Biology subjects

Chadwick, G. L.

Publications and source records attributed to Chadwick, G. L..

7 recordsLinked to original sources

bioRxiv2025

Methanogenesis marker 16 metalloprotein is the primary coenzyme M synthase in Methanosarcina acetivorans

2-mercaptoethanesulfonate (Coenzyme M, CoM) is an organic sulfur-containing cofactor used for hydrocarbon metabolism in Archaea and Bacteria. In Archaea, CoM serves as an alkyl group carrier for enzymes belonging to the alkyl-CoM reductase family, including methyl-CoM reductase, which catalyzes methane formation in methanogens. Two pathways for the biosynthesis of CoM are present in methanogenic archaea. The initial steps of these pathways are distinct but the last two reactions, leading up to CoM formation, are universally conserved. The final step is proposed to be mediated by methanogenesis marker metalloprotein 16 (MMP16), a putative sulfurtransferase, that replaces the aldehyde group of sulfoacetaldehyde with a thiol to generate CoM. The assignment of MMP16 as CoM synthase (ComF) is not widely accepted as deletion mutants have been shown to grow without any CoM dependence. Here, we investigate the role of MMP16 in the model methanogen, Methanosarcina acetivorans. We show that a mutant lacking MMP16 has a CoM-dependent growth phenotype and a global transcriptomic profile reflective of CoM-starvation. Additionally, the {Delta}MMP16 mutant is a CoM auxotroph in sulfide-free medium. These data reinforce prior claims that MMP16 is a bona fide ComF but point to backup pathway(s) that can conditionally compensate for its absence. We found that L- aspartate semialdehyde sulfurtransferase (L-ASST), catalyzing a sulfurtransferase reaction during homocysteine biosynthesis in methanogens, is potentially involved in genetic compensation of the MMP16 deletion. Even though, both, L-ASST and MMP16 are members of the COG1900 family, site-directed mutagenesis of conserved cysteine residues implicated in catalysis reveal that the underlying reaction mechanisms may be distinct. Altogether, we have provided concrete evidence that MMP16 is the primary ComF in methanogenic archaea. Author SummaryMethane is a high energy renewable fuel that is the primary constituent of natural gas and a potent greenhouse gas. A significant fraction of global methane emissions is generated by the activity of methanogenic archaea. These microorganisms use a cofactor called Coenzyme M (CoM) as a methyl carrier for methane production mediated by the enzyme Methyl-Coenzyme M reductase. Since methane production is essential for energy conservation in methanogens, they need to synthesize or import CoM. Accordingly, most methanogens encode either one of two CoM biosynthesis pathways. Methanogenesis marker 16 metalloprotein (MMP16) is proposed to catalyze the last step of CoM biosynthesis in both pathways however experimental evidence to this effect is lacking. Here we demonstrate that MMP16 is, indeed, the primary CoM synthase (ComF) in the model methanogen, Methanosarcina acetivorans. Since MMP16 is uniquely and widely distributed in methanogens, it can serve as an ideal candidate for the design of anti- methanogenic chemical inhibitors.

microbiology↗

bioRxiv2023

Physiological and transcriptomic response to methyl-coenzyme M reductase limitation in Methanosarcina acetivorans

Methyl-coenzyme M reductase (MCR) catalyzes the final step of methanogenesis, the microbial metabolism responsible for nearly all biological methane emissions to the atmosphere. Decades of biochemical and structural studies have generated detailed insights into MCR function in vitro, yet very little is known about the interplay between MCR and methanogen physiology. For instance, while it is routinely stated that MCR catalyzes the rate-limiting step of methanogenesis, this statement has not been categorically tested. Here, to gain a more direct understanding of MCRs control on the growth of Methanosarcina acetivorans, we generate a strain with an inducible mcr operon on the chromosome, allowing for careful control of MCR expression. We show that MCR is not growth rate limiting in substrate-replete batch cultures. However, through careful titration of MCR expression, growth-limiting state(s) can be obtained. Transcriptomic analysis of M. acetivorans experiencing MCR-limitation reveals a global response with hundreds of differentially expressed genes across diverse functional categories. Notably, MCR limitation leads to a strong induction of methylsulfide methyltransferases, likely due to insufficient recycling of metabolic intermediates. In addition, the mcr operon does not seem to be transcriptionally regulated, i.e., it is constitutively expressed, suggesting that the overabundance of MCR might be beneficial when cells experience nutrient limitation or stressful conditions. Altogether, we show that there is wide range of cellular MCR concentrations that can sustain optimal growth, suggesting that other factors like anabolic reactions might be rate-limiting for methanogenic growth. ImportanceMethane is a potent greenhouse gas that has contributed to ca. 25% of global warming in the post-industrial era. Atmospheric methane is primarily of biogenic origin, mostly produced by microorganisms called methanogens. In methanogens, methyl-coenzyme M reductase (MCR) catalyzes methane formation. Even though MCR comprises ca. 10% of the cellular proteome, it is hypothesized to be growth-limiting during methanogenesis. Here, we show that Methanosarcina acetivorans grown under standard laboratory conditions produces more MCR than its cellular demand for optimal growth. The tools outlined in this study can be used to refine metabolic models of methanogenesis and assay lesions in MCR in a higher throughput manner than isolation and biochemical characterization of pure protein.

microbiology↗

bioRxiv2023

Discovery of two archaeal GDGT lipid modifying enzymes reveals diverse microbes capable of H-GDGT biosynthesis and modification

Archaea produce unique membrane-spanning lipids, termed glycerol dialkyl glycerol tetraethers (GDGTs), which are thought to aid in adaptive responses to various environmental challenges. GDGTs can be modified in a variety of ways, including cyclization, bridging or cross-linking, methylation, hydroxylation, and desaturation, to give rise to a plethora of structurally distinct GDGT lipids with different properties. Here we report the discovery of a pair of radical SAM enzymes responsible for two of these modifications - an H-GDGT bridge synthase (Hbs), responsible for cross-linking the two hydrocarbon tails of a GDGT to produce H-GDGTs and an H-GDGT methylase (Hgm), responsible for the subsequent methylation of H-GDGTs. Heterologous expression of Hbs proteins from various archaea in Thermococcus kodakarensis results in the production of H-GDGTs in two isomeric forms. Further, co-expression of Hbs and Hgm results in the production of mono- and di-methylated H-GDGTs and minor amounts of tri-methylated H- GDGTs while expression of Hgm alone results in minor production of mono- and di- methylated GDGTs. Phylogenetic analyses reveal the presence of Hbs homologs in diverse archaeal genomes spanning all four archaeal superphyla. We also find Hbs homologs in bacterial genomes that have the genetic potential to synthesize fatty acid- based membrane-spanning lipids such as brGDGTs. We subsequently demonstrate H- GDGT production in three Hbs-encoding archaea, identifying an increase in H-GDGTs in response to elevated temperature in members of the genus Archaeoglobus and observing the production of highly cyclized H-GDGTs with up to 6 rings in the Thermoproteales archaeon Vulcanisaeta distributa. Such highly cyclized H-GDGTs are the precursors of ARN acids, a class of tetraprotic naphthenic acids that cause destructive mineral deposition during crude oil processing. Co-occurrence of the H-GDGT synthase with the previously identified GDGT ring synthases in archaeal genomes allowed identification of multiple archaeal phyla with the genetic potential to produce highly cyclized H-GDGTs, with particularly interesting candidates in the class Thermoplasmata from oil rich environments.

microbiology↗

bioRxiv2023

McrD binds asymmetrically to methyl-coenzyme M reductase improving active site accessibility during assembly

Methyl-coenzyme M reductase (MCR) catalyzes the formation of methane and its activity accounts for nearly all biologically produced methane released into the atmosphere. The assembly of MCR is an intricate process involving the installation of a complex set of post-translational modifications and the unique Ni porphyrin cofactor F430. Despite decades of research, details of MCR assembly remain largely unresolved. Here, we report the structural characterization of MCR in two intermediate states of assembly. These intermediate states lack one or both F430 cofactors and form complexes with the previously uncharacterized McrD protein. McrD is found to bind asymmetrically to MCR, displacing large regions of the alpha subunit and increasing active site accessibility for the installation of F430--shedding light on the assembly of MCR and the role of McrD therein. This work offers crucial information for the expression of MCR in a heterologous host and provides new targets for the design of MCR inhibitors. One-sentence summaryStructural characterization of methyl-coenzyme M reductase assembly intermediates.

biochemistry↗

bioRxiv2022

Metabolic strategies shared by basement residents of the Lost City hydrothermal field

Alkaline fluids venting from chimneys of the Lost City hydrothermal field flow from a potentially vast microbial habitat within the seafloor where energy and organic molecules are released by chemical reactions within rocks uplifted from Earths mantle. In this study, we investigated hydrothermal fluids venting from Lost City chimneys as windows into subseafloor environments where the products of geochemical reactions, such as hydrogen (H2), formate, and methane, may be the only available sources of energy for biological activity. Our deep sequencing of metagenomes and metatranscriptomes from these hydrothermal fluids revealed a few key species of archaea and bacteria that are likely to play critical roles in the subseafloor microbial ecosystem. We identified a population of Thermodesulfovibrionales (belonging to phylum Nitrospirae) as a prevalent sulfate-reducing bacterium that may be responsible for much of the consumption of H2 and sulfate in Lost City fluids. Metagenome-assembled genomes (MAGs) classified as Methanosarcinaceae and Candidatus Bipolaricaulota were also recovered from venting fluids and represent potential methanogenic and acetogenic members of the subseafloor ecosystem. These genomes share novel hydrogenases and formate dehydrogenase-like sequences that may be unique to hydrothermal and subsurface alkaline environments where hydrogen and formate are much more abundant than carbon dioxide. The results of this study include multiple examples of metabolic strategies that appear to be advantageous in hydrothermal and subsurface environments where energy and carbon are provided by geochemical reactions. IMPORTANCEThe Lost City hydrothermal field is an iconic example of a microbial ecosystem fueled by energy and carbon from Earths mantle. Uplift of mantle rocks into the seafloor can trigger a process known as serpentinization that releases hydrogen and creates unusual environmental conditions where simple organic carbon molecules are more stable than dissolved inorganic carbon. This study provides an initial glimpse into the kinds of microbes that live deep within the seafloor where serpentinization takes place, by sampling hydrothermal fluids exiting from the Lost City chimneys. The metabolic strategies that these microbes appear to be using are also shared by microbes that inhabit other sites of serpentinization, including continental subsurface environments and natural springs. Therefore, the results of this study contribute to a broader, interdisciplinary effort to understand the general principles and mechanisms by which serpentinization-associated processes can support life on Earth and perhaps other worlds.

microbiology↗

bioRxiv2021

Comparative genomics on cultivated and uncultivated, freshwater and marine Candidatus Manganitrophaceae species implies their worldwide reach in manganese chemolithoautotrophy

Chemolithoautotrophic manganese oxidation has long been theorized, but only recently demonstrated in a bacterial co-culture. The majority member of the co-culture, Candidatus Manganitrophus noduliformans, is a distinct but not yet isolated lineage in the phylum Nitrospirota (Nitrospirae). Here, we established two additional MnCO3-oxidizing cultures using inocula from Santa Barbara (USA) and Boetsap (South Africa). Both cultures were dominated by strains of a new species, designated Candidatus Manganitrophus morganii. The next abundant members differed in the available cultures, suggesting that while Ca. Manganitrophus species have not been isolated in pure culture, they may not require a specific syntrophic relationship with another species. Phylogeny of cultivated Ca. Manganitrophus and related metagenome-assembled genomes revealed a coherent taxonomic family, Candidatus Manganitrophaceae, from both freshwater and marine environments and distributed globally. Comparative genomic analyses support this family being Mn(II)-oxidizing chemolithoautotrophs. Among the 895 shared genes were a subset of those hypothesized for Mn(II) oxidation (Cyc2 and PCC_1) and oxygen reduction (TO_1 and TO_2) that could facilitate Mn(II) lithotrophy. An unusual, plausibly reverse Complex 1 containing 2 additional pumping subunits was also shared by the family, as were genes for the reverse TCA carbon fixation cycle, which could enable Mn(II) autotrophy. All members of the family lacked genes for nitrification found in Nitrospira species. The results suggest that Ca. Manganitrophaceae share a core set of candidate genes for the newly discovered manganese dependent chemolithoautotrophic lifestyle, and likely have a broad, global distribution. ImportanceManganese (Mn) is an abundant redox-active metal that cycled in many of Earths biomes. While diverse bacteria and archaea have been demonstrated to respire Mn(III/IV), only recently have bacteria been implicated in Mn(II) oxidation dependent growth. Here, two new Mn(II)-oxidizing enrichment cultures originated from two continents and hemispheres were examined. By comparing the community composition of the enrichments and performing phylogenomic analysis on the abundant Nitrospirota therein, new insights are gleaned on cell interactions, taxonomy, and machineries that may underlie Mn(II)-based lithotrophy and autotrophy.

microbiology↗

bioRxiv2021

Comparative genomics reveals electron transfer and syntrophic mechanisms differentiating methanotrophic and methanogenic archaea

The anaerobic oxidation of methane coupled to sulfate reduction is a microbially mediated process requiring a syntrophic partnership between anaerobic methanotrophic (ANME) archaea and sulfate reducing bacteria (SRB). Based on genome taxonomy, ANME lineages are polyphyletic within the phylum Halobacterota, none of which have been isolated in pure culture. Here we reconstruct 28 ANME genomes from environmental metagenomes and flow sorted syntrophic consortia. Together with a reanalysis of previously published datasets, these genomes enable a comparative analysis of all marine ANME clades. We review the genomic features which separate ANME from their methanogenic relatives and identify what differentiates ANME clades. Large multiheme cytochromes and bioenergetic complexes predicted to be involved in novel electron bifurcation reactions are well-distributed and conserved in the ANME archaea, while significant variations in the anabolic C1 pathways exists between clades. Our analysis raises the possibility that methylotrophic methanogenesis may have evolved from a methanotrophic ancestor.

microbiology↗