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10 result(s) for "Galushko, Alexander"
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Growth of nitrite-oxidizing bacteria by aerobic hydrogen oxidation
The bacterial oxidation of nitrite to nitrate is a key process of the biogeochemical nitrogen cycle. Nitrite-oxidizing bacteria are considered a highly specialized functional group, which depends on the supply of nitrite from other microorganisms and whose distribution strictly correlates with nitrification in the environment and in wastewater treatment plants. On the basis of genomics, physiological experiments, and single-cell analyses, we show that Nitrospira moscoviensis, which represents a widely distributed lineage of nitrite-oxidizing bacteria, has the genetic inventory to utilize hydrogen (H₂) as an alternative energy source for aerobic respiration and grows on H₂ without nitrite. CO₂ fixation occurred with H₂ as the sole electron donor. Our results demonstrate a chemolithoautotrophic lifestyle of nitrite-oxidizing bacteria outside the nitrogen cycle, suggesting greater ecological flexibility than previously assumed.
Enrichment and Genome Sequence of the Group I.1a Ammonia-Oxidizing Archaeon “Ca. Nitrosotenuis uzonensis” Representing a Clade Globally Distributed in Thermal Habitats
The discovery of ammonia-oxidizing archaea (AOA) of the phylum Thaumarchaeota and the high abundance of archaeal ammonia monooxygenase subunit A encoding gene sequences in many environments have extended our perception of nitrifying microbial communities. Moreover, AOA are the only aerobic ammonia oxidizers known to be active in geothermal environments. Molecular data indicate that in many globally distributed terrestrial high-temperature habits a thaumarchaeotal lineage within the Nitrosopumilus cluster (also called \"marine\" group I.1a) thrives, but these microbes have neither been isolated from these systems nor functionally characterized in situ yet. In this study, we report on the enrichment and genomic characterization of a representative of this lineage from a thermal spring in Kamchatka. This thaumarchaeote, provisionally classified as \"Candidatus Nitrosotenuis uzonensis\", is a moderately thermophilic, non-halophilic, chemolithoautotrophic ammonia oxidizer. The nearly complete genome sequence (assembled into a single scaffold) of this AOA confirmed the presence of the typical thaumarchaeotal pathways for ammonia oxidation and carbon fixation, and indicated its ability to produce coenzyme F420 and to chemotactically react to its environment. Interestingly, like members of the genus Nitrosoarchaeum, \"Candidatus N. uzonensis\" also possesses a putative artubulin-encoding gene. Genome comparisons to related AOA with available genome sequences confirmed that the newly cultured AOA has an average nucleotide identity far below the species threshold and revealed a substantial degree of genomic plasticity with unique genomic regions in \"Ca. N. uzonensis\", which potentially include genetic determinants of ecological niche differentiation.
Recent Origin of the Methacrylate Redox System in Geobacter sulfurreducens AM-1 through Horizontal Gene Transfer
The origin and evolution of novel biochemical functions remains one of the key questions in molecular evolution. We study recently emerged methacrylate reductase function that is thought to have emerged in the last century and reported in Geobacter sulfurreducens strain AM-1. We report the sequence and study the evolution of the operon coding for the flavin-containing methacrylate reductase (Mrd) and tetraheme cytochrome с (Mcc) in the genome of G. sulfurreducens AM-1. Different types of signal peptides in functionally interlinked proteins Mrd and Mcc suggest a possible complex mechanism of biogenesis for chromoproteids of the methacrylate redox system. The homologs of the Mrd and Mcc sequence found in δ-Proteobacteria and Deferribacteres are also organized into an operon and their phylogenetic distribution suggested that these two genes tend to be horizontally transferred together. Specifically, the mrd and mcc genes from G. sulfurreducens AM-1 are not monophyletic with any of the homologs found in other Geobacter genomes. The acquisition of methacrylate reductase function by G. sulfurreducens AM-1 appears linked to a horizontal gene transfer event. However, the new function of the products of mrd and mcc may have evolved either prior or subsequent to their acquisition by G. sulfurreducens AM-1.
Cysteine-mediated electron transfer in syntrophic acetate oxidation by cocultures of Geobacter sulfurreducens and Wolinella succinogenes
Syntrophic cocultures of Geobacter sulfurreducens and Wolinella succinogenes oxidize acetate with nitrate as terminal electron acceptor. It has been postulated earlier that electrons are transferred in these cocultures not via hydrogen, but via a different carrier, e.g., a small c-type cytochrome that is detected in the supernatant of growing cultures. In the present study, L -cysteine, which was provided as a reducing agent, was found to mediate the electron transfer between the two partners. Low concentrations of L -cysteine or L -cystine (10-100 microM) supported syntrophic growth, and no acetate oxidation was observed in the absence of cysteine or cystine. Cell suspensions of G. sulfurreducens or coculture cell suspensions reduced cystine to cysteine, and suspensions of W. succinogenes or coculture suspensions oxidized cysteine with nitrate, as measured by the formation or depletion of free thiol groups. Added cysteine was rapidly oxidized by the coculture during growth, but the formed cystine was not entirely rereduced even under acceptor-limited conditions. The redox potential prevailing in acetate-oxidizing cocultures was -160 to -230 mV. Sulfide at low concentrations supported syntrophic growth as well and could replace cysteine. Neither growth nor acetate degradation was found with D-cysteine, homocysteine, cysteamine, 3-mercaptopropionate, dithiothreithol, thioglycolate, glutathione, coenzyme M, dimethylsulfoxide, trimethylamine- N-oxide, anthraquinone-2,6-disulfonate, or ascorbate.
Cyanate as an energy source for nitrifiers
The ammonia-oxidizing archaeon Nitrososphaera gargensis can utilize cyanate as the only source of energy for growth due to the presence of a cyanase enzyme, and cyanase-encoding nitrite-oxidizing bacteria can work together with cyanase-negative ammonia oxidizers to collectively grow on cyanate via reciprocal feeding; cyanases are widespread in the environment according to metagenomic data sets, pointing to the potential importance of cyanate in the nitrogen cycle. Cyanate an unexpected energy source Nitrification is a central process in the global nitrogen cycle and plays a major role in fertilizer loss in industrial agriculture. Here Michael Wagner and colleagues report that the ammonia-oxidizing archaeon Nitrosphaera gargensis can grow on cyanate as its sole energy source — possibly the only known organism capable of doing so. The archaeon converts cyanate to ammonium and carbon dioxide using a cyanase enzyme. Further investigation of metagenomes shows that cyanases are widespread in the environment. This work highlights the potential importance of cyanate in the nitrogen cycle as a source of reduced nitrogen in the environment. Ammonia- and nitrite-oxidizing microorganisms are collectively responsible for the aerobic oxidation of ammonia via nitrite to nitrate and have essential roles in the global biogeochemical nitrogen cycle. The physiology of nitrifiers has been intensively studied, and urea and ammonia are the only recognized energy sources that promote the aerobic growth of ammonia-oxidizing bacteria and archaea. Here we report the aerobic growth of a pure culture of the ammonia-oxidizing thaumarchaeote Nitrososphaera gargensis 1 using cyanate as the sole source of energy and reductant; to our knowledge, the first organism known to do so. Cyanate, a potentially important source of reduced nitrogen in aquatic and terrestrial ecosystems 2 , is converted to ammonium and carbon dioxide in Nitrososphaera gargensis by a cyanase enzyme that is induced upon addition of this compound. Within the cyanase gene family, this cyanase is a member of a distinct clade also containing cyanases of nitrite-oxidizing bacteria of the genus Nitrospira. We demonstrate by co-culture experiments that these nitrite oxidizers supply cyanase-lacking ammonia oxidizers with ammonium from cyanate, which is fully nitrified by this microbial consortium through reciprocal feeding. By screening a comprehensive set of more than 3,000 publically available metagenomes from environmental samples, we reveal that cyanase-encoding genes clustering with the cyanases of these nitrifiers are widespread in the environment. Our results demonstrate an unexpected metabolic versatility of nitrifying microorganisms, and suggest a previously unrecognized importance of cyanate in cycling of nitrogen compounds in the environment.
Fabrication of composite electrodes based on cobalt (II) hydroxide for microbiological fuel cells
Electrodes of two types have been fabricated for a use in an experimental microbiological fuel cell (MFC). One series consists of a piece of steel mesh covered with a coating of electrodeposited cobalt (II) hydroxide. The other one includes a silicon oxide under-layer obtained with a sol–gel synthesis. Composition, morphology, and electrochemical behavior of the materials have been examined using X-ray photoelectron spectroscopy, scanning electron microscopy, and cyclic voltammetry, respectively. Oxidation state of +2 has been assigned to cobalt species in the as-deposited material. Dynamic cycling of potentials of modified electrodes has resulted in the increase of the cobalt oxidation state in the tested material. Formulas of the cobalt compounds have been proposed. The optimization of electrolyte composition (1 M CH 3 COOK/0.004 M KOH) has allowed to reduce the pH of the solution and extend the voltage window by 100 mV in the positive range of potentials. Cyclic voltammetric experiments have revealed a better cyclability for silica pre-modified electrodes than for electrodes without the under-layer. Microbiological tests have shown compatibility of the obtained electrode materials with bacteria Geobacter sulfurreducens . Two pieces of steel mesh are taken. One of them is used for electrodeposition of cobalt hydroxide without any previous processing. The other one is pre-coated with a layer of silicon oxide before the electrodeposition of cobalt hydroxide. Then cyclic voltammograms of both modified electrodes are compared to show a better electrochemical performance for the electrode with the silica layer. Highlights Silica under-layer improves electrochemical performance of the material based on cobalt (II) hydroxide. The use of an optimized electrolyte composition diminishes pH of solution and extends the voltage range. The electrodes modified with Co(OH) 2 are more preferential for Geobacter sulfurreducens than bare steel mesh.
Recent Origin of the Methacrylate Redox System in Geobacter sulfurreducens AM-1 through Horizontal Gene Transfer: e0125888
The origin and evolution of novel biochemical functions remains one of the key questions in molecular evolution. We study recently emerged methacrylate reductase function that is thought to have emerged in the last century and reported in Geobacter sulfurreducens strain AM-1. We report the sequence and study the evolution of the operon coding for the flavin-containing methacrylate reductase (Mrd) and tetraheme cytochrome с (Mcc) in the genome of G. sulfurreducens AM-1. Different types of signal peptides in functionally interlinked proteins Mrd and Mcc suggest a possible complex mechanism of biogenesis for chromoproteids of the methacrylate redox system. The homologs of the Mrd and Mcc sequence found in delta -Proteobacteria and Deferribacteres are also organized into an operon and their phylogenetic distribution suggested that these two genes tend to be horizontally transferred together. Specifically, the mrd and mcc genes from G. sulfurreducens AM-1 are not monophyletic with any of the homologs found in other Geobacter genomes. The acquisition of methacrylate reductase function by G. sulfurreducens AM-1 appears linked to a horizontal gene transfer event. However, the new function of the products of mrd and mcc may have evolved either prior or subsequent to their acquisition by G. sulfurreducens AM-1.
Anaerobic degradation of m -cresol by Desulfobacterium cetonicum is initiated by formation of 3-hydroxybenzylsuccinate
The anaerobic bacterium Desulfobacterium cetonicum oxidized m-cresol completely with sulfate as electron acceptor. During growth, 3-hydroxybenzylsuccinate (identified by gas chromatography/mass spectroscopy and by comparison of high-performance liquid chromatography retention time and UV spectrum with a chemically synthesized reference compound) accumulated in the medium. This finding indicates that the methyl group of m-cresol is activated by addition to fumarate as in the case of anaerobic toluene metabolism. In cell-free extracts of D. cetonicum, the formation of 3-hydroxybenzylsuccinate from m-cresol and fumarate was detected at an activity of 0.5 nmol min(-1) (mg protein)(-1). This reaction depended strictly on anoxic assay conditions. Treatment with air resulted in a complete loss of activity; however, some activity could be recovered after restoring anoxic conditions. The activity was slightly membrane-associated. 3-Hydroxybenzylsuccinate was degraded via CoA thioesterification and further oxidation to 3-hydroxybenzoyl-CoA as subsequent steps in the degradation pathway.
Enrichment and Genome Sequence of the Group I.1a Ammonia-Oxidizing Archaeon \Ca. Nitrosotenuis uzonensis\ Representing a Clade Globally Distributed in Thermal Habitats: e80835
The discovery of ammonia-oxidizing archaea (AOA) of the phylum Thaumarchaeota and the high abundance of archaeal ammonia monooxygenase subunit A encoding gene sequences in many environments have extended our perception of nitrifying microbial communities. Moreover, AOA are the only aerobic ammonia oxidizers known to be active in geothermal environments. Molecular data indicate that in many globally distributed terrestrial high-temperature habits a thaumarchaeotal lineage within the Nitrosopumilus cluster (also called \"marine\" group I.1a) thrives, but these microbes have neither been isolated from these systems nor functionally characterized in situ yet. In this study, we report on the enrichment and genomic characterization of a representative of this lineage from a thermal spring in Kamchatka. This thaumarchaeote, provisionally classified as \"Candidatus Nitrosotenuis uzonensis\", is a moderately thermophilic, non-halophilic, chemolithoautotrophic ammonia oxidizer. The nearly complete genome sequence (assembled into a single scaffold) of this AOA confirmed the presence of the typical thaumarchaeotal pathways for ammonia oxidation and carbon fixation, and indicated its ability to produce coenzyme F420 and to chemotactically react to its environment. Interestingly, like members of the genus Nitrosoarchaeum, \"Candidatus N. uzonensis\" also possesses a putative artubulin-encoding gene. Genome comparisons to related AOA with available genome sequences confirmed that the newly cultured AOA has an average nucleotide identity far below the species threshold and revealed a substantial degree of genomic plasticity with unique genomic regions in \"Ca. N. uzonensis\", which potentially include genetic determinants of ecological niche differentiation.
Feeling severely affected by Multiple Sclerosis: What does this mean?
Background: The situation for people feeling severely affected by Multiple Sclerosis (MS) remains largely unexamined and the term ‘severe MS’ is not clearly defined. Aim: Our study describes this sub-group of patients utilizing exclusively a subjective inclusion criterion to analyse their reasons for feeling severely affected and document their perceived unmet needs. Design: A questionnaire with open- and closed-ended items addressing only patients feeling severely affected was sent out nationwide. Expanded Disability Status Score (EDSS) and subjectively severe affectedness were analysed for correlation. After dichotomizing both scores by a median split, the answers were allocated to these groups and tested for significant differences. Setting/participants: 1,110 questionnaires were analysed regarding the closed-ended questions while a subsample of 40% (n = 445) was analysed regarding the open-ended questions. Average age of participants was 51.87 years. Average time since diagnosis was 16.6 years. Main course of the disease was secondary progressive (35.5%). Results: The most frequently mentioned reasons for feeling severely affected were lack of mobility (56.4%) and fatigue (27.4%). Significant percentages for unmet needs were seen in the categories of funding services (31.0%), better social integration (24.7%) and medical support (25.2%). A significant correlation was observed between EDSS and subjectively felt affectedness (p ≤ 0.01). Motor disorders explained differences in patient needs behind a higher EDSS score; higher severe affectedness referred to other issues like dependency and immobility. Conclusions: EDSS is insufficient for usage as the sole instrument for measuring severe affectedness as it does not take into account other potential reasons. Complex patient needs necessitate multi-professional care as offered by palliative medicine.