Metabolic versatility of the nitrite-oxidizing bacterium Nitrospira marina and its proteomic response to oxygen-limited conditions

The genus Nitrospira is the most widespread group of nitrite-oxidizing bacteria and thrives in diverse natural and engineered ecosystems. Nitrospira marina Nb-295^T was isolated from the ocean over 30 years ago; however, its genome has not yet been analyzed. Here, we investigated the metabolic potential of N. marina based on its complete genome sequence and performed physiological experiments to test genome-derived hypotheses. Our data confirm that N. marina benefits from additions of undefined organic carbon substrates, has adaptations to resist oxidative, osmotic, and UV light-induced stress and low dissolved pCO₂, and requires exogenous vitamin B₁₂. In addition, N. marina is able to grow chemoorganotrophically on formate, and is thus not an obligate chemolithoautotroph. We further investigated the proteomic response of N. marina to low (∼5.6 µM) O₂ concentrations. The abundance of a potentially more efficient CO₂-fixing pyruvate:ferredoxin oxidoreductase (POR) complex and a high-affinity cbb₃-type terminal oxidase increased under O₂ limitation, suggesting a role in sustaining nitrite oxidation-driven autotrophy. This putatively more O₂-sensitive POR complex might be protected from oxidative damage by Cu/Zn-binding superoxide dismutase, which also increased in abundance under low O₂ conditions. Furthermore, the upregulation of proteins involved in alternative energy metabolisms, including Group 3b [NiFe] hydrogenase and formate dehydrogenase, indicate a high metabolic versatility to survive conditions unfavorable for aerobic nitrite oxidation. In summary, the genome and proteome of the first marine Nitrospira isolate identifies adaptations to life in the oxic ocean and provides insights into the metabolic diversity and niche differentiation of NOB in marine environments.Subject terms: Water microbiology, Microbial biooceanography, Marine microbiology, Bacterial genomics, Bacterial physiology     

Nitrifying bacterial community structures and their nitrification performance under sufficient and limited inorganic carbon conditions

This study examined the hypothesis that different inorganic carbon (IC) conditions enrich different ammonia-oxidizing bacteria (AOB) and nitrite-oxidizing bacteria (NOB) populations by operating two laboratory-scale continuous-flow bioreactors fed with 15 and 100 mg IC/L, respectively. During this study, both bioreactors maintained satisfactory nitrification performance and stably oxidized 250 mg?N/L of influent ammonium without nitrite accumulation. Based on results of cloning/sequencing and terminal restriction fragment length polymorphism targeting on the ammonia monooxygenase subunit A (amoA) gene, Nitrosomonas nitrosa lineage was identified as the dominant AOB population in the high-IC bioreactor, while Nitrosomonas europaea and Nitrosomonas nitrosa lineage AOB were dominant in the low-IC bioreactor. Results of real-time polymerase chain reactions for Nitrobacter and Nitrospira 16S rRNA genes indicated that Nitrospira was the predominant NOB population in the high-IC bioreactor, while Nitrobacter was the dominant NOB in the low-IC bioreactor. Furthermore, batch experiment results suggest that N. europaea and Nitrobacter populations are proliferated in the low-IC bioreactor due to their higher rates under low IC conditions despite the fact that these two populations have been identified as weak competitors, compared with N. nitrosa and Nitrospira, under low ammonium/nitrite environments. This study revealed that in addition to ammonium/nitrite concentrations, limited IC conditions may also be important in selecting dominant AOB/NOB communities of nitrifying bioreactors.     

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     

Cyanobacterial H<Subscript>2</Subscript> production — a comparative analysis

Several unicellular and filamentous, nitrogen-fixing and non-nitrogen-fixing cyanobacterial strains have been investigated on the molecular and the physiological level in order to find the most efficient organisms for photobiological hydrogen production. These strains were screened for the presence or absence of hup and hox genes, and it was shown that they have different sets of genes involved in H₂ evolution. The uptake hydrogenase was identified in all N₂-fixing cyanobacteria, and some of these strains also contained the bidirectional hydrogenase, whereas the non-nitrogen fixing strains only possessed the bidirectional enzyme. In N₂-fixing strains, hydrogen was mainly produced by the nitrogenase as a by-product during the reduction of atmospheric nitrogen to ammonia. Therefore, hydrogen production was investigated both under non-nitrogen-fixing conditions and under nitrogen limitation. It was shown that the hydrogen uptake activity is linked to the nitrogenase activity, whereas the hydrogen evolution activity of the bidirectional hydrogenase is not dependent or even related to diazotrophic growth conditions. With regard to large-scale hydrogen evolution by N₂-fixing cyanobacteria, hydrogen uptake-deficient mutants have to be used because of their inability to re-oxidize the hydrogen produced by the nitrogenase. On the other hand, fermentative H₂ production by the bidirectional hydrogenase should also be taken into account in further investigations of biological hydrogen production.Abbreviations Chl chlorophyll - MV methyl viologen     

Autotrophic growth of nitrifying community in an agricultural soil

The two-step nitrification process is an integral part of the global nitrogen cycle, and it is accomplished by distinctly different nitrifiers. By combining DNA-based stable isotope probing (SIP) and high-throughput pyrosequencing, we present the molecular evidence for autotrophic growth of ammonia-oxidizing bacteria (AOB), ammonia-oxidizing archaea (AOA) and nitrite-oxidizing bacteria (NOB) in agricultural soil upon ammonium fertilization. Time-course incubation of SIP microcosms indicated that the amoA genes of AOB was increasingly labeled by ¹³CO₂ after incubation for 3, 7 and 28 days during active nitrification, whereas labeling of the AOA amoA gene was detected to a much lesser extent only after a 28-day incubation. Phylogenetic analysis of the ¹³C-labeled amoA and 16S rRNA genes revealed that the Nitrosospira cluster 3-like sequences dominate the active AOB community and that active AOA is affiliated with the moderately thermophilic Nitrososphaera gargensis from a hot spring. The higher relative frequency of Nitrospira-like NOB in the ¹³C-labeled DNA suggests that it may be more actively involved in nitrite oxidation than Nitrobacter-like NOB. Furthermore, the acetylene inhibition technique showed that ¹³CO₂ assimilation by AOB, AOA and NOB occurs only when ammonia oxidation is not blocked, which provides strong hints for the chemolithoautotrophy of nitrifying community in complex soil environments. These results show that the microbial community of AOB and NOB dominates the nitrification process in the agricultural soil tested.     

Interactions between Thaumarchaea,Nitrospira and methanotrophs modulate autotrophic nitrification in volcanic grassland soil

Ammonium/ammonia is the sole energy substrate of ammonia oxidizers, and is also an essential nitrogen source for other microorganisms. Ammonia oxidizers therefore must compete with other soil microorganisms such as methane-oxidizing bacteria (MOB) in terrestrial ecosystems when ammonium concentrations are limiting. Here we report on the interactions between nitrifying communities dominated by ammonia-oxidizing archaea (AOA) and Nitrospira-like nitrite-oxidizing bacteria (NOB), and communities of MOB in controlled microcosm experiments with two levels of ammonium and methane availability. We observed strong stimulatory effects of elevated ammonium concentration on the processes of nitrification and methane oxidation as well as on the abundances of autotrophically growing nitrifiers. However, the key players in nitrification and methane oxidation, identified by stable-isotope labeling using ¹³CO₂ and ¹³CH₄, were the same under both ammonium levels, namely type 1.1a AOA, sublineage I and II Nitrospira-like NOB and Methylomicrobium-/Methylosarcina-like MOB, respectively. Ammonia-oxidizing bacteria were nearly absent, and ammonia oxidation could almost exclusively be attributed to AOA. Interestingly, although AOA functional gene abundance increased 10-fold during incubation, there was very limited evidence of autotrophic growth, suggesting a partly mixotrophic lifestyle. Furthermore, autotrophic growth of AOA and NOB was inhibited by active MOB at both ammonium levels. Our results suggest the existence of a previously overlooked competition for nitrogen between nitrifiers and methane oxidizers in soil, thus linking two of the most important biogeochemical cycles in nature.     

Hydrogenase mediated nitrite reduction in chlorella

The assay of the hydrogenase of glucose-grown cells of Chlorella pyrenoidosa, strain 7-11-05 by means of nitrite reduction with molecular hydrogen is described. The hydrogenase of Chlorella shows maximum activity immediately after equilibration in the hydrogen atmosphere. The hydrogenase mediated reduction of nitrite to ammonia requires the presence of CO₂. However, at pH 6.4. when the reaction proceeds optimally, there is apparently sufficient retention of metabolic CO₂ to support the reaction, which goes to completion, at near maximum rates.

Reduction of nitrite in the hydrogenase system when CO₂ is present results in the uptake of 3 moles of H₂ per mole of nitrite and ammonia is the product. When CO₂ is absent or limiting, ammonia is also formed from nitrite but with the uptake of less than the stoichiometric amount of H₂. It is concluded that CO₂ is essential for the uptake of H₂, and that in the absence of CO₂ internal hydrogen donors support nitrite reduction.

The possibility that CO₂ exerts a catalytic effect in all reductions mediated by hydrogenase in algae is considered, and a further hypothesis, that hydrogenase arises from that portion of the photosynthetic machinery which also shows a catalytic requirement for CO₂, is proposed.

     

Rapid nitrification involving comammox and canonical Nitrospira at extreme pH in saline-alkaline lakes

Nitrite-oxidizing bacteria (NOB) catalyse the second nitrification step and are the main biological source of nitrate. The most diverse and widespread NOB genus is Nitrospira, which also contains complete ammonia oxidizers (comammox) that oxidize ammonia to nitrate. To date, little is known about the occurrence and biology of comammox and canonical nitrite oxidizing Nitrospira in extremely alkaline environments. Here, we studied the seasonal distribution and diversity, and the effect of short-term pH changes on comammox and canonical Nitrospira in sediments of two saline, highly alkaline lakes. We identified diverse canonical and comammox Nitrospira clade A-like phylotypes as the only detectable NOB during more than a year, suggesting their major importance for nitrification in these habitats. Gross nitrification rates measured in microcosm incubations were highest at pH 10 and considerably faster than reported for other natural, aquatic environments. Nitrification could be attributed to canonical and comammox Nitrospira and to Nitrososphaerales ammonia-oxidizing archaea. Furthermore, our data suggested that comammox Nitrospira contributed to ammonia oxidation at an extremely alkaline pH of 11. These results identify saline, highly alkaline lake sediments as environments of uniquely strong nitrification with novel comammox Nitrospira as key microbial players.     

The purification of hydrogenase II (uptake hydrogenase) from the anaerobic N2-fixing bacterium Clostridium pasteurianum

The H₂ uptake activity (units/mg protein) of Clostridium pasteurianum cells with methylene blue as the electron acceptor increases with cell density independent of the growth conditions. The H₂ evolution activity (units/mg protein) of the same cells with reduced methyl viologen as the electron donor remains fairly constant under all growth conditions tested. Cells grown under N₂-fixing conditions have the highest H₂ uptake activity and were used for the purification of hydrogenase II (uptake hydrogenase). Attempts to separate hydrogenase II from hydrogenase I (bidirectional hydrogenase) by a previously published method were unreliable. We report here a new large-scale purification procedure which employs a rapid membrane filtration system to fractionate cell-free extracts. Hydrogenases I and II were easily filtered into the low-molecular-weight fraction (M_r less than 100 000), and from this, hydrogenase II was further purified to a homogeneous state. Hydrogenase II is a monomeric iron-sulfur protein of molecular weight 53 000 containing eight iron atoms and eight acid-labile sulfur atoms per molecule. Hydrogenase II catalyzes both H₂ oxidation and H₂ evolution at rates of 3000 and 5.9 μmol H₂ consumed or evolved/min per mg protein, respectively. The purification procedure for hydrogenase II using the filtration system described greatly facilitates the large-scale purification of hydrogenase I and other enzymes from cell-free extracts of C. pasteurianum.     

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.     

Nitrotoga-like bacteria are previously unrecognized key nitrite oxidizers in full-scale wastewater treatment plants

Numerous past studies have shown members of the genus Nitrospira to be the predominant nitrite-oxidizing bacteria (NOB) in nitrifying wastewater treatment plants (WWTPs). Only recently, the novel NOB ‘Candidatus Nitrotoga arctica'' was identified in permafrost soil and a close relative was enriched from activated sludge. Still, little is known about diversity, distribution and functional importance of Nitrotoga in natural and engineered ecosystems. Here we developed Nitrotoga 16S rRNA-specific PCR primers and fluorescence in situ hybridization (FISH) probes, which were applied to screen activated sludge samples from 20 full-scale WWTPs. Nitrotoga-like bacteria were detected by PCR in 11 samples and reached abundances detectable by FISH in seven sludges. They coexisted with Nitrospira in most of these WWTPs, but constituted the only detectable NOB in two systems. Quantitative FISH revealed that Nitrotoga accounted for nearly 2% of the total bacterial community in one of these plants, a number comparable to Nitrospira abundances in other WWTPs. Spatial statistics revealed that Nitrotoga coaggregated with ammonia-oxidizing bacteria, strongly supporting a functional role in nitrite oxidation. This activity was confirmed by FISH in combination with microradiography, which revealed nitrite-dependent autotrophic carbon fixation by Nitrotoga in situ. Correlation of the presence or absence with WWTP operational parameters indicated low temperatures as a main factor supporting high Nitrotoga abundances, although in incubation experiments these NOB remained active over an unexpected range of temperatures, and also at different ambient nitrite concentrations. In conclusion, this study demonstrates that Nitrotoga can be functionally important nitrite oxidizers in WWTPs and can even represent the only known NOB in engineered systems.     

Exploring the upper pH limits of nitrite oxidation: diversity,ecophysiology, and adaptive traits of haloalkalitolerant Nitrospira

Nitrite-oxidizing bacteria of the genus Nitrospira are key players of the biogeochemical nitrogen cycle. However, little is known about their occurrence and survival strategies in extreme pH environments. Here, we report on the discovery of physiologically versatile, haloalkalitolerant Nitrospira that drive nitrite oxidation at exceptionally high pH. Nitrospira distribution, diversity, and ecophysiology were studied in hypo- and subsaline (1.3–12.8 g salt/l), highly alkaline (pH 8.9–10.3) lakes by amplicon sequencing, metagenomics, and cultivation-based approaches. Surprisingly, not only were Nitrospira populations detected, but they were also considerably diverse with presence of members from  Nitrospira lineages I, II and IV. Furthermore, the ability of Nitrospira enrichment cultures to oxidize nitrite at neutral to highly alkaline pH of 10.5 was demonstrated. Metagenomic analysis of a newly enriched Nitrospira lineage IV species, “Candidatus Nitrospira alkalitolerans”, revealed numerous adaptive features of this organism to its extreme environment. Among them were a sodium-dependent N-type ATPase and NADH:quinone oxidoreductase next to the proton-driven forms usually found in Nitrospira. Other functions aid in pH and cation homeostasis and osmotic stress defense. “Ca. Nitrospira alkalitolerans” also possesses group 2a and 3b [NiFe] hydrogenases, suggesting it can use hydrogen as alternative energy source. These results reveal how Nitrospira cope with strongly fluctuating pH and salinity conditions and expand our knowledge of nitrogen cycling in extreme habitats.Subject terms: Environmental microbiology, Microbial ecology     

Hydrogen utilization by Methylocystis sp. strain SC2 expands the known metabolic versatility of type IIa methanotrophs

Methane, a non-expensive natural substrate, is used by Methylocystis spp. as a sole source of carbon and energy. Here, we assessed whether Methylocystis sp. strain SC2 is able to also utilize hydrogen as an energy source. The addition of 2% H₂ to the culture headspace had the most significant positive effect on the growth yield under CH₄ (6%) and O₂ (3%) limited conditions. The SC2 biomass yield doubled from 6.41 (±0.52) to 13.82 (±0.69) mg cell dry weight per mmol CH₄, while CH₄ consumption was significantly reduced. Regardless of H₂ addition, CH₄ utilization was increasingly redirected from respiration to fermentation-based pathways with decreasing O₂/CH₄ mixing ratios. Theoretical thermodynamic calculations confirmed that hydrogen utilization under oxygen-limited conditions doubles the maximum biomass yield compared to fully aerobic conditions without H₂ addition. Hydrogen utilization was linked to significant changes in the SC2 proteome. In addition to hydrogenase accessory proteins, the production of Group 1d and Group 2b hydrogenases was significantly increased in both short- and long-term incubations. Both long-term incubation with H₂ (37 d) and treatments with chemical inhibitors revealed that SC2 growth under hydrogen-utilizing conditions does not require the activity of complex I. Apparently, strain SC2 has the metabolic capacity to channel hydrogen-derived electrons into the quinone pool, which provides a link between hydrogen oxidation and energy production. In summary, H₂ may be a promising alternative energy source in biotechnologically oriented methanotroph projects that aim to maximize biomass yield from CH_4, such as the production of high-quality feed protein.     

Enrichment and Physiological Characterization of a Novel Nitrospira-Like Bacterium Obtained from a Marine Sponge

Members of the nitrite-oxidizing genus Nitrospira are most likely responsible for the second step of nitrification, the conversion of nitrite (NO₂⁻) to nitrate (NO₃⁻), within various sponges. We succeeded in obtaining an enrichment culture of Nitrospira derived from the mesohyl of the marine sponge Aplysina aerophoba using a traditional cultivation approach. Electron microscopy gave first evidence of the shape and ultrastructure of this novel marine Nitrospira-like bacterium (culture Aa01). We characterized these bacteria physiologically with regard to optimal incubation conditions, especially the temperature and substrate range in comparison to other Nitrospira cultures. Best growth was obtained at temperatures between 28°C and 30°C in mineral medium with 70% North Sea water and a substrate concentration of 0.5 mM nitrite under microaerophilic conditions. The Nitrospira culture Aa01 is very sensitive against nitrite, because concentrations higher than 1.5 mM resulted in a complete inhibition of growth. Sequence analyses of the 16S rRNA gene revealed that the novel Nitrospira-like bacterium is separated from the sponge-specific subcluster and falls together with an environmental clone from Mediterranean sediments (98.6% similarity). The next taxonomically described species Nitrospira marina is only distantly related, with 94.6% sequence similarity, and therefore the culture Aa01 represents a novel species of nitrite-oxidizing bacteria.Numerous sponges have the capacity to accommodate large amounts of diverse microbes and represent significant sources for bioactive natural compounds (13). Many marine invertebrates excrete ammonium as a metabolic waste product (9), and the excretion of nitrite and nitrate has been taken as primary evidence that nitrifiers are active in these animals (10). By modulation of their pumping, sponges are a suitable habitat not only for aerobic microbes but also for anaerobic microbes. Accordingly, Hoffmann et al. (19) were able to detect major microbial pathways of the nitrogen cycle in the sponge Geodia barretti, including nitrification, the anammox process, and denitrification.Nitrification involves the biological oxidation of ammonia (NH₃) to nitrite (NO₂⁻) and further to nitrate (NO₃⁻) for energy purposes. It is of fundamental importance for the global nitrogen cycle in aquatic and terrestrial habitats. Nitrification is catalyzed by two phylogenetically distinct groups of microorganisms: in the first step, ammonia-oxidizing bacteria and archaea (AOB and AOA) take part in the oxidation of ammonia to nitrite, and in the second step nitrite-oxidizing bacteria (NOB) convert nitrite to nitrate (38).Nitrite has a central position in the nitrogen cycle, connecting aerobic and anaerobic pathways. Nitrite-oxidizing bacteria play a major role in removing nitrite from the environment because it is toxic for living organisms (31). Based on morphological characteristics, NOB have been divided into five genera. This classification also reflects the phylogenetic diversity of NOB, which includes Nitrobacter and Nitrococcus (Alpha- and Gammaproteobacteria), Nitrospina (putative Deltaproteobacteria), and the candidate genus “Candidatus Nitrotoga” (Betaproteobacteria) (2). The genus Nitrospira is more distantly related to the other known NOB because it is part of its own deep-branching bacterial phylum Nitrospirae. Marine species are present in all genera of NOB except in the newly identified genus “Candidatus Nitrotoga.”As all known nitrifying prokaryotes are slow growing and hard to maintain, their enrichment and isolation from environmental samples is difficult. Most physiological studies have been performed with pure cultures of a few “model” nitrifiers, in particular AOB related to the genus Nitrosomonas and NOB of the genus Nitrobacter. For the genus Nitrospira there are only four pure cultures available: the marine species Nitrospira marina (37), Nitrospira moscoviensis (12), “Candidatus Nitrospira bockiana” (25), and Nitrospira calida (E. Lebedeva, personal communication).Sponges of the family Aplysinidae contain large amounts of bacteria embedded within the sponge tissue matrix (15). For example, the biomass of Aplysina aerophoba consists of up to 40% bacteria (36). These sponges are able to differentiate between food bacteria and their own bacterial symbionts (41). Investigations of the diversity of sponge-associated bacteria, including different genetic and also cultivation approaches, have been made with several specimens (15, 16, 39). In terms of nitrification, Hentschel et al. (17) gave first evidence for the presence of nitrite oxidizers, and it has been verified that sponges harbor AOB and AOA (8). Most of the recognized NOB in sponges are Nitrospira-like bacteria (17, 32, 35), although in the beginning, there were further hints to 16S rRNA sequences, which are most closely related to Nitrospina gracilis (17). However, as these sequences were found only once, it could be assumed that Nitrospira is the main nitrite oxidizer in this environment. Nitrospira-like bacteria are deemed to be recalcitrant and fastidious, and they are easily overgrown by other bacteria under suboptimal conditions. Despite these limitations in the laboratory, Nitrospira was determined to be the most important nitrite oxidizer during wastewater treatment (21, 33), in aquaculture biofilters (14) and in freshwater systems (20, 29).Identification of sponge-associated microorganisms has been performed largely with culture-independent methods, which are 16S rRNA gene based (denaturing gradient gel electrophoresis [DGGE], terminal restriction fragment-length polymorphism [TRFLP]) or visual (fluorescence in situ hybridization [FISH], electron microscopy) (8, 11). Nevertheless, the cultivation of microorganisms is still essential for the investigation of their physiological potential and function in the environment. Information about physiological characteristics helps us to understand the metabolism and possible nutritional interactions of nitrifiers with the host sponge (8).This is the first report about cultivation of nitrifying bacteria originating from a marine sponge. We obtained a nitrite-oxidizing enrichment culture of a Nitrospira-like bacterium derived from Aplysina aerophoba, characterized it phylogenetically, and analyzed the most important physiological features.     

Distinct physiological roles of the three [NiFe]-hydrogenase orthologs in the hyperthermophilic archaeon Thermococcus kodakarensis

Hydrogenases catalyze the reversible oxidation of molecular hydrogen (H₂) and play a key role in the energy metabolism of microorganisms in anaerobic environments. The hyperthermophilic archaeon Thermococcus kodakarensis KOD1, which assimilates organic carbon coupled with the reduction of elemental sulfur (S⁰) or H₂ generation, harbors three gene operons encoding [NiFe]-hydrogenase orthologs, namely, Hyh, Mbh, and Mbx. In order to elucidate their functions in vivo, a gene disruption mutant for each [NiFe]-hydrogenase ortholog was constructed. The Hyh-deficient mutant (PHY1) grew well under both H₂S- and H₂-evolving conditions. H₂S generation in PHY1 was equivalent to that of the host strain, and H₂ generation was higher in PHY1, suggesting that Hyh functions in the direction of H₂ uptake in T. kodakarensis under these conditions. Analyses of culture metabolites suggested that significant amounts of NADPH produced by Hyh are used for alanine production through glutamate dehydrogenase and alanine aminotransferase. On the other hand, the Mbh-deficient mutant (MHD1) showed no growth under H₂-evolving conditions. This fact, as well as the impaired H₂ generation activity in MHD1, indicated that Mbh is mainly responsible for H₂ evolution. The copresence of Hyh and Mbh raised the possibility of intraspecies H₂ transfer (i.e., H₂ evolved by Mbh is reoxidized by Hyh) in this archaeon. In contrast, the Mbx-deficient mutant (MXD1) showed a decreased growth rate only under H₂S-evolving conditions and exhibited a lower H₂S generation activity, indicating the involvement of Mbx in the S⁰ reduction process. This study provides important genetic evidence for understanding the physiological roles of hydrogenase orthologs in the Thermococcales.     

Nitrite oxidation in the Namibian oxygen minimum zone

Nitrite oxidation is the second step of nitrification. It is the primary source of oceanic nitrate, the predominant form of bioavailable nitrogen in the ocean. Despite its obvious importance, nitrite oxidation has rarely been investigated in marine settings. We determined nitrite oxidation rates directly in ¹⁵N-incubation experiments and compared the rates with those of nitrate reduction to nitrite, ammonia oxidation, anammox, denitrification, as well as dissimilatory nitrate/nitrite reduction to ammonium in the Namibian oxygen minimum zone (OMZ). Nitrite oxidation (⩽372 nM NO₂⁻ d⁻¹) was detected throughout the OMZ even when in situ oxygen concentrations were low to non-detectable. Nitrite oxidation rates often exceeded ammonia oxidation rates, whereas nitrate reduction served as an alternative and significant source of nitrite. Nitrite oxidation and anammox co-occurred in these oxygen-deficient waters, suggesting that nitrite-oxidizing bacteria (NOB) likely compete with anammox bacteria for nitrite when substrate availability became low. Among all of the known NOB genera targeted via catalyzed reporter deposition fluorescence in situ hybridization, only Nitrospina and Nitrococcus were detectable in the Namibian OMZ samples investigated. These NOB were abundant throughout the OMZ and contributed up to ∼9% of total microbial community. Our combined results reveal that a considerable fraction of the recently recycled nitrogen or reduced NO₃⁻ was re-oxidized back to NO₃⁻ via nitrite oxidation, instead of being lost from the system through the anammox or denitrification pathways.     

H2-dependent azoreduction by Shewanella oneidensis MR-1: involvement of secreted flavins and both [Ni–Fe] and [Fe–Fe] hydrogenases

In this paper, the hydrogen (H₂)-dependent discoloration of azo dye amaranth by Shewanella oneidensis MR-1 was investigated. Experiments with hydrogenase-deficient strains demonstrated that periplasmic [Ni–Fe] hydrogenase (HyaB) and periplasmic [Fe–Fe] hydrogenase (HydA) are both respiratory hydrogenases of dissimilatory azoreduction in S. oneidensis MR-1. These findings suggest that HyaB and HydA can function as uptake hydrogenases that couple the oxidation of H₂ to the reduction of amaranth to sustain cellular growth. This constitutes to our knowledge the first report of the involvement of [Fe-Fe] hydrogenase in a bacterial azoreduction process. Assays with respiratory inhibitors indicated that a menaquinone pool and different cytochromes were involved in the azoreduction process. High-performance liquid chromatography analysis revealed that flavin mononucleotide and riboflavin were secreted in culture supernatant by S. oneidensis MR-1 under H₂-dependent conditions with concentration of 1.4 and 2.4 μmol g protein^-1, respectively. These endogenous flavins were shown to significantly accelerate the reduction of amaranth at micromolar concentrations acting as electron shuttles between the cell surface and the extracellular azo dye. This work may facilitate a better understanding of the mechanisms of azoreduction by S. oneidensis MR-1 and may have practical applications for microbiological treatments of dye-polluted industrial effluents.     

Chloroplast Respiration : A MEANS OF SUPPLYING OXIDIZED PYRIDINE NUCLEOTIDE FOR DARK CHLOROPLASTIC METABOLISM

A spinach (Spinacia oleracia var. America) chloroplast particle fortified with ferredoxin, fructose-1,6-bisphosphate, or ribose-5-phosphate and NADP has been shown to generate NADPH by the oxidation of glyceraldehyde-3 phosphate to glycerate-3-phosphate (PGA) and to reduce ferredoxin with the NADPH. The resulting reduced ferredoxin can reduce O₂ to H₂O₂, nitrite to ammonia, or protons to H₂. Hydrogen production was the result of adding hydrogenase from Chlamydomonas reinhardii to the chloroplast preparation. The predicted stoichiometry of 1 PGA:1 O₂ in the absence of and 2 PGA:1 O₂ in the presence of catalase was observed indicating H₂O₂ as the end product of O₂ reduction. The predicted stoichiometry of 3 PGA:1 nitrite:1 ammonia was also observed. A scheme is presented to account for a sustained generation of NADP and ATP necessary for the dissimilation of starch in the darkened chloroplast. The unifying term chloroplast respiration is introduced to account for those reactions in which reduced ferredoxin interacts with physiological acceptors other than NADP or nitrite, hydrogen, or O₂ respiration when nitrite, protons, or O₂ is the ultimate electron acceptor.     

Localization of hydrogenase and nitrate reductase in Campylobacter sputorum subsp. bubulus

Campylobacter sputorum subsp. bubulus contained hydrogenase activity after growth with lactate and nitrate and after growth with hydrogen and nitrate. After growth with hydrogen and nitrate a molar growth yield (g dry cells/mol hydrogen) of 5.6 was measured. Hydrogenase and nitrate reductase were membrane-bound enzymes. In cells with high hydrogenase activity the H⁺/O, H⁺/NO _inf2 ^sup- and H⁺/NO _inf3 ^sup- values with hydrogen as the electron donor were 3.74, 2.61 and 4.36 respectively. In cells with low hydrogenase activity these values were 2.33,-0.86 and 1.31 respectively. These values and the stoichiometry of respiration-driven proton translocation (H⁺/2e=2) led to the conclusion that hydrogenase is located at the periplasmic side of the cytoplasmic membrane. In cells with low lactate dehydrogenase activity or low hydrogenase activity the reduction of nitrate to nitrite could be separated from the reduction of nitrite to ammonia. Positive H⁺/NO _inf3 ^sup- values (between 0.9 and 1.7) with lactate or hydrogen as the electron donor were measured in these cells whereas H⁺/NO _inf2 ^sup- values were negative. From this result it was concluded that nitrate reductase is located at the cytoplasmic face of the cytoplasmic membrane. The results explain the previous observation that molar growth yields with nitrate were somewhat higher than those with nitrite.