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Item Physiological adaptations to serpentinization in the Samail Ophiolite, Oman(2019-03) Fones, Elizabeth M.; Colman, Daniel R.; Kraus, Emily A.; Nothaft, Daniel B.; Poudel, Saroj; Rempfert, Kaitlin R.; Spear, John R.; Templeton, Alexis S.; Boyd, Eric S.Hydration of ultramafic rock during the geologic process of serpentinization can generate reduced substrates that microorganisms may use to fuel their carbon and energy metabolisms. However, serpentinizing environments also place multiple constraints on microbial life by generating highly reduced hyperalkaline waters that are limited in dissolved inorganic carbon. To better understand how microbial life persists under these conditions, we performed geochemical measurements on waters from a serpentinizing environment and subjected planktonic microbial cells to metagenomic and physiological analyses. Metabolic potential inferred from metagenomes correlated with fluid type, and genes involved in anaerobic metabolisms were enriched in hyperalkaline waters. The abundance of planktonic cells and their rates of utilization of select single-carbon compounds were lower in hyperalkaline waters than alkaline waters. However, the ratios of substrate assimilation to dissimilation were higher in hyperalkaline waters than alkaline waters, which may represent adaptation to minimize energetic and physiologic stress imposed by highly reducing, carbon-limited conditions. Consistent with this hypothesis, estimated genome sizes and average oxidation states of carbon in inferred proteomes were lower in hyperalkaline waters than in alkaline waters. These data suggest that microorganisms inhabiting serpentinized waters exhibit a unique suite of physiological adaptations that allow for their persistence under these polyextremophilic conditions.Item The path of electron transfer to nitrogenase in a phototrophic alpha-proteobacterium(2018-07) Fixen, Kathryn R.; Pal Chowdhury, Nilanjan; Martinez-Perez, Marta; Poudel, Saroj; Boyd, Eric S.; Harwood, Caroline S.The phototrophic alpha-proteobacterium, Rhodopseudomonas palustris, is a model for studies of regulatory and physiological parameters that control the activity of nitrogenase. This enzyme produces the energy-rich compound H2 , in addition to converting N2 gas to NH3 . Nitrogenase is an ATP-requiring enzyme that uses large amounts of reducing power, but the electron transfer pathway to nitrogenase in R. palustris was incompletely known. Here, we show that the ferredoxin, Fer1, is the primary but not sole electron carrier protein encoded by R. palustris that serves as an electron donor to nitrogenase. A flavodoxin, FldA, is also an important electron donor, especially under iron limitation. We present a model where the electron bifurcating complex, FixABCX, can reduce both ferredoxin and flavodoxin to transfer electrons to nitrogenase, and we present bioinformatic evidence that FixABCX and Fer1 form a conserved electron transfer pathway to nitrogenase in nitrogen-fixing proteobacteria. These results may be useful in the design of strategies to reroute electrons generated during metabolism of organic compounds to nitrogenase to achieve maximal activity.Item Evolution and function of flavin-based electron bifurcation(Montana State University - Bozeman, College of Letters & Science, 2018) Poudel, Saroj; Chairperson, Graduate Committee: Eric Boyd; John W. Peters (co-chair); Eric C. Dunham, Melody R. Lindsay, Maximiliano J. Amenabar, Elizabeth M. Fones, Daniel R. Colman and Eric S. Boyd were co-authors of the article, 'Origin and evolution of flavin-based electron bifurcating enzymes' in the journal 'Frontiers in microbiology' which is contained within this thesis.; Amaya M. Garcia Costas was an author and Anne-Frances Miller, Gerrit J. Schut, Rhesa N. Ledbetter, Kathryn R. Fixen, Lance C. Seefeldt, Michael W. W. Adams, Caroline S. Harwood, Eric S. Boyd and John W. Peters were co-authors of the article, 'Defining electron bifurcation in the electron transferring flavoprotein family' in the journal 'Journal of bacteriology' which is contained within this thesis.; Daniel R. Colman was an author and Kathryn R. Fixen, Rhesa N. Ledbetter, Yanning Zheng, Natasha Pence, Lance C. Seefeldt, John W. Peters, Caroline S. Harwood and Eric S. Boyd, were co-authors of the article, 'Electron transfer to nitrogenase in different genomic and metabolic backgrouns' in the journal 'Journal of bacteriology' which is contained within this thesis.Anaerobic microorganisms live in energy limited environments with low nutrient fluxes. Thus, selection has likely acted on these cells to innovate mechanisms that improve the efficiency of anaerobic energy metabolism. In 2008, the process of flavin-based electron bifurcation (FBEB) was discovered and has since been shown to be a critical process that allows anaerobic cells to overcome thermodynamic barriers and to improve metabolic efficiency. FBEB enzymes catalyze the coupling of exergonic and endergonic oxidation--reduction reactions with the same electron donor to circumvent thermodynamic barriers and minimize free energy loss. To date, a total of 12 FBEB enzymes have been discovered that share common features that include the presence of protein-bound flavin, the proposed site of bifurcation, and the electron carrier ferredoxin. Due to its recent discovery, a comprehensive description of the natural history of bifurcating enzymes is lacking. In this thesis, we report the taxonomic and ecological distribution, functional diversity, and evolutionary history of bifurcating enzyme homologs in available complete genomes and environmental metagenomes. Moreover, we investigated the functional and ecological constraints that led to the emergence of FBEB enzymes. Bioinformatics analyses revealed that FBEB enzyme homologs were primarily detected in the genomes of anaerobes, including those of sulfate-reducers, acetogens, fermenters, and methanogens. Phylogenetic analyses of these enzyme homologs suggest that they were not a property of the Last Universal Common Ancestor of Archaea and Bacteria indicating that they are a more recent evolutionary innovation. Consistent with the role of these enzymes in the energy metabolism of anaerobes, FBEB homologs were enriched in metagenomes from subsurface environments relative to those from surface environments. In fact, the earliest evolving homologs of most bifurcating enzymes were detected in subsurface environments, including fluids from subsurface rock fractures and hydrothermal systems. Together, these data highlight the central role that FBEB played and continued to play in the energy metabolism of anaerobic microbial cells inhabiting subsurface environments.Item Electron transfer to nitrogenase in different genomic and metabolic backgrounds(2018-02) Poudel, Saroj; Colman, Daniel R.; Fixen, Kathryn R.; Ledbetter, Rhesa N.; Zheng, Yanning; Pence, Natasha; Seefeldt, Lance C.; Peters, John W.; Hardwood, Caroline S.; Boyd, Eric S.Nitrogenase catalyzes the reduction of dinitrogen (N2) using low potential electrons from ferredoxin (Fd) or flavodoxin (Fld) through an ATP dependent process. Since its emergence in an anaerobic chemoautotroph, this oxygen (O2) sensitive enzyme complex has evolved to operate in a variety of genomic and metabolic backgrounds including those of aerobes, anaerobes, chemotrophs, and phototrophs. However, whether pathways of electron delivery to nitrogenase are influenced by these different metabolic backgrounds is not well understood. Here, we report the distribution of homologs of Fds, Flds, and Fd/Fld-reducing enzymes in 359 genomes of putative N2 fixers (diazotrophs). Six distinct lineages of nitrogenase were identified and their distributions largely corresponded to differences in the host cells' ability to integrate O2 or light into energy metabolism. Predicted pathways of electron transfer to nitrogenase in aerobes, facultative anaerobes, and phototrophs varied from those in anaerobes at the level of Fds/Flds used to reduce nitrogenase, the enzymes that generate reduced Fds/Flds, and the putative substrates of these enzymes. Proteins that putatively reduce Fd with hydrogen or pyruvate were enriched in anaerobes, while those that reduce Fd with NADH/NADPH were enriched in aerobes, facultative anaerobes, and anoxygenic phototrophs. The energy metabolism of aerobic, facultatively anaerobic, and anoxygenic phototrophic diazotrophs often yields reduced NADH/NADPH that is not sufficiently reduced to drive N2 reduction. At least two mechanisms have been acquired by these taxa to overcome this limitation and to generate electrons with potentials capable of reducing Fd. These include the bifurcation of electrons or the coupling of Fd reduction to reverse ion translocation.IMPORTANCE Nitrogen fixation supplies fixed nitrogen to cells from a variety of genomic and metabolic backgrounds including those of aerobes, facultative anaerobes, chemotrophs, and phototrophs. Here, using informatics approaches applied to genomic data, we show that pathways of electron transfer to nitrogenase in metabolically diverse diazotrophic taxa have diversified primarily in response to host cells' acquired ability to integrate O2 or light into their energy metabolism. Acquisition of two key enzyme complexes enabled aerobic and facultatively anaerobic phototrophic taxa to generate electrons of sufficiently low potential to reduce nitrogenase: the bifurcation of electrons via the Fix complex or the coupling of Fd reduction to reverse ion translocation via the Rhodobacter nitrogen fixation (Rnf) complex.Item Electron Acceptor Availability Alters Carbon and Energy Metabolism in a Thermoacidophile(2018-05) Amenabar, Maximiliano J.; Colman, Daniel R.; Poudel, Saroj; Roden, Eric E.; Boyd, Eric S.The thermoacidophilic Acidianus strain DS80 displays versatility in its energy metabolism and can grow autotrophically and heterotrophically with elemental sulfur (S°), ferric iron (Fe3+) or oxygen (O2) as electron acceptors. Here, we show that autotrophic and heterotrophic growth with S° as the electron acceptor is obligately dependent on hydrogen (H2) as electron donor; organic substrates such as acetate can only serve as a carbon source. In contrast, organic substrates such as acetate can serve as electron donor and carbon source for Fe3+ or O2 grown cells. During growth on S° or Fe3+ with H2 as an electron donor, the amount of CO2 assimilated into biomass decreased when cultures were provided with acetate. The addition of CO2 to cultures decreased the amount of acetate mineralized and assimilated and increased cell production in H2/Fe3+ grown cells but had no effect on H2/S° grown cells. In acetate/Fe3+ grown cells, the presence of H2 decreased the amount of acetate mineralized as CO2 in cultures compared to those without H2. These results indicate that electron acceptor availability constrains the variety of carbon sources used by this strain. Addition of H2 to cultures overcomes this limitation and alters heterotrophic metabolism.Item Origin and Evolution of Flavin-Based Electron Bifurcating Enzymes(2018-08) Poudel, Saroj; Dunham, Eric C.; Lindsay, Melody R.; Amenabar, Maximiliano J.; Fones, Elizabeth M.; Colman, Daniel R.; Boyd, Eric S.Twelve evolutionarily unrelated oxidoreductases form enzyme complexes that catalyze the simultaneous coupling of exergonic and endergonic oxidation–reduction reactions to circumvent thermodynamic barriers and minimize free energy loss in a process known as flavin-based electron bifurcation. Common to these 12 bifurcating (Bf) enzymes are protein-bound flavin, the proposed site of bifurcation, and the electron carrier ferredoxin. Despite the documented role of Bf enzymes in balancing the redox state of intracellular electron carriers and in improving the efficiency of cellular metabolism, a comprehensive description of the diversity and evolutionary history of Bf enzymes is lacking. Here, we report the taxonomic distribution, functional diversity, and evolutionary history of Bf enzyme homologs in 4,588 archaeal, bacterial, and eukaryal genomes and 3,136 community metagenomes. Bf homologs were primarily detected in the genomes of anaerobes, including those of sulfate-reducers, acetogens, fermenters, and methanogens. Phylogenetic analyses of Bf enzyme catalytic subunits (oxidoreductases) suggest they were not a property of the Last Universal Common Ancestor of Archaea and Bacteria, which is consistent with the limited and unique taxonomic distributions of enzyme homologs among genomes. Further, phylogenetic analyses of oxidoreductase subunits reveal that non-Bf homologs predate Bf homologs. These observations indicate that multiple independent recruitments of flavoproteins to existing oxidoreductases enabled coupling of numerous new electron Bf reactions. Consistent with the role of these enzymes in the energy metabolism of anaerobes, homologs of Bf enzymes were enriched in metagenomes from subsurface environments relative to those from surface environments. Phylogenetic analyses of homologs from metagenomes reveal that the earliest evolving homologs of most Bf enzymes are from subsurface environments, including fluids from subsurface rock fractures and hydrothermal systems. Collectively, these data suggest strong selective pressures drove the emergence of Bf enzyme complexes via recruitment of flavoproteins that allowed for an increase in the efficiency of cellular metabolism and improvement in energy capture in anaerobes inhabiting a variety of subsurface anoxic habitats where the energy yield of oxidation-reduction reactions is generally low.Item H/D exchange mass spectrometry and statistical coupling analysis reveal a role for allostery in a ferredoxin-dependent bifurcating transhydrogenase catalytic cycle(2018-01) Berry, Luke; Poudel, Saroj; Tokmina-Lukaszewska, Monika; Colman, Daniel R.; Nguyen, Diep M. N.; Schut, Gerrit J.; Adams, Michael W. W.; Peters, John W.; Boyd, Eric S.; Bothner, BrianRecent investigations into ferredoxin-dependent transhydrogenases, a class of enzymes responsible for electron transport, have highlighted the biological importance of flavin-based electron bifurcation (FBEB). FBEB generates biomolecules with very low reduction potential by coupling the oxidation of an electron donor with intermediate potential to the reduction of high and low potential molecules. Bifurcating systems can generate biomolecules with very low reduction potentials, such as reduced ferredoxin (Fd), from species such as NADPH. Metabolic systems that use bifurcation are more efficient and confer a competitive advantage for the organisms that harbor them. Structural models are now available for two NADH-dependent ferredoxin-NADP(+) oxidoreductase (Nfn) complexes. These models, together with spectroscopic studies, have provided considerable insight into the catalytic process of FBEB. However, much about the mechanism and regulation of these multi-subunit proteins remains unclear. Using hydrogen/deuterium exchange mass spectrometry (HDX-MS) and statistical coupling analysis (SCA), we identified specific pathways of communication within the model FBEB system, Nfn from Pyrococus furiosus, under conditions at each step of the catalytic cycle. HDX-MS revealed evidence for allosteric coupling across protein subunits upon nucleotide and ferredoxin binding. SCA uncovered a network of co-evolving residues that can provide connectivity across the complex. Together, the HDX-MS and SCA data show that protein allostery occurs across the ensemble of iron-sulfur cofactors and ligand binding sites using specific pathways that connect domains allowing them to function as dynamically coordinated units.Item Defining Electron Bifurcation in the Electron Transferring Flavoprotein Family(2017-11) Garcia Costas, Amaya M.; Poudel, Saroj; Miller, Anne-Frances; Schut, Gerrit J.; Ledbetter, Rhesa N.; Fixen, Kathryn R.; Seefeldt, Lance C.; Adams, Michael W. W.; Harwood, Caroline S.; Boyd, Eric S.; Peters, John W.Electron bifurcation is the coupling of exergonic and endergonic redox reactions to simultaneously generate (or utilize) low and high potential electrons. It is the third recognized form of energy conservation in biology and has recently been described in select electron transferring flavoproteins (Etfs). Etfs are flavin-containing heterodimers best known for donating electrons derived from fatty acid and amino acid oxidation to an electron transfer respiratory chain via ETF quinone oxidoreductase. Canonical examples contain a flavin adenine dinucleotide (FAD) that is involved in electron transfer as well as a non-redox active adenosine monophosphate (AMP). However, Etfs demonstrated to bifurcate electrons contain a second FAD in place of the AMP. To expand our understanding of the functional variety and metabolic significance of Etfs and to identify amino acid sequence motifs that potentially enable electron bifurcation, we compiled 1,314 Etf protein sequences from genome sequence databases and subjected them to informatics and structural analyses. Etfs were identified in diverse archaea and bacteria, and these clustered into five distinct well-supported groups based on amino acid sequences. Gene neighborhood analyses indicate that these Etf group designations largely correspond to putative differences in functionality. Etfs with the demonstrated ability to bifurcate were found to form one group, suggesting distinct and conserved amino acid sequence motifs enable this capability. Indeed, structural modeling and sequence alignments revealed that identifying residues occur in the NADH and FAD-binding regions of bifurcating Etfs. Collectively, a new classification scheme is presented for Etf proteins that demarcates putative bifurcating vs. non-bifurcating members and suggests that Etf mediated bifurcation is associated with surprisingly diverse enzymes.IMPORTANCE Electron bifurcation has recently been recognized as an electron transfer mechanism used by microorganisms to maximize energy conservation. Bifurcating enzymes couple thermodynamically unfavorable reactions with thermodynamically favorable reactions in an overall spontaneous process. Here we show that the electron transferring flavoprotein (Etf) enzyme family exhibits far greater diversity than previously recognized and we provide a phylogenetic analysis that clearly delineates bifurcating and non-bifurcating members of this family. Structural modeling of proteins within these groups reveals key differences between the bifurcating and non-bifurcating Etfs.Item Geobiological feedbacks and the evolution of thermoacidophiles(2017-10) Colman, Daniel R.; Poudel, Saroj; Hamilton, Trinity L.; Havig, Jeff R.; Selensky, Matthew J.; Shock, Everett L.; Boyd, Eric S.Oxygen-dependent microbial oxidation of sulfur compounds leads to the acidification of natural waters. How acidophiles and their acidic habitats evolved, however, is largely unknown. Using 16S rRNA gene abundance and composition data from 72 hot springs in Yellowstone National Park, Wyoming, we show that hyperacidic (pH<3.0) hydrothermal ecosystems are dominated by a limited number of archaeal lineages with an inferred ability to respire O2. Phylogenomic analyses of 584 existing archaeal genomes revealed that hyperacidophiles evolved independently multiple times within the Archaea, each coincident with the emergence of the ability to respire O2, and that these events likely occurred in the recent evolutionary past. Comparative genomic analyses indicated that archaeal thermoacidophiles from independent lineages are enriched in similar protein-coding genes, consistent with convergent evolution aided by horizontal gene transfer. Because the generation of acidic environments and their successful habitation characteristically require O2, these results suggest that thermoacidophilic Archaea and the acidity of their habitats co-evolved after the evolution of oxygenic photosynthesis. Moreover, it is likely that dissolved O2 concentrations in thermal waters likely did not reach levels capable of sustaining aerobic thermoacidophiles and their acidifying activity until ~0.8Ga, when present day atmospheric levels were reached, a time period that is supported by our estimation of divergence times for archaeal thermoacidophilic clades.Item The deep, hot biosphere: Twenty-five years of retrospection(2017-07) Colman, Daniel R.; Poudel, Saroj; Stamps, Blake W.; Boyd, Eric S.; Spear, John R.Twenty-five years ago this month, Thomas Gold published a seminal manuscript suggesting the presence of a \deep, hot biosphere\" in the Earth\'s crust. Since this publication, a considerable amount of attention has been given to the study of deep biospheres, their role in geochemical cycles, and their potential to inform on the origin of life and its potential outside of Earth. Overwhelming evidence now supports the presence of a deep biosphere ubiquitously distributed on Earth in both terrestrial and marine settings. Furthermore, it has become apparent that much of this life is dependent on lithogenically sourced high-energy compounds to sustain productivity. A vast diversity of uncultivated microorganisms has been detected in subsurface environments, and we show that H2, CH4, and CO feature prominently in many of their predicted metabolisms. Despite 25 years of intense study, key questions remain on life in the deep subsurface, including whether it is endemic and the extent of its involvement in the anaerobic formation and degradation of hydrocarbons. Emergent data from cultivation and next-generation sequencing approaches continue to provide promising new hints to answer these questions. As Gold suggested, and as has become increasingly evident, to better understand the subsurface is critical to further understanding the Earth, life, the evolution of life, and the potential for life elsewhere. To this end, we suggest the need to develop a robust network of interdisciplinary scientists and accessible field sites for long-term monitoring of the Earth\'s subsurface in the form of a deep subsurface microbiome initiative."