On the energetics of chemolithotrophy in nonequilibrium systems: case studies of geothermal springs in Yellowstone National Park

Chemolithotrophic micro‐organisms are important primary producers in high‐temperature geothermal environments and may catalyse a number of different energetically favourable redox reactions as a primary energy source. Analysis of geochemical constituents followed by chemical speciation and subsequent calculation of reaction free energies (ΔG_rxn) is a useful tool for evaluating the thermodynamic favourability and potential energy available for microbial metabolism. The primary goal of this study was to examine relationships among geochemical gradients and microbial population distribution, and to evaluate the utility of energetic approaches for predicting microbial metabolism from free‐energy calculations, utilizing as examples, several geothermal habitats in Yellowstone National Park where thorough geochemical and phylogenetic analyses have been performed. Acidic (pH ～ 3) and near‐neutral (pH ～ 6–7) geothermal springs were chosen for their range in geochemical properties. Aqueous and solid phase samples obtained from the source pools and the outflow channels of each spring were characterized for all major chemical constituents using laboratory and field methods to accurately measure the concentrations of predominant oxidized and reduced species. Reaction free energies (ΔG_rxn) for 33 oxidation–reduction reactions potentially important to chemolithotrophic micro‐organisms were calculated at relevant spring temperatures after calculating ion activities using an aqueous equilibrium model. Free‐energy values exhibit significant variation among sites for reactions with pH dependence. For example, free‐energy values for reactions involving Fe³⁺ are especially variable across sites due in large part to the pH dependence of Fe³⁺ activity, and exhibit changes of up to 40 kJ mol^?1 electron from acidic to near neutral geothermal springs. Many of the detected 16S rRNA gene sequences represent organisms whose metabolisms are consistent with exergonic processes. However, sensitivity analyses demonstrated that reaction free energies do not generally represent the steep gradients in local geochemical conditions resulting from air–water gas exchange and solid phase deposition that are important in defining microbial habitats and 16S rRNA gene sequence distribution within geothermal outflow channels.     

Ammonia oxidation, denitrification and dissimilatory nitrate reduction to ammonium in two US Great Basin hot springs with abundant ammonia-oxidizing archaea

Many thermophiles catalyse free energy-yielding redox reactions involving nitrogenous compounds; however, little is known about these processes in natural thermal environments. Rates of ammonia oxidation, denitrification and dissimilatory nitrate reduction to ammonium (DNRA) were measured in source water and sediments of two ≈ 80°C springs in the US Great Basin. Ammonia oxidation and denitrification occurred mainly in sediments. Ammonia oxidation rates measured using (15)N-NO(3)(-) pool dilution ranged from 5.5 ± 0.8 to 8.6 ± 0.9 nmol N g(-1) h(-1) and were unaffected or only mildly stimulated by amendment with NH(4) Cl. Denitrification rates measured using acetylene block ranged from 15.8 ± 0.7 to 51 ± 12 nmol N g(-1) h(-1) and were stimulated by amendment with NO(3)(-) and complex organic compounds. The DNRA rate in one spring sediment measured using an (15)N-NO(3)(-) tracer was 315 ± 48 nmol N g(-1) h(-1). Both springs harboured distinct planktonic and sediment microbial communities. Close relatives of the autotrophic, ammonia-oxidizing archaeon 'Candidatus Nitrosocaldus yellowstonii' represented the most abundant OTU in both spring sediments by 16S rRNA gene pyrotag analysis. Quantitative PCR (qPCR) indicated that 'Ca. N. yellowstonii'amoA and 16S rRNA genes were present at 3.5-3.9 × 10(8) and 6.4-9.0 × 10(8) copies g(-1) sediment. Potential denitrifiers included members of the Aquificales and Thermales. Thermus spp. comprised <1% of 16S rRNA gene pyrotags in both sediments and qPCR for T. thermophilus narG revealed sediment populations of 1.3-1.7 × 10(6) copies g(-1) sediment. These data indicate a highly active nitrogen cycle (N-cycle) in these springs and suggest that ammonia oxidation may be a major source of energy fuelling primary production.     

Energy sources for chemolithotrophs in an arsenic- and iron-rich shallow-sea hydrothermal system

The hydrothermally influenced sediments of Tutum Bay, Ambitle Island, Papua New Guinea, are ideal for investigating the chemolithotrophic activities of micro-organisms involved in arsenic cycling because hydrothermal vents there expel fluids with arsenite (As(III)) concentrations as high as 950 μg L(-1) . These hot (99 °C), slightly acidic (pH ~6), chemically reduced, shallow-sea vent fluids mix with colder, oxidized seawater to create steep gradients in temperature, pH, and concentrations of As, N, Fe, and S redox species. Near the vents, iron oxyhydroxides precipitate with up to 6.2 wt% arsenate (As(V)). Here, chemical analyses of sediment porewaters from 10 sites along a 300-m transect were combined with standard Gibbs energies to evaluate the energy yields (-ΔG(r)) from 19 potential chemolithotrophic metabolisms, including As(V) reduction, As(III) oxidation, Fe(III) reduction, and Fe(II) oxidation reactions. The 19 reactions yielded 2-94 kJ mol(-1) e(-) , with aerobic oxidation of sulphide and arsenite the two most exergonic reactions. Although anaerobic As(V) reduction and Fe(III) reduction were among the least exergonic reactions investigated, they are still potential net metabolisms. Gibbs energies of the arsenic redox reactions generally correlate linearly with pH, increasing with increasing pH for As(III) oxidation and decreasing with increasing pH for As(V) reduction. The calculated exergonic energy yields suggest that micro-organisms could exploit diverse energy sources in Tutum Bay, and examples of micro-organisms known to use these chemolithotrophic metabolic strategies are discussed. Energy modeling of redox reactions can help target sampling sites for future microbial collection and cultivation studies.     

Hyperthermophilic Anaerobic Nitrate-Dependent Fe(II) Oxidization by Tibetan Hot Spring Microbiota and the Formation of Fe Minerals

Fe(II) in geothermal fluids was among the most important electron and energy sources for extremophiles and early life, and microbial oxidation of Fe(II) in turn contributed to the global Fe deposits such as banded iron formation (BIF). However, information was rare on Fe(II) bio-oxidation and consequent mineral formation in geothermal systems. In the present study, we investigated the anaerobic nitrate-depending Fe(II) oxidation (ANDFO) in the Tibetan hot springs with temperature ranging 52–86°C. ANDFO cultivation was established by inoculating sediments from the studied hot springs. Positive ANDFO reaction was observed in the cultures from three high-temperature hot springs (>80°C). Phylogenetic analysis showed that bacteria in the three obtained ANDFO cultures were mainly affiliated with phyla of Betaproteobacteria, Alphaproteobacteria, and Firmicutes. In the obtained ANDFO cultures, ferrous iron oxidation occurred with nitrate reduction, accompanied with the formation of magnetite and/or siderite, which could be finished within one week. The resulting euhedral magnetite was at the micrometer scale, which was larger in size and showed better crystallinity than its counterparts (usually <1?µm) formed by chemical reactions. Thus, it can be concluded that ANDFO bacteria and denitrifiers played important roles in the magnetite and siderite precipitation in the studied Tibetan hot springs. The coupling between Fe(II) oxidation and nitrate reduction mediated by thermophiles might provide a new mechanism for euhedral magnetite and siderite deposition in BIFs during the Precambrian period.     

PRODUCTS OF THE OXIDATION OF THIOSULFATE BY BACTERIA IN MINERAL MEDIA

Various cultures (previously described), which oxidize thiosulfate in mineral media have been studied in an attempt to determine the products of oxidation. The transformation of sodium thiosulfate by Cultures B, T, and K yields sodium tetrathionate and sodium hydroxide; secondary chemical reactions result in the accumulation of some tri- and pentathionates, sulfate, and elemental sulfur. As a result of the initial reaction, the pH increases; the secondary reactions cause a drop in pH after this initial rise. The primary reaction yields much less energy than the reactions effected by autotrophic bacteria. No significant amounts of assimilated organic carbon were detected in media supporting representatives of these cultures. It is concluded that they are heterotrophic bacteria. Th. novellus oxidizes sodium thiosulfate to sodium sulfate and sulfuric acid; the pH drops progressively with growth and oxidation. Carbon assimilation typical of autotrophic bacteria was detected; the ratio of sulfate-sulfur formed to carbon assimilated was 56:1. It is calculated that 5.1 per cent of the energy yielded by the oxidation of thiosulfate is accounted for in the organic cell substance synthesized from inorganic materials. This organism is a facultative autotroph. The products of oxidation of sodium thiosulfate by Th. thioparus are sodium sulfate, sulfuric acid, and elemental sulfur; the ratio of sulfate sulfur to elemental sulfur is 3 to 2. The pH decreases during growth and oxidation. The elemental sulfur is produced by the primary reaction and is not a product of secondary chemical changes. The bacterium synthesizes organic compounds from mineral substances during growth. The ratio of thiosulfate-sulfur oxidized to carbon assimilated was 125:1, with 4.7 per cent of the energy of oxidation recovered as organic cell substance. This bacterium is a strict autotroph.     

Standard thermodynamic formation properties for the adenosine 5'-triphosphate series.

The criterion for chemical equilibrium at specified temperature, pressure, pH, concentration of free magnesium ion, and ionic strength is the transformed Gibbs energy, which can be calculated from the Gibbs energy. The apparent equilibrium constant (written in terms of the total concentrations of reactants like adenosine 5'-triphosphate, rather than in terms of species) yields the standard transformed Gibbs energy of reaction, and the effect of temperature on the apparent equilibrium constant at specified pressure, pH, concentration of free magnesium ion, and ionic strength yields the standard transformed enthalpy of reaction. From the apparent equilibrium constants and standard transformed enthalpies of reaction that have been measured in the adenosine 5'-triphosphate series and the dissociation constants of the weak acids and magnesium complexes involved, it is possible to calculate standard Gibbs energies of formation and standard enthalpies of formation of the species involved at zero ionic strength. This requires the convention that the standard Gibbs energy of formation and standard enthalpy of formation for adenosine in dilute aqueous solutions be set equal to zero. On the basis of this convention, standard transformed Gibbs energies of formation and standard transformed enthalpies of formation of adenosine 5'-trisphosphate, adenosine 5'-diphosphate, adenosine 5'-monophosphate, and adenosine at 298.15 K, 1 bar, pH = 7, a concentration of free magnesium ions of 10(-3) M, and an ionic strength of 0.25 M have been calculated.     

Nitrification in terrestrial hot springs of Iceland and Kamchatka

Archaea have been detected recently as a major and often dominant component of the microbial communities performing ammonia oxidation in terrestrial and marine environments. In a molecular survey of archaeal ammonia monooxygenase (AMO) genes in terrestrial hot springs of Iceland and Kamchatka, the amoA gene encoding the alpha-subunit of AMO was detected in a total of 14 hot springs out of the 22 investigated. Most of these amoA-positive hot springs had temperatures between 82 and 97 degrees C and pH range between 2.5 and 7. In phylogenetic analyses, these amoA genes formed three independent lineages within the known sequence clusters of marine or soil origin. Furthermore, in situ gross nitrification rates in Icelandic hot springs were estimated by the pool dilution technique directly on site. At temperatures above 80 degrees C, between 56 and 159 mumol NO(3)(-) L(-1) mud per day was produced. Furthermore, addition of ammonium to the hot spring samples before incubation yielded a more than twofold higher potential nitrification rate, indicating that the process was limited by ammonia supply. Our data provide evidence for an active role of archaea in nitrification of hot springs in a wide range of pH values and at a high temperature.     

Reactivity of hydrogen sulfide with peroxynitrite and other oxidants of biological interest

Hydrogen sulfide (H(2)S) is an endogenously generated gas that can also be administered exogenously. It modulates physiological functions and has reported cytoprotective effects. To evaluate a possible antioxidant role, we investigated the reactivity of hydrogen sulfide with several one- and two-electron oxidants. The rate constant of the direct reaction with peroxynitrite was (4.8±1.4)×10(3)M(-1) s(-1) (pH 7.4, 37°C). At low hydrogen sulfide concentrations, oxidation by peroxynitrite led to oxygen consumption, consistent with a one-electron oxidation that initiated a radical chain reaction. Accordingly, pulse radiolysis studies indicated that hydrogen sulfide reacted with nitrogen dioxide at (3.0±0.3)×10(6)M(-1) s(-1) at pH 6 and (1.2±0.1)×10(7)M(-1) s(-1) at pH 7.5 (25°C). The reactions of hydrogen sulfide with hydrogen peroxide, hypochlorite, and taurine chloramine had rate constants of 0.73±0.03, (8±3)×10(7), and 303±27M(-1) s(-1), respectively (pH 7.4, 37°C). The reactivity of hydrogen sulfide was compared to that of low-molecular-weight thiols such as cysteine and glutathione. Considering the low tissue concentrations of endogenous hydrogen sulfide, direct reactions with oxidants probably cannot completely account for its protective effects.     

Nitrospira-dominated biofilm within a thermal artesian spring: a case for nitrification-driven primary production in a geothermal setting

Water chemistry, energetic modeling, and molecular analyses were combined to investigate the microbial ecology of a biofilm growing in a thermal artesian spring within Hot Springs National Park, AR. This unique fresh water spring has a low dissolved chemical load and is isolated from both light and direct terrestrial carbon input - resulting in an oligotrophic ecosystem limited for fixed carbon and electron donors. Evaluation of energy yields of lithotrophic reactions putatively linked to autotrophy identified the aerobic oxidation of methane, hydrogen, sulfide, ammonia, and nitrite as the most exergonic. Small subunit (SSU) rRNA gene libraries from biofilm revealed a low-diversity microbial assemblage populated by bacteria and archaea at a gene copy ratio of 45:1. Members of the bacterial family 'Nitrospiraceae', known for their autotrophic nitrite oxidation, dominated the bacterial SSU rRNA gene library (approximately 45%). Members of the Thaumarchaeota ThAOA/HWCGIII (>96%) and Thaumarchaeota Group I.1b (2.5%), which both contain confirmed autotrophic ammonia oxidizers, dominated the archaeal SSU rRNA library. Archaea appear to dominate among the ammonia oxidizers, as only ammonia monooxygenase subunit A (amoA) genes belonging to members of the Thaumarchaeota were detected. The geochemical, phylogenetic, and genetic data support a model that describes a novel thermophilic biofilm built largely by an autotrophic nitrifying microbial assemblage. This is also the first observation of 'Nitrospiraceae' as the dominant organisms within a geothermal environment.     

Archaeal and bacterial communities in geochemically diverse hot springs of Yellowstone National Park, USA

Microbiological and geochemical surveys were conducted at three hot springs (Obsidian Pool, Sylvan Spring, and ‘Bison Pool’) in Yellowstone National Park (Wyoming, USA). Microbial community structure was investigated by polymerase chain reaction (PCR) amplification of 16S rRNA gene sequences from DNA extracted from sediments of each hot spring, followed by molecular cloning. Both bacterial and archaeal DNA was retrieved from all samples. No Euryarchaea were found, but diverse Crenarchaea exist in all three pools, particularly affiliating with deep‐branching, but uncultivated organisms. In addition, cloned DNA affiliating with the Desulphurococcales and Thermoproteales was identified, but the distribution of taxa differs in each hot spring. The bacterial community at all three locations is dominated by members of the Aquificales and Thermodesulfobacteriales, indicating that the ‘knallgas’ reaction (aerobic hydrogen oxidation) may be a central metabolism in these ecosystems. To provide geochemical context for the microbial community structures, energy‐yields for a number of chemolithoautotrophic reactions are provided for >80 sampling sites in Yellowstone, including Obsidian Pool, Sylvan Spring, and ‘Bison Pool’. This energy profile shows that the knallgas reaction is just one of many exergonic reactions in the Yellowstone hot springs, that energy‐yields for certain reactions can vary substantially from one site to the next, and that few of the demonstrated exergonic reactions are known to support microbial metabolism.     

Comparative oxidation studies of methionine residues reflect a structural effect on chemical kinetics in rhG-CSF

The effect of protein conformation on the rate of chemical degradation is poorly understood. To address the role of structure on chemical degradation kinetics, comparative oxidation studies of methionine residues in recombinant human granulocyte colony-stimulating factor (rhG-CSF) were performed. The kinetics of oxidation of methionine residues by hydrogen peroxide (H2O2) in rhG-CSF and corresponding chemically synthesized peptides thereof was measured at different temperatures. To assess structural effects, equilibrium denaturation experiments also were conducted on rhG-CSF, yielding the free energy of unfolding as a function of temperature. A comparison of the relative rates of oxidation of methionine residues in short peptides with those of corresponding methionine residues in rhG-CSF yields an understanding of how protein tertiary structure affects oxidation reactions. For the temperature range that was studied, 4-45 degrees C, the oxidation rate constants followed an Arrhenius equation quite well, suggesting the lack of temperature-induced local structural perturbations that affect chemical degradation rates. One of the four methionine residues, Met 122, exhibited an activation energy significantly different from that of the corresponding peptide. Extrapolation of kinetic data predicts non-Arrhenius behavior around the melting temperature. Three phenomenological models based on different mechanisms are discussed, and an application to shelf life prediction of pharmaceuticals is presented.     

A structural and mechanistic study of the oxidation of methionine residues in hPTH(1-34) via experiments and simulations

The relationship between the conformational properties of 1-34 human parathyroid hormone [hPTH(1-34)] and the oxidation of its methionine residues, Met8 and Met18, by hydrogen peroxide is analyzed as a function of pH by measuring the rates of oxidation and by performing MD simulations with an explicit representation of water molecules. Between pH 4 and pH 8, both Met8 and Met18 have nearly pH independent rates of oxidation, and Met18 is oxidized at a rate that is 90-100% of that of freeMet and 10-20% faster than that of Met8. We also found that average 2SWCNs calculated from MD simulations correlate well to the rates of oxidation of Met8 and Met18. The use of 2SWCNs is based on the mechanism that we proposed, the water-mediated mechanism, in which water molecules stabilize the transition state via specific interactions, but the transfer of protons (acid-catalyzed mechanism) does not play a role [Chu, J. W., and Trout, B. L. (2004) J. Am. Chem. Soc. 126 (3), 900-908]. Only at very low pH values, pH 1 for the oxidation of freeMet, does the acid-catalyzed oxidation mechanism become important. For the oxidation of Met8 and Met18 in hPTH(1-34), the acid-catalyzed mechanism becomes significant at a higher pH value, pH 2, probably due to the proximity of nearby acidic residues to Met8 (Glu4) and Met18 (Glu22). In this study, we have demonstrated that the chemistry of oxidation and the structure of polypeptides can be correlated via a detailed understanding of the reaction mechanism, appropriate sampling of configurational space, and a suitable choice of a structural property, water coordination number.     

Reaction of substituted pyrimidines with photochemically generated t-BuO* radicals

Humans are exposed to various organic peroxides through chemical, pharmaceutical and cosmetic products. On photolysis, these peroxides produce alkoxyl radicals and hydroxyl radicals. The reaction of *OH radicals with DNA and its constituents have been extensively studied, but very little is known about the reactions of alkoxyl radicals with DNA and its constituents. In view of this, the oxidation of pyrimidine bases viz., thymine, uracil, cytosine, 5-bromouracil, 6-methyluracil and 1,3-dimethyluracil by t-BuO* radicals in aqueous solution at pH 7.5 has been carried out. The reaction between pyrimidine and t-BuO* is followed by measuring the absorbance of pyrimidine at the respective lambdamax. The rates of oxidation of pyrimidines are calculated from the plot of absorbance vs time. The rates of oxidation of pyrimidines have been found to increase with increase in [t-BuOOH], [pyrimidine] and light intensity. The quantum yields are calculated from the initial rates of oxidation of pyrimidine and the measured light intensity at 254 nm the wavelength at which t-BuOOH is activated to give radicals. The quantum yields are found to depend on [pyrimidine] as well as on [t-BuOOH] while they are independent of light intensity. The product analysis was carried out on HPLC with UV-visible detector. The corresponding 5,6-dihydroxypyrimidine and isobarbituric acid have been identified by comparing the retention times of the authentic samples. On the basis of experimental results and product analysis, it is suggested that t-BuOOH on photolysis gives t-BuO* radical, which initiates the reaction by adding to C (5) or C (6) position of pyrimidine base, leading to the formation of pyrimidine base radical via hydrolysis. The pyrimidine radical further reacts with t-BuO* radical to give the final product. This study predicts the probable transient pyrimidine radicals.     

Monte Carlo calculations of free ammonia production in deoxygenated solutions of glycylglycine irradiated by X rays and 60Co gamma rays

Detailed-history Monte Carlo computer codes were used to simulate the formation, diffusion, and chemical reaction of free-radical species within deoxygenated aqueous solutions of glycylglycine irradiated by 250-kVp X rays and by 60Co gamma rays. In one reaction, hydrated electrons react with the glycylglycine solute to produce unbound, or free, ammonia. This reaction is complete by 10(-6) s within individual electron tracks for glycylglycine concentrations greater than or equal to 0.025 M. For solute concentrations from 0.025 to 1.2 M, calculated G values of free ammonia are in excellent agreement with measured values. In addition, the computer model predicts a statistically significant difference between the G value of free ammonia produced under X irradiation and that produced under 60Co gamma irradiation.     

Cell-cycle-dependent phosphorylation of serine and threonine in Chinese hamster cell F1 histones.

Imido esters are widely employed for the chemical modification of amino groups in proteins between pH 7–10. We have found that near pH 8 the initial products of reaction of simple primary amines with imido esters are N-alkyl imidates which subsequently react either with ammonia to yield the expected amidine or with water to form free amine. In contrast, near pH 10 amidine formation occurs more rapidly and in better yield, apparently without the accumulation of an intermediate. The observed mechanism of amidine formation implies the possible occurrence of novel side reactions and suggests improved conditions for protein amidination.     

Inactivation of Cryptosporidium parvum Oocysts by Ammonia

The survival of Cryptosporidium parvum oocysts in soil and water microhabitats may be affected by the environmental production and release of free ammonia. The objective of this study was to determine the effects of increasing free ammonia concentrations and times of exposure on oocyst viability. Wild-type oocysts were obtained from naturally infected calf feces by chemical (continuous-flow) centrifugation and sucrose gradients. Ammonia (NH₃) from a commercial solution was applied in concentrations ranging from 0.007 to 0.148 M. Exposure times ranged from 10 min to 24 h at a constant temperature of 24 ± 1°C. Viability of oocysts was determined with a dye permeability assay and an in vitro excystation assay (M. B. Jenkins, L. J. Anguish, D. D. Bowman, M. J. Walker, and W. C. Ghiorse, Appl. Environ. Microbiol. 63:3844–3850, 1997). Even the lowest concentration of ammonia decreased significantly the viability of oocysts after 24 h of exposure. Increasing concentrations of ammonia increased inactivation rates, which ranged from 0.014 to 0.066 h⁻¹. At the highest concentration of ammonia, a small fraction of viable oocysts still remained. Exposure to pH levels corresponding to those associated with the ammonia concentrations showed minimal effects of alkaline pH alone on oocyst viability. This study shows that environmentally relevant concentrations of free ammonia may significantly increase the inactivation of oocysts in ammonia-containing environments.     

Oxidative Transformation of Trithioarsenate Along Alkaline Geothermal Drainages—Abiotic versus Microbially Mediated Processes

Trithioarsenate is the predominant arsenic species at the source of alkaline, sulfidic geothermal springs in Yellowstone National Park. Kinetic studies along seven drainage channels showed that upon discharge the major initial reaction is rapid transformation to arsenite. When aerating a trithioarsenate solution in the laboratory, 10 to 20% of trithioarsenate dissociates abiotically before reaching a steady state with arsenite and thiosulfate. In the geothermal springs, trithioarsenate is completely converted to arsenite and rate constants of 0.2 to 1.9 min?1 are 40 to 500 times higher than in the laboratory, indicating microbial catalysis. Abiotic transformation of trithioarsenate to arsenate requires the presence of a strong oxidizing agent in the laboratory and no evidence was found for direct transformation of thioarsenates to arsenate in the geothermal drainage channels. The simultaneous increase of arsenite and arsenate observed upon trithioarsenate dissociation in some hot springs confirms that the main reaction is thioarsenate transformation to arsenite before microbially catalyzed oxidation to arsenate. In contrast to previous investigations in acidic hot springs, microbially catalyzed arsenate production in near-neutral to alkaline hot springs is not inhibited by the presence of sulfide. Phylogenetic analysis showed that arsenate production coincides with the temperature-dependent occurrence of organisms closely related to Thermocrinis ruber, a sulfur-oxidizing bacterium.     

Energetics of overall metabolic reactions of thermophilic and hyperthermophilic Archaea and bacteria

Thermophilic and hyperthermophilic Archaea and Bacteria have been isolated from marine hydrothermal systems, heated sediments, continental solfataras, hot springs, water heaters, and industrial waste. They catalyze a tremendous array of widely varying metabolic processes. As determined in the laboratory, electron donors in thermophilic and hyperthermophilic microbial redox reactions include H2, Fe(2+), H2S, S, S2O3(2-), S4O6(2-), sulfide minerals, CH4, various mono-, di-, and hydroxy-carboxylic acids, alcohols, amino acids, and complex organic substrates; electron acceptors include O2, Fe(3+), CO2, CO, NO3(-), NO2(-), NO, N2O, SO4(2-), SO3(2-), S2O3(2-), and S. Although many assimilatory and dissimilatory metabolic reactions have been identified for these groups of microorganisms, little attention has been paid to the energetics of these reactions. In this review, standard molal Gibbs free energies (DeltaGr(0)) as a function of temperature to 200 degrees C are tabulated for 370 organic and inorganic redox, disproportionation, dissociation, hydrolysis, and solubility reactions directly or indirectly involved in microbial metabolism. To calculate values of DeltaGr(0) for these and countless other reactions, the apparent standard molal Gibbs free energies of formation (DeltaG(0)) at temperatures to 200 degrees C are given for 307 solids, liquids, gases, and aqueous solutes. It is shown that values of DeltaGr(0) for many microbially mediated reactions are highly temperature dependent, and that adopting values determined at 25 degrees C for systems at elevated temperatures introduces significant and unnecessary errors. The metabolic processes considered here involve compounds that belong to the following chemical systems: H-O, H-O-N, H-O-S, H-O-N-S, H-O-C(inorganic), H-O-C, H-O-N-C, H-O-S-C, H-O-N-S-C(amino acids), H-O-S-C-metals/minerals, and H-O-P. For four metabolic reactions of particular interest in thermophily and hyperthermophily (knallgas reaction, anaerobic sulfur and nitrate reduction, and autotrophic methanogenesis), values of the overall Gibbs free energy (DeltaGr) as a function of temperature are calculated for a wide range of chemical compositions likely to be present in near-surface and deep hydrothermal and geothermal systems.     

Quinone-dependent delayed fluorescence from the reaction center of photosynthetic bacteria

Millisecond delayed fluorescence from the isolated reaction center of photosynthetic bacteria Rhodobacter sphaeroides was measured after single saturating flash excitation and was explained by thermal repopulation of the excited bacteriochlorophyll dimer from lower lying charge separated states. Three exponential components (fastest, fast, and slow) were found with lifetimes of 1.5, 102, and 865 ms and quantum yields of 6.4 x 10(-9), 2.2 x 10(-9), and 2.6 x 10(-9) (pH 8.0), respectively. While the two latter phases could be related to transient absorption changes, the fastest one could not. The fastest component, dominating when the primary quinone was prereduced, might be due to a small fraction of long-lived triplet states of the radical pair and/or the dimer. The fast phase observed in the absence of the secondary quinone, was sensitive to pH, temperature, and the chemical nature of the primary quinone. The standard free energy of the primary stable charge pair relative to that of the excited dimer was -910 +/- 20 meV at pH 8 and with native ubiquinone, and it showed characteristic changes upon pH and quinone replacement. The interaction energy ( approximately 50 meV) between the cluster of the protonatable groups around GluL212 and the primary semiquinone provides evidence for functional linkage between the two quinone binding pockets. An empirical relationship was found between the in situ free energy of the primary quinone and the rate of charge recombination, with practical importance in the estimation of the free energy levels from the easily available lifetime of the charge recombination. The ratio of the slow and fast components could be used to determine the pH dependence of the free energy level of the secondary stable charge pair relative to that of the excited dimer.     

Kinetics of appearance of sulfhydryl groups in alpha 2-macroglobulin on reaction of the inhibitor with amines

The mechanism of the appearance of sulfhydryl groups in alpha 2-macroglobulin in the reaction with amines was characterized by analyses of the kinetics with ammonia and methylamine. All reactions occurred under pseudo-first-order conditions in the range of pH (7.0-8.6) and amine concentration (10-600 mM) investigated. The logarithm of the pseudo-first-order rate constant increased linearly as a function of pH with a slope of unity, indicating that the unprotonated amine is the active species in the reaction. Plots of the observed pseudo-first-order rate constants vs. concentration of unprotonated amine at constant pH were also linear and gave second-order-rate constants of 0.32 and 13.8 M-1 s-1 for ammonia and methylamine, respectively, at pH 8.0; similar values were obtained at pH 8.6. Activation energies of 85 and 100 kJ mol-1 and activation entropies of 10 and 95 J K-1 mol-1 for ammonia and methylamine, respectively, were estimated from Arrhenius plots, suggesting that the higher reaction rate for methylamine is due primarily to a higher activation entropy. These results are consistent with the release of sulfhydryl groups being caused by a nucleophilic attack of the uncharged amine on a thio ester bond of alpha 2-macroglobulin in a bimolecular reaction occurring under pseudo-first-order conditions. The characteristics of the reaction suggest that the thio ester in each alpha 2-macroglobulin subunit reacts independently and equivalently with the amine and also that the thio ester bond cleavage initiates the reaction sequence leading to inactivation of the inhibitor.(ABSTRACT TRUNCATED AT 250 WORDS)