Methylation at arginine 17 of histone H3 is linked to gene activation

The nuclear hormone receptor co-activator CARM1 has the potential to methylate histone H3 at arginine residues in vitro. The methyltransferase activity of CARM1 is necessary for its co-activator functions in transient transfection assays. However, the role of this methyltransferase in vivo is unclear, given that methylation of arginines is not easily detectable on histones. We have raised an antibody that specifically recognizes methylated arginine 17 (R17) of histone H3, the major site of methylation by CARM1. Using this antibody we show that methylated R17 exists in vivo. Chromatin immunoprecipitation analysis shows that R17 methylation on histone H3 is dramatically upregulated when the estrogen receptor-regulated pS2 gene is activated. Coincident with the appearance of methylated R17, CARM1 is found associated with the histones on the pS2 gene. Together these results demonstrate that CARM1 is recruited to an active promoter and that CARM1-mediated R17 methylation on histone H3 takes place in vivo during this active state.     

Promiscuous methylation of non-canonical DNA sites by HaeIII methyltransferase

The cytosine C5 methyltransferase M.HaeIII recognises and methylates the central cytosine of its canonical site GGCC. Here we report that M.HaeIII can also, with lower efficiency, methylate cytosines located in a wide range of non-canonical sequences. Using bisulphite sequencing we mapped the methyl- cytosine residues in DNA methylated in vitro and in vivo by M.HaeIII. Methyl-cytosine residues were observed in multiple sequence contexts, most commonly, but not exclusively, at star sites (sites differing by a single base from the canonical sequence). The most frequently used star sites had changes at positions 1 and 4, but there is little or no methylation at star sites changed at position 2. The rate of methylation of non-canonical sites can be quite significant: a DNA substrate lacking a canonical site was methylated by M.HaeIII in vitro at a rate only an order of magnitude slower than an otherwise identical substrate containing the canonical site. In vivo methylation of non-canonical sites may therefore be significant and may have provided the starting point for the evolution of restriction–modification systems with novel sequence specificities.     

Volatilisation of metals and metalloids: An inherent feature of methanoarchaea?

As shown by recent studies, anaerobic members of Archaea and Bacteria are involved in processes that transform ionic species of metals and metalloids (arsenic, antimony, bismuth, selenium, tellurium and mercury) into volatile and mostly toxic derivatives (mainly methyl derivatives or hydrides). Since the fact that these transformations proceed in both environmental settings and in parts of the human body, we have to consider that these processes also interfere directly with human health. The diversity of the volatile derivatives produced and their emission rates were significantly higher in methanoarchaeal than in bacterial strains, which supports the pivotal role of methanoarchaea in transforming metals and metalloids (metal(loid)s) into their volatile derivatives. Compared with methanoarchaea, 14 anaerobic bacterial strains showed a significantly restricted spectrum of volatilised derivatives and mostly lower production rates of volatile bismuth and selenium derivatives. Since methanoarchaea isolated from the human gut (Methanosphaera stadtmanae, Methanobrevibacter smithii) showed a higher potential for metal(loid) derivatisation compared to bacterial gut isolates, we assume that methanoarchaea in the human gut are mainly responsible for the production of these volatile derivatives. The observation that trimethylbismuth ((CH(3))(3)Bi), the main volatile derivative of bismuth produced in human feces, inhibited growing cultures of Bacteroides thetaiotaomicron, a representative member of the human physiological gut flora, suggests that these volatiles exert their toxic effects on human health not only by direct interaction with host cells but also by disturbing the physiological gut microflora.     

Arsenic Methylation and Volatilization by Arsenite S-Adenosylmethionine Methyltransferase in Pseudomonas alcaligenes NBRC14159

Inorganic arsenic (As) is highly toxic and ubiquitous in the environment. Inorganic As can be transformed by microbial methylation, which constitutes an important part of the As biogeochemical cycle. In this study, we investigated As biotransformation by Pseudomonas alcaligenes NBRC14159. P. alcaligenes was able to methylate arsenite [As(III)] rapidly to dimethylarsenate and small amounts of trimethylarsenic oxide. An arsenite S-adenosylmethionine methyltransferase, PaArsM, was identified and functionally characterized. PaArsM shares low similarities with other reported ArsM enzymes (<55%). When P. alcaligenes arsM gene (PaarsM) was disrupted, the mutant lost As methylation ability and became more sensitive to As(III). PaarsM was expressed in the absence of As(III) and the expression was further enhanced by As(III) exposure. Heterologous expression of PaarsM in an As-hypersensitive strain of Escherichia coli conferred As(III) resistance. Purified PaArsM protein methylated As(III) to dimethylarsenate as the main product in the medium and also produced dimethylarsine and trimethylarsine gases. We propose that PaArsM plays a role in As methylation and detoxification of As(III) and could be exploited in bioremediation of As-contaminated environments.     

Shifting microbial communities sustain multiyear iron reduction and methanogenesis in ferruginous sediment incubations

Reactive Fe(III) minerals can influence methane (CH₄) emissions by inhibiting microbial methanogenesis or by stimulating anaerobic CH₄ oxidation. The balance between Fe(III) reduction, methanogenesis, and CH₄ oxidation in ferruginous Archean and Paleoproterozoic oceans would have controlled CH₄ fluxes to the atmosphere, thereby regulating the capacity for CH₄ to warm the early Earth under the Faint Young Sun. We studied CH₄ and Fe cycling in anoxic incubations of ferruginous sediment from the ancient ocean analogue Lake Matano, Indonesia, over three successive transfers (500 days in total). Iron reduction, methanogenesis, CH₄ oxidation, and microbial taxonomy were monitored in treatments amended with ferrihydrite or goethite. After three dilutions, Fe(III) reduction persisted only in bottles with ferrihydrite. Enhanced CH₄ production was observed in the presence of goethite, highlighting the potential for reactive Fe(III) oxides to inhibit methanogenesis. Supplementing the media with hydrogen, nickel and selenium did not stimulate methanogenesis. There was limited evidence for Fe(III)‐dependent CH₄ oxidation, although some incubations displayed CH₄‐stimulated Fe(III) reduction. 16S rRNA profiles continuously changed over the course of enrichment, with ultimate dominance of unclassified members of the order Desulfuromonadales in all treatments. Microbial diversity decreased markedly over the course of incubation, with subtle differences between ferrihydrite and goethite amendments. These results suggest that Fe(III) oxide mineralogy and availability of electron donors could have led to spatial separation of Fe(III)‐reducing and methanogenic microbial communities in ferruginous marine sediments, potentially explaining the persistence of CH₄ as a greenhouse gas throughout the first half of Earth history.     

Arsenic methylation by a novel ArsM As(III) S‐adenosylmethionine methyltransferase that requires only two conserved cysteine residues

Arsenic (As) biomethylation is an important component of the As biogeochemical cycle that can influence As toxicity and mobility in the environment. Biomethylation of As is catalyzed by the enzyme arsenite (As[III]) S‐adenosylmethionine methyltransferase (ArsM). To date, all identified ArsM orthologs with As(III) methylation activities have four conserved cysteine residues, which are thought to be essential for As(III) methylation. Here, we isolated an As(III)‐methylating bacterium, Bacillus sp. CX‐1, and identified a gene encoding a S‐adenosylmethionine methyltranserase termed BlArsM with low sequence similarities (≤ 39%) to other ArsMs. BlArsM has six cysteine residues (Cys10, Cys11, Cys145, Cys193, Cys195 and Cys268), three of which (Cys10, Cys145 and Cys195) align with conserved cysteine residues found in most ArsMs. BlarsM is constitutively expressed in Bacillus sp. CX‐1. Heterologous expression of BlarsM conferred As(III) resistance. Purified BlArsM methylated both As(III) and methylarsenite (MAs[III]), with a final product of dimethylarsenate (DMAs[V]). When all six cysteines were individually altered to serine residues, only C145S and C195S derivatives lost the ability to methylate As(III) and MAs(III). The derivative C10S/C11S/C193S/C268S was still active. These results suggest that BlArsM is a novel As(III) S‐adenosylmethionine methyltransferase requiring only two conserved cysteine residues. A model of As(III) methylation by BlArsM is proposed.     

The Legionella pneumophila Methyltransferase RomA Methylates Also Non-histone Proteins during Infection

RomA is a SET-domain containing protein lysine methyltransferase encoded by the Gram-negative bacterium Legionella pneumophila. It is exported into human host cells during infection and has been previously shown to methylate histone H3 at lysine 14 [Rolando et al. (2013), Cell Host Microbe, 13, 395–405]. Here, we investigated the substrate specificity of RomA on peptide arrays showing that it mainly recognizes a G-K-X-(PA) sequence embedded in a basic amino acid sequence context. Based on the specificity profile, we searched for possible additional RomA substrates in the human proteome and identified 34 novel peptide substrates. For nine of these, the corresponding full-length protein or protein domains could be cloned and purified. Using radioactive and antibody-based methylation assays, we showed that seven of them are methylated by RomA, four of them strongly, one moderately, and two weakly. Mutagenesis confirmed for the seven methylated proteins that methylation occurs at target lysine residues fitting to the specificity profile. Methylation of one novel substrate (AROS) was investigated in HEK293 cells overexpressing RomA and during infection with L. pneumophila. Methylation could be detected in both conditions, confirming that RomA methylates non-histone proteins in human cells. Our data show that the bacterial methyltransferase RomA methylates also human non-histone proteins suggesting a multifaceted role in the infection process.     

Determination of methylation specificity of DsaV methyltransferase by a simple biochemical method.

We have developed a simple new method that can identify the base methylated by a sequence-specific DNA methyltransferase and have used it to identify the cytosine that is methylated by DsaV methyltransferase (M. DsaV) within its recognition sequence 5'-CCNGG. The method utilizes the fact that exonuclease III of E. coli does not degrade DNA ends with 3' overhangs and cannot hydrolyze a phosphorothioate linkage. DNA duplexes containing phosphorothioate linkages at specific positions were methylated with M. DsaV in the presence of [methyl-3H] S-adenosylmethionine and were subjected to exonuclease III digestion. The pattern of [methyl-3H] dCMP release from the duplexes was consistent with the methylation of the internal cytosine in CCNGG, but not of the outer cytosine. To establish the accuracy of this method, we confirmed the known specificity of EcoRII methyltransferase by the method. We also confirmed the specificity of M. DsaV using an established biochemical method that involves the use of a type IIS restriction enzyme. Methylation of CCWGG (W = A or T) sequences at the internal cytosines is native to E. coli and is not restricted by the modified cytosine restriction (Mcr) systems. Surprisingly, the gene for M. DsaV was significantly restricted by the McrBC system. We interpret this to mean that M. DsaV may occasionally methylate at sequences other than CCNGG or may occasionally methylate the outer cytosine in its recognition sequence.     

Sulfate-Reducing Bacteria Methylate Mercury at Variable Rates in Pure Culture and in Marine Sediments

Differences in methylmercury (CH₃Hg) production normalized to the sulfate reduction rate (SRR) in various species of sulfate-reducing bacteria (SRB) were quantified in pure cultures and in marine sediment slurries in order to determine if SRB strains which differ phylogenetically methylate mercury (Hg) at similar rates. Cultures representing five genera of the SRB (Desulfovibrio desulfuricans, Desulfobulbus propionicus, Desulfococcus multivorans, Desulfobacter sp. strain BG-8, and Desulfobacterium sp. strain BG-33) were grown in a strictly anoxic, minimal medium that received a dose of inorganic Hg 120 h after inoculation. The mercury methylation rates (MMR) normalized per cell were up to 3 orders of magnitude higher in pure cultures of members of SRB groups capable of acetate utilization (e.g., the family Desulfobacteriaceae) than in pure cultures of members of groups that are not able to use acetate (e.g., the family Desulfovibrionaceae). Little or no Hg methylation was observed in cultures of Desulfobacterium or Desulfovibrio strains in the absence of sulfate, indicating that Hg methylation was coupled to respiration in these strains. Mercury methylation, sulfate reduction, and the identities of sulfate-reducing bacteria in marine sediment slurries were also studied. Sulfate-reducing consortia were identified by using group-specific oligonucleotide probes that targeted the 16S rRNA molecule. Acetate-amended slurries, which were dominated by members of the Desulfobacterium and Desulfobacter groups, exhibited a pronounced ability to methylate Hg when the MMR were normalized to the SRR, while lactate-amended and control slurries had normalized MMR that were not statistically different. Collectively, the results of pure-culture and amended-sediment experiments suggest that members of the family Desulfobacteriaceae have a greater potential to methylate Hg than members of the family Desulfovibrionaceae have when the MMR are normalized to the SRR. Hg methylation potential may be related to genetic composition and/or carbon metabolism in the SRB. Furthermore, we found that in marine sediments that are rich in organic matter and dissolved sulfide rapid CH₃Hg accumulation is coupled to rapid sulfate reduction. The observations described above have broad implications for understanding the control of CH₃Hg formation and for developing remediation strategies for Hg-contaminated sediments.     

Volatilisation of metals and metalloids by the microbial population of an alluvial soil

In order to assess the microbial contribution to the volatilisation of metal(loid)s by methylation and hydridisation in the environment, we focused on soils of different origin. Here, we describe the biogenic production of volatile metal(loid) species of an alluvial soil with rather low metal(loid) contamination. The production of volatile metal(loid) compounds was monitored in soil suspensions kept under anaerobic conditions over an incubation time of 3 months. In the headspace of the samples, we detected mainly hydrids and methylated derivatives of a broad variety of elements such as arsenic, antimony, bismuth, selenium, tellurium, mercury, tin and lead, with the volatile products of arsenic, antimony and selenium representing the highest portions. Classical cultivation-dependent procedures resulted in the isolation of a strictly anaerobic Gram-positive strain (ASI-1), which shows a high versatility in transforming metal(loid) ions to volatile derivatives. Strain ASI-1 is affiliated to the species Clostridium glycolicum due to its high 16S rDNA sequence similarity with members of that species. As shown by fluorescence in situ hybridisation, strain ASI-1 amounts to approximately 2% of the total microbial flora of the alluvial soil. Since the spectrum of volatile metal(loid) compounds produced by this strain is very similar to that obtained by the whole population regarding both the broad variety of metal(loid)s converted and the preference for volatilising arsenic, antimony and selenium, we suggest that this strain may represent a dominant member of the metal(loid) volatilisating population in this habitat.     

DNA methylation in mouse A-repeats in DNA methyltransferase-knockout ES cells and in normal cells determined by bisulfite genomic sequencing

Mouse ES cells with a null mutation of the known DNA methyltransferase retain some residual DNA methylation and can methylate foreign sequences de novo. We have used bisulfite genomic sequencing to examine the sequence specificity and distributions of methylation of a hypermethylated CG island sequence, mouse A-repeats. There were 13 CG dinucleotides in the region examined, 12 of which were methylated to variable extents in all DNAs. We found that: (1) there is considerable residual DNA methylation in ES cells lacking the known DNA methyltransferase (29% of normal methylation in the complete knockout ES DNA); (2) this other activity methylates at exactly the same CG sites as the major methyltransferase; and (3) differences in the distribution of methylated sites between A-repeats in these DNAs are consistent with this other activity methylating in a random de novo fashion. Also, the lack of any methylation in non-CG sites argues that, in other studies where non-CG methylation sites have been found by bisulfite sequencing, detection of such sites of non-CG methylation is not an inherent artifact in this methodology.     

Two dedicated class C radical S-adenosylmethionine methyltransferases concertedly catalyse the synthesis of 7,8-dimethylmenaquinone

Dimethylmenaquinone (DMMK), a prevalent menaquinone (MK) derivative of uncertain function, is characteristic for members of the class Coriobacteriia. Such bacteria are frequently present in intestinal microbiomes and comprise several pathogenic species. The coriobacterial model organism Adlercreutzia equolifaciens was used to investigate the enzymology of DMMK biosynthesis. A HemN-like class C radical S-adenosylmethionine methyltransferase (MenK2) from A. equolifaciens was produced in Wolinella succinogenes or Escherichia coli cells and found to methylate MK specifically at position C-7. In combination with a previously described MK methyltransferase (MqnK/MenK) dedicated to MK methylation at C-8, 7,8-DMMK₆ was produced in W. succinogenes. The position of the two methyl groups was confirmed by two-dimensional NMR and midpoint redox potentials of 7-MMK₆, 8-MMK₆ and 7,8-DMMK₆ were determined by cyclic voltammetry. A phylogenetic tree of MenK, MenK2 and HemN proteins revealed a Coriobacteriia-specific MenK2 clade. Using chimeric A. equolifaciens MenK/MenK2 proteins produced in E. coli it was shown that the combined linker and HemN domains determined the site-specificity of methylation. The results suggest that the use of MenK2 as a biomarker allows predicting the ability of DMMK synthesis in microbial species.     

2��-O Methylation of Internal Adenosine by Flavivirus NS5 Methyltransferase

RNA modification plays an important role in modulating host-pathogen interaction. Flavivirus NS5 protein encodes N-7 and 2′-O methyltransferase activities that are required for the formation of 5′ type I cap (m⁷GpppAm) of viral RNA genome. Here we reported, for the first time, that flavivirus NS5 has a novel internal RNA methylation activity. Recombinant NS5 proteins of West Nile virus and Dengue virus (serotype 4; DENV-4) specifically methylates polyA, but not polyG, polyC, or polyU, indicating that the methylation occurs at adenosine residue. RNAs with internal adenosines substituted with 2′-O-methyladenosines are not active substrates for internal methylation, whereas RNAs with adenosines substituted with N⁶-methyladenosines can be efficiently methylated, suggesting that the internal methylation occurs at the 2′-OH position of adenosine. Mass spectroscopic analysis further demonstrated that the internal methylation product is 2′-O-methyladenosine. Importantly, genomic RNA purified from DENV virion contains 2′-O-methyladenosine. The 2′-O methylation of internal adenosine does not require specific RNA sequence since recombinant methyltransferase of DENV-4 can efficiently methylate RNAs spanning different regions of viral genome, host ribosomal RNAs, and polyA. Structure-based mutagenesis results indicate that K61-D146-K181-E217 tetrad of DENV-4 methyltransferase forms the active site of internal methylation activity; in addition, distinct residues within the methyl donor (S-adenosyl-L-methionine) pocket, GTP pocket, and RNA-binding site are critical for the internal methylation activity. Functional analysis using flavivirus replicon and genome-length RNAs showed that internal methylation attenuated viral RNA translation and replication. Polymerase assay revealed that internal 2′-O-methyladenosine reduces the efficiency of RNA elongation. Collectively, our results demonstrate that flavivirus NS5 performs 2′-O methylation of internal adenosine of viral RNA in vivo and host ribosomal RNAs in vitro.     

Dedication

Mixed cultures derived from Boston Harbor sediments, which gave evidence of methylating tin compounds, yielded two isolates, each a Bacillus sp., which methylated CH₃SnCl₃ to form (CH₃)₃SnX in coculture. Neither organism alone gave evidence of methylation. SnCl₄ and (CH₃)₂SnCl₂ were not methylated. Transfer of either organism to filtered medium containing CH₃SnCl₃ in which the other had grown did not lead to methylation. Therefore methylation by the coculture is not simply a matter of cross‐feeding.     

Methylation of inorganic and organic selenium by the bacterial thiopurine methyltransferase

Escherichia coli cells expressing the tpm gene encoding the bacterial thiopurine methyltransferase (bTPMT) are shown to methylate selenite and (methyl)selenocysteine into dimethylselenide (DMSe) and dimethyldiselenide (DMDSe). E. coli cells expressing tpm from a gene library cosmid clone (harboring a Pseudomonas syringae insert of about 20 kb) also methylated selenate into DMSe and DMDSe. bTPMT is the first methyltransferase shown to be involved in the methylation of these selenium derivatives.     

Heterodimeric DNA methyltransferases as a platform for creating designer zinc finger methyltransferases for targeted DNA methylation in cells

The ability to target methylation to specific genomic sites would further the study of DNA methylation’s biological role and potentially offer a tool for silencing gene expression and for treating diseases involving abnormal hypomethylation. The end-to-end fusion of DNA methyltransferases to zinc fingers has been shown to bias methylation to desired regions. However, the strategy is inherently limited because the methyltransferase domain remains active regardless of whether the zinc finger domain is bound at its cognate site and can methylate non-target sites. We demonstrate an alternative strategy in which fragments of a DNA methyltransferase, compromised in their ability to methylate DNA, are fused to two zinc fingers designed to bind 9 bp sites flanking a methylation target site. Using the naturally heterodimeric DNA methyltransferase M.EcoHK31I, which methylates the inner cytosine of 5′-YGGCCR-3′, we demonstrate that this strategy can yield a methyltransferase capable of significant levels of methylation at the target site with undetectable levels of methylation at non-target sites in Escherichia coli. However, some non-target methylation could be detected at higher expression levels of the zinc finger methyltransferase indicating that further improvements will be necessary to attain the desired exclusive target specificity.     

Suppression of methanogenesis by dissimilatory Fe(III)-reducing bacteria in tropical rain forest soils: implications for ecosystem methane flux

Tropical forests are an important source of atmospheric methane (CH₄), and recent work suggests that CH₄ fluxes from humid tropical environments are driven by variations in CH₄ production, rather than by bacterial CH₄ oxidation. Competition for acetate between methanogenic archaea and Fe(III)‐reducing bacteria is one of the principal controls on CH₄ flux in many Fe‐rich anoxic environments. Upland humid tropical forests are also abundant in Fe and are characterized by high organic matter inputs, steep soil oxygen (O₂) gradients, and fluctuating redox conditions, yielding concomitant methanogenesis and bacterial Fe(III) reduction. However, whether Fe(III)‐reducing bacteria coexist with methanogens or competitively suppress methanogenic acetate use in wet tropical soils is uncertain. To address this question, we conducted a process‐based laboratory experiment to determine if competition for acetate between methanogens and Fe(III)‐reducing bacteria influenced CH₄ production and C isotope composition in humid tropical forest soils. We collected soils from a poor to moderately drained upland rain forest and incubated them with combinations of ¹³C‐bicarbonate, ¹³C‐methyl labeled acetate (¹³CH₃COO^?), poorly crystalline Fe(III), or fluoroacetate. CH₄ production showed a greater proportional increase than Fe²⁺ production after competition for acetate was alleviated, suggesting that Fe(III)‐reducing bacteria were suppressing methanogenesis. Methanogenesis increased by approximately 67 times while Fe²⁺ production only doubled after the addition of ¹³CH₃COO^?. Large increases in both CH₄ and Fe²⁺ production also indicate that the two process were acetate limited, suggesting that acetate may be a key substrate for anoxic carbon (C) metabolism in humid tropical forest soils. C isotope analysis suggests that competition for acetate was not the only factor driving CH₄ production, as ¹³C partitioning did not vary significantly between ¹³CH₃COO^? and ¹³CH₃COO^?+Fe(III) treatments. This suggests that dissimilatory Fe(III)‐reduction suppressed both hydrogenotrophic and aceticlastic methanogenesis. These findings have implications for understanding the CH₄ biogeochemistry of highly weathered wet tropical soils, where CH₄ efflux is driven largely by CH₄ production.