Regulation of metabolic pathways in sulfobacilli under different aeration regimes

A comparative study of the activities of the enzymes of carbon metabolism from the cells of moderately thermophilic chemolithotrophic bacteria Sulfobacillus sibiricus (strains N1 and SSO) and Sulfobacillus thermosulfidooxidans subsp. asporogenes (strain 41) was carried out grown in a high layer of medium without forced aeration and cells grown with intense aeration. Limited air access to the growing S. sibiricus N1 cells resulted in switching from the pentose phosphate pathway of glucose metabolism to the Entner-Doudoroff pathway while the Embden-Meyerhof-Parnas pathway persisted. Irrespective of the level of the aeration, in the cells of S. sibiricus SSO and S. thermosulfidooxidans subsp. asporogenes 41, degradation of the glucose occurred via the Entner-Doudoroff and pentose phosphate metabolic pathways, respectively, as well as via the Embden-Meyerhof-Parnas pathway. Prolonged growth of S. sibiricus, strains N1 and SSO, in a high layer of the medium without forced aeration led to the repression of synthesis of most of the tricarboxylic acid cycle (TCA cycle) enzymes, in particular dehydrogenases, as well as of some carboxylases including RuBisCO. The traits of carbon metabolism in various strains of Sulfobacillus under conditions of oxygen deficiency are discussed.     

Sulfur-Metabolizing Enzymes in Thermoacidophilic Bacteria Sulfobacillus sibiricus

Sulfur oxygenase, sulfite oxidase, adenylyl sulfate reductase, rhodanase, sulfur : Fe(III) oxidoreductase, and sulfite : Fe(III) oxidoreductase were found in cells of aerobic thermoacidophilic bacteria Sulfobacillus sibiricus, strains N1 and SSO. Enzyme activity was revealed in the cells grown on medium with elemental sulfur or in the presence of various sulfide minerals and concentrates of sulfide ores. The activity of enzymes of sulfur metabolism depended little on the degree of aeration during bacterial growth.     

Sulfur metabolism enzymes in thermoacidophilus bacteria Sulfobacillus sibiricus

Sulfur oxygenase, sulfite oxidase, adenylyl sulfate reductase, rhodanase, sulfur:Fe(III) oxidoreductase, and sulfite:Fe(III) oxidoreductase were found in cells of aerobic thermoacidophilic bacteria Sulfobacillus sibiricus strains N1 and SSO. Enzyme activity was revealed in cells grown on the medium with elemental sulfur or in the presence of various sulfide elements and concentrates of sulfide ores. The activity of sulfur-metabolizing enzymes depended little on the degree of aeration during bacterial growth.     

The dependence of intracellular ATP level on the nutrition mode of the acidophilic bacteria <Emphasis Type="Italic">Sulfobacillus thermotolerans</Emphasis> and <Emphasis Type="Italic">Alicyclobacillus tolerans</Emphasis>

The dynamics of the ATP pool in the aerobic spore-forming acidothermophilic mixotrophic bacteria Sulfobacillus thermotolerans Kr1^T and Alicyclobacillus tolerans K1^T were studied in the course of their chemolithoheterotrophic, chemoorganoheterotrophic, and chemolithoautotrophic growth. It was established that, during mixotrophic growth, the maximum ATP concentrations in the cells of S. thermotolerans Kr1 and A. tolerans K1 were 3.8 and 0.6 nmol/mg protein, respectively. The ATP concentrations in sulfobacilli and alicyclobacilli during organotrophic growth were 2.2 and 3.1 nmol/mg protein, respectively. In the cells of the obligately heterotrophic bacterium Alicyclobacillus cycloheptanicus 4006^T, the maximum ATP concentration was several times higher and reached 12.3 nmol/mg protein. During lithotrophic growth, the maximum values of the ATP concentration in the cells of S. thermotolerans Kr1 and A. tolerans K1 were 0.3 and <0.1 nmol/mg protein, respectively; in the cells of the autotrophic bacterium Acidithiobacillus ferrooxidans TFBk, the ATP content was about 60–300 times higher (17.0 nmol/mg protein). It is concluded that low ATP content is among the possible causes of growth cessation of S. thermotolerans Kr1 and A. tolerans K1 under auto-and heterotrophic conditions after several culture transfers.     

Patterns of growth and oxidation of natural pyrites by the representatives of acidophilic chemolithotrophic microorganisms

The patterns of the growth and oxidation of different types of natural pyrites were studied for the three microbial species adapted to these substrates and belonging to phylogenetically remote groups: gram-negative bacterium Acidithiobacillus ferrooxidans, gram-positive bacterium Sulfobacillus thermotolerans, and the archaeon Ferroplasma acidiphilum. For both A. ferrooxidans strains, TFV-1 and TFBk, pyrite 4 appeared to be the most difficult to oxidize and grow; pyrite 5 was oxidized by both strains at an average rate, and pyrite 3 was the most readily oxidized. On each of the three pyrites, growth and oxidation by TFBk were more active than by TFV-1. The effectiveness of the adaptation of S. thermotolerans Kr1^T was low compared to the A. ferrooxidans strains; however, the adapted strain Kr1^T showed the highest growth rate on pyrite 3 among all the cultures studied. No adaptation of strain Kr1^T to pyrite 5 was observed; the rates of growth and pyrite oxidation in the third transfer were lower than in the first transfer. The strain F. acidiphilum Y^T was not adapted to pyrites 3 and 5; the rates of growth and pyrite oxidation were the same in the first five transfers. The strains of three species of the microorganisms studied, A. ferrooxidans, S. thermotolerans, and F. acidiphilum, grew on pyrite 3 (holetype (p) conductivity) and oxidized it better than pyrite 5 (mixed-type (n-p) conductivity). The most readily oxidized were the pyrites with a density of 5.6–5.7 g/cm³ and high resistance values (ln R = 8.8). The pyrite oxidation rate did not depend on the type of conductivity. Changes in the chromosomal DNA structure were revealed in strain TFBk on adaptation to pyrites 3 and 4 and in the TFV-1 plasmid profile on adaptation to pyrite 3. Correlation between genetic variability and adaptive capabilities was shown for A. ferrooxidans. No changes in the chromosomal DNA structure were found in S. thermotolerans Kr1^T and F. acidiphilum Y^T on adaptation to pyrites 3 and 5. Plasmids were absent in the cells of these cultures.     

Strain polymorphism of the plasmid profiles in <Emphasis Type="Italic">Sulfobacillus</Emphasis> species

Plasmids were discovered for the first time in strains belonging to different species of the genus Sulfobacillus: S. thermosulfidooxidans, S. sibiricus, S. thermotolerans, “S. olympiadicus”, and S. acidophilus. The plasmids were detected in the cells of four out of eight strains grown on a medium with ferrous iron. Adaptation to elementary sulfur was accompanied by changes in the plasmid profiles in two out of seven strains. Plasmids were detected in all the studied strains of sulfobacilli after adaptation to the pyrite-arsenopyrite ore concentrate from the Nezhdaninskoe deposit containing gold, silver, zinc, copper, and lead. No plasmids were found in S. thermotolerans Kr1^T after four transfers on a medium containing iron and 0.018 mM Ag⁺. After adaptation of the same strain to 765 mM Zn²⁺, only one plasmid was found in the cells, the largest among those detected earlier in this culture adapted to the Nezhdaninskoe ore concentrate. The strain S. thermotolerans Kr1^T, after four transfers on media with either 78 mM Cu²⁺ or 2 mM Pb²⁺, did not contain plasmids. The presence of plasmids in the cells of sulfobacilli did not influence their resistance to the ions of the studied metals.     

Genotypic and phenotypic polymorphism of environmental strains of the moderately thermophilic bacterium <Emphasis Type="Italic">Sulfobacillus sibiricus</Emphasis>

Five cultures of moderately thermophilic spore-forming acidophilic chemolithotrophic bacteria were isolated from the zones of spontaneous heating of pyrrhotite-containing pyrite-arsenopyrite gold-arsenic sulfide ores in an operating open pit (strains B1, B2, B3, OFO, and SSO). Analysis of the chromosomal DNA structure revealed the differences between these cultures at the strain level (apart from B3 and SSO, which had identical restriction profiles). All the strains had a similar G+C DNA molar content (47.4–48.3%). The level of DNA reassociation was 85 to 95%. The similarity between the DNA of the type strain Sulfobacillus sibiricus N1 isolated from arsenopyrite ore concentrate and that of these strains (83–93%) indicates that they belong to the same species. The strains had similar values of pH and temperature optimal for growth on ferrous iron (1.6–2.0 and 45–55°C, respectively). They were mixotrophs; Fe(II), S^o, and sulfide minerals along with organic compounds were used as energy sources and electron donors. However, the kinetic parameters of growth and substrate oxidation varied from strain to strain. Genetic variety of the strains from diverse ecosystems and environments is possibly the result of the different rates of microevolution processes.     

Phenotypic properties of <Emphasis Type="Italic">Sulfobacillus thermotolerans</Emphasis>: Comparative aspects

The phenotypic characteristics of the species Sulfobacillus thermotolerans Kr1^T, as dependent on the cultivation conditions, are described in detail. High growth rates (0.22–0.30 h^?1) and high oxidative activity were recorded under optimum mixotrophic conditions at 40 °C on medium with inorganic (Fe(II), S⁰, or pyrite-arsenopyrite concentrate) and organic (glucose and/or yeast extract) substrates. In cells grown under optimum conditions on medium with iron, hemes a, b, and, most probably, c were present, indicating the presence of the corresponding cytochromes. Peculiar extended structures in the form of cylindrical cords, never observed previously, were revealed; a mucous matrix, likely of polysaccharide nature, occurred around the cells. In the cells of sulfobacilli grown litho-, organo-, and mixotrophically at 40 °C, the enzymes of the three main pathways of carbon utilization and some enzymes of the TCA cycle were revealed. The enzyme activity was maximum under mixotrophic growth conditions. The growth rate in the regions of limiting temperatures (55 °C and 12–14 °C) decreased two-and tenfold, respectively; no activity of 6-phosphogluconate dehydrogenase, one of the key enzymes of the oxidative pentose phosphate pathway, could be revealed; and a decrease in the activity of almost all enzymes of glucose metabolism and of the TCA cycle was observed. The rate of ¹⁴CO₂ fixation by cells under auto-, mixo-, and heterotrophic conditions constituted 31.8, 23.3, and 10.3 nmol/(h mg protein), respectively. The activities of RuBP carboxylase (it peaked during lithotrophic growth) and of carboxylases of heterotrophic carbon dioxide fixation were recorded. The physiological and biochemical peculiarities of the thermotolerant bacillus are compared versus moderately thermophilic sulfobacilli.     

Activity of the Enzymes of Carbon Metabolism in Sulfobacillus sibiricus under Various Conditions of Cultivation

The thermoacidophilic iron-oxidizing chemolithotroph Sulfobacillus sibiricus N1^T is characterized by steady growth and amplified cell yield when grown in vigorously aerated medium containing Fe²⁺, glucose, and yeast extract as energy sources. In this case, carbon dioxide, glucose, and yeast extract are used as carbon sources. Glucose is assimilated through the fructose-bisphosphate pathway and the pentose-phosphate pathway. The glyoxylate bypass does not function in S. sibiricus, and the tricarboxylic acid cycle is disrupted at the level of 2-oxoglutarate dehydrogenase. The presence of ribulose-bisphosphate carboxylase indicates that carbon dioxide fixation proceeds through the Calvin cycle. The activity of ribulose-bisphosphate carboxylase is highest in autotrophically grown cells. The cells also contain pyruvate carboxylase, phosphoenolpyruvate carboxylase, phosphoenolpyruvate carboxykinase, and phosphoenolpyruvate carboxytransphosphorylase.     

Melanin Production and Use as a Soluble Electron Shuttle for Fe(III) Oxide Reduction and as a Terminal Electron Acceptor by Shewanella algae BrY

Dissimilatory metal-reducing bacteria (DMRB) utilize numerous compounds as terminal electron acceptors, including insoluble iron oxides. The mechanism(s) of insoluble-mineral reduction by DMRB is not well understood. Here we report that extracellular melanin is produced by Shewanella algae BrY. The extracted melanin served as the sole terminal electron acceptor. Upon reduction the reduced, soluble melanin reduced insoluble hydrous ferric oxide in the absence of bacteria, thus demonstrating that melanin produced by S. algae BrY is a soluble Fe(III)-reducing compound. In the presence of bacteria, melanin acted as an electron conduit to Fe(III) minerals and increased Fe(III) mineral reduction rates. Growth of S. algae BrY occurred in anaerobic minimal medium supplemented with melanin extracted from previously grown aerobic cultures of S. algae BrY. Melanin produced by S. algae BrY imparts increased versatility to this organism as a soluble Fe(III) reductant, an electron conduit for iron mineral reduction, and a sole terminal electron acceptor that supports growth.     

Comparative analysis of membranous proteomics of Shewanella decolorationis S12 grown with azo compound or Fe (III) citrate as sole terminal electron acceptor

Shewanella decolorationis S12 is capable of carrying out anaerobic respiration using azo dyes and Fe (III) citrate as electron acceptors. In the present study, proteomic techniques including two-dimensional gel electrophoresis (2-DE) and matrix-assisted laser desorption/ionization time-of-flight/time-of-flight mass spectrometry were used to analyze the similarity and the dissimilarity of the membrane proteins isolated from strain S12 cells grown in amaranth or Fe (III) citrate with defined inorganic salt medium. The cells of strain S12 grown under a saturated dissolved oxygen condition served as controls. This is the first work that made the comparative analysis of cell membranous proteomics of strain S12 grown with azo compound or Fe (III) citrate as a sole terminal electron acceptor. The results showed that most of the membrane proteins of strain S12 under azo respiration are similar to those under Fe (III) respiration, but dissimilar from those of oxygen-grown cells. FdnH and FrdB were expressed specifically in azo respiration. NqrA-2, DctP, and hypothetical protein SO_4719 showed relative overexpression in azo respiration compared with Fe (III) respiration. OmpA family protein SO_3545 was detected to be specific to Fe (III) respiration. Furthermore, ArgF, SdhA, and HoxK were expressed markedly in both amaranth- and Fe (III) citrate-grown cultures compared with oxygen-grown cultures.     

Going Wireless: Fe(III) Oxide Reduction without Pili by Geobacter sulfurreducens Strain JS-1

Previous studies have suggested that the conductive pili of Geobacter sulfurreducens are essential for extracellular electron transfer to Fe(III) oxides and for optimal long-range electron transport through current-producing biofilms. The KN400 strain of G. sulfurreducens reduces poorly crystalline Fe(III) oxide more rapidly than the more extensively studied DL-1 strain. Deletion of the gene encoding PilA, the structural pilin protein, in strain KN400 inhibited Fe(III) oxide reduction. However, low rates of Fe(III) reduction were detected after extended incubation (>30 days) in the presence of Fe(III) oxide. After seven consecutive transfers, the PilA-deficient strain adapted to reduce Fe(III) oxide as fast as the wild type. Microarray, whole-genome resequencing, proteomic, and gene deletion studies indicated that this adaptation was associated with the production of larger amounts of the c-type cytochrome PgcA, which was released into the culture medium. It is proposed that the extracellular cytochrome acts as an electron shuttle, promoting electron transfer from the outer cell surface to Fe(III) oxides. The adapted PilA-deficient strain competed well with the wild-type strain when both were grown together on Fe(III) oxide. However, when 50% of the culture medium was replaced with fresh medium every 3 days, the wild-type strain outcompeted the adapted strain. A possible explanation for this is that the necessity to produce additional PgcA, to replace the PgcA being continually removed, put the adapted strain at a competitive disadvantage, similar to the apparent selection against electron shuttle-producing Fe(III) reducers in many anaerobic soils and sediments. Despite increased extracellular cytochrome production, the adapted PilA-deficient strain produced low levels of current, consistent with the concept that long-range electron transport through G. sulfurreducens biofilms is more effective via pili.     

Effect of Growth Conditions and Trehalose Content on Cryotolerance of Bakers' Yeast in Frozen Doughs

The cryotolerance in frozen doughs and in water suspensions of bakers' yeast (Saccharomyces cerevisiae) previously grown under various industrial conditions was evaluated on a laboratory scale. Fed-batch cultures were very superior to batch cultures, and strong aeration enhanced cryoresistance in both cases for freezing rates of 1 to 56°C min⁻¹. Loss of cell viability in frozen dough or water was related to the duration of the dissolved-oxygen deficit during fed-batch growth. Strongly aerobic fed-batch cultures grown at a reduced average specific rate (μ = 0.088 h⁻¹ compared with 0.117 h⁻¹) also showed greater trehalose synthesis and improved frozen-dough stability. Insufficient aeration (dissolved-oxygen deficit) and lower growth temperature (20°C instead of 30°C) decreased both fed-batch-grown yeast cryoresistance and trehalose content. Although trehalose had a cryoprotective effect in S. cerevisiae, its effect was neutralized by even a momentary lack of excess dissolved oxygen in the fed-batch growth medium.     

Functional analysis of phosphorylation on Saccharomyces cerevisiae syntaxin 1 homologues Sso1p and Sso2p

Background

The Saccharomyces cerevisiae syntaxin1 homologues Sso1p and Sso2p perform an essential function in membrane fusion in exocytosis. While deletion of either SSO1 or SSO2 causes no obvious phenotype in vegetatively grown cells, deletion of both genes is lethal. In sporulating diploid S. cerevisiae cells only Sso1p, but not Sso2p, is needed for membrane fusion during prospore membrane formation. Mass spectrometry and in vivo labeling data suggest that serines 23, 24, and 79 in Sso1p and serines 31 and 34 in Sso2p can be phosphorylated in vivo. Here we set out to assess the contribution of phosphorylation on Sso protein in vivo function.

Principal Findings

Different mutant versions of SSO1 and SSO2 were generated to target the phosphorylation sites in Sso1p and Sso2p. Basal or overexpression of phospho-mimicking or putative non-phosphorylated Sso1p or Sso2p mutants resulted in no obvious growth phenotype. However, S79A and S79E mutations caused a mild defect in the ability of Sso1p to complement the temperature-sensitive growth phenotype of sso2-1 sso1Δ cells. Combination of all mutations did not additionally compromise Sso1p in vivo function. When compared to the wild type SSO1 and SSO2, the phosphoamino acid mutants displayed similar genetic interactions with late acting sec mutants. Furthermore, diploid cells expressing only the mutant versions of Sso1p had no detectable sporulation defects. In addition to sporulation, also pseudohyphal and invasive growth modes are regulated by the availability of nutrients. In contrast to sporulating diploid cells, deletion of SSO1 or SSO2, or expression of the phospho-mutant versions of SSO1 or SSO2 as the sole copies of SSO genes caused no defects in haploid or diploid pseudohyphal and invasive growth.

Conclusions

The identified phosphorylation sites do not significantly contribute to the in vivo functionality of Sso1p and Sso2p in S. cerevisiae.     

Role of dissimilatory fermentative iron-reducing bacteria in Fe uptake by common bean (Phaseolus vulgaris L.) plants grown in alkaline soil

Iron (Fe) is an essential element for plant growth and development. Some plant growth-promoting rhizobacteria can increase Fe uptake by plants through reduction of Fe(III) to Fe(II) at the root surface. The aim of this work was to identify novel bacterial strains with high Fe(III) reduction ability and to evaluate their role in plant Fe uptake. Four bacterial strains (UMCV1 to UMCV4) showing dissimilatory Fe-reducing activity were isolated from the rhizosphere of bean and maize plants and further identified by 16S rDNA amplification and sequence analysis. From these analyses, UMCV1 and UMCV2 isolates were identified as Bacillus megaterium and Arthrobacter spp., respectively, whereas UMCV3 and UMCV4 were identified as Stenotrophomonas maltophilia. All four isolates showed Fe reduction in a nonflooded soil and when associated with roots of bean plants grown in alkaline soil or in mineral medium. In addition, the bacterial isolates were able to stimulate plant growth in vitro and on a broad level, plants grown in inoculated soil were generally bigger and with higher Fe content than those grown in sterilized soil. These results indicate that bacterial species isolated from the rhizosphere of bean and maize plants contribute significantly to Fe uptake by plants likely through increased Fe(III) reduction in the rhizosphere.     

Use of Fe(III) as an Electron Acceptor To Recover Previously Uncultured Hyperthermophiles: Isolation and Characterization of Geothermobacterium ferrireducens gen. nov., sp. nov.

It has recently been recognized that the ability to use Fe(III) as a terminal electron acceptor is a highly conserved characteristic in hyperthermophilic microorganisms. This suggests that it may be possible to recover as-yet-uncultured hyperthermophiles in pure culture if Fe(III) is used as an electron acceptor. As part of a study of the microbial diversity of the Obsidian Pool area in Yellowstone National Park, Wyo., hot sediment samples were used as the inoculum for enrichment cultures in media containing hydrogen as the sole electron donor and poorly crystalline Fe(III) oxide as the electron acceptor. A pure culture was recovered on solidified, Fe(III) oxide medium. The isolate, designated FW-1a, is a hyperthermophilic anaerobe that grows exclusively by coupling hydrogen oxidation to the reduction of poorly crystalline Fe(III) oxide. Organic carbon is not required for growth. Magnetite is the end product of Fe(III) oxide reduction under the culture conditions evaluated. The cells are rod shaped, about 0.5 μm by 1.0 to 1.2 μm, and motile and have a single flagellum. Strain FW-1a grows at circumneutral pH, at freshwater salinities, and at temperatures of between 65 and 100°C with an optimum of 85 to 90°C. To our knowledge this is the highest temperature optimum of any organism in the Bacteria. Analysis of the 16S ribosomal DNA (rDNA) sequence of strain FW-1a places it within the Bacteria, most closely related to abundant but uncultured microorganisms whose 16S rDNA sequences have been previously recovered from Obsidian Pool and a terrestrial hot spring in Iceland. While previous studies inferred that the uncultured microorganisms with these 16S rDNA sequences were sulfate-reducing organisms, the physiology of the strain FW-1a, which does not reduce sulfate, indicates that these organisms are just as likely to be Fe(III) reducers. These results further demonstrate that Fe(III) may be helpful for recovering as-yet-uncultured microorganisms from hydrothermal environments and illustrate that caution must be used in inferring the physiological characteristics of at least some thermophilic microorganisms solely from 16S rDNA sequences. Based on both its 16S rDNA sequence and physiological characteristics, strain FW-1a represents a new genus among the Bacteria. The name Geothermobacterium ferrireducens gen. nov., sp. nov., is proposed (ATCC BAA-426).     

Effect of cycloheximide, iodoacetamide, and antimycin A on inorganic phosphate synthesis in Saccharomyces cerevisiae VKM Y-1173

The effect of inhibitors of protein synthesis (cycloheximide, CHI), glycolysis (iodoacetamide, IAA), and oxidative phosphorylation (antimycin A, ANM) on inorganic phosphate (polyP) synthesis during the first 0.5 h of their hypercompensation in Saccharomyces cerevisiae VKM Y-l173 grown on 2% glucose-containing media at low (hypoxia) or high aeration rates or in the presence of 1 vol % ethanol under high aeration conditions was studied. PolyP accumulation was highest in the medium with glucose under hypoxia; lower, with glucose at high aeration; and lowest, in the medium with ethanol. CHI had a small effect on the total polyP level but significantly stimulated ATP accumulation, irrespective of the culture growth conditions. The low-polymer acid-soluble polyP1 were synthesized most actively by the cells grown on glucose under hypoxia, alkali-soluble polyP3 were synthesized at en hanced aeration, and the most hig-molecular fraction, polyP5, was actively accumulated along with polyP3 at cultivation on ethanol. Regardless of the growth conditions, CHI inhibited accumulation of polyP4, the synthesis of which is associated with the synthesis of mannoproteins. IAA and ANM largely inhibited synthesis of all fractions at yeast growth under hypoxia and on ethanol, respectively. The results as a whole demonstrate the dependence of polyP formation on the main energy-generating cell processes and, at the same time, the absence of direct dependence of their synthesis on ATP concentration in Saccharomyces cerevisiae VKM Y-l 173.     

HdrC2 from Acidithiobacillus ferrooxidans Owns Two Iron–Sulfur Binding Motifs But Binds Only One Variable Cluster Between [4Fe–4S] and [3Fe–4S]

The heterodisulfide reductase complex HdrABC from Acidithiobacillus ferrooxidans was suggested to own novel features that act in reverse to convert the sulfane sulfur of GS _n H species (n > 1) into sulfite in sulfur oxidation. The HdrC subunit is potentially encoded by two different highly upregulated genes sharing only 29 % identity in A. ferrooxidans grown in sulfur-containing medium, which were named as HdrC1 and HdrC2, respectively and had been confirmed to contain iron–sulfur cluster by expression and characterization, especially the HdrC1 which had been showed to bind only one [4Fe–4S] cluster by mutations. However, the mutations of the HdrC2 remain to be done and the detailed binding information of it is still unclear. Here, we report the expression, mutations, and molecular modeling of the HdrC2 from A. ferrooxidans. This HdrC2 had two identical motifs (Cx₂Cx₂Cx₃C) containing total of eight cysteine residues potentially for iron–sulfur cluster binding. This purified HdrC2 was exhibited to contain one variable cluster converted between [4Fe–4S] and [3Fe–4S] according to different conditions by the UV-scanning and EPR spectra. The site-directed mutagenesis results of these eight residues further confirmed that the HdrC2 in reduction with Fe²⁺ condition loaded only one [4Fe–4S]⁺ with spin S = 1/2 ligated by the residues of Cys73, Cys109, Cys112, and Cys115; the HdrC2 in natural aeration condition lost the Fe atom ligated by the residue of Cys73 and loaded only one [3Fe–4S]⁰ with spin S = 0; the HdrC2 in oxidation condition loaded only one [3Fe–4S]⁺ with spin S = 1/2. Molecular modeling results were also in line with the experiment results.     

Dissimilatory Fe(III) Reduction by the Marine Microorganism Desulfuromonas acetoxidans

The ability of the marine microorganism Desulfuromonas acetoxidans to reduce Fe(III) was investigated because of its close phylogenetic relationship with the freshwater dissimilatory Fe(III) reducer Geobacter metallireducens. Washed cell suspensions of the type strain of D. acetoxidans reduced soluble Fe(III)-citrate and Fe(III) complexed with nitriloacetic acid. The c-type cytochrome(s) of D. acetoxidans was oxidized by Fe(III)-citrate and Mn(IV)-oxalate, as well as by two electron acceptors known to support growth, colloidal sulfur and malate. D. acetoxidans grew in defined anoxic, bicarbonate-buffered medium with acetate as the sole electron donor and poorly crystalline Fe(III) or Mn(IV) as the sole electron acceptor. Magnetite (Fe₃O₄) and siderite (FeCO₃) were the major end products of Fe(III) reduction, whereas rhodochrosite (MnCO₃) was the end product of Mn(IV) reduction. Ethanol, propanol, pyruvate, and butanol also served as electron donors for Fe(III) reduction. In contrast to D. acetoxidans, G. metallireducens could only grow in freshwater medium and it did not conserve energy to support growth from colloidal S⁰ reduction. D. acetoxidans is the first marine microorganism shown to conserve energy to support growth by coupling the complete oxidation of organic compounds to the reduction of Fe(III) or Mn(IV). Thus, D. acetoxidans provides a model enzymatic mechanism for Fe(III) or Mn(IV) oxidation of organic compounds in marine and estuarine sediments. These findings demonstrate that 16S rRNA phylogenetic analyses can suggest previously unrecognized metabolic capabilities of microorganisms.     

A culture-independent PCR-based method for the detection of Lachancea thermotolerans in wine

When inoculated in association with Saccharomyces cerevisiae, the yeast Lachancea thermotolerans determines a reduction of volatile acidity and an increase in the production of glycerol, 2-phenylethanol, and polysaccharides. Moreover, L. thermotolerans is a natural L-lactic acid producer, thus it contributes to wine acidification and microbiological stabilization. In view of its utilization in winemaking, a culture-independent PCR-based method was developed for the detection of L. thermotolerans during wine fermentations. This method, which utilizes species-specific PCR primer pairs that anneal to intron 2 of the mitochondrial COX1 gene, is rapid and reliable, and detects L. thermotolerans in wine at 10⁴ cells/ml and with a S. cerevisiae/L. termotholerans ratio of 1,000/1.