A nitrite-oxidising bacterium constitutively consumes atmospheric hydrogen

Chemolithoautotrophic nitrite-oxidising bacteria (NOB) of the genus Nitrospira contribute to nitrification in diverse natural environments and engineered systems. Nitrospira are thought to be well-adapted to substrate limitation owing to their high affinity for nitrite and capacity to use alternative energy sources. Here, we demonstrate that the canonical nitrite oxidiser Nitrospira moscoviensis oxidises hydrogen (H₂) below atmospheric levels using a high-affinity group 2a nickel-iron hydrogenase [K_m(app) = 32 nM]. Atmospheric H₂ oxidation occurred under both nitrite-replete and nitrite-deplete conditions, suggesting low-potential electrons derived from H₂ oxidation promote nitrite-dependent growth and enable survival during nitrite limitation. Proteomic analyses confirmed the hydrogenase was abundant under both conditions and indicated extensive metabolic changes occur to reduce energy expenditure and growth under nitrite-deplete conditions. Thermodynamic modelling revealed that H₂ oxidation theoretically generates higher power yield than nitrite oxidation at low substrate concentrations and significantly contributes to growth at elevated nitrite concentrations. Collectively, this study suggests atmospheric H₂ oxidation enhances the growth and survival of NOB amid variability of nitrite supply, extends the phenomenon of atmospheric H₂ oxidation to an eighth phylum (Nitrospirota), and reveals unexpected new links between the global hydrogen and nitrogen cycles. Long classified as obligate nitrite oxidisers, our findings suggest H₂ may primarily support growth and survival of certain NOB in natural environments.Subject terms: Environmental microbiology, Microbial ecology, Metabolism     

Coral Fluorescent Proteins as Antioxidants

Background

A wide array of fluorescent proteins (FP) is present in anthozoans, although their biochemical characteristics and function in host tissue remain to be determined. Upregulation of FP''s frequently occurs in injured or compromised coral tissue, suggesting a potential role of coral FPs in host stress responses.

Methodology/Principal Findings

The presence of FPs was determined and quantified for a subsample of seven healthy Caribbean coral species using spectral emission analysis of tissue extracts. FP concentration was correlated with the in vivo antioxidant potential of the tissue extracts by quantifying the hydrogen peroxide (H₂O₂) scavenging rates. FPs of the seven species varied in both type and abundance and demonstrated a positive correlation between H₂O₂ scavenging rate and FP concentration. To validate this data, the H₂O₂ scavenging rates of four pure scleractinian FPs, cyan (CFP), green (GFP), red (RFP) and chromoprotein (CP), and their mutant counterparts (without chromophores), were investigated. In vitro, each FP scavenged H₂O₂ with the most efficient being CP followed by equivalent activity of CFP and RFP. Scavenging was significantly higher in all mutant counterparts.

Conclusions/Significance

Both naturally occurring and pure coral FPs have significant H₂O₂ scavenging activity. The higher scavenging rate of RFP and the CP in vitro is consistent with observed increases of these specific FPs in areas of compromised coral tissue. However, the greater scavenging ability of the mutant counterparts suggests additional roles of scleractinian FPs, potentially pertaining to their color. This study documents H₂O₂ scavenging of scleractinian FPs, a novel biochemical characteristic, both in vivo across multiple species and in vitro with purified proteins. These data support a role for FPs in coral stress and immune responses and highlights the multi-functionality of these conspicuous proteins.     

Novel,Oxygen-Insensitive Group 5 [NiFe]-Hydrogenase in Ralstonia eutropha

Recently, a novel group of [NiFe]-hydrogenases has been defined that appear to have a great impact in the global hydrogen cycle. This so-called group 5 [NiFe]-hydrogenase is widespread in soil-living actinobacteria and can oxidize molecular hydrogen at atmospheric levels, which suggests a high affinity of the enzyme toward H₂. Here, we provide a biochemical characterization of a group 5 hydrogenase from the betaproteobacterium Ralstonia eutropha H16. The hydrogenase was designated an actinobacterial hydrogenase (AH) and is catalytically active, as shown by the in vivo H₂ uptake and by activity staining in native gels. However, the enzyme does not sustain autotrophic growth on H₂. The AH was purified to homogeneity by affinity chromatography and consists of two subunits with molecular masses of 65 and 37 kDa. Among the electron acceptors tested, nitroblue tetrazolium chloride was reduced by the AH at highest rates. At 30°C and pH 8, the specific activity of the enzyme was 0.3 μmol of H₂ per min and mg of protein. However, an unexpectedly high Michaelis constant (K_m) for H₂ of 3.6 ± 0.5 μM was determined, which is in contrast to the previously proposed low K_m of group 5 hydrogenases and makes atmospheric H₂ uptake by R. eutropha most unlikely. Amperometric activity measurements revealed that the AH maintains full H₂ oxidation activity even at atmospheric oxygen concentrations, showing that the enzyme is insensitive toward O₂.     

Advances in the biotechnology of hydrogen production with the microalga Chlamydomonas reinhardtii

Biological hydrogen production is being evaluated for use as a fuel, since it is a promising substitute for carbonaceous fuels owing to its high conversion efficiency and high specific energy content. The basic advantages of biological hydrogen production over other “green” energy sources are that it does not compete for agricultural land use, and it does not pollute, as water is the only by-product of the combustion. These characteristics make hydrogen a suitable fuel for the future. Among several biotechnological approaches, photobiological hydrogen production carried out by green microalgae has been intensively investigated in recent years. A select group of photosynthetic organisms has evolved the ability to harness light energy to drive hydrogen gas production from water. Of these, the microalga Chlamydomonas reinhardtii is considered one of the most promising eukaryotic H₂ producers. In this model microorganism, light energy, H₂O and H₂ are linked by two excellent catalysts, the photosystem 2 (PSII) and the [FeFe]-hydrogenase, in a pathway usually referred to as direct biophotolysis. This review summarizes the main advances made over the past decade as an outcome of the discovery of the sulfur-deprivation process. Both the scientific and technical barriers that need to be overcome before H₂ photoproduction can be scaled up to an industrial level are examined. Actual and theoretical limits of the efficiency of the process are also discussed. Particular emphasis is placed on algal biohydrogen production outdoors, and guidelines for an optimal photobioreactor design are suggested.     

Ascorbate–glutathione pathways mediated by cytokinin regulate H2O2 levels in light-controlled rose bud burst

Rosebush (Rosa “Radrazz”) plants are an excellent model to study light control of bud outgrowth since bud outgrowth only arises in the presence of light and never occurs in darkness. Recently, we demonstrated high levels of hydrogen peroxide (H₂O₂) present in the quiescent axillary buds strongly repress the outgrowth process. In light, the outgrowing process occurred after H₂O₂ scavenging through the promotion of Ascorbic acid–Glutathione (AsA–GSH)-dependent pathways and the continuous decrease in H₂O₂ production. Here we showed Respiratory Burst Oxidase Homologs expression decreased in buds during the outgrowth process in light. In continuous darkness, the same decrease was observed although H₂O₂ remained at high levels in axillary buds, as a consequence of the strong inhibition of AsA–GSH cycle and GSH synthesis preventing the outgrowth process. Cytokinin (CK) application can evoke bud outgrowth in light as well as in continuous darkness. Furthermore, CKs are the initial targets of light in the photocontrol process. We showed CK application to cultured buds in darkness decreases bud H₂O₂ to a level that is similar to that observed in light. Furthermore, this treatment restores GSH levels and engages bud burst. We treated plants with buthionine sulfoximine, an inhibitor of GSH synthesis, to solve the sequence of events involving H₂O₂/GSH metabolisms in the photocontrol process. This treatment prevented bud burst, even in the presence of CK, suggesting the sequence of actions starts with the positive CK effect on GSH that in turn stimulates H₂O₂ scavenging, resulting in initiation of bud outgrowth.

Light-induced bud outgrowth in rosebush results from cytokinin-mediated peroxide scavenging and glutathione metabolism stimulation.     

Hydrogen peroxide in artificial photosynthesizing systems

From the point of view of the concepts of hydrogen peroxide as a source of photosynthetic oxygen (hydrogen) coordination and photochemical properties of chlorophyll and its aggregates towards hydrogen peroxide were considered. The binding energy of H₂O and H₂O₂ with chlorophyll and chlorophyllide depending on their form (monomers, dimers and trimers) was estimated by quantum chemical calculations. It is shown that at an increase of the degree of the pigment aggregation binding energy of H₂O₂ was more than the energy of H₂O. Analysis of experimental results of the photochemical decomposition of hydrogen peroxide using chlorophyll was carried out. Estimates of the thermodynamic parameters (ΔG° and ΔH°) of the formation of organic compounds from CO₂ with water and hydrogen peroxide were compared. The interaction of CO₂ with H₂O₂ requires much less energy consumption than with water for all considered cases. The formation of organic products (formaldehyde, alcohols, carboxylic and carbonylic compounds) and simultaneous production of O₂ under the influence of visible light in the systems of inorganic carbon-hydrogen peroxide - chlorophyll (phthalocyanine) is detected by GC/MS method, FTIR spectroscopy, and chemical analysis.     

A widely distributed hydrogenase oxidises atmospheric H2 during bacterial growth

Diverse aerobic bacteria persist by consuming atmospheric hydrogen (H₂) using group 1h [NiFe]-hydrogenases. However, other hydrogenase classes are also distributed in aerobes, including the group 2a [NiFe]-hydrogenase. Based on studies focused on Cyanobacteria, the reported physiological role of the group 2a [NiFe]-hydrogenase is to recycle H₂ produced by nitrogenase. However, given this hydrogenase is also present in various heterotrophs and lithoautotrophs lacking nitrogenases, it may play a wider role in bacterial metabolism. Here we investigated the role of this enzyme in three species from different phylogenetic lineages and ecological niches: Acidithiobacillus ferrooxidans (phylum Proteobacteria), Chloroflexus aggregans (phylum Chloroflexota), and Gemmatimonas aurantiaca (phylum Gemmatimonadota). qRT-PCR analysis revealed that the group 2a [NiFe]-hydrogenase of all three species is significantly upregulated during exponential growth compared to stationary phase, in contrast to the profile of the persistence-linked group 1h [NiFe]-hydrogenase. Whole-cell biochemical assays confirmed that all three strains aerobically respire H₂ to sub-atmospheric levels, and oxidation rates were much higher during growth. Moreover, the oxidation of H₂ supported mixotrophic growth of the carbon-fixing strains C. aggregans and A. ferrooxidans. Finally, we used phylogenomic analyses to show that this hydrogenase is widely distributed and is encoded by 13 bacterial phyla. These findings challenge the current persistence-centric model of the physiological role of atmospheric H₂ oxidation and extend this process to two more phyla, Proteobacteria and Gemmatimonadota. In turn, these findings have broader relevance for understanding how bacteria conserve energy in different environments and control the biogeochemical cycling of atmospheric trace gases.Subject terms: Environmental microbiology, Biogeochemistry     

Leveraging substrate flexibility and product selectivity of acetogens in two-stage systems for chemical production

Carbon dioxide (CO₂) stands out as sustainable feedstock for developing a circular carbon economy whose energy supply could be obtained by boosting the production of clean hydrogen from renewable electricity. H₂-dependent CO₂ gas fermentation using acetogenic microorganisms offers a viable solution of increasingly demonstrated value. While gas fermentation advances to achieve commercial process scalability, which is currently limited to a few products such as acetate and ethanol, it is worth taking the best of the current state-of-the-art technology by its integration within innovative bioconversion schemes. This review presents multiple scenarios where gas fermentation by acetogens integrate into double-stage biotechnological production processes that use CO₂ as sole carbon feedstock and H₂ as energy carrier for products' synthesis. In the integration schemes here reviewed, the first stage can be biotic or abiotic while the second stage is biotic. When the first stage is biotic, acetogens act as a biological platform to generate chemical intermediates such as acetate, formate and ethanol that become substrates for a second fermentation stage. This approach holds the potential to enhance process titre/rate/yield metrics and products' spectrum. Alternatively, when the first stage is abiotic, the integrated two-stage scheme foresees, in the first stage, the catalytic transformation of CO₂ into C₁ products that, in the second stage, can be metabolized by acetogens. This latter scheme leverages the metabolic flexibility of acetogens in efficient utilization of the products of CO₂ abiotic hydrogenation, namely formate and methanol, to synthesize multicarbon compounds but also to act as flexible catalysts for hydrogen storage or production.     

Knock-out of metacaspase and/or cytochrome c results in the activation of a ROS-independent acetic acid-induced programmed cell death pathway in yeast

To gain further insight into yeast acetic acid-induced programmed cell death (AA-PCD) we analyzed the effects of the antioxidant N-acetyl-l-cysteine (NAC) on cell viability, hydrogen peroxide (H₂O₂) production, DNA fragmentation, cytochrome c (cyt c) release and caspase-like activation in wild type (wt) and metacaspase and/or cyt c-lacking cells. We found that NAC prevents AA-PCD in wt cells, by scavenging H₂O₂ and by inhibiting both cyt c release and caspase-like activation. This shows the occurrence of a reactive oxygen species (ROS)-dependent AA-PCD. Contrarily no NAC dependent change in AA-PCD of mutant cells was detectable, showing that a ROS-independent AA-PCD can also occur.     

Ecosystem fluxes of hydrogen in a mid‐latitude forest driven by soil microorganisms and plants

Molecular hydrogen (H₂) is an atmospheric trace gas with a large microbe‐mediated soil sink, yet cycling of this compound throughout ecosystems is poorly understood. Measurements of the sources and sinks of H₂ in various ecosystems are sparse, resulting in large uncertainties in the global H₂ budget. Constraining the H₂ cycle is critical to understanding its role in atmospheric chemistry and climate. We measured H₂ fluxes at high frequency in a temperate mixed deciduous forest for 15 months using a tower‐based flux‐gradient approach to determine both the soil‐atmosphere and the net ecosystem flux of H₂. We found that Harvard Forest is a net H₂ sink (?1.4 ± 1.1 kg H₂ ha^?1) with soils as the dominant H₂ sink (?2.0 ± 1.0 kg H₂ ha^?1) and aboveground canopy emissions as the dominant H₂ source (+0.6 ± 0.8 kg H₂ ha^?1). Aboveground emissions of H₂ were an unexpected and substantial component of the ecosystem H₂ flux, reducing net ecosystem uptake by 30% of that calculated from soil uptake alone. Soil uptake was highly seasonal (July maximum, February minimum), positively correlated with soil temperature and negatively correlated with environmental variables relevant to diffusion into soils (i.e., soil moisture, snow depth, snow density). Soil microbial H₂ uptake was correlated with rhizosphere respiration rates (r = 0.8, P < 0.001), and H₂ metabolism yielded up to 2% of the energy gleaned by microbes from carbon substrate respiration. Here, we elucidate key processes controlling the biosphere–atmosphere exchange of H₂ and raise new questions regarding the role of aboveground biomass as a source of atmospheric H₂ and mechanisms linking soil H₂ and carbon cycling. Results from this study should be incorporated into modeling efforts to predict the response of the H₂ soil sink to changes in anthropogenic H₂ emissions and shifting soil conditions with climate and land‐use change.     

Individuals with higher metabolic rates have lower levels of reactive oxygen species in vivo

There is increasing interest in the effect of energy metabolism on oxidative stress, but much ambiguity over the relationship between the rate of oxygen consumption and the generation of reactive oxygen species (ROS). Production of ROS (such as hydrogen peroxide, H₂O₂) in the mitochondria is primarily inferred indirectly from measurements in vitro, which may not reflect actual ROS production in living animals. Here, we measured in vivo H₂O₂ content using the recently developed MitoB probe that becomes concentrated in the mitochondria of living organisms, where it is converted by H₂O₂ into an alternative form termed MitoP; the ratio of MitoP/MitoB indicates the level of mitochondrial H₂O₂ in vivo. Using the brown trout Salmo trutta, we tested whether this measurement of in vivo H₂O₂ content over a 24 h-period was related to interindividual variation in standard metabolic rate (SMR). We showed that the H₂O₂ content varied up to 26-fold among fish of the same age and under identical environmental conditions and nutritional states. Interindividual variation in H₂O₂ content was unrelated to mitochondrial density but was significantly associated with SMR: fish with a higher mass-independent SMR had a lower level of H₂O₂. The mechanism underlying this observed relationship between SMR and in vivo H₂O₂ content requires further investigation, but may implicate mitochondrial uncoupling which can simultaneously increase SMR but reduce ROS production. To our knowledge, this is the first study in living organisms to show that individuals with higher oxygen consumption rates can actually have lower levels of H₂O₂.     

Detection of a Reproducible,Single-Member Shift in Soil Bacterial Communities Exposed to Low Levels of Hydrogen

Soil is exposed to hydrogen when symbiotic rhizobia in legume root nodules cannot recycle the hydrogen that is generated during nitrogen fixation. The hydrogen emitted is most likely taken up by free-living soil bacteria that use hydrogen as an energy source, though the bacteria that do this in situ remain unclear. In this study, we investigated the effect of hydrogen exposure on the bacteria of two different soils in a microcosm setup designed to simulate hydrogen-emitting root nodules. Although the size and overall composition of the soil bacterial community did not significantly alter after hydrogen exposure, one ribotype increased in relative abundance within each soil. This single-ribotype shift was identified by generating multiple terminal restriction fragment length polymorphism (T-RFLP) profiles of 16S rRNA genes from each soil sample, with gene sequence confirmation to identify terminal restriction fragments. The increased abundance of a single ribotype after hydrogen exposure, within an otherwise similar community, was found in replicate samples taken from each microcosm and was reproducible across replicate experiments. Similarly, only one member of the soil bacterial community increased in abundance in response to hydrogen exposure in soil surrounding the root nodules of field-grown soybean (Glycine max). The ribotypes that increased after hydrogen exposure in each soil system tested were all from known hydrogen-oxidizing lineages within the order Actinomycetales. We suggest that soil actinomycetes are important utilizers of hydrogen at relevant concentrations in soil and could be key contributors to soil''s function as a sink in the global hydrogen cycle.Soil is the major sink in the global hydrogen cycle and accounts for approximately 75 to 80% of uptake from the atmosphere (7, 11). Soil is such a strong sink that the atmospheric mixing ratio of molecular hydrogen, H₂, is hemispherically asymmetric because of the greater landmass in the Northern Hemisphere (11). Many nitrogen-fixing bacteria that form symbiotic relationships with legume plants cannot recycle the H₂ that is generated during N₂ fixation (2, 13). Most of the H₂ emitted from legume root nodules is taken up by the surrounding soil, within a few centimeters of the nodule surface, and is not released to the atmosphere (20). Although the H₂ emitted by the rhizobial symbionts costs the legume approximately 5% of its daily photosynthate and “represents a significant investment by the plant” (9), there is growing evidence to suggest that soil exposed to H₂ is beneficial to plant growth, separate from the benefits derived from N₂ fixation (8, 10, 28). Previously, La Favre and Focht have hypothesized that “the hydrogen which is evolved during N₂ fixation represents an additional energy input into the plant-soil ecosystem… since metabolism of H₂ by chemolithotrophic bacteria results in an input of fixed carbon to the system” (20). A number of studies have found that when H₂ is taken up by soil, net CO₂ fixation occurs at the rate of 7 to 8 nmol CO₂ per g of soil per h (22, 34). For a legume fixing 200 kg of atmospheric N₂ per hectare, over 200,000 liters of H₂ could be released into the legume''s rhizosphere over the duration of the growing season and CO₂ fixation could result in an extra 25 kg of soil carbon fixed per hectare (9, 10, 28).Many bacteria isolated from soil are able to utilize H₂ as an energy source (2, 5-7, 21), and free-living bacteria are most likely responsible for the H₂ uptake observed by soil surrounding legume roots (22). Adding a bacterial energy source, such as H₂, could affect the microbial population size, as has been observed previously (34), but more specific shifts within the bacterial community may occur if just the microorganisms able to utilize the energy source multiply. Their activity could also have downstream consequences specifically on other members of the community. Most H₂-oxidizing cultures have required enrichment with concentrations of H₂ that are not environmentally relevant and therefore cannot be assumed to be carrying out H₂ oxidation at much lower, naturally occurring concentrations (5-7). Recent surveys of microbes present in soil samples, via their nucleic acids, have revealed many novel bacterial inhabitants that have been little studied and thus may also be contributing to the repertoire of bacterial soil processes, such as H₂ uptake (16). A recent study into the effect of H₂ on soil bacteria focused on a few groups of H₂-oxidizing, autotrophic bacteria and thus ignored many other H₂ utilizers potentially present in soil (34).There are now many ways of characterizing the entire microbial community in environmental samples, either via their entire genomic content, though metagenomic analysis of soil is difficult at present, or via analysis of the lineages present according to 16S rRNA gene sequences, or ribotypes (36). A recent study comparing high-throughput pyrosequencing of 16S rRNA genes and an easily accessible profiling method, known as terminal restriction fragment length polymorphism (T-RFLP), found the simpler profiles were appropriate for comparing the dominant ribotypes in multiple samples (24). Although T-RFLP profiles only provide a simplified snapshot of the dominant members in microbial communities, compared to the deeper analyses provided by microarrays or high-throughput sequencing technologies, T-RFLP profiling is a cost-effective, reproducible, and robust method of “fingerprinting” many soil samples rapidly and efficiently (14, 24, 25, 32).In this study, we chose to assess the dominant members of the soil bacterial community via T-RFLP profiles of ribotypes present in H₂-treated and control soils to avoid a narrow focus on well-studied H₂ oxidizers. We investigated the bacterial community structure in two different soils, utilizing a microcosm setup with concentrations of H₂ calculated to occur in the rhizosphere of N₂-fixing legumes, to determine whether common responses to H₂ exposure could be predicted from soils that differ by climate, edaphic characteristics, and starting communities. Soil in microcosms has previously been shown to have similar H₂ uptake properties to soil close to H₂-emitting legume nodules (9), but we also complemented our plant-free microcosm work with an examination of soil collected from the root systems of field-grown soybean (Glycine max (L.) Merr.).     

Symbiotic Legume Nodules Employ Both Rhizobial Exo- and Endo-Hydrogenases to Recycle Hydrogen Produced by Nitrogen Fixation

Background

In symbiotic legume nodules, endosymbiotic rhizobia (bacteroids) fix atmospheric N₂, an ATP-dependent catalytic process yielding stoichiometric ammonium and hydrogen gas (H₂). While in most legume nodules this H₂ is quantitatively evolved, which loss drains metabolic energy, certain bacteroid strains employ uptake hydrogenase activity and thus evolve little or no H₂. Rather, endogenous H₂ is efficiently respired at the expense of O₂, driving oxidative phosphorylation, recouping ATP used for H₂ production, and increasing the efficiency of symbiotic nodule N₂ fixation. In many ensuing investigations since its discovery as a physiological process, bacteroid uptake hydrogenase activity has been presumed a single entity.

Methodology/Principal Findings

Azorhizobium caulinodans, the nodule endosymbiont of Sesbania rostrata stems and roots, possesses both orthodox respiratory (exo-)hydrogenase and novel (endo-)hydrogenase activities. These two respiratory hydrogenases are structurally quite distinct and encoded by disparate, unlinked gene-sets. As shown here, in S. rostrata symbiotic nodules, haploid A. caulinodans bacteroids carrying single knockout alleles in either exo- or-endo-hydrogenase structural genes, like the wild-type parent, evolve no detectable H₂ and thus are fully competent for endogenous H₂ recycling. Whereas, nodules formed with A. caulinodans exo-, endo-hydrogenase double-mutants evolve endogenous H₂ quantitatively and thus suffer complete loss of H₂ recycling capability. More generally, from bioinformatic analyses, diazotrophic microaerophiles, including rhizobia, which respire H₂ may carry both exo- and endo-hydrogenase gene-sets.

Conclusions/Significance

In symbiotic S. rostrata nodules, A. caulinodans bacteroids can use either respiratory hydrogenase to recycle endogenous H₂ produced by N₂ fixation. Thus, H₂ recycling by symbiotic legume nodules may involve multiple respiratory hydrogenases.     

Characterization of Two Subsurface H2-Utilizing Bacteria, Desulfomicrobium hypogeium sp. nov. and Acetobacterium psammolithicum sp. nov., and Their Ecological Roles

We examined the relative roles of acetogenic and sulfate-reducing bacteria in H₂ consumption in a previously characterized subsurface sandstone ecosystem. Enrichment cultures originally inoculated with ground sandstone material obtained from a Cretaceous formation in central New Mexico were grown with hydrogen in a mineral medium supplemented with 0.02% yeast extract. Sulfate reduction and acetogenesis occurred in these cultures, and the two most abundant organisms carrying out the reactions were isolated. Based on 16S rRNA analysis data and on substrate utilization patterns, these organisms were named Desulfomicrobium hypogeium sp. nov. and Acetobacterium psammolithicum sp. nov. The steady-state H₂ concentrations measured in sandstone-sediment slurries (threshold concentration, 5 nM), in pure cultures of sulfate reducers (threshold concentration, 2 nM), and in pure cultures of acetogens (threshold concentrations 195 to 414 nM) suggest that sulfate reduction is the dominant terminal electron-accepting process in the ecosystem examined. In an experiment in which direct competition for H₂ between D. hypogeium and A. psammolithicum was examined, sulfate reduction was the dominant process.     

Hydrogen peroxide and the evolution of oxygenic photosynthesis

The early atmosphere of the Earth is considered to have been reducing (H₂ rich) or neutral (CO₂-N₂). The present atmosphere by contrast is highly oxidizing (20% O₂). The source of this oxygen is generally agreed to have been oxygenic photosynthesis, whereby organisms use water as the electron donor in the production of organic matter, liberating oxygen into the atmosphere. A major question in the evolution of life is how oxygenic photosynthesis could have evolved under anoxic conditions — and also when this capability evolved. It seems unlikely that water would be employed as the electron donor in anoxic environments that were rich in reducing agents such as ferrous or sulfide ions which could play that role. The abiotic production of atmospheric oxidants could have provided a mechanism by which locally oxidizing conditions were sustained within spatially confined habitats thus removing the available reductants and forcing photosynthetic organisms to utilize water as the electron donor. We suggest that atmospheric H₂O₂ played the key role in inducing oxygenic photosynthesis because as peroxide increased in a local environment, organisms would not only be faced with a loss of reductant, but they would also be pressed to develop the biochemical apparatus (e.g., catalase) that would ultimately be needed to protect against the products of oxygenic photosynthesis. This scenario allows for the early evolution of oxygenic photosynthesis while global conditions were still anaerobic.     

Hydrogen uptake by the nitrogen-starved cyanobacterium Anabaena cylindrica

The role of the oxyhydrogen reaction in the nitrogen metabolism of Anabaena cylin-drica, particularly under conditions of dinitrogen starvation, was investigated. It was shown that although this reaction supports nitrogenase activity in the dark, when the cells are deprived of nitrogen the rate of hydrogen uptake is little changed. Measurements of ammonia excretion into the medium in the presence of methionine sulfoximine under such conditions indicated that hydrogen uptake supported the turnover of cell protein as an alternative source of nitrogen. In the absence of H₂ and O₂ in the dark, nitrogenase activity was negligible but protein turnover continued. In their presence nitrogenase activity was greatly stimulated; turnover was also stimulated but to a greater extent in the absence of nitrogenase substrates. The oxyhydrogen reaction also stimulated uptake of ammonium ions by intact filaments in argon in the dark. Only at very low hydrogen tensions can net hydrogen formation be obtained in argon/CO₂ in the light, casting considerable doubt on the suitability of hydrogenase-containing organisms for biophotolytic hydrogen formation. Addition of exogenous ammonia to the cultures incubated in argon resulted in a pronounced stimulation of H₂ uptake; nitrate and its derivatives had no such effect, nor did various amino acid derivatives of ammonia.     

Evaluation of antioxidant and neuroprotective effect of Hippophae rhamnoides (L.) on oxidative stress induced cytotoxicity in human neural cell line IMR32

Aim and objectiveHippophae rhamnoides is an edible, nutrient rich plant found in the northern regions of India. It belongs to the family Elaeagnaceae and is well known for its traditional pharmacological activities. The present study was aimed to investigate the antioxidant and neuroprotective activities of H. rhamnoides.MethodologyThe hydroalcoholic extract of H. rhamnoides was evaluated for free radical scavenging activity using DPPH, hydroxyl radical scavenging and ferric thiocyanate assays. In vitro neuroprotective activity was assessed on human neuroblastoma cell line-IMR32 against hydrogen peroxide (H₂O₂) induced cytotoxicity. The neuroprotective effect was determined by measuring the cell viability through tetrazolium dye MTT (3-(4,5-dimethylthiazol-2-yl)-2,5-diphenyltetrazolium bromide) reducing assay and propidium iodide (PI) staining. Also the intracellular reactive oxygen species (ROS) activity was assessed using dichloro-dihydro-fluorescein diacetate (DCFDA) assay by flowcytometer.ResultsThe results of the study demonstrated that H. rhamnoides extract possesses potential free radical scavenging activity. The IC₅₀ value for DPPH and OH radical scavenging assay was 70.92 μg/ml and 0.463 mg/ml, also the extract was also found to have considerable level of lipid peroxidation activity. The neuroprotective effect of H. rhamnoides was confirmed by its cell viability enhancing capacity against hydrogen peroxide induced cell cytotoxicity. The extract acted on IMR32 cells in a dose dependent manner as observed through PI and MTT assays. The percentage intracellular ROS activity was reduced by 60–70% in treated cells compared to H₂O₂ control.ConclusionThus the outcome of the study suggests that H. rhamnoides acts as a neuroprotectant against oxidative stress induced neurodegeneration.     

Microbial diversity and genomics in aid of bioenergy

In view of the realization that fossil fuels reserves are limited, various options of generating energy are being explored. Biological methods for producing fuels such as ethanol, diesel, hydrogen (H₂), methane, etc. have the potential to provide a sustainable energy system for the society. Biological H₂ production appears to be the most promising as it is non-polluting and can be produced from water and biological wastes. The major limiting factors are low yields, lack of industrially robust organisms, and high cost of feed. Actually, H₂ yields are lower than theoretically possible yields of 4 mol/mol of glucose because of the associated fermentation products such as lactic acid, propionic acid and ethanol. The efficiency of energy production can be improved by screening microbial diversity and easily fermentable feed materials. Biowastes can serve as feed for H₂ production through a set of microbial consortia: (1) hydrolytic bacteria, (2) H₂ producers (dark fermentative and photosynthetic). The efficiency of the bioconversion process may be enhanced further by the production of value added chemicals such as polydroxyalkanoate and anaerobic digestion. Discovery of enormous microbial diversity and sequencing of a wide range of organisms may enable us to realize genetic variability, identify organisms with natural ability to acquire and transmit genes. Such organisms can be exploited through genome shuffling for transgenic expression and efficient generation of clean fuel and other diverse biotechnological applications. JIMB 2008: BioEnergy-Special issue