[35S]Thiosulphate oxidation by Thiobacillus strain C

1. Thiobacillus strain C oxidized [(35)S]thiosulphate completely to sulphate. 2. During thiosulphate oxidation [(35)S]sulphate was formed more rapidly from (S.(35)SO(3))(2-) than from ((35)S.SO(3))(2-). (35)S disappeared less rapidly from thiosulphate with ((35)S.SO(3))(2-) as substrate than with (S.(35)SO(3))(2-). 3. Thiosulphate labelled in both atoms was produced during ((35)S.SO(3))(2-) oxidation, but not during (S.(35)SO(3))(2-) oxidation. 4. No (35)S was precipitated as elementary sulphur either in the presence or absence of exogenous unlabelled sulphur. 5. During [(35)S]thiosulphate oxidation, appreciable quantities of [(35)S]trithionate accumulated and later disappeared. Other polythionates did not accumulate consistently. 6. [(35)S]Trithionate was formed initially at a greater rate from (S.(35)SO(3))(2-) than from ((35)S.SO(3))(2-), but subsequently at a similar rate from each. 7. Trithionate formed from (S.(35)SO(3))(2-) was labelled only in the oxidized sulphur atoms, but that formed from ((35)S.SO(3))(2-) was labelled in both oxidized and reduced atoms. The proportion of (35)S in the oxidized atoms increased as more trithionate accumulated. 8. The results eliminate some mechanisms of trithionate formation but are consistent both with a mechanism of thiosulphate oxidation based on an initial reductive cleavage of the molecule and with a mechanism in which thiosulphate undergoes an initial oxidative reaction.     

[35S]Thiosulphate oxidation by rat liver mitochondria in the presence of glutathione

1. Rat liver mitochondria incubated in oxygen with glutathione and [(35)S]-thiosulphate produced labelled sulphate. 2. Inner-labelled thiosulphate (S.(35)SO(3))(2-) was converted into [(35)S]sulphate more rapidly than outer-labelled thiosulphate ((35)S.SO(3))(2-). 3. Thiosulphate labelled in both sulphur atoms was formed during ((35)S.SO(3))(2-) oxidation; the outer sulphur atom before oxidation to sulphate was incorporated into the inner position. 4. A thiosulphate cycle in the metabolic pathway of sulphate formation in animal tissues is discussed.     

Characterization of Saccharomyces cerevisiae strains isolated from must of grape grown in experimental vineyard

AIMS: Isolation and characterization of indigenous Saccharomyces cerevisiae strains from 12 grape varieties grown in an experimental vineyard of Apulia. METHODS AND RESULTS: Thirty to 40 colonies from each of the 12 fermentations were obtained at the end stage of spontaneous fermentation. By using morphological and physiological methods and by the PCR analysis of internal transcribed ITS1-5,8S-ITS2, the isolates belonging to Saccharomyces genus were identified. These isolates were further characterized by amplification with S. cerevisiae species- and delta element-specific primers, thus allowing the identification of S. cerevisiae strains selected from each of the 12 fermentations. By means of RFLP analysis of mtDNA, each S. cerevisiae population isolated from a single fermentation appeared to constitute a genetically homogenous group. The comparison of the 12 cultivar-specific mtDNA RFLP patterns, allowed classifying the 12 S. cerevisiae populations into three genetically homogenous groups. The isolated strains fermented vigorously in synthetic and grape juice medium and showed high alcohol and sulphur dioxide (SO(2)) resistance and low hydrogen sulphite (H(2)S) production. CONCLUSIONS: The molecular analysis, in conjunction with the traditional morphological and physiological methods, was useful in discriminating at strain level the indigenous population of S. cerevisiae present in a vineyard of Apulia. The dominant S. cerevisiae strains identified in the 12 fermented musts showed potentially important oenological characteristics. SIGNIFICANCE AND IMPACT OF THE STUDY: The characterization of natural S. cerevisiae strains from several typical Italian grapes grown in a restricted experimental vineyard is an important step towards the preservation and exploitation of yeast biodiversity of Apulia, a relevant wine-producing region. The close relationship between the S. cerevisiae strains from different grapes grown in the same vineyard indicated that the occurrence of native strains is representative of the area rather than of the variety of grapes.     

Transfer of sulphur to the digestive tract of sheep.

The transfer of sulphate from plasma to digestive tract and from digestive tract to plasma in crossbred sheep was estimated by the use of isotope dilution techniques with Na235SO4. The passage of 35S along the digestive tract was simultaneously measured by reference to two inert radioactive markers infused intraruminally. In the first experiment, three sheep given a roughage-based diet containing 174 +/- 7 mg S/day received an intravenous infusion of Na235SO4 for 7 days before collections were made of plasma and of digesta from the rumen, abomasum and terminal ileum. Similar collections were made in the second experiment in which four sheep received intraruminal infusions of Na235SO4. From estimates of infusion rate of 35S, specific radioactivity of 35S in plasma and digesta and rate of flow of sulphur in the digestive tract the following calculations were made: The transfer of sulphate from the plasma to the rumen was calculated as 29 mg S/day. Of this only 12 mg S/day passed as organic sulphur in digesta from the stomach. As the net gain of sulphur in the stomach in this experiment was 153 mg/day, sulphate transferred from the plasma contributed only a small amount of sulphur derived from endogenous sources in the stomach. In contrast, the substantial passage of 35S into the intestinal lumen during intravenous infusion of 35SO4 suggested that 38 and 41 mg S/day of the 236 and 145 mg organic S/day flowing from the small and large intestine respectively was derived from plasma sulphate, corresponding to about 26% of the dose.     

Impact of pedospheric and atmospheric sulphur nutrition on sulphur metabolism of Allium cepa L., a species with a potential sink capacity for secondary sulphur compounds

Onion (Allium cepa L.) was able to use atmospheric H(2)S as sole sulphur source for growth. The foliarly absorbed H(2)S was rapidly metabolized into water-soluble, non-protein thiol compounds, including cysteine, and subsequently into other sulphur compounds in the shoots. In H(2)S-exposed plants, the accumulation of sulphur compounds in the shoots was nearly linear with the concentration (0.15-0.6 microl l(-1)) and duration of the exposure. Exposure of onion to H(2)S for up to 1 week did not affect the sulphur content of the roots. Secondary sulphur compounds formed a sink for the foliarly absorbed sulphide, and the sulphur accumulation upon H(2)S exposure could, for a great part, be ascribed to enhancement of the content of gamma-glutamyl peptides and/or alliins. Furthermore, there was a substantial increase in the sulphate content in the shoots upon H(2)S exposure. The accumulation of sulphate originated both from the pedosphere and from the oxidation of absorbed atmospheric sulphide, and/or from the degradation of accumulated secondary sulphur compounds. From studies on the interaction between atmospheric and pedospheric sulphur nutrition it was evident that H(2)S exposure did not result in a down-regulation of the sulphate uptake by the roots.     

Inhibition of sulphur redistribution into new leaves of vegetative soybean by excision of the maturing leaf

When soybean plants are pulsed with [³⁵S]sulphate, label is subsequently redistributed from the roots to the leaves. This confounds studies to measure the redistribution of label from leaves. Accordingly, soybean plants ( Glycine max [L.] Merr. cv. Stephens) were grown in 20 μ M sulphate and a small portion of the root system (donor root) was pulsed with [³⁵S]sulphate for 24 h. After removing the donor root, the plants were transferred into unlabelled solution, either without sulphate (S20→SO) or with 20 μ M sulphate (S20→20) (intact plants). Also at this time, the expanding leaf (L3) was excised from half of the plants in each treatment (excised plants). Immediately after the pulse, only ca 15% of the label occurred in the roots and ca 40% in the expanding leaf, L3, mostly in the soluble fraction. In intact S20→20 plants, ³⁵S-label was exported from the soluble fraction of L3, mostly as sulphate, whilst L4 and L5 imported label. Similar responses occurred in S20→SO plants except that export of label from L3 was more rapid. Excision of L3 from S20→S20 plants inhibited labelling of leaves L4-L6 but not total sulphur, whereas in S20→SO plants, excision of L3 inhibited the import of both total sulphur and ³⁵S-label in leaves L4, L5 and L6. The data suggest that the soluble fraction of almost fully expanded leaves is an important reserve of sulphur for redistribution to growing leaves. The ³⁵S-label in the root system exhibited fluctuations consistent with its proposed role in the recycling of soluble sulphur from the leaves.     

Atmospheric deposition of nitrogen and sulphur compounds in the Czech Republic

Estimates of dry and wet deposition of nitrogen and sulphur compounds in the Czech Republic for the years 1994 and 1998 are presented. Deposition has been estimated from monitored and modeled concentrations in the atmosphere and in precipitation, where the most important acidifying compounds are sulphur dioxide, nitrogen oxides, ammonia, and their reaction products. Measured atmospheric concentrations of SO2, NOx, NH3, and aerosol particles (SO4(2-), NO3-, and NH4+), along with measured concentrations of SO4(2-), NO3-, and NH4+ in precipitation, weighted by precipitation amounts, were interpolated with Kriging technique on a 10- x 10-km grid covering the whole Czech Republic. Wet deposition was derived from concentration values for SO4(2-), NO3-, and NH4+ in precipitation and from precipitation amounts. Dry deposition was derived from concentrations of gaseous components and aerosol in the air, and from their deposition velocities. A multiple resistance model was used for calculation of SO2, NOx, and NH3 deposition velocities. Deposition velocities of particles were parameterized. It was estimated that the annual average deposition of SOx in the Czech Republic decreased from 1384 to 1027 mol H + ha(-1) a(-1) between 1994 and 1998. The annual average NOy deposition was estimated to be 972 and 919 mol H + ha(-1) a(-1) in 1994 and 1998, respectively. The annual average NHx deposition was estimated to be 887 mol H+ ha(-1) a(-1) and 779 mol H + ha(-1) a(-1) in 1994 and 1998, respectively. It was estimated that the annual average of the total potential acid deposition decreased from 3243 to 2725 mol H + ha(-1) a(-1) between 1994 and 1998. Sulphur compounds (SOx) contributed about 38%, oxidized nitrogen species (NOy) 34%, and reduced nitrogen species (NHx) 28% to the total potential acid deposition in 1998. The wet deposition contributed 42% to the total potential acid deposition in 1998.     

Isolation of a sulphate reductase-less mutant of the blue-green alga Nostoc muscorum.

The wild type Nostoc muscorum (UW strain) has yielded various physiological mutants altered in utilization of sulphate, following mutagenic treatments with N-methyl, N'-nitro N-nitrosoguanidine (NTG). One of the mutant strains designated as Sat-20 failed to grow in a medium containing sulphate (MgSO4.7 H2O). However, the mutant strain could grow when supplemented with thiosulphate (Na2S2O3.5 H2O), while methionine could fulfil the sulphur requirement only partially. On comparative reasons, the wild type as well as the mutant showed preference for thiosulphate over other sulphur sources employed.     

Calcium content of liming material and its effect on sulphur release in a coniferous forest soil

Soil columns with O + A (Experiment I) or Ohorizons (Experiment II) from a Haplic Podsol wereincubated at 15 °C for 368 and 29 + 106 days,respectively. Three types of liming material differingin Ca²⁺ content, i.e. calcium carbonate(CaCO₃), dolomite (CaMg(CO₃)₂) andmagnesium carbonate (MgCO₃), were mixed into theO horizons in equimolar amounts corresponding to 6000kg of CaCO₃ per ha. In the limed treatments ofExperiment I, the leaching of dissolved organic carbon(DOC) and the net sulphur mineralization (estimated asaccumulated SO ₄ ^2– leaching corrected forchanges in the soil pools of adsorbed and waterextractable SO ₄ ^2– ) increased with decreasingCa²⁺ content of the lime and increasing degree oflime dissolution. In relation to the controltreatment, only the MgCO₃ treatment resulted ina significantly higher net sulphur mineralization. InExperiment I the net sulphur mineralization was 4.06,1.68, 0.57, and 2.14 mg S in the MgCO₃,CaMg(CO₃)₂, CaCO₃ and control treatment,respectively. The accumulated SO ₄ ^2– leachingin Experiment II during the first 29 days was 1.70,0.74 and 0.48 mg S in the MgCO₃,CaMg(CO₃)₂ and control treatment,respectively. In the two experiments there wereconsistently significant positive correlations betweenleached amounts of SO ₄ ^2– and DOC. It wasconcluded that net sulphur mineralization was stronglyconnected to the solubilization of the organic matter(DOC formation) and that pH and/or Ca²⁺ ionsaffected the net sulphur mineralization through theireffects on organic matter solubility.     

含硫、硒化合物在油菜中的积累及其对硫甙水平的影响

温室条件下,对硫胁迫与供硫充足的油菜植株,分别用Ｌ－甲硫氨酸和硒酸盐（ＳｅＯ＾２－４）代替营养液中的硫酸协以及增加ＳＯ＾２－４供应浓度的方法,探讨了不同处理对油菜植株硫甙合成积累的影响,结果说明,增加供硫浓度可明显促进硫甙的合成速率,且在４８ｈ内以两个供硫水平的植株皆呈密切的二次回归递增趋势,ＳｅＯ＾２－４对植株甙的合成积累具有强烈的阻抑效应,并对供硫充足的植株影响更大,４８ｈ内呈直线下降,Ｌ－甲     

Assimilatory reduction of sulfate and sulfite by methanogenic bacteria.

A variety of sulfur-containing compounds were investigated for use as medium reductants and sulfur sources for growth of four methanogenic bacteria. Sulfide (1 to 2 mM) served all methanogens investigated well. Methanococcus thermolithotrophicus and Methanobacterium thermoautotrophicum Marburg and delta H grew well with S0, SO3(2-), or thiosulfate as the sole sulfur source. Only Methanococcus thermolithotrophicus was able to grow with SO4(2-) as the sole sulfur source. 2-Mercaptoethanol at 20 mM was greatly inhibitory to growth of Methanococcus thermolithotrophicus on SO4(2-) or SO2(2-) and Methanobacterium thermoautotrophicum Marburg on SO3(2-) but not to growth of strain delta H on SO3(2-). Sulfite was metabolized during growth by Methanococcus thermolithotrophicus. Sulfide was produced in cultures of Methanococcus thermolithotrophicus growing on SO4(2-), SO3(2-), thiosulfate, and S0. Methanobacterium thermoautotrophicum Marburg was successfully grown in a 10-liter fermentor with S0, SO3(2-), or thiosulfate as the sole sulfur source.     

含硫气体信号分子对心血管调节的效应及机制研究进展

含硫气体信号分子硫化氢(hydrogen sulfide,H2S)和二氧化硫(sulfur dioxide,SO2)过去被认为是废气,但是研究先后发现这两种含硫气体能在哺乳动物体内通过含硫氨基酸代谢内源性生成。心血管系统存在H2S和SO2的生成体系,并且H2S和SO2具有重要的心血管生理学效应,包括舒张血管和心肌负性肌力作用。H2S和SO2的心血管病理生理学效应也逐渐被认识,如缓解高血压和肺动脉高压、抑制动脉粥样硬化进展、保护心肌缺血再灌注损伤和异丙肾诱导的心肌损伤。ATP敏感性钾通道、L型钙通道、c GMP、NF-κB信号通路及MAPK信号通路等都参与H2S和SO2的生物学效应。以上发现表明H2S和SO2是重要的心血管内源性气体信号分子,为阐明心血管疾病的发病机制和治疗靶点提供新的思路。     

Assimilatory reduction of sulfate and sulfite by methanogenic bacteria

A variety of sulfur-containing compounds were investigated for use as medium reductants and sulfur sources for growth of four methanogenic bacteria. Sulfide (1 to 2 mM) served all methanogens investigated well. Methanococcus thermolithotrophicus and Methanobacterium thermoautotrophicum Marburg and delta H grew well with S0, SO3(2-), or thiosulfate as the sole sulfur source. Only Methanococcus thermolithotrophicus was able to grow with SO4(2-) as the sole sulfur source. 2-Mercaptoethanol at 20 mM was greatly inhibitory to growth of Methanococcus thermolithotrophicus on SO4(2-) or SO2(2-) and Methanobacterium thermoautotrophicum Marburg on SO3(2-) but not to growth of strain delta H on SO3(2-). Sulfite was metabolized during growth by Methanococcus thermolithotrophicus. Sulfide was produced in cultures of Methanococcus thermolithotrophicus growing on SO4(2-), SO3(2-), thiosulfate, and S0. Methanobacterium thermoautotrophicum Marburg was successfully grown in a 10-liter fermentor with S0, SO3(2-), or thiosulfate as the sole sulfur source.     

The uptake of labelled sulphur by the proteins of human liver slices incubated with L-(35S)-methionine or (35S)-sulphate

Transfer of labelled sulphur from methionine into protein-bound cysteine was observed in human foetal liver $\text{in}$$\text{vitro}$. Inorganic sulphate could not be utilized as sulphur donor for cystein synthesis in human foetal liver.     

The hypothesis of the main role of H2S in coupled sulphide-nitroso signalling pathway

As a part of the nitroso signalling pathway, nitroso-compounds serve as stores and carriers of NO; as part of the sulphide signalling pathway, bound sulfane-sulphur compounds serve as stores and carriers of H2S. Here we hypothesise a coupled sulphide-nitroso signalling pathway, in which H2S plays a main role. H2S releases NO from the endogenous S-nitroso-compounds nitroso-cysteine, nitroso-acetylcysteine and nitroso-albumin. Relaxation of noradrenaline-precontracted aortic rings by H2S is also enhanced in the presence of nitroso-albumin, which may implicate the involvement of the nitroso signalling pathway. Pretreatment of albumin, cysteine, N-acetylcysteine and lipids with H2S results in binding of sulphur to these compounds creating thus new-modified sulphur compounds that release NO from nitroso-compounds directly and/or through released H2S, which suggests sulphide-nitroso signalling pathway participation. This hypothesis is supported by the observation that the pretreatment of noradrenaline-precontracted aortic rings with H2S significantly enhanced relaxation induced by nitroso-glutathione in the absence of H2S. We assume that the NO release from nitroso-compounds directly by H2S or indirectly by the H2S-induced sulphur-bound compounds represents coupled sulphide-nitroso signalling, which may explain some of the numerous biological effects of H2S that are shared with NO.     

Ecology of the bacteria of the sulphur cycle with special reference to anoxic-oxic interface environments

H2S is produced as a main end-product of anaerobic mineralization in anoxic, sulphate-rich environments by a diverse population of sulphate-reducing bacteria. The sulphate reducers can carry out an almost complete oxidation of detrital organic matter to CO2. The H2S consequently becomes an important electron carrier from the anoxic to the oxic world. Thiobacilli and other colourless sulphur bacteria have the potential to oxidize the H2S at the oxic-anoxic interface in sediments or stratified waters, but their role is still poorly understood. A comparison of sulphide oxidation processes in the chemoclines of the Black Sea, the Solar Lake and in A beggiatoa mat indicated that depth scales and retention times of coexisting O2 and H2S regulate the bacterial involvement in the sulphide oxidation. The H2S specialists, Beggiatoa and Thiovulum, are optimally adapted to compete with the autocatalytic oxidation of H2S by O2. Microelectrode measurements show retention times of O2-H2S in the bacterial mats or veils of less than 1 s. In photic chemoclines of stratified waters or sulfureta, the phototrophic sulphur bacteria or cyanobacteria interact with the sulphide oxidation at the O2-H2S interface. Short cycles between H2S and intermediate oxidation products, So or S2O2 3-, are created. The bacteria of the sulfuretum are highly adapted to the diurnal rhythm of light, O2 and H2S.     

Sulfide oxidation at halo-alkaline conditions in a fed-batch bioreactor

A biotechnological process is described to remove hydrogen sulfide (H(2)S) from high-pressure natural gas and sour gases produced in the petrochemical industry. The process operates at halo-alkaline conditions and combines an aerobic sulfide-oxidizing reactor with an anaerobic sulfate (SO(4) (2-)) and thiosulfate (S(2)O(3) (2-)) reducing reactor. The feasibility of biological H(2)S oxidation at pH around 10 and total sodium concentration of 2 mol L(-1) was studied in gas-lift bioreactors, using halo-alkaliphilic sulfur-oxidizing bacteria (HA-SOB). Reactor operation at different oxygen to sulfide (O(2):H(2)S) supply ratios resulted in a stable low redox potential that was directly related with the polysulfide (S(x) (2-)) and total sulfide concentration in the bioreactor. Selectivity for SO(4) (2-) formation decreased with increasing S(x) (2-) and total sulfide concentrations. At total sulfide concentrations above 0.25 mmol L(-1), selectivity for SO(4) (2-) formation approached zero and the end products of H(2)S oxidation were elemental sulfur (S(0)) and S(2)O(3) (2-). Maximum selectivity for S(0) formation (83.3+/-0.7%) during stable reactor operation was obtained at a molar O(2):H(2)S supply ratio of 0.65. Under these conditions, intermediary S(x) (2-) plays a major role in the process. Instead of dissolved sulfide (HS(-)), S(x) (2-) seemed to be the most important electron donor for HA-SOB under S(0) producing conditions. In addition, abiotic oxidation of S(x) (2-) was the main cause of undesirable formation of S(2)O(3) (2-). The observed biomass growth yield under SO(4) (2-) producing conditions was 0.86 g N mol(-1) H(2)S. When selectivity for SO(4) (2-) formation was below 5%, almost no biomass growth was observed.     

Carbon and sulphur utilization during growth of Pseudomonas fluorescens on potassium d-glucose 6-O-sulphate as the sole sulphur source

Pseudomonas fluorescens N.C.I.B. 8248 was adapted to grow on potassium d-glucose 6-O-sulphate as the sole carbon and sulphur source. Adapted bacteria grew optimally at 37 degrees C on 1.6% (w/v) sulphate ester and growth coincided with the disappearance of the ester from the culture medium at a rate of 2.4mg/h per ml. Three sulphated compounds were detected in the culture fluid at the termination of growth. One of these was present in traces only and has not been identified. The second was present in somewhat greater amounts and was identified as the 6-O-sulphate ester of d-gluconate, and the major metabolite was identified as d-glycerate 3-O-sulphate. Sulphur utilization by the organism was not associated with the appearance of a glycosulphatase enzyme in the cells. However, a novel enzyme system (or systems) was present that liberated inorganic (35)SO(4) (2-) ions from dipotassium d-gluconate 6[(35)S]-O-sulphate and from dipotassium dl-glycerate 3[(35)S]-O-sulphate. Activity towards the latter substrate could not be detected when the adapted or parent Pseudomonas strain was cultured on d-glucose and potassium sulphate as respective carbon and sulphur sources. Some properties of the enzyme acting on the glycerate ester are recorded.     

Effect of acetylene on nitrous oxide reduction and sulfide oxidation in batch and gradient cultures of Thiobacillus denitrificans.

Anaerobic enrichment cultures with H2S and N2O as substrates which were inoculated with a biofilm sample showed rapid growth and gas formation after 2 to 3 days at 27 degrees C. By using the deep-agar dilution technique, a pure culture was obtained. The strain was tentatively identified as Thiobacillus denitrificans. The isolate was used for batch and gradient culture studies under denitrifying conditions, oxidizing H2S with concomitant reduction of N2O to N2. In batch culture, oxidation of H2S was stepwise, with transient accumulation of elemental sulfur; the final oxidation product was SO4(2-). In gradient culture, there was no notable accumulation of elemental sulfur and microsensor measurements of H2S and N2O showed that H2S was oxidized directly to SO4(2-). In the presence of C2H2, however, oxidation of H2S stopped at the level of elemental sulfur and no SO4(2-) was produced in either batch or gradient cultures. This is a hitherto unknown inhibitory effect of C2H2. The inhibition is suggested to occur at the level of sulfite reductase, which catalyzes the oxidation of elemental sulfur to SO3(2-) in T. denitrificans. However, reduction of N2O in this strain was, surprisingly, not affected by C2H2. The isolate is the first chemolithoautotrophic organism shown to reduce N2O in the presence of C2H2. Denitrification in natural ecosystems is often quantified as N2O accumulation after C2H2 addition. However, the presence of large numbers of similar organisms with C2H2-insensitive N2O reduction could lead to underestimation of in situ rates.