Anaerobic Sulfide Oxidation with Nitrate by a Freshwater Beggiatoa Enrichment Culture

A lithotrophic freshwater Beggiatoa strain was enriched in O₂-H₂S gradient tubes to investigate its ability to oxidize sulfide with NO₃⁻ as an alternative electron acceptor. The gradient tubes contained different NO₃⁻ concentrations, and the chemotactic response of the Beggiatoa mats was observed. The effects of the Beggiatoa sp. on vertical gradients of O₂, H₂S, pH, and NO₃⁻ were determined with microsensors. The more NO₃⁻ that was added to the agar, the deeper the Beggiatoa filaments glided into anoxic agar layers, suggesting that the Beggiatoa sp. used NO₃⁻ to oxidize sulfide at depths below the depth that O₂ penetrated. In the presence of NO₃⁻ Beggiatoa formed thick mats (>8 mm), compared to the thin mats (ca. 0.4 mm) that were formed when no NO₃⁻ was added. These thick mats spatially separated O₂ and sulfide but not NO₃⁻ and sulfide, and therefore NO₃⁻ must have served as the electron acceptor for sulfide oxidation. This interpretation is consistent with a fourfold-lower O₂ flux and a twofold-higher sulfide flux into the NO₃⁻-exposed mats compared to the fluxes for controls without NO₃⁻. Additionally, a pronounced pH maximum was observed within the Beggiatoa mat; such a pH maximum is known to occur when sulfide is oxidized to S⁰ with NO₃⁻ as the electron acceptor.     

Impact of Bacterial NO3? Transport on Sediment Biogeochemistry

Experiments demonstrated that Beggiatoa could induce a H₂S-depleted suboxic zone of more than 10 mm in marine sediments and cause a divergence in sediment NO₃⁻ reduction from denitrification to dissimilatory NO₃⁻ reduction to ammonium. pH, O₂, and H₂S profiles indicated that the bacteria oxidized H₂S with NO₃⁻ and transported S⁰ to the sediment surface for aerobic oxidation.     

Colorless Sulfur Bacteria, Beggiatoa spp. and Thiovulum spp., in O2 and H2S Microgradients

The interactions between colorless sulfur bacteria and the chemical microgradients at the oxygen-sulfide interface were studied in Beggiatoa mats from marine sediments and in Thiovulum veils developing above the sediments. The gradients of O₂, H₂S, and pH were measured by microelectrodes at depth increments of 50 μm. An unstirred boundary layer in the water surrounding the mats and veils prevented microturbulent or convective mixing of O₂ and H₂S. The two substrates reached the bacteria only by molecular diffusion through the boundary layer. The bacteria lived as microaerophiles or anaerobes even under stirred, oxic water. Oxygen and sulfide zones overlapped by 50 μm in the bacterial layers. Both compounds had concentrations in the range of 0 to 10 μmol liter⁻¹ and residence times of 0.1 to 0.6 s in the overlapping zone. The sulfide oxidation was purely biological. Diffusion calculations showed that formation of mats on solid substrates or of veils in the water represented optimal strategies for the bacteria to achieve a stable microenvironment, a high substrate supply, and an efficient competition with chemical sulfide oxidation. The continuous gliding movement of Beggiatoa cells in mats or the flickering motion of Thiovulum cells in veils were important for the availability of both O₂ and H₂S for the individual bacteria.     

Polysulfides as Intermediates in the Oxidation of Sulfide to Sulfate by Beggiatoa spp.

Zero-valent sulfur is a key intermediate in the microbial oxidation of sulfide to sulfate. Many sulfide-oxidizing bacteria produce and store large amounts of sulfur intra- or extracellularly. It is still not understood how the stored sulfur is metabolized, as the most stable form of S⁰ under standard biological conditions, orthorhombic α-sulfur, is most likely inaccessible to bacterial enzymes. Here we analyzed the speciation of sulfur in single cells of living sulfide-oxidizing bacteria via Raman spectroscopy. Our results showed that under various ecological and physiological conditions, all three investigated Beggiatoa strains stored sulfur as a combination of cyclooctasulfur (S₈) and inorganic polysulfides (S_n²⁻). Linear sulfur chains were detected during both the oxidation and reduction of stored sulfur, suggesting that S_n²⁻ species represent a universal pool of bioavailable sulfur. Formation of polysulfides due to the cleavage of sulfur rings could occur biologically by thiol-containing enzymes or chemically by the strong nucleophile HS⁻ as Beggiatoa migrates vertically between oxic and sulfidic zones in the environment. Most Beggiatoa spp. thus far studied can oxidize sulfur further to sulfate. Our results suggest that the ratio of produced sulfur and sulfate varies depending on the sulfide flux. Almost all of the sulfide was oxidized directly to sulfate under low-sulfide-flux conditions, whereas only 50% was oxidized to sulfate under high-sulfide-flux conditions leading to S⁰ deposition. With Raman spectroscopy we could show that sulfate accumulated in Beggiatoa filaments, reaching intracellular concentrations of 0.72 to 1.73 M.     

Transition from Anoxygenic to Oxygenic Photosynthesis in a Microcoleus chthonoplastes Cyanobacterial Mat

Benthic cyanobacterial mats with the filamentous Microcoleus chthonoplastes as the dominant phototroph grow in oxic hypersaline environments such as Solar Lake, Sinai. The cyanobacteria are in situ exposed to chemical variations between 200 μmol of sulfide liter⁻¹ at night and 1 atm pO₂ during the day. During experimental H₂S to O₂ transitions the microbial community was shown to shift from anoxygenic photosynthesis, with H₂S as the electron donor, to oxygenic photosynthesis. Microcoleus filaments could carry out both types of photosynthesis concurrently. Anoxygenic photosynthesis dominated at high sulfide levels, 500 μmol liter⁻¹, while the oxygenic reaction became dominant when the sulfide level was reduced below 100 to 300 μmol liter⁻¹ (25 to 75 μmol of H₂S liter⁻¹). An increasing inhibition of the oxygenic photosynthesis was observed upon transition to oxic conditions from increasing sulfide concentrations. Oxygen built up within the Microcoleus layer of the mat even under 5 mmol of sulfide liter⁻¹ (500 μmol of H₂S liter⁻¹) in the overlying water. The implications of such a localized O₂ production in a highly reducing environment are discussed in relation to the evolution of oxygenic photosynthesis during the Proterozoic era.     

Hydrogen Sulfide Prolongs Postharvest Storage of Fresh-Cut Pears (Pyrus pyrifolia) by Alleviation of Oxidative Damage and Inhibition of Fungal Growth

Hydrogen sulfide (H₂S) has proved to be a multifunctional signaling molecule in plants and animals. Here, we investigated the role of H₂S in the decay of fresh-cut pears (Pyrus pyrifolia). H₂S gas released by sodium hydrosulfide (NaHS) prolonged the shelf life of fresh-cut pear slices in a dose-dependent manner. Moreover, H₂S maintained higher levels of reducing sugar and soluble protein in pear slices. H₂S significantly reduced the accumulation of hydrogen peroxide (H₂O₂), superoxide radicals (•O₂ ⁻) and malondialdehyde (MDA). Further investigation showed that H₂S fumigation up-regulated the activities of antioxidant enzymes ascorbate peroxidase (APX), catalase (CAT), and guaiacol peroxidase (POD), while it down-regulated those of lipoxygenase (LOX), phenylalanine ammonia lyase (PAL) and polyphenol oxidase (PPO). Furthermore, H₂S fumigation effectively inhibited the growth of two fungal pathogens of pear, Aspergillus niger and Penicillium expansum, suggesting that H₂S can be developed as an effective fungicide for postharvest storage. The present study implies that H₂S is involved in prolonging postharvest storage of pears by acting as an antioxidant and fungicide.     

Oxygen Responses and Mat Formation by Beggiatoa spp

The behavioral response of single Beggiatoa sp. filaments moving on a gas-permeable membrane was studied by the combined use of microscopy and oxygen microelectrodes during controlled oscillations of oxygen tension. The bacteria reacted to increasing oxygen by reversing the direction of movement. The same step-up phobic response to oxygen was observed when a filament tip or loop glided into a stable microgradient of increasing oxygen. The response was sensitive to a change in oxygen tension of <5% of air saturation min⁻¹. The response time was 20 to 50 s. Frequently, only part of the filament responded, which led to the formation of sharp bends, loops, and coils. This partial response facilitated the positioning of the long filaments within the narrow O₂-H₂S interface. The structure of whole Beggiatoa mats on sediment surfaces varied from loose to dense in relation to shallow or steep oxygen gradients in the 0.3- to 2-mm-thick, unstirred boundary layer. In an illuminated sediment Beggiatoa spp. lived together with photosynthetic organisms and migrated vertically in accordance with light/dark variations. The combined effect of phobic responses to light and oxygen can explain this migration.     

Die Mixotrophie von Beggiatoa

Zusammenfassung Axenische Kulturen von Beggiatoa wurden zur Prüfung der Frage verwendet, ob autotrophe Ernährung möglich ist. Dazu wurde eine neue Technik ausgearbeitet, bei der FeS als H₂S-Quelle dient.Es bestätigte sich, daß entweder heterotrophe Ernährung oder neben H₂S kleinste Konzentrationen organischer Energiesubstrate nötig sind. Es liegt dann eine Sonderform von Mixotrophie vor, anders als bei chemoautotrophen Bakterien.Der aus H₂S entstehende S ist ein Reservestoff, der aber nicht nur, etwa wie Stärke, der Überschuß-Speicherung dient, sondern eine Zwischenstufe in der Verwertung der Oxydationsenergie darstellt, denn es wird sogleich H₂SO₄ gebildet.Unter Bedingungen, die in Reinkulturen die stärkste Vermehrung bewirken, kann Beggiatoa wegen des Wettbewerbes in der Natur nicht leben. Die ökologisch besten Lebensumstände sind von besonderer Art und von den physiologisch optimalen verschieden.

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The mixotrophy of Beggiatoa

Summary Axenic cultures of Beggiatoa were used to answer the question whether permanent autotrophic growth is feasible, so that oxidation of sulfur compounds would supply energy for all living processes, and organic substances were not needed.For that purpose a new technique was devised with FeS as a source of H₂S. Results confirmed the assumption that for Beggiatoa either heterotrophic nutrition or in addition to H₂S minute quantities of an organic substrate are required.The colorless Cyanophycean Beggiatoa represents therefore nutritionally a special mode of mixotrophy differing from the nutrition of chemo-autotrophic bacteria.Sulfur as a reserve material does not only serve as a surplus deposit but also represents a step in the utilization of oxidation energy from H₂S to H₂SO₄.Ecologically its living conditions are characterized by low tensions of O₂ and H₂S, a supply of CO₂ and low concentrations of organic nutrients. Under optimum conditions of nutrition. Beggiatoa would not stand competition by other organisms.

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Herrn Professor C. B. van Niel in Freundschaft und Verehrung zum 70. Geburtstag gewidmet.     

Lipid Biomarkers and Carbon Isotope Signatures of a Microbial (Beggiatoa) Mat Associated with Gas Hydrates in the Gulf of Mexico

White and orange mats are ubiquitous on surface sediments associated with gas hydrates and cold seeps in the Gulf of Mexico. The goal of this study was to determine the predominant pathways for carbon cycling within an orange mat in Green Canyon (GC) block GC 234 in the Gulf of Mexico. Our approach incorporated laser-scanning confocal microscopy, lipid biomarkers, stable carbon isotopes, and 16S rRNA gene sequencing. Confocal microscopy showed the predominance of filamentous microorganisms (4 to 5 μm in diameter) in the mat sample, which are characteristic of Beggiatoa. The phospholipid fatty acids extracted from the mat sample were dominated by 16:1ω7c/t (67%), 18:1ω7c (17%), and 16:0 (8%), which are consistent with lipid profiles of known sulfur-oxidizing bacteria, including Beggiatoa. These results are supported by the 16S rRNA gene analysis of the mat material, which yielded sequences that are all related to the vacuolated sulfur-oxidizing bacteria, including Beggiatoa, Thioploca, and Thiomargarita. The δ¹³C value of total biomass was −28.6‰; those of individual fatty acids were −29.4 to −33.7‰. These values suggested heterotrophic growth of Beggiatoa on organic substrates that may have δ¹³C values characteristic of crude oil or on their by-products from microbial degradation. This study demonstrated that integrating lipid biomarkers, stable isotopes, and molecular DNA could enhance our understanding of the metabolic functions of Beggiatoa mats in sulfide-rich marine sediments associated with gas hydrates in the Gulf of Mexico and other locations.     

Hydrogen Peroxide Metabolism in Yeasts

A catalase-negative mutant of the yeast Hansenula polymorpha consumed methanol in the presence of glucose when the organism was grown in carbon-limited chemostat cultures. The organism was apparently able to decompose the H₂O₂ generated in the oxidation of methanol by alcohol oxidase. Not only H₂O₂ generated intracellularly but also H₂O₂ added extracellularly was effectively destroyed by the catalase-negative mutant. From the rate of H₂O₂ consumption during growth in chemostat cultures on mixtures of glucose and H₂O₂, it appeared that the mutant was capable of decomposing H₂O₂ at a rate as high as 8 mmol · g of cells⁻¹ · h⁻¹. Glutathione peroxidase (EC 1.11.1.9) was absent under all growth conditions. However, cytochrome c peroxidase (CCP; EC 1.11.1.5) increased to very high levels in cells which decomposed H₂O₂. When wild-type H. polymorpha was grown on mixtures of glucose and methanol, the CCP level was independent of the rate of methanol utilization, whereas the level of catalase increased with increasing amounts of methanol in the substrate feed. Also, the wild type decomposed H₂O₂ at a high rate when cells were grown on mixtures of glucose and H₂O₂. In this case, an increase of both CCP and catalase was observed. When Saccharomyces cerevisiae was grown on mixtures of glucose and H₂O₂, the level of catalase remained low, but CCP increased with increasing rates of H₂O₂ utilization. From these observations and an analysis of cell yields under the various conditions, two conclusions can be drawn. (i) CCP is a key enzyme of H₂O₂ detoxification in yeasts. (ii) Catalase can effectively compete with mitochondrial CCP for hydrogen peroxide only if hydrogen peroxide is generated at the site where catalase is located, namely in the peroxisomes.     

Changes in Microbial Biofilm Communities during Colonization of Sewer Systems

The coexistence of sulfate-reducing bacteria (SRB) and methanogenic archaea (MA) in anaerobic biofilms developed in sewer inner pipe surfaces favors the accumulation of sulfide (H₂S) and methane (CH₄) as metabolic end products, causing severe impacts on sewerage systems. In this study, we investigated the time course of H₂S and CH₄ production and emission rates during different stages of biofilm development in relation to changes in the composition of microbial biofilm communities. The study was carried out in a laboratory sewer pilot plant that mimics a full-scale anaerobic rising sewer using a combination of process data and molecular techniques (e.g., quantitative PCR [qPCR], denaturing gradient gel electrophoresis [DGGE], and 16S rRNA gene pyrotag sequencing). After 2 weeks of biofilm growth, H₂S emission was notably high (290.7 ± 72.3 mg S-H₂S liter⁻¹ day⁻¹), whereas emissions of CH₄ remained low (17.9 ± 15.9 mg COD-CH₄ liter⁻¹ day⁻¹). This contrasting trend coincided with a stable SRB community and an archaeal community composed solely of methanogens derived from the human gut (i.e., Methanobrevibacter and Methanosphaera). In turn, CH₄ emissions increased after 1 year of biofilm growth (327.6 ± 16.6 mg COD-CH₄ liter⁻¹ day⁻¹), coinciding with the replacement of methanogenic colonizers by species more adapted to sewer conditions (i.e., Methanosaeta spp.). Our study provides data that confirm the capacity of our laboratory experimental system to mimic the functioning of full-scale sewers both microbiologically and operationally in terms of sulfide and methane production, gaining insight into the complex dynamics of key microbial groups during biofilm development.     

Hydrogen-Dependent Oxygen Reduction by Homoacetogenic Bacteria Isolated from Termite Guts

Although homoacetogenic bacteria are generally considered to be obligate anaerobes, they colonize the intestinal tracts of termites and other environments that are not entirely anoxic in space or time. In this study, we investigated how homoacetogenic bacteria isolated from the hindguts of various termites respond to the presence of molecular oxygen. All strains investigated formed growth bands in oxygen gradient agar tubes under a headspace of H₂-CO₂. The position of the bands coincided with the oxic-anoxic interface and depended on the O₂ partial pressure in the headspace; the position of the bands relative to the meniscus remained stable for more than 1 month. Experiments with dense cell suspensions, performed with Clark-type O₂ and H₂ electrodes, revealed a large capacity for H₂-dependent oxygen reduction in Sporomusa termitida and Sporomusa sp. strain TmAO3 (149 and 826 nmol min⁻¹ mg of protein⁻¹, respectively). Both strains also reduced O₂ with endogenous reductants, albeit at lower rates. Only in Acetonema longum did the basal rates exceed the H₂-dependent rates considerably (181 versus 28 nmol min⁻¹ mg of protein)⁻¹). Addition of organic substrates did not stimulate O₂ consumption in any of the strains. Nevertheless, reductive acetogenesis by cell suspensions of strain TmAO3 was inhibited even at the lowest O₂ fluxes, and growth in nonreduced medium occurred only after the bacteria had rendered the medium anoxic. Similar results were obtained with Acetobacterium woodii, suggesting that the results are not unique to the strains isolated from termites. We concluded that because of their tolerance to temporary exposure to O₂ at low partial pressures (up to 1.5 kPa in the case of strain TmAO3) and because of their large capacity for O₂ reduction, homoacetogens can reestablish conditions favorable for growth by actively removing oxygen from their environment.     

Inorganic Sulfur Oxidation by Aureobasidium pullulans

Aureobasidium pullulans (de Bary) Arnaud isolated from the phylloplane of sycamore exposed to heavy atmospheric pollution oxidized S⁰ to S₂O₃²⁻, S₄O₆²⁻, and SO₄²⁻ in vitro. The intermediates S₂O₃²⁻ and S₄O₆²⁻ were also oxidized to SO₄²⁻. Cell-free extracts of A. pullulans also oxidized reduced forms of S, the oxidation increasing linearly with increasing protein concentration, showing that the process is enzymatic. The possible role of fungi in S oxidation in soils is discussed.     

H<Subscript>2</Subscript>S biotreatment with sulfide-oxidizing heterotrophic bacteria

Many industrial activities produce H₂S, which is toxic at high levels and odorous at even very low levels. Chemolithotrophic sulfur-oxidizing bacteria are often used in its remediation. Recently, we have reported that many heterotrophic bacteria can use sulfide:quinone oxidoreductase and persulfide dioxygenase to oxidize H₂S to thiosulfate and sulfite. These bacteria may also potentially be used in H₂S biotreatment. Here we report how various heterotrophic bacteria with these enzymes were cultured with organic compounds and the cells were able to rapidly oxidize H₂S to zero-valence sulfur and thiosulfate, causing no apparent acidification. Some also converted the produced thiosulfate to tetrathionate. The rates of sulfide oxidation by some of the tested bacteria in suspension, ranging from 8 to 50 µmol min^?1 g^?1 of cell dry weight at pH 7.4, sufficient for H₂S biotreatment. The immobilized bacteria removed H₂S as efficiently as the bacteria in suspension, and the inclusion of Fe₃O₄ nanoparticles during immobilization resulted in increased efficiency for sulfide removal, in part due to chemical oxidation H₂S by Fe₃O₄. Thus, heterotrophic bacteria may be used for H₂S biotreatment under aerobic conditions.     

Selective and Reversible Inhibition of Active CO(2) Transport by Hydrogen Sulfide in a Cyanobacterium

The active transport of CO₂ in the cyanobacterium Synechococcus UTEX 625 was inhibited by H₂S. Treatment of the cells with up to 150 micromolar H₂S + HS⁻ at pH 8.0 had little effect on Na⁺-dependent HCO₃⁻ transport or photosynthetic O₂ evolution, but CO₂ transport was inhibited by more than 90%. CO₂ transport was restored when H₂S was removed by flushing with N₂. At constant total H₂S + HS⁻ concentrations, inhibition of CO₂ transport increased as the ratio of H₂S to HS⁻ increased, suggesting a direct role for H₂S in the inhibitory process. Hydrogen sulfide does not appear to serve as a substrate for transport. In the presence of H₂S and Na⁺ -dependent HCO₃⁻ transport, the extracellular CO₂ concentration rose considerably above its equilibrium level, but was maintained far below its equilibrium level in the absence of H₂S. The inhibition of CO₂ transport, therefore, revealed an ongoing leakage from the cells of CO₂ which was derived from the intracellular dehydration of HCO₃⁻ which itself had been recently transported into the cells. Normally, leaked CO₂ is efficiently transported back into the cell by the CO₂ transport system, thus maintaining the extracellular CO₂ concentration near zero. It is suggested that CO₂ transport not only serves as a primary means of inorganic carbon acquisition for photosynthesis but also serves as a means of recovering CO₂ lost from the cell. A schematic model describing the relationship between the CO₂ and HCO₃⁻ transport systems is presented.     

Succession of Internal Sulfur Cycles and Sulfur-Oxidizing Bacterial Communities in Microaerophilic Wastewater Biofilms

The succession of sulfur-oxidizing bacterial (SOB) community structure and the complex internal sulfur cycle occurring in wastewater biofilms growing under microaerophilic conditions was analyzed by using a polyphasic approach that employed 16S rRNA gene-cloning analysis combined with fluorescence in situ hybridization, microelectrode measurements, and standard batch and reactor experiments. A complete sulfur cycle was established via S⁰ accumulation within 80 days in the biofilms in replicate. This development was generally split into two phases, (i) a sulfur-accumulating phase and (ii) a sulfate-producing phase. In the first phase (until about 40 days), since the sulfide production rate (sulfate-reducing activity) exceeded the maximum sulfide-oxidizing capacity of SOB in the biofilms, H₂S was only partially oxidized to S⁰ by mainly Thiomicrospira denitirificans with NO₃⁻ as an electron acceptor, leading to significant accumulation of S⁰ in the biofilms. In the second phase, the SOB populations developed further and diversified with time. In particular, S⁰ accumulation promoted the growth of a novel strain, strain SO07, which predominantly carried out the oxidation of S⁰ to SO₄²⁻ under oxic conditions, and Thiothrix sp. strain CT3. In situ hybridization analysis revealed that the dense populations of Thiothrix (ca. 10⁹ cells cm⁻³) and strain SO07 (ca. 10⁸ cells cm⁻³) were found at the sulfur-rich surface (100 μm), while the population of Thiomicrospira denitirificans was distributed throughout the biofilms with a density of ca. 10⁷ to 10⁸ cells cm⁻³. Microelectrode measurements revealed that active sulfide-oxidizing zones overlapped the spatial distributions of different phylogenetic SOB groups in the biofilms. As a consequence, the sulfide-oxidizing capacities of the biofilms became high enough to completely oxidize all H₂S produced by SRB to SO₄²⁻ in the second phase, indicating establishment of the complete sulfur cycle in the biofilms.     

Enhanced removability of odorous sulfur-containing gases by mixed cultures of purified bacteria from peat biofilters

Four bacteria isolated from peat biofilters, Thiobacillus thioparus DW44, Thiobacillus sp. HA43, Xanthomonas sp. DY44 and Hyphomicrobium sp. I55, were selected to enhance the removal ratios of hydrogen sulfide (H₂S), methanethiol (MT) and dimethyl sulfide (DMS) in a mixed gas system. Two bacteria, DW44 and I55, which degrade H₂S, MT, DMS and dimethyl disulfide (DMDS), were mixed with DY44 or HA43 which degrade only H₂S and MT. Although DMS removal was significantly inhibited by the presence of H₂S and MT in a peat biofilter inoculated with the single bacterium, enhanced removability of H₂S, MT and DMS was observed by mixing Hyphomicrobium sp. I55 either with Thiobacillus sp. HA43 or Xanthomonas sp. DY44. The removal rate (g-S-kg-dry peat⁻¹·d⁻¹) by I55 after 8 d was 0.664 in total sulfur load, 0.827 g-S·kg-dry g-S·-kg-dry peat⁻¹·d⁻¹, but the rates by the mixed cultures of I55 plus HA43, and I55 plus DY44 were 0.760 and 0.801, respectively. In particular, DMS removability in mixed gases by a mixed culture of I55 and DY44 was almost equivalent to that by I55 when only DMS was supplied, suggesting that removal of H₂S and MT, which inhibited DMS removal, was preferentially conducted by DY44 and led to improved DMS removability by I55.     

Role of Polysulfides in Reduction of Elemental Sulfur by the Hyperthermophilic Archaebacterium Pyrococcus furiosus

Polysulfides formed through the breakdown of elemental sulfur or other sulfur compounds were found to be reduced to H₂S by the hyperthermophilic archaebacterium Pyrococcus furiosus during growth. Metabolism of polysulfides by the organism was dissimilatory, as no incorporation of ³⁵S-labeled elemental sulfur was detected. However, [³⁵S]cysteine and [³⁵S]methionine were incorporated into cellular protein. Contact between the organism and elemental sulfur is not necessary for metabolism. The sulfide generated from metabolic reduction of polysulfides dissociates to a strong nucleophile, HS⁻, which in turn opens up the S₈ elemental sulfur ring. In addition to H₂S, P. furiosus cultures produced methyl mercaptan in a growth-associated fashion.     

TRPA1 Has a Key Role in the Somatic Pro-Nociceptive Actions of Hydrogen Sulfide

Hydrogen sulfide (H₂S), which is produced endogenously from L-cysteine, is an irritant with pro-nociceptive actions. We have used measurements of intracellular calcium concentration, electrophysiology and behavioral measurements to show that the somatic pronociceptive actions of H₂S require TRPA1. A H₂S donor, NaHS, activated TRPA1 expressed in CHO cells and stimulated DRG neurons isolated from Trpa1^+/+ but not Trpa1^−/− mice. TRPA1 activation by NaHS was pH dependent with increased activity at acidic pH. The midpoint of the relationship between NaHS EC₅₀ values and external pH was pH 7.21, close to the expected dissociation constant for H₂S (pK_a 7.04). NaHS evoked single channel currents in inside-out and cell-attached membrane patches consistent with an intracellular site of action. In behavioral experiments, intraplantar administration of NaHS and L-cysteine evoked mechanical and cold hypersensitivities in Trpa1^+/+ but not in Trpa1^−/− mice. The sensitizing effects of L-cysteine in wild-type mice were inhibited by a cystathionine β-synthase inhibitor, D,L-propargylglycine (PAG), which inhibits H₂S formation. Mechanical hypersensitivity evoked by intraplantar injections of LPS was prevented by PAG and the TRPA1 antagonist AP-18 and was absent in Trpa1^−/− mice, indicating that H₂S mediated stimulation of TRPA1 is necessary for the local pronociceptive effects of LPS. The pro-nociceptive effects of intraplantar NaHS were retained in Trpv1^−/− mice ruling out TRPV1 as a molecular target. In behavioral studies, NaHS mediated sensitization was also inhibited by a T-type calcium channel inhibitor, mibefradil. In contrast to the effects of NaHS on somatic sensitivity, intracolonic NaHS administration evoked similar nociceptive effects in Trpa1^+/+ and Trpa1^−/− mice, suggesting that the visceral pro-nociceptive effects of H₂S are independent of TRPA1. In electrophysiological studies, the depolarizing actions of H₂S on isolated DRG neurons were inhibited by AP-18, but not by mibefradil indicating that the primary excitatory effect of H₂S on DRG neurons is TRPA1 mediated depolarization.