Expression of rat liver canalicular sulfate carrier in Xenopus laevis oocytes

Poly(A)+ RNA (mRNA)extracted from rat liver was injected into Xenopus laevis oocytes and the expression of sulfate transport was determined by measuring [35S] sulfate uptake. Compared to water-injected oocytes, which exhibited virtually no sulfate uptake, injection of rat liver mRNA resulted in a time- and dose-dependent increase in uptake of sulfate. Depending on the method used for the isolation of the mRNA, sulfate uptake was stimulated after injection (40 ng after 6 days) between 8- and 72-fold compared to water-injected oocytes. Sulfate uptake of oocytes injected with mRNA was found to be sensitive to 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid (IC50 less than 20 microM) and could also be inhibited by thiosulfate. Sulfate uptake of injected oocytes showed Michaelis-Menten kinetics (apparent Km, 0.31 mM) which is similar to the Km of the sulfate/bicarbonate antiporter of rat liver canalicular plasma membranes. After fractionation by a sucrose density gradient, the mRNA encoding for the expressed rat liver sulfate carrier was found in fractions containing messages of 3.5-4.0 kilobases in length.     

Increased sulfate uptake in skin fibroblasts isolated from cystic fibrosis patients

Sulfate uptake into skin fibroblasts from patients with cystic fibrosis is increased. Sulfate transport studies were carried out in skin fibroblasts isolated from age/sex matched cystic fibrosis and normal subjects. Sulfate transport occurred mainly via a carrier-mediated proton-stimulated S04(2)-/Cl-exchange. The capacity (Vmax) of the uptake system operating at physiological concentrations of sulfate was stimulated in cystic fibrosis, but the affinity of the carrier for sulfate was not altered.     

Sulfate Uptake in Saccharomyces cerevisiae: Biochemical and Genetic Study

Sulfate uptake is the first step of the sulfate assimilation pathway, which has been shown in our laboratory to be part of the methionine biosynthetic pathway. Kinetic study of sulfate uptake has shown a biphasic curve in a Lineweaver-Burk plot. The analysis of this plot indicates that two enzymes participate in sulfate uptake. One (permease I) has a high affinity for the substrate (K(m) = 0.005 mM); the other (permease II) shows a much lower affinity for sulfate (K(m) = 0.35 mM). Regulation of the synthesis of both permeases is under the control of exogenous methionine or S-adenosylmethionine. It was shown, moreover, that synthesis of sulfate permeases is coordinated with the synthesis of the other methionine biosynthetic enzymes thus far studied in our laboratory. An additional specific regulation of sulfate permeases by inhibition of their activity by endogenous sulfate and adenosyl phosphosulfate (an intermediate metabolite in sulfate assimilation) has been shown. A mutant unable to concentrate sulfate has been selected. This strain carried mutations in two independent genes. These two mutations, separated in two different strains, lead to modified kinetics of sulfate uptake. The study of these strains leads us to postulate that there is an interaction in situ between the products of these two genes.     

Assimilatory sulfur metabolism in marine microorganisms: characteristics and regulation of sulfate transport in Pseudomonas halodurans and Alteromonas luteo-violaceus.

Sulfate transport capacity was not regulated by cysteine, methionine, or glutathione in Pseudomonas halodurans, but growth on sulfate or thiosulfate suppressed transport. Subsequent sulfur starvation of cultures grown on all sulfur sources except glutathione stimulated uptake. Only methionine failed to regulate sulfate transport in Alteromonas luteo-violaceus, and sulfur starvation of all cultures enhanced transport capacity. During sulfur starvation of sulfate-grown cultures of both bacteria, the increase in transport capacity was mirrored by a decrease in the low-molecular-weight organic sulfur pool. Little metabolism of endogenous inorganic sulfate occurred. Cysteine was probably the major regulatory compound in A. luteo-violaceus, but an intermediate in sulfate reduction, between sulfate and cysteine, controlled sulfate transport in P. halodurans. Kinetic characteristics of sulfate transport in the marine bacteria were similar to those of previously reported nonmarine systems in spite of significant regulatory differences. Sulfate and thiosulfate uptake in P. halodurans responded identically to inhibitors, were coordinately regulated by growth on various sulfur compounds and sulfur starvation, and were mutually competitive inhibitors of transport, suggesting that they were transported by the same mechanism. The affinity of P. halodurans for thiosulfate was much greater than for sulfate.     

Sulfate transport in cultured tobacco cells

Sulfate transport by tobacco (Nicotiana tabacum L. var. Xanthi) cells cultured on either l-cysteine or sulfate as a sole sulfur source was measured. The transport rate on either sulfur source was low during pre-exponential growth, increased during exponential growth, and was maximal in late exponential cells. The initial increase in transport rate was correlated with a decline in the intracellular sulfate, but was not correlated with the amino acid content of the cells which remained relatively constant before the depletion of the endogenous sulfate pool. The previously reported inhibition of sulfate transport by l-cysteine was shown to be caused by an elevation in intracellular sulfate resulting from the degradation of cysteine to sulfate. It is proposed that the intracellular sulfate pool is the major factor regulating the entry of sulfate into tobacco cells.     

Characteristics of assimilatory sulfate transport in Rhodobacter sulfidophilus

Abstract Sulfate uptake was investigated with four species of phototrophic sulfur bacteria. Rhodobacter sulfidophilus and Chromatium vinosum took up ³⁵S-labeled sulfate added in micromolar concentrations. Sulfate uptake by C. vinosum was expressed only under sulfate starvation. R. sulfidophilus took up 10 μM sulfate almost completely and accumulated it up to 5300-fold, also when grown with excess sulfate. Sulfite (1 mM) as an intermediate of sulfate assimilation inhibited sulfate uptake completely within 1 min. Moderate inhibition was observed with cysteine (1 mM) and none with sulfide (1 mM). Transport was not dependent on the cations K⁺, Na⁺, Li⁺ or protons, but was sensitive to uncouplers and to the ATPase inhibitor dicyclohexylcarbodiimide (DCCD). The accumulation of sulfate correlated with the ATP concentration in the cells, indicating an ATP-dependent uptake mechanism.     

Plant sulfate assimilation genes: redundancy versus specialization

Sulfur is an essential nutrient present in the amino acids cysteine and methionine, co-enzymes and vitamins. Plants and many microorganisms are able to utilize inorganic sulfate and assimilate it into these compounds. Sulfate assimilation in plants has been extensively studied because of the many functions of sulfur in plant metabolism and stress defense. The pathway is highly regulated in a demand-driven manner. A characteristic feature of this pathway is that most of its components are encoded by small multigene families. This may not be surprising, as several steps of sulfate assimilation occur in multiple cellular compartments, but the composition of the gene families is more complex than simply organellar versus cytosolic forms. Recently, several of these gene families have been investigated in a systematic manner utilizing Arabidopsis reverse genetics tools. In this review, we will assess how far the individual isoforms of sulfate assimilation enzymes possess specific functions and what level of genetic redundancy is retained. We will also compare the genomic organization of sulfate assimilation in the model plant Arabidopsis thaliana with other plant species to find common and species-specific features of the pathway.     

Regulation of sulfate assimilation in Arabidopsis and beyond

BACKGROUND AND AIMS: Sulfate assimilation is a pathway used by prokaryotes, fungi and photosynthetic organisms to convert inorganic sulfate to sulfide, which is further incorporated into carbon skeletons of amino acids to form cysteine or homocysteine. The pathway is highly regulated in a demand-driven manner; however, this regulation is not necessarily identical in various plant species. Therefore, our knowledge of the regulation of sulfate assimilation is reviewed here in detail with emphasis on different plant species. SCOPE: Although demand-driven control plays an essential role in regulation of sulfate assimilation in all plants, the molecular mechanisms of the regulation and the effects of various treatments on the individual enzymes and metabolites are often different. This review summarizes (1) the molecular regulation of sulfate assimilation in Arabidopsis thaliana, especially recent data derived from platform technologies and functional genomics, (2) the co-ordination of sulfate, nitrate and carbon assimilations in Lemna minor, (3) the role of sulfate assimilation and glutathione in plant-Rhizobia symbiosis, (4) the cell-specific distribution of sulfate reduction and glutathione synthesis in C(4) plants, (5) the regulation of glutathione biosynthesis in poplar, (6) the knock-out of the adenosine 5'phosphosulfate reductase gene in Physcomitrella patens and identification of 3'-phosphoadenosyl 5'-phosphosulfate reductase in plants, and (7) the sulfur sensing mechanism in green algae. CONCLUSIONS: As the molecular mechanisms of regulation of the sulfate assimilation pathway are not known, the role of Arabidopsis as a model plant will be further strengthened. However, this review demonstrates that investigations of other plant species will still be necessary to address specific questions of regulation of sulfur nutrition.     

Sulfate-dependent iron oxidation by Thiobacillus ferrooxidans: characterization of a new EPR detectable electron transport component on the reducing side of rusticyanin

Iron(II) oxidation by pH 2.5 HCl-washed cells of Thiobacillus ferrooxidans is known to be sulfate dependent. Sulfate dependence of the autooxidation of a novel component in the electron transport pathway is demonstrated. This component exhibits an electron paramagnetic resonance (EPR) signal in the oxidized state at g = 2.005 distinguishable from the g = 2.08 signal attributed to rusticyanin. The novel component is proposed to be a three-iron-sulfur cluster based upon the g value, lineshape, and temperature dependence. Oxyanion specificity for the EPR signal has the same dependence on sulfate as does iron(II) oxidation. By using azide to inhibit electron transfer to oxygen, sulfate was shown to be involved in electron transfer from the g = 2.005 component to the copper of rusticyanin.     

Translocation of Sulfate in Soybean (Glycine max L. Merr)

Sulfate translocation in soybean (Glycine max L. Merr) was investigated. More than 90% of the sulfate entering the shoot system was recoverable in one or two developing trifoliate leaves. In young plants, the first trifoliate leaf contained between 10 to 20 times as much sulfate as the primary leaves, even though both types of leaf had similar rates of transpiration and photosynthesis. We conclude that most of the sulfate entering mature leaves is rapidly loaded into the phloem and translocated to sinks elsewhere in the plant. This loading was inhibited by carbonylcyanide m-chlorophenylhydrazone and selenate. At sulfate concentrations below 0.1 millimolar, more than 95% of the sulfate entering primary leaves was exported. At higher concentrations the rate of export increased but so did the amount of sulfate remaining in the leaves. Removal of the first trifoliate leaf increased two-fold the transport of sulfate to the apex, indicating that these are competing sinks for sulfate translocated from the primary leaves. The small amount of sulfate transported into the mesophyll cells of primary leaves is a result of feedback regulation by the intracellular sulfate pool, not a consequence of their metabolic inactivity. For example, treatment of plants with 2 millimolar aminotriazole caused a 700 nanomoles per gram fresh weight increase in the glutathione content of primary leaves, but had no effect on sulfate aquisition.     

Sulfate inhibition of molybdate assimilation by planktonic algae and bacteria: some implications for the aquatic nitrogen cycle

Molybdenum is required for both dinitrogen fixation and nitrate assimilation. In oxic waters the primary form of molybdenum is the molybdate anion. Using radioactive [⁹⁹Mol Na₂MoO₄, we have shown that the transport of molybdate by a natural assemblage of freshwater phytoplankton is light-dependent and follows typical saturation kinetics. The molybdate anion is strikingly similar to sulfate and we present data to show that sulfate is a competitive inhibitor of molybdate assimilation by planktonic algae and bacteria. The ability of freshwater phytoplankton to transport molybdate is inhibited at sulfate concentrations as low as 5% of those in seawater and at sulfate: molybdate ratios as low as 50 to 100 times lower than those found in seawater, Similarly, the growth of both a freshwater bacterium and a saltwater diatom was inhibited at sulfate: molybdate ratios lower than those in seawater.The ratio of sulfate to molybdate is 10 to 100 times greater in seawater than in fresh water. This unfavorable sulfate: molybdate ratio may make molybdate less biologically available in the sea. The sulfate: molybdate ratio may explain, in part, the low rates of nitrogen fixation in N-limited salt waters.     

Sodium-Sulfate Symport by Aplysia californica Gut

Sulfate transport across plasma membranes has been described in a wide variety of organisms and cell types including gastrointestinal epithelia. Sulfate transport can be coupled to proton, sodium symport or antiport processes involving chloride or bicarbonate. It had previously been observed in Aplysia gut that sulfate was actively absorbed. To understand the mechanism for this transport, short-circuited Aplysia californica gut was used. Bidirectional transepithelial fluxes of both sodium and sulfate were measured to see whether there was interaction between the fluxes. The net mucosal-to-serosal flux of Na(+) was enhanced by the presence of sulfate and it was abolished by the presence of serosal ouabain. Similarly, the net mucosal-to-serosal flux of sulfate was dependent upon the presence of Na(+) and was abolished by the presence of serosal ouabain. Theophylline, DIDS and bumetanide, added to either side, had no effect on transepithelial potential difference or short-circuit current in the Aplysia gut bathed in a Na2SO4 seawater medium. However, mucosal thiosulfate inhibited the net mucosal-to-serosal fluxes of both sulfate and Na(+) and the thiosulfate-sensitive Na(+) flux to that of sulfate was 2:1. These results suggest the presence of a Na-SO4 symporter in the mucosal membrane of the Aplysia californica foregut absorptive cell.     

Localization of the sulfate/anion exchanger in the rat liver

Although the sulfate/anion transporter (sat-1; SLC26A1) was isolated from a rat liver cDNA library by expression cloning, localization of sat-1 within the liver and its contribution to the transport of sulfate and organo sulfates have remained unresolved. In situ hybridization and immunohistochemical studies were undertaken to demonstrate the localization of sat-1 in liver tissue. RT-PCR studies on isolated hepatocytes and liver endothelial and stellate cells in culture were performed to test for the presence of sat-1 in these cells. In sulfate uptake and efflux experiments, the substrate specificity of sat-1 was evaluated. Sat-1 mRNA was found in hepatocytes and endothelial cells. Sat-1 protein was localized in sinusoidal membranes and along the borders of hepatocytes. The canalicular region and bile capillaries were not stained. Sulfate uptake was only slightly affected by sulfamoyl diuretics or organo sulfates. Sulfate efflux from sat-1-expressing oocytes was enhanced in the presence of bicarbonate, indicating sulfate/bicarbonate exchange. Estrone sulfate was not transported by sat-1. Sat-1 may be responsible for the uptake of inorganic sulfate from the blood into hepatocytes to enable sulfation reactions. In hepatocytes and endothelial cells, sat-1 may also supply sulfate for proteoglycan synthesis.     

Methanogenesis and Sulfate Reduction: Competitive and Noncompetitive Substrates in Estuarine Sediments

Sulfate ions did not inhibit methanogenesis in estuarine sediments supplemented with methanol, trimethylamine, or methionine. However, sulfate greatly retarded methanogenesis when hydrogen or acetate was the substrate. Sulfate reduction was stimulated by acetate, hydrogen, and acetate plus hydrogen, but not by methanol or trimethylamine. These results indicate that sulfate-reducing bacteria will outcompete methanogens for hydrogen, acetate, or both, but will not compete with methanogens for compounds like methanol, trimethylamine, or methionine, thereby allowing methanogenesis and sulfate reduction to operate simultaneously within anoxic, sulfate-containing sediments.     

Sulfate transport in Desulfobulbus propionicus and Desulfococcus multivorans

Uptake of ³⁵S-labelled sulfate was studied with two sulfate-reducing bacteria, the freshwater species Desulfobulbus propionicus and the marine species Desulfococcus multivorans. Both bacteria were able to highly accumulate micromolar additions (2.5 M) of sulfate, if the reduction of sulfate to H₂S was prevented by low temperature (0° C) or oxygen. Sulfate accumulation was highest (accumulation factors 10³ to 10⁴) after growth under sulfate-limiting conditions, while cells grown with excess sulfate revealed accumulation factors below 300. With increasing sulfate concentrations added (up to 25 mM), the accumulation factors decreased down to 1.4. Sulfate accumulation in both strains was sensitive to carbonyl cyanide m-chlorophenylhydrazone (CCCP) and thiocyanate, but not directly correlated to the ATP content of the cells. Pasteurized cells did not accumulate sulfate. Sulfate transport was reversible. Accumulated ³⁵S-labelled sulfate was quickly released after addition of non-labelled sulfate or structural sulfate analogues (thiosulfate, selenate, chromate, less effect by molybdate, tungstate, sulfite, selenite). In D. propionicus, sulfate accumulation was independent of the presence or absence of Na⁺, K⁺, Li⁺, Mg²⁺, Cl^- and Br^-. Sulfate accumulation was reversibly enhanced at pH 5 and diminished at pH 9. In the marine bacterium D. multivorans, sulfate accumulation depended on the presence of Na⁺ ions. Na⁺ could partially be replaced by Li⁺. Sulfate accumulation in D. multivorans was sensitive to the Na⁺/H⁺ antiporter monensin and the Na⁺/H⁺ antiport inhibitor amiloride. It is concluded that in D. propionicus sulfate is accumulated electrogenically in symport with at least three protons, whereas for D. multivorans electrogenic symport with sodium ions is proposed. In both species, more than one sulfate transport system must be present. High affinity transport systems appear to be derepressed under sulfate limitation only. The high affinity transport system must be regulated to avoid energy-spoiling accumulation at high sulfate concentrations.Abbreviations CCCP carbonyl cyanide m-chlorophenylhydrazone - DCCD dicyclohexylcarbodiimide     

Effect of sulfate on carbon and electron flow during microbial methanogenesis in freshwater sediments.

The effect of sulfate on methane production in Lake Mendota sediments was investigated to clarify the mechanism of sulfate inhibition of methanogenesis. Methanogenesis was shown to be inhibited by the addition of as little as 0.2 mM sulfate. Sulfate inhibition was reversed by the addition of either H2 or acetate. Methane evolved when inhibition was reversed by H2 additions was derived from 14CO2. Conversely, when acetate was added to overcome sulfate inhibition, the evolved methane was derived from [2-14C]acetate. A competition for available H2 and acetate was proposed as the mechanism by which sulfate inhibited methanogenesis. Acetate was shown to be metabolized even in the absence of methanogenic activity. In the presence of sulfate, the methyl position of acetate was converted to CO2. The addition of sulfate to sediments did not result in the accumulation of significant amounts of sulfide in the pore water. Sulfate additions did not inhibit methanogenesis unless greater than 100 mug of free sulfide per ml was present in the pore water. These results indicate that carbon and electron flow are altered when sulfate is added to sediments. Sulfate-reducing organisms appear to assume the role of methanogenic bacteria in sulfate-containing sediments by utilizing methanogenic precursors.