01a001B) affiliated with Methylophilaceae (Betaproteobacteria) in Lake Zurich, Switzerland, by a combination of molecular and cultivation-based approaches. Their spatio-temporal distribution was monitored at high resolution (n=992 samples) for 4 consecutive years. LD28 methylotrophs constituted up to 11 × 10(7) cells l(-1) with pronounced peaks in spring and autumn-winter, concomitant with blooms of primary producers. They were rare in the warm water layers during summer but abundant in the cold hypolimnion, hinting at psychrophilic growth. Members of the PRD01a001B lineage were generally less abundant but also had maxima in spring. More than 120 axenic strains from these so far uncultivated lineages were isolated from the pelagic zone by dilution to extinction. Phylogenetic analysis separated isolates into two distinct genotypes. Isolates grew slowly (µmax=0.4 d(-1)), were of conspicuously small size, and were indeed psychrophilic, with higher growth yield at low temperatures. Growth was enhanced upon addition of methanol and methylamine to sterile lake water. Genomic analyses of two strains confirmed a methylotrophic lifestyle with a reduced set of genes involved in C1 metabolism. The very small and streamlined genomes (1.36 and 1.75 Mb) shared several pathways with the marine OM43 lineage. As the closest described taxa (Methylotenera sp.) are only distantly related to either set of isolates, we propose a new genus with two species, that is, 'Candidatus Methylopumilus planktonicus' (LD28) and 'Candidatus Methylopumilus turicensis' (PRD01a001B).

Bacterial metabolism of methylated amines and identification of novel methylotrophs in Movile Cave.

Movile Cave, Romania, is an unusual underground ecosystem that has been sealed off from the outside world for several million years and is sustained by non-phototrophic carbon fixation. Methane and sulfur-oxidising bacteria are the main primary producers, supporting a complex food web that includes bacteria, fungi and cave-adapted invertebrates. A range of methylotrophic bacteria in Movile Cave grow on one-carbon compounds including methylated amines, which are produced via decomposition of organic-rich microbial mats. The role of methylated amines as a carbon and nitrogen source for bacteria in Movile Cave was investigated using a combination of cultivation studies and DNA stable isotope probing (DNA-SIP) using (13)C-monomethylamine (MMA). Two newly developed primer sets targeting the gene for gamma-glutamylmethylamide synthetase (gmaS), the first enzyme of the recently-discovered indirect MMA-oxidation pathway, were applied in functional gene probing. SIP experiments revealed that the obligate methylotroph Methylotenera mobilis is one of the dominant MMA utilisers in the cave. DNA-SIP experiments also showed that a new facultative methylotroph isolated in this study, Catellibacterium sp. LW-1 is probably one of the most active MMA utilisers in Movile Cave. Methylated amines were also used as a nitrogen source by a wide range of non-methylotrophic bacteria in Movile Cave. PCR-based screening of bacterial isolates suggested that the indirect MMA-oxidation pathway involving GMA and N-methylglutamate is widespread among both methylotrophic and non-methylotrophic MMA utilisers from the cave.

The expanded diversity of methylophilaceae from Lake Washington through cultivation and genomic sequencing of novel ecotypes.

We describe five novel Methylophilaceae ecotypes from a single ecological niche in Lake Washington, USA, and compare them to three previously described ecotypes, in terms of their phenotype and genome sequence divergence. Two of the ecotypes appear to represent novel genera within the Methylophilaceae. Genome-based metabolic reconstruction highlights metabolic versatility of Methylophilaceae with respect to methylotrophy and nitrogen metabolism, different ecotypes possessing different combinations of primary substrate oxidation systems (MxaFI-type methanol dehydrogenase versus XoxF-type methanol dehydrogenase; methylamine dehydrogenase versus N-methylglutamate pathway) and different potentials for denitrification (assimilatory versus respiratory nitrate reduction). By comparing pairs of closely related genomes, we uncover that site-specific recombination is the main means of genomic evolution and strain divergence, including lateral transfers of genes from both closely- and distantly related taxa. The new ecotypes and the new genomes contribute significantly to our understanding of the extent of genomic and metabolic diversity among organisms of the same family inhabiting the same ecological niche. These organisms also provide novel experimental models for studying the complexity and the function of the microbial communities active in methylotrophy.

Novel methylotrophic isolates from lake sediment, description of Methylotenera versatilis sp. nov. and emended description of the genus Methylotenera.

Phylogenetic positions, and genotypic and phenotypic characteristics of three novel methylotrophic isolates, strains 301(T), 30S and SIP3-4, from sediment of Lake Washington, Seattle, USA, are described. The strains were restricted facultative methylotrophs capable of growth on single carbon compounds (methylamine and methanol) in addition to a limited range of multicarbon compounds. All strains used the N-methylglutamate pathway for methylamine oxidation. Strain SIP3-4 possessed the canonical (MxaFI) methanol dehydrogenase, but strains 301(T) and 30S did not. All three strains used the ribulose monophosphate pathway for C1 assimilation. The major fatty acids in the three strains were C(16:0) and C(16:1)ω7c. The DNA G+C contents of strains 301(T) and SIP3-4 were 42.6 and 54.6 mol%, respectively. Based on 16S rRNA gene sequence phylogeny and the relevant phenotypic characteristics, strain SIP3-4 was assigned to the previously defined species Methylovorus glucosotrophus. Strains 301(T) and 30S were closely related to each other (100% 16S rRNA gene sequence similarity) and shared 96.6% 16S rRNA gene sequence similarity with a previously described isolate, Methylotenera mobilis JLW8(T). Based on significant genomic and phenotypic divergence with the latter, strains 301(T) and 30S represent a novel species within the genus Methylotenera, for which the name Methylotenera versatilis sp. nov. is proposed; the type strain is 301(T) (=VKM B-2679(T)=JCM 17579(T)). An emended description of the genus Methylotenera is provided.

Genomes of three methylotrophs from a single niche reveal the genetic and metabolic divergence of the methylophilaceae.

The genomes of three representatives of the family Methylophilaceae, Methylotenera mobilis JLW8, Methylotenera versatilis 301, and Methylovorus glucosetrophus SIP3-4, all isolated from a single study site, Lake Washington in Seattle, WA, were completely sequenced. These were compared to each other and to the previously published genomes of Methylobacillus flagellatus KT and an unclassified Methylophilales strain, HTCC2181. Comparative analysis revealed that the core genome of Methylophilaceae may be as small as approximately 600 genes, while the pangenome may be as large as approximately 6,000 genes. Significant divergence between the genomes in terms of both gene content and gene and protein conservation was uncovered, including the varied presence of certain genes involved in methylotrophy. Overall, our data demonstrate that metabolic potentials can vary significantly between different species of Methylophilaceae, including organisms inhabiting the very same environment. These data suggest that genetic divergence among the members of this family may be responsible for their specialized and nonredundant functions in C1 cycling, which in turn suggests means for their successful coexistence in their specific ecological niches.

Insights into the physiology of Methylotenera mobilis as revealed by metagenome-based shotgun proteomic analysis.

While the shotgun proteomics approach is gaining momentum in understanding microbial physiology, it remains limited by the paucity of high-quality genomic data, especially when it comes to poorly characterized newly identified phyla. At the same time, large-scale metagenomic sequencing projects produce datasets representing genomes of a variety of environmental microbes, although with lower sequence coverage and sequence quality. In this work we tested the utility of a metagenomic dataset enriched in sequences of environmental strains of Methylotenera mobilis, to assess the protein profile of a laboratory-cultivated strain, M. mobilis JLW8, as a proof of principle. We demonstrate that a large portion of the proteome predicted from the metagenomic sequence (approx. 20 %) could be identified with high confidence (three or more peptide sequences), thus gaining insights into the physiology of this bacterium, which represents a new genus within the family Methylophilaceae.

Theanine production by coupled fermentation with energy transfer using gamma-glutamylmethylamide synthetase of Methylovorus mays No. 9.

Gamma-glutamylmetylamide synthetase (GMAS) of Methylovorus mays No. 9, produced by Eschericia coli AD494 (DE3) harboring pET21aGM, formed theanine from glutamic acid and ethylamine with coupling of the reaction with sugar fermentation of baker's yeast cells as an ATP-regeneration system. Theanine formation was stimulated by the addition of Mn(2+) to the reaction mixture, whereas Mg(2+) was less effective. Increases to a certain level in the concentrations of GMAS and the substrates in the mixture were effective in increasing theanine formation, but high concentrations of ethylamine (900 mM or more) inhibited yeast sugar fermentation, and eventually decreased theanine formation. The inhibitory effect of ethylamine was restored by increasing the concentration of potassium phosphate buffer in the mixture. Approximately 600 mM (110 mg/ml) theanine was formed in 48 h in an improved reaction mixture containing 600 mM sodium glutamate, 600 mM ethylamine.HCl, 300 mM glucose, 200 mM potassium phosphate buffer (pH 7.0), 30 mM MgCl(2), 5 mM MnCl(2), 5 mM AMP, 30 units/ml of GMAS, and 40 mg/ml of yeast cells. The yield of theanine was 100% on the substrates (glutamic acid and ethylamine) and also on the energy source (glucose consumed).

Methylotenera mobilis gen. nov., sp. nov., an obligately methylamine-utilizing bacterium within the family Methylophilaceae.

A novel obligate methylamine utilizer (strain JLW8(T)), isolated from Lake Washington sediment, was characterized taxonomically. The isolate was an aerobic, Gram-negative bacterium. Cells were rod-shaped and motile by means of a single flagellum. Reproduction was by binary fission and no resting bodies were formed. Growth was observed within a pH range of 5-8.5, with optimum growth at pH 7.5. It utilized methylamine as a single source of energy, carbon and nitrogen. Methylamine was oxidized via methylamine dehydrogenase and formaldehyde was assimilated via the ribulose monophosphate cycle. The cellular fatty acid profile was dominated by C(16 : 0)omega7c and C(16 : 0) and the major phospholipid was phosphatidylethanolamine. The DNA G+C content was 54 mol%. 16S rRNA gene sequence analysis indicated that the new isolate was closely related (97-98 % similarity) to a broad group of sequences from uncultured or uncharacterized Betaproteobacteria, but only distantly related (93-96 % similarity) to known methylotrophs of the family Methylophilaceae. Strain JLW8(T) (=ATCC BAA-1282(T)=DSM 17540(T)) is proposed as the type strain of a novel species in a new genus within the family Methylophilaceae, Methylotenera mobilis gen. nov., sp. nov.

Phylogenetic position and emended description of the genus Methylovorus.

The genus Methylovorus, currently represented by the restricted facultative methylotroph Methylovorus glucosotrophus Govorukhina and Trotsenko 1991 and the obligate methylotroph Methylovorus mays Doronina et al. 2001, is here established by direct sequencing of amplified 16S rRNA genes and DNA-DNA hybridization to be clearly separated from the extant ribulose monophosphate (RuMP) pathway methylobacteria and to form a distinct branch within the beta-Proteobacteria.

Stable isotope probing of rRNA and DNA reveals a dynamic methylotroph community and trophic interactions with fungi and protozoa in oxic rice field soil.

Stable isotope probing (SIP) is a novel technique to characterize structure and in situ function of active microbial populations, which is based on the incorporation of 13C-labelled substrates into nucleic acids. Here, we have traced methylotrophic members of a rice field soil microbial community, which became active upon continuous addition of 13C-methanol (< 22 mM) as studied in microcosms. By combining rRNA- and DNA-based SIP, as well as domain-specific real-time PCR detection of templates in fractions of centrifugation gradients, we were able to detect 13C-labelled bacterial rRNA after 6 days of incubation. Fingerprinting and comparative sequence analysis of 'heavy' bacterial rRNA showed that mostly members of the Methylobacteriaceae and a novel clade within the Methylophilaceae formed part of the indigenous methylotrophic community. Over time, however, the Methylophilaceae were enriched. Unexpectedly, nucleic acids of eukaryotic origin were detected, mostly in intermediately 13C-labelled gradient fractions. These eukaryotes were identified as fungi mostly related to Fusarium and Aspergillus spp., and also Cercozoa, known as predatory soil flagellates. The detection of fungi and protozoa in 13C-enriched nucleic acid fractions suggests a possible involvement in either direct assimilation of label by the fungi, or a food web, i.e. that primary 13C-methanol consuming methylotrophs were decomposed by fungi and grazed by protozoa.