5-Oxo-prolinase activity in tobacco suspension cultures: Regulation by sulfate nutrition

In heterotrophic and photoheterotrophic tobacco ( Nicotiana tabacum L., var. Samsun) suspensions cultured with growth-limiting amounts of sulfate, 5-oxo-prolinase activity declines at the same time as the growth rate of the cells decreases. However, 5-oxo-prolinase activity is reduced to a greater extent than growth. As a result, the specific activity of 5-oxo-prolinase also declines when sulfur is scarce. The decrease in both growth and 5-oxo-prolinase activity can be prevented by adding sulfate to the suspensions during exponential growth. Addition of sulfate after the exponential growth phase restored neither growth nor 5-oxo-prolinase activity. These observations show that 5-oxo-prolinase activity in tobacco cells is regulated by the sulfate supply in the medium. Such a regulation is an essential prerequisite, but not a proof, for a role of 5-oxo-prolinase as the rate-limiting factor in glutathione degradation.
During exponential growth the average specific activity of 5-oxo-prolinase in heterotrophic tobacco cells is twice as high as in photoheterotrophic cells. This difference is consistent with the idea that green cells are equipped for glutathione synthesis and export, and chloroplast-free cells for uptake and degradation of this peptide.     

Importance of sulphur in crop production

Sulphur in agricultural soils occurs in organic and inorganic forms, with organic S accounting for > 95% of the total S. Analysis of a wide range of soils shows that from 25 to 75% of the organic S in soils is HI-reducible, from 7 to 30% is C-bonded, and from 11 to 22% is unidentified S. Nitrogen is associated with S in soil organic matter in a ratio of about 8 : 1, although the extreme ratios may vary from 5: 1 to 13: 1. Laboratory studies showed that humus S is depleted faster than humus N. Mineralization of S in crop residues varied with type of crop residue and soil studied The amounts of S fertilizers (gypsum, elemental S, and sulfuric acid) used in the United States in 1981 and 1982 were 1.9 × 10⁶ and 1.5 × 10⁶ tons, respectively. Of the total amount used in 1982, 3, 5, 20, and 71% were used in the West North Central, Mountain, South Atlantic, and Pacific regions, respecitively. A survey of S deposition at about 100 sites in the United States and many other sites in Canada in 1980 showed that annual addition by precipitation in North America ranged from 0.5 to slightly above 10 kg/ha. The usual ranges of values in concentrations and spatial rates of N, P, and S in precipitation is well within the ranges of these elements in natural waters. Atmospheric sources are important components in meeting crops S requirements and should be considered in benefit-cost analyses relating to S emissions.Contribution from a symposium on the role of sulfur in ecosystem processes held August 10, 1983, at the annual meeting of the A.I.B.S., Grand Forks, ND; Myron Mitchell, convenor.     

Modelling of sulfur oxidation from elemental sulfur

An elemental S oxidation model has been developed which combines a maximum S release rate with modifiers for temperature and soil moisture conditions. This model has been combined with a pasture growth and CNSP nutrient cycling model to match S oxidation rate to pasture S demand. In two Southern Australian enviroments, 100m elemental S was superior to 200m particles whilst in Northern Australia the 200m particles were superior. These models can be used to match S release to plant demand.     

Insights into the sulfur metabolism of Chlorobaculum tepidum by label-free quantitative proteomics

Chlorobaculum tepidum is an anaerobic green sulfur bacterium which oxidizes sulfide, elemental sulfur, and thiosulfate for photosynthetic growth. It can also oxidize sulfide to produce extracellular S⁰ globules, which can be further oxidized to sulfate and used as an electron donor. Here, we performed label-free quantitative proteomics on total cell lysates prepared from different metabolic states, including a sulfur production state (10 h post-incubation [PI]), the beginning of sulfur consumption (20 h PI), and the end of sulfur consumption (40 h PI), respectively. We observed an increased abundance of the sulfide:quinone oxidoreductase (Sqr) proteins in 10 h PI indicating a sulfur production state. The periplasmic thiosulfate-oxidizing Sox enzymes and the dissimilatory sulfite reductase (Dsr) subunits showed an increased abundance in 20 h PI, corresponding to the sulfur-consuming state. In addition, we found that the abundance of the heterodisulfide-reductase and the sulfhydrogenase operons was influenced by electron donor availability and may be associated with sulfur metabolism. Further, we isolated and analyzed the extracellular sulfur globules in the different metabolic states to study their morphology and the sulfur cluster composition, yielding 58 previously uncharacterized proteins in purified globules. Our results show that C. tepidum regulates the cellular levels of enzymes involved in sulfur metabolism in response to the availability of reduced sulfur compounds.     

Is hydrogen sulfide a circulating “gasotransmitter” in vertebrate blood?

Hydrogen sulfide (H₂S) is gaining acceptance as a signaling molecule and has been shown to elicit a variety of biological effects at concentrations between 10 and 1000 μmol/l. Dissolved H₂S is a weak acid in equilibrium with HS⁻ and S²⁻ and under physiological conditions these species, collectively referred to as sulfide, exist in the approximate ratio of 20% H₂S, 80% HS⁻ and 0% S²⁻. Numerous analyses over the past 8 years have reported plasma or blood sulfide concentrations also in this range, typically between 30 and 300 μmol/l, thus supporting the biological studies. However, there is some question whether or not these concentrations are physiological. First, many of these values have been obtained from indirect methods using relatively harsh chemical conditions. Second, most studies conducted prior to 2000 failed to find blood sulfide in micromolar concentrations while others showed that radiolabeled ³⁵S-sulfide is rapidly removed from blood and that mammals have a relatively high capacity to metabolize exogenously administered sulfide. Very recent studies using H₂S gas-sensing electrodes to directly measure sulfide in plasma or blood, or HPLC analysis of head-space gas, have also indicated that sulfide does not circulate at micromolar levels and is rapidly consumed by blood or tissues. Third, micromolar concentrations of sulfide in blood or exhaled air should be, but are not, malodorous. Fourth, estimates of dietary sulfur necessary to sustain micromolar levels of plasma sulfide greatly exceed the daily intake. Collectively, these studies imply that many of the biological effects of sulfide are only achieved at supra-physiological concentrations and they question whether circulating sulfide is a physiologically relevant signaling molecule. This review examines the blood/plasma sulfide measurements that have been reported over the past 30 years from the perspective of the analytical methods used and the potential sources of error.     

Anaerobic Elemental Sulfur Reduction by Fungus Fusarium oxysporum

Reduction of inorganic sulfur compounds by the fungus Fusarium oxysporum was examined. When transferred from a normoxic to an anoxic environment, F. oxysporum reduced elemental sulfur to hydrogen sulfide (H₂S). This reaction accompanied fungal growth and oxidation of the carbon source (ethanol) to acetate. Over 2-fold more of H₂S than of acetate was produced, which is the theoretical correlation for the oxidation of ethanol to acetate. NADH-dependent sulfur reductase (SR) activity was detected in cell-free extracts of the H₂S-producing fungus, and was found to be up-regulated under the anaerobic conditions. On the other hands both O₂ consumption by the cells and cytochrome c oxidase activity by the crude mitochondrial fractions decreased. These results indicate that H₂S production involving SR was due to a novel dissimilation mechanism of F. oxysporum, and that the fungus adapts to anaerobic conditions by replacing the energy-producing mechanism of O₂ respiration with sulfur reduction.     

Isotope effects associated with the anaerobic oxidation of sulfite and thiosulfate by the photosynthetic bacterium, Chromatium vinosum

Abstract The purple photosynthetic bacterium Chromatium vinosum , strain D, catalyzes several oxidations of reduced sulfur compounds under anaerobic conditions in the light: e.g., sulfide → sulfur → sulfate, sulfite → sulfate, and thiosulfate → sulfur + sulfate. Here it is shown that no sulfur isotope effect is associated with the last of these processes; isotopic compositions of the sulfur and sulfate produced can differ, however, if the sulfane and sulfonate positions within the thiosulfate have different isotopic compositions. In the second process, an observed change from an inverse to a normal isotope effect during oxidation of sulfite may indicate the operation of 2 enzymatic pathways. In contrast to heterotrophic anaerobic reduction of oxidized sulfur compounds, anaerobic oxidations of inorganic sulfur compounds by photosynthetic bacteria are characterized by relatively small isotope effects.     

Chemical reactivity of labile sulfur of iron-sulfur proteins The reaction of triphenyl phosphine

The reaction of triphenyl phosphine to iron-sulfur proteins from adrenal cortex mitochondria, spinach chloroplasts, and Clostridium pasteurianum was investigated. As ethanol concentrations in the reaction mixture increased, the rate of the reaction decreased. In the simultaneous presence of 1 M KCl and 5 M urea, the reaction rate reached at maximum. Under these conditions the initial rates of the decolorization reaction by the phosphine were found to be 8.7, 0.88, and 1.8 nmol of ferrodoxin per min at 25°C for adrenal, spinach, and clostridial ferredoxins, respectively. The kinetic curves for the reaction of the phosphine sulfide formation, the loss of labile sulfur, and the deterioriation of visible absorption showed a similar pattern with a comparable rate. During this reaction, the complete reduction of ferric ions present in ferredoxin was observed with a fast rate under either aerobic or anaerobic conditions.These results suggest that the iron atoms in ferredoxin are first reduced by the intramolecular reductants in the presence of triphenyl phosphine with the concomitant formation of S₂^2?, which then reacts with triphenyl phosphine resulting in the formation of triphenyl phosphine sulfide.     

微生物硫循环网络的研究进展

硫元素是所有生物的基本组成成分,是生物体必需的营养元素之一。硫氧化还原微生物的数量多、分布广、代谢途径多样化,硫化合物之间的平衡依赖于微生物代谢网络中的各种硫转化反应与代谢过程。此外,硫循环与碳、氮循环紧密相关,对地球生态循环起到了至关重要的作用。本文综述了近期微生物硫循环网络的研究进展,包括所涉及的主要微生物、硫循环的生物化学途径、硫循环的环境意义和工业应用潜能等,深入了解自然和人工生态系统中存在的硫循环过程,可为控制工农业生产中硫元素的增减与利用提供理论基础与应用方案。     

Oxidative metabolism of inorganic sulfur compounds by bacteria

The history of the elucidation of the microbiology and biochemistry of the oxidation of inorganic sulfur compounds in chemolithotrophic bacteria is briefly reviewed, and the contribution of Martinus Beijerinck to the study of sulfur-oxidizing bacteria highlighted. Recent developments in the biochemistry, enzymology and molecular biology of sulfur oxidation in obligately and facultatively lithotrophic bacteria are summarized, and the existence of at least two major pathways of thiosulfate (sulfur and sulfide) oxidation confirmed. These are identified as the Paracoccus sulfur oxidation (or PSO) pathway and the S4intermediate (or S4I) pathway respectively. The former occurs in organisms such as Paracoccus (Thiobacillus) versutus and P. denitrificans, and possibly in Thiobacillus novellus and Xanthobacter spp. The latter pathway is characteristic of the obligate chemolithotrophs (e.g. Thiobacillus tepidarius, T. neapolitanus, T. ferrooxidans, T. thiooxidans) and facultative species such as T. acidophilus and T. aquaesulis, all of which can produce or oxidize tetrathionate when grown on thiosulfate. The central problem, as yet incompletely resolved in all cases, is the enzymology of the conversion of sulfane-sulfur (as in the outer [S-] atom of thiosulfate [-S-SO3-]), or sulfur itself, to sulfate, and whether sulfite is involved as a free intermediate in this process in all, or only some, cases. The study of inorganic sulfur compound oxidation for energetic purposes in bacteria (i.e. chemolithotrophy and sulfur photolithotrophy) poses challenges for comparative biochemistry. It also provides evidence of convergent evolution among diverse bacterial groups to achieve the end of energy-yielding sulfur compound oxidation (to drive autotrophic growth on carbon dioxide) but using a variety of enzymological systems, which share some common features. Some new data are presented on the oxidation of 35S-thiosulfate, and on the effect of other anions (selenate, molybdate, tu ngstate, chromate, vanadate) on sulfur compound oxidation, including observations which relate to the roles of polythionates and elemental sulfur as intermediates.     

Sulfur distribution in lake sediment profiles as an index of historical depositional patterns

Changes in S concentration in sediment profiles from South Lake (Adirondack region, New York, USA) and Ledge Pond (western Maine, USA) indicated an increased input of S beginning around 1850. This S was probably derived from anthropogenic sources. The S budget for South Lake indicated that sedimentation of seston rich in S (0.9% dry mass) accounts for most of the input of S in sediment. Sulfur in both seston and sediment is primarily organic (57 and 22% ester sulfate, 32 and 52% carbon-bonded S, respectively). The transformation and translocation of organic S constitutes a major pathway of S flux in South Lake.     

中国温带草地土壤硫的分布特征及其与环境因子的关系

以内蒙古和青藏高原的6种主要草地类型为研究对象,分析了不同类型草地表层土壤硫(S)的分布特征及其与环境因子的关系。结果表明:1)青藏高原草原表层土壤(0—10 cm)的全硫含量(430.8 mg/kg)显著高于内蒙古草原(181.4 mg/kg;P0.01)。土壤硫素一般以有机硫的形式存在,具有植物有效性的土壤无机硫所占比例较少,内蒙古土壤这一比例为14.7%,青藏高原为24.5%。2)土壤硫的含量与土壤C、N的分布格局关系紧密,呈显著正相关关系;与土壤p H呈负相关关系。内蒙古与青藏高原研究区土壤的C/S和N/S值较低,这表明硫可能成为对草原生产力起限制性作用的营养元素。3)内蒙古草原表层土壤全硫、水溶性硫、吸附性硫均与年均温呈显著负相关(P0.05);土壤硫与年均降水呈显著正相关关系(P0.05)。青藏高原草地土壤硫中,除水溶性硫与年均降水呈显著正相关关系外,其余土壤硫含量均未与气候因子呈现显著相关关系。     

Effect of N source during soybean pod filling on nitrogen and sulfur assimilation and remobilization

During pod filling, a grain legume remobilizes vegetative nitrogen and sulfur to its developing fruit. This study was conducted to determine whether different nitrogen sources affected N and S assimilation and remobilization during pod filling. Well-nodulated plants fed 1.0 mM KNO₃, 0.5 mM urea, or 2.5 mM urea assimilated 0%, 37%, or 114% more N, respectively, and 25%, 46%, or 56% more S, respectively, than did the average non-nodulated control plant fed 5.0 mM KNO₃. Thus, N source during pod filling greatly affected both N and S assimilation. Depending upon N source, plant N concentration during pod filling decreased from 2.96% to between 1.36% and 1.82%. Non-nodulated control plants fed 5.0 mM KNO₃ had the highest residual N at harvest. During the same treatments, plant S concentration decreased from 0.246% to a relatively uniform 0.215%. Thus, during pod filling, vegetative N was seemingly remobilized more efficiently (38–54%) than was S (13%). N source also affected seed yield and seed quality. Non-nodulated control plants fed 5.0 mM KNO₃ produced the lowest yield (21.1 g seeds plant^-1), whereas well nodulated plants fed 1.0 mM KNO₃, 0.5 mM urea, or 2.5 mM urea produced yields of 26.2 g, 31.8 g, and 36.7 g seeds plant^-1, respectively. Non-nodulated plants fed 2.5 mM urea yielded 28.6 g of seeds plant^-1. Seed N concentrations of non-nodulated plants and nodulated plants fed 2.5 mM urea were high, 6.30% and 6.11% N, respectively, whereas their seed S concentrations were low, 0.348% and 0.330% S, respectively. N sources that produced both a relatively high seed yield and seed N concentration (i.e., a relatively high total seed N plant^-1) produced a proportionately smaller increase in total seed sulfur. Consequently, seed quality, as judged solely by seed S concentration, was lowered.     

A Polyaniline‐Coated Sulfur/Carbon Composite with an Enhanced High‐Rate Capability as a Cathode Material for Lithium/Sulfur Batteries

Polyaniline‐coated sulfur/conductive‐carbon‐black (PANI@S/C) composites with different contents of sulfur are prepared via two facile processes including ball‐milling and thermal treatment of the conductive carbon black and sublimed sulfur, followed by an in situ chemical oxidative polymerization of the aniline monomer in the presence of the S/C composite and ammonium persulfate. The microstructure and electrochemical performance of the as‐prepared composites are investigated systematically. It is demonstrated that the polyaniline, with a thickness of ≈5–10 nm, is coated uniformly onto the surface of the S/C composite forming a core/shell structure. The PANI@S/C composite with 43.7 wt% sulfur presents the optimum electrochemical performance, including a large reversible capacity, a good coulombic efficiency, and a high active‐sulfur utilization. The formation of the unique core/shell structure in the PANI@S/C composites is responsible for the improvement of the electrochemical performance. In particular, the high‐rate charge/discharge capability of the PANI@S/C composites is excellent due to a synergistic effect on the high electrical conductivity from both the conductive carbon black in the matrix and the PANI on the surface. Even at an ultrahigh rate (10C), a maximum discharge capacity of 635.5 mA h per g of sulfur is still retained for the PANI@S/C composite after activation, and the discharge capacity retention is over 60% after 200 cycles.     

硫稳定同位素技术在生态学研究中的应用

随着人为SO₂释放的增加, 硫稳定同位素的动态已成为生物地球化学循环过程中研究的热点。该文对天然硫稳定同位素在大气自然过程中的硫来源分析及其在森林生态系统、农田生态系统和水域生态系统中的硫动态研究, 人为添加的硫稳定同位素在生态环境中的应用及硫稳定同位素技术在我国酸雨研究中的潜在贡献等进行了综述, 并从硫稳定同位素技术应用研究的范围、分析手段及源解析模型方面介绍了可能的发展方向。     

Susceptibility of various purple and green sulfur bacteria to different antimicrobial agents

Abstract Several purple and green sulfur bacteria (genera Chromatium, Thiocapsa and Chlorobium ) were tested for their sensitivity to different antimicrobial agents by a disc diffusion assay, using thioacetamide as a source of hydrogen sulfide for plate growth. Chlorobium limicola strains were more sensitive to amoxicillin, erythromycin and nalidixic acid, whereas gentamicin and netilmicin were more active against the purple bacteria tested. None of the organisms were sensitive to oxacillin and trimethoprim + sulfamethoxazole. The critical concentrations at the edge of the inhibition zone were also calculated for three organisms and the antimicrobials colistin, mitomycin C, penicillin G, rifampicin, and streptomycin. The results obtained suggest that colistin, mitomycin C, penicillin G would provide selective conditions against the growth of Chlorobium limicola strains, while streptomycin and other aminoglycoside antibiotics would select against purple bacteria.     

Molecular aspects of photosystem I

Photosystem I (PSI) in higher plants consists of 17 polypeptide subunits. Cofactors are chlorophyll a and b , β-carotene, phylloquinone and iron-sulfur clusters. Eight subunits are specific for higher plants while the remaining ones are also present in cyanobacteria. Two 80-kDa subunits (PSI-A and -B) constitute the major part of PSI and bind most of the pigments and electron donors and acceptors. The 9-kDa PSI-C carries the remaining electron acceptors which are [4Fe-4S] iron sulfur clusters. PSI-D, -E and -H have importance for integrity and function at the stromal face of PSI while PSI-F has importance for function at the lumenal face. PSI-N is localized at the lumenal side, but its function is unknown. Four subunits are light-harvesting chlorophyll a/b -binding proteins. The remaining subunits are integral membrane proteins with poorly understood function. Subunit interactions have been studied in reconstitution experiments and by cross-linking studies. Based on these data, it is concluded that iron-sulfur cluster F_B is proximal to F_X and that F_A is the terminal acceptor in PSI. Similarities between PSI and the reaction center from green sulfur bacteria are discussed.     

Complete genome sequence of Halorhodospira halophila SL1

Halorhodospira halophila is among the most halophilic organisms known. It is an obligately photosynthetic and anaerobic purple sulfur bacterium that exhibits autotrophic growth up to saturated NaCl concentrations. The type strain H. halophila SL1 was isolated from a hypersaline lake in Oregon. Here we report the determination of its entire genome in a single contig. This is the first genome of a phototrophic extreme halophile. The genome consists of 2,678,452 bp, encoding 2,493 predicted genes as determined by automated genome annotation. Of the 2,407 predicted proteins, 1,905 were assigned to a putative function. Future detailed analysis of this genome promises to yield insights into the halophilic adaptations of this organism, its ability for photoautotrophic growth under extreme conditions, and its characteristic sulfur metabolism.