Ferric iron-reducing Shewanella putrefaciens and N2-fixing Bradyrhizobium japonicum with uptake hydrogenase are unable to oxidize atmospheric H2

Abstract Bradyrhizobium japonicum and Shewanella putrefaciens were unable to oxidize hydrogen at atmospheric concentrations (0.55 ppmv), neither in suspension nor when added to sterile soil. The K _m-value of S. putrefaciens for H₂ (39 ppmv in gas phase, 0.22 μM in aqueous phase), using Fe(III) as electron acceptor, showed a 4–5-fold higher affinity for H₂ than that of B. japonicum (1200 ppmv; 0.84 μM) or other hydrogen-oxidizing bacteria. However, the V _max (4.54 fmol H₂ h⁻¹ cell ⁻¹) and threshold (> 0.5 ppmv; 0.35 nM) of S. putrefaciens and the V _max (7.19 fmol H₂ h⁻¹ cell⁻¹) and threshold (> 0.5 ppmv; 0.35 nM) of B. japonicum were in the same order of magnitude as data for Knallgas bacteria from relevant literature. To enable hydrogen oxidation in soil the soil-samples with S. putrefaciens even had to be supplemented with Fe(III). Fresh soil, on the other hand, oxidized hydrogen very efficiently below atmospheric mixing ratios, demonstrating that there must be other oxidation activities in soil.     

Soils contain two different activities for oxidation of hydrogen

Abstract Hydrogen oxidation rates were measured in a neutral compost soil and an acidic sandy loam at H₂ mixing ratios of 0.01 to 5000 ppmv. The kinetics were biphasic showing two different K _m values for H₂, one at about 10–40 nM dissolved H₂, the other at about 1.2–1.4 μM H₂. The low- K _m activity was less sensitive to chloroform fumigation than the high- K _m activity. If sterile soil was amended with Paracoccus denitrificans or a H₂-oxidizing strain isolated from compost soil, it exhibited only a high- K _m (0.7–0.9 μM) activity. It also failed to utilize H₂ mixing ratios below a threshold of 1.6–3.0 ppmv H₂ (160–300 mPa). A similar result was obtained when fresh soil samples were suspended in water, and H₂ oxidation was determined from the decrease of dissolved H₂. However, H₂ was again utilized to mixing ratios lower than 0.05 ppmv, if the supernatant of the soil suspension or the settled soil particles were dried onto sterile soil or purified quarz sand. Obviously, soils contain two different activities for oxidation of H₂: (1) a high- K _m, high-threshold activity which apparently is due to aerobic H₂-oxidizing bacteria, and (2) a low- K _m, low-threshold activity whose origin is unknown but presumably is due to soil enzymes.     

Vacuolating cytotoxic activity of Pasteurella multocida causing haemorrhagic septicaemia in buffalo and cattle

Abstract Sequence data had indicated that cyanobacteria might possess a bidirectional hydrogenase with properties similar to the soluble enzymes from Alcaligenes eutrophus, Nocardia opaca and Desulfovibrio fructosovorans . The present study shows that extracts from the cyanobacterium Anacystis nidulans catalyse NAD(P)H-dependent H₂ evolution with low but significant activity and uptake of the gas with NAD(P)⁺ as the electron acceptor. NAD⁺ is the preferred electron acceptor and NADH the preferred donor compared to NADP⁺ and NADPH, respectively. Activity levels of this NAD(P)⁺dependent, bidirectional hydrogenase are too low to support chemoautotrophic growth in A. nidulans .     

The metabolism of hydrogen by extremely thermophilic, sulfur-dependent bacteria

Abstract In just the last few years, a group of bacteria have been discovered that have the remarkable property of growing near and above 100°C. These extremely thermophilic organisms, defined here as having the ability to grow at 90°C with optimum growth at 80°C and above, have been isolated mainly from sulfur-rich, marine geothermal environments, both shallow and deep sea. They comprise over a dozen different genera, and except for one novel eubacterium, all may be classified as archaebacteria. The majority of the extremely thermophilic genera metabolize elemental sulfur (S°) and a survey of the various organisms reveals that most of them also depend upon the oxidation of hydrogen gas (H₂) as an energy source. In addition, two extremely thermophilic genera are known that actively produce H₂ as end-products of novel fermentative metabolisms. The enzyme hydrogenase, which is responsible for catalysing H₂ activation and H₂ production, appears to play several roles in electron and energy transfer during the growth of these organisms. Hydrogenase has so far been purified from only one extremely thermophilic species, from Pyrococcus furiosus ( T _opt = 100°C), and hydrogenase activity has been exmained in cell-free extracts of only a few others. However, a comparison of their properties with those of hydrogenases from mesophilic bacteria suggests that (a) the hydrogenase responsible for catalysing H₂ oxidation in extremely thermophilic organisms may be an extremely thermostable version of the mesophilic enzyme, and (b) a new type of 'evolution' hydrogenase, lacking the Ni-S or Fe-S catalytic sites of the mesophilic enzymes, is required for catalysing H₂ evolution at temperatures near and above 100°C.     

Growth of thermophilic obligately autotrophic hydrogen-oxidizing bacteria on thiosulfate

Thermophilic obligately autotrophic H₂-oxidizing bacteria from Icelandic hot springs were tested for growth on thiosulfate. Ten strains were tested and all grew on thiosulfate but not on sulfite or sulfur. The product of thiosulfate oxidation was sulfate. The growth rate on thiosulfate was slower (μ=0.12 h^-1) than on H₂ (μ=0.34 h^-1). Washed cells which had been grown on thiosulfate could oxidize thiosulfate rapidly but H₂-grown cells oxidized thiosulfate much more slowly and with about a 3 h lag time. The bacteria would not grow on agar medium under H₂ but grew on agar medium containing thiosulfate.     

Temporal change of gas metabolism by hydrogen-syntrophic methanogenic bacterial associations in anoxic paddy soil

Abstract Interspecies H₂ transfer within methanogenic bacterial associations (MBA) accounted for 95–97% of the conversion of ¹⁴CO₂ to ¹⁴CH₄ in anoxic paddy soil. Only 3–5% of the ¹⁴CH₄ were produced from the turnover of dissolved H₂. The H₂-syntrophic MBA developed within 5 days after the paddy soil had been submerged and placed under anoxic atmosphere. Afterwards, both the contribution of MBA to H₂-dependent methanogenesis and the turnover of dissolved H₂ did not change significantly for up to 7 months of incubation. However, while the rates of H₂-dependent methanogenesis stayed relatively constant, the rates of total methanogenesis decreased. The contribution of MBA to H₂-dependent methanogenesis was further enhanced to 99% when the temperature was shifted from 30°C to 17°C, or when the soil had been planted with rice. This enhancement was partially due to an increased utilization of dissolved H₂ by chloroform-insensitive non-methanogenic bacteria, most probably homoacetogens, so that CH₄ production was almost completely restricted to H₂-syntrophic MBA. The activity of MBA, as measured by the conversion of ¹⁴CO₂ to ¹⁴CH₄, was stimulated by glucose, lactate, and ethanol to a similar or greater extent than by exogenous H₂. Propionate and acetate had no effect.     

H2 oxidation in the presence of thiosulfate, by a Thermoanaerobacter strain isolated from an oil-producing well

Abstract A thermophilic rod (strain SEBR 5268), isolated from an oil-producing well, was identified as a Thermoanaerobacter strain that was phenotypically related to T. finnii . Both SEBR 5268 and T. finnii oxidized H₂ by reducing thiosulfate to sulfide using yeast extract as growth substrate. H₂ oxidation in the presence of thiosulfate was significant at the end of the exponential growth of SEBR 5268 and was maintained during the lysis phase. In the absence of thiosulfate, H₂ was inhibitory for both strains. The role of H₂ consumption by these bacteria is discussed with regard to their metabolism on organic compounds.     

H2 and CO2 production from methanol or formaldehyde by the methanogenic bacterium strain Gö1 treated with 2-bromoethanesulfonic acid

Abstract In cell suspensions of the methanogenic bacterium strain Gö1 or Methanosarcina barkeri H₂ formation from methanol in the presence of 2-bromoethanesulfonic acid (BES) was strictly dependent on sodium ions; apparent K _S for Na⁺, 1.3±0.3 mM.H₂ formation was inhibited by the uncoupler tetrachlorosalicylanilide (TCS), but this inhibition could be temporarily overcome, when a sodium pulse (100 mM) was given to the cell suspension. On the other hand, H₂ formation from formaldehyde in the presence of BES (rate: 300 nmol H₂/h·mg protein as compared to 25 nmol H₂/h·mg protein from methanol) was not sodium-dependent, not TCS-sensitive and not inhibited by addition of monensin. H₂ formation was accompanied by CO₂ formation in stoichiometric amounts, 3 H₂:1 CO₂ for methanol and 2 H₂:1 CO₂ for formaldehyde oxidation.     

Appearance of a reversible hydrogenase activity in Anabaena cylindrica grown in high light

In vivo H₂ evolution by Anabaena cylindrica Lemm. strain PCC 7122 grown in the presence of ammonia at low and high light intensities was studied. We found that after 2 h of anaerobic incubation, H₂ evolution [at a rate of 0.5 μmol (mg dry weight)¹ h⁻¹] via reversible hydrogenase occurred in high light grown cells, while this kind of activity was not found in low light grown cells. H₂ evolution was inhibited by 3-(3'. 4'-dichlorophenyl-1, 1-dimethylurea (DCMU). Illuminating the cells in the phycocyanin absorption region resulted in a higher rate of H₂ evolution than illuminating the cells in the chlorophyll absorption region. The results indicate that reversible hydrogenase receives reducing equivalents from photosynthetic water photolysis and that both photosystem II and photosystem I participate in the H₂ production. Hydrogenase activity was found in the soluble fraction after mild sonication in the case of low light grown cells. After this treatment high light grown cells retained 70% of their hydrogenase activity in the particulate fraction, but released it into the soluble fraction in the presence of 2% deoxycholic acid.
In vitro H₂ evolution did not differ significantly in the low and high light grown cells. Hence, the differences in the in vivo H₂ evolution reflect the different availability of endogenous reductants for hydrogenase in the two kinds of cells. On the basis of our results it is suggested that high light grown Anabaena cells eliminate part of the photosynthetically produced excess electrons via an induced reversible hydrogenase activity. This is the first report of H₂ evolution associated with water photolysis and catalyzed by hydrogenase in cyanobacteria.     

Fusarium response to oxidative stress by H2O2 is trichothecene chemotype-dependent

The present study aims at clarifying the impact of oxidative stress on type B trichothecene production. The responses to hydrogen peroxide (H₂O₂) of an array of Fusarium graminearum and Fusarium culmorum strains were compared, both species carrying either the chemotype deoxynivalenol (DON) or nivalenol (NIV). In both cases, levels of in vitro toxin production are greatly influenced by the oxidative parameters of the medium. A 0.5 mM H₂O₂ stress induces a two- to 50-fold enhancement of DON and acetyldeoxynivalenol production, whereas the same treatment results in a 2.4- to sevenfold decrease in NIV and fusarenone X accumulation. Different effects of oxidative stress on toxin production are the result of a variation in Fusarium 's antioxidant defence responses according to the chemotype of the isolate. Compared with DON strains, NIV isolates have a higher H₂O₂-destroying capacity, which partially results from a significant enhancement of catalase activity induced by peroxide stress. A 0.5 mM H₂O₂ treatment leads to a 1.3- to 1.7-fold increase in the catalase activity of NIV isolates. Our data, which show the higher adaptation to oxidative stress developed by NIV isolates, are consistent with the higher virulence of these Fusarium strains on maize compared with DON isolates.     

The acetylene reduction assay inactivates root nodule uptake hydrogenase in some actinorhizal plants

Actinorhizal nodules do not usually evolve H₂ due to the action of an uptake hydrogenase. We have found that nodules of several Frankia symbioses evolved large amounts of H₂ gas when returned to air following exposure to 10 kPa C₂HT₂ during an acetylene reduction assay. Increased H₂ evolution in air persisted for several days when intact root systems of Alnus incana (L.) Moench (inoculated with Frankia UGL 011101) were treated with 10 kPa C.H₂ for 1 h. Full recovery of uptake hydrogenase activity required 4 to 8 days. Studies with crude homogenates of nodules of the same plants showed that hydrogenase (measured amperometrically with phenazine metho-sulfate as electron acceptor) was directly affected, since activity in treated nodules was only 10% of that in untreated nodules. A survey of actinorhizal symbioses revealed variation in the effect of an acetylene reduction assay on hydrogen metabolism. Nodules of three species, including Alnus rubra Bong, inoculated with Frankia HFPArD. showed complete inactivation of hydrogenase. H₂ evolution in air was 25% of the C₂H₂ reduction rate and H, evolution in Ar/O₂ was equal to the QH₂ reduction rate. Two symbioses, Ceanothus americanus L. (soil inoculant) and Batista glomerata Baill. (soil inoculant) showed no change following an acetylene reduction assay. A third group of symbioses showed an intermediate response.     

Hydrogen turnover by psychrotrophic homoacetogenic and mesophilic methanogenic bacteria in anoxic paddy soil and lake sediment

Abstract The effect of temperature on CH₄ production, turnover of dissolved H₂, and enrichment of H₂-utilizing anaerobic bacteria was studied in anoxic paddy soil and sediment of Lake Constance. When anoxic paddy soil was incubated under an atmosphere of H₂/CO₂, rates of CH₄ production increased 25°C, but decreased at temperatures lower than 20°C. Chloroform completely inhibited methano-genesis in anoxic paddy soil and lake sediment, but did not or only partially inhibit the turnover of dissolved H₂, especially at low incubation temperatures. Cultures with H₂ as energy source resulted in the enrichment of chemolithotrophic homoacetogenic bacteria whenever incubation temperatures were lower than 20°C. Hydrogenotrophic methanogens could only be enriched at 30°C from anoxic paddy soil. A homoacetogen     

Hydrogenase- and outer membrane c-type cytochrome-facilitated reduction of technetium(VII) by Shewanella oneidensis MR-1

Pertechnetate, ⁹⁹Tc(VII)O₄^–, is a highly mobile radionuclide contaminant at US Department of Energy sites that can be enzymatically reduced by a range of anaerobic and facultatively anaerobic microorganisms, including Shewanella oneidensis MR-1, to poorly soluble Tc(IV)O_2(s). In other microorganisms, Tc(VII)O₄^– reduction is generally considered to be catalysed by hydrogenase. Here, we provide evidence that although the NiFe hydrogenase of MR-1 was involved in the H₂-driven reduction of Tc(VII)O₄^–[presumably through a direct coupling of H₂ oxidation and Tc(VII) reduction], the deletion of both hydrogenase genes did not completely eliminate the ability of MR-1 to reduce Tc(VII). With lactate as the electron donor, mutants lacking the outer membrane c -type cytochromes MtrC and OmcA or the proteins required for the maturation of c -type cytochromes were defective in reducing Tc(VII) to nanoparticulate TcO₂·nH₂O_(s) relative to MR-1 or a NiFe hydrogenase mutant. In addition, reduced MtrC and OmcA were oxidized by Tc(VII)O₄^–, confirming the capacity for direct electron transfer from these OMCs to TcO₄^–. c -Type cytochrome-catalysed Tc(VII) reduction could be a potentially important mechanism in environments where organic electron donor concentrations are sufficient to allow this reaction to dominate.     

Molecular cloning and characterization of a Candida albicans gene (EFB1) coding for the elongation factor EF-1β

Abstract The formation of H₂ by chemolithoautrophically growing Oligotropha carboxidovorans has been identified as the result of the oxidation of CO mediated by the cytoplasmic species of the molybdenum-containing CO dehydrogenase multienzyme complex as follows: CO + H ₂ O → CO ₂+ H ₂. Purified CO dehydrogenase was shown to carry hydrogen uptake and formation activities in addition to its catabolic function which is the oxidation of CO. Among the electron donors supporting H₂ formation were CO, NADH, reduced flavins and reduced viologen dyes. The reduction of protons to H₂ by cytoplasmic CO dehydrogenase is interpreted as a detoxification reaction for electrons to prevent cell damage in O. carboxidovorans .     

Isolation and characterization of methanogenic bacteria from rice paddies

Abstract Enrichment cultures for H₂-CO₂, methanol- or acetate-utilizing methanogens were prepared from two rice field soil samples. All the cultures except one acetate enrichment showed significant methane production. Pure cultures of Methanobacterium - and Methanosarcina -like organisms were isolated from H₂-CO₂ and methanol enrichment cultures, respectively, and were characterized for various nutritional and growth conditions. The organisms had an optimal pH range of 6.4–6.6 and a temperature optimum of 37°C. The Methanobacterium isolates were able to utilize H₂-CO₂ but no other substrates as sole energy source, while the Methanosarcina isolates were able to utilize methanol, methylamines or H₂-CO₂ as sole energy sources. Both Methanobacterium isolates and one isolate of Methanosarcina were able to use dinitrogen as the sole source of nitrogen for growth. The isolates used several sulfur compounds as sole sources of sulfur.     

The C Terminal Tail of the Histamine H2 Receptor Contains Positive and Negative Signals Important for Signal Transduction and Receptor Down-Regulation

Abstract: To examine the role of the C terminal tail in H₂ receptor regulation, three cDNAs, encoding truncated histamine H₂ receptor mutants (H₂T295, H₂T307, and H₂T341), were constructed and stably transfected in Chinese hamster ovary (CHO) cells. The amino acids before position 307 appear to be necessary for proper receptor transport or folding, as no detectable H₂ receptor binding of the H₂T295 was observed after transfection. Truncation of the C terminal tail by 51 amino acids (H₂T307) did not affect the binding properties of H₂ antagonists and histamine or histamine-induced signaling. Yet, removal of 17 amino acids generated a mutant receptor (H₂T341), which was able to form a ternary complex but was unable to fully activate the G_s protein on histamine exposure. Agonist-induced but not the cyclic AMP-dependent H₂ receptor down-regulation was more profound for the H₂T307 receptor, indicating that different structural elements of the H₂ receptor protein are involved in the cyclic AMP-dependent and independent pathways of H₂ receptor down-regulation. Taken together, in this study we identified regions in the C terminal tail of the H₂ receptor that act as positive and/or negative signals in H₂ receptor signaling and down-regulation.     

Formate oxidation by Wolinella recta ATCC 33238 with oxygen as electron acceptor

Abstract The formate oxidizing capacity of Wolinella recta ATCC 33238 was studied in relation to growth under anaerobic and microaerobic conditions. Three distinct activities could be recognized: (a) cyanide-insensitive H₂O₂-producing oxidation of formate; (b) peroxidation of formate (H₂O₂-consuming); (c) oxidation of formate via an electron transport chain with oxygen as the electron acceptor. The contribution of these different formate oxidizing components during the growth of W. recta was dependent on the extent of aeration. It is suggested that due to the relative increase in overall H₂O₂ formation at higher oxygen tensions growth of W. recta appears possible only under anaerobic and microaerobic conditions.     

Methyl sulfides as intermediates in the anaerobic oxidation of methane

While it is clear that microbial consortia containing Archaea and sulfate-reducing bacteria (SRB) can mediate the anaerobic oxidation of methane (AOM), the interplay between these microorganisms remains unknown. The leading explanation of the AOM metabolism is 'reverse methanogenesis' by which a methanogenesis substrate is produced and transferred between species. Conceptually, the reversal of methanogenesis requires low H₂ concentrations for energetic favourability. We used ¹³C-labelled CH₄ as a tracer to test the effects of elevated H₂ pressures on incubations of active AOM sediments from both the Eel River basin and Hydrate Ridge. In the presence of H₂, we observed a minimal reduction in the rate of CH₄ oxidation, and conclude H₂ does not play an interspecies role in AOM. Based on these results, as well as previous work, we propose a new model for substrate transfer in AOM. In this model, methyl sulfides produced by the Archaea from both CH₄ oxidation and CO₂ reduction are transferred to the SRB. Metabolically, CH₄ oxidation provides electrons for the energy-yielding reduction of CO₂ to a methyl group ('methylogenesis'). Methylogenesis is a dominantly reductive pathway utilizing most methanogenesis enzymes in their forward direction. Incubations of seep sediments demonstrate, as would be expected from this model, that methanethiol inhibits AOM and that CO can be substituted for CH₄ as the electron donor for methylogenesis.     

Selective protection by phosphatidic acid against staurosporine-induced neuronal apoptosis

Phosphatidic acid, the main product of lipid breakdown through phospholipase D activation, has been implicated in important signal transduction pathways able to influence cell fate in many ways. The purpose of this work was to determine possible effects of phosphatidic acid on neuronal cell death pathways. Here we used cerebellar granular cell cultures and cell death was triggered with either staurosporine or H₂O₂. Cell viability was quantified by spectrophotometry, using the 3- (4, 5-dimethylthiazol-2-y1)-2, 5-diphenyl-tetrazolium bromide (MTT) test. Staurosporine (1-3 μM) or H₂O₂ (50-800 μM) induced cell death in a dose-dependent manner. Using fluorescent staining (propidium iodide or annexin V-Cy3/6-carboxyfluorescein) we showed that cell death was mostly apoptotic in staurosporine treated cells and mostly non-apoptotic (necrotic) in H2O2 treated cells. Phosphatidic acid was able to increase cell viability in staurosporine-, but not in H₂O₂ - treated cells. We therefore conclude that phosphatidic acid has neuroprotective potential in neurons exposed to stimuli that trigger apoptosis.