Sulfur metabolism in Thiorhodaceae. V. Enzymes of sulfur metabolism inThiocapsa floridana andChromatium species

In extracts ofThiocapsa floridana strain 6311 andChromatium strains 1611, 2811 and 6412 a high specific activity of adenosine 5-phosphosulfate reductase was found. In contrast, little activity of this enzyme was found inChromatium strain D.Adenosine 5-diphosphate sulfurylase is present in extracts fromThiocapsa floridana strain 6311. The enzyme appears to be involved in the oxidation of reduced sulfur compounds to sulfate.Sulfite oxidase could not be demonstrated in any of the strains examined.     

Sulphur metabolism in Thiorhodaceae. III. Storage and turnover of thiosulphate sulphur inThiocapsa floridana andChromatium species

Thiocapsa floridana strain 1711 andChromatium strains 1211 and 1611 utilize sulphide, thiosulphate, and elementary sulphur as electron donors for growth; sulphite can be used only byChromatium strain 1611. In contrast to the other strains, thiosulphate utilization inChromatium strain 1211 is inducible and not constitutive: thiosulphate is consumed only after an induction period of about 20 hours. The turnover rate of different sulphur compounds is controlled by the CO₂ fixation rate. Using differently labeled³⁵S thiosulphates in short term experiments in a special stirred cuvette, it was shown that the maximum amount of stored intracellular sulphur depends on the strain as well as on the experimental conditions like pH and thiosulphate concentration. WhileChromatium strain 1211 showed a maximum storage of only 10% from sulphane-labeled thiosulphate at pH 6.7, and of 25.7% at pH 6.2,Thiocapsa floridana accumulated 75–90% of the radioactivity into the cells at pH 6.7. While in theChromatium strains the labeling of the cells remained at a constant level until all thiosulphate was consumed, inThiocapsa floridana a defined peak of radioactivity storage was obtained, followed by a steady but 3–4 times slower rate of excretion. With sulphonelabeled thiosulphate no significant accumulation of radioactivity occurred in the cells. During dark-incubation ofThiocapsa floridana (free of intracellular sulphur) in phosphate buffer, pH 6.5, with thiosulphate a production of sulphide could be measured while sulphite was not detected; no sulphide was produced by disrupted cells under the same conditions. The results obtained withThiocapsa floridana strongly support the concept of an initial cleavage of thiosulphate. The present observations do not allow a decision concerning the enzymatic mechanism of the cleavage itself.     

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.     

Assimilatory sulfate reduction in an Escherichia coli mutant lacking thioredoxin activity.

An investigation of sulfate reduction in B tsnC*7004, a mutant of Escherichia coli lacking thioredoxin, is reported. Although thioredoxin is indispensable for the adenosine 3'-phosphate 5'-phosphosulfate (PAPS) sulfotransferase reaction under the usual conditions of assay in extracts of wild-type cells, the mutant grew as well as the wild type on sulfate, indicating that sulfate reduction is not rate limiting for growth. Another cofactor for the PAPS sulfotransferase reaction was found in extracts of the mutant that is absent from wild type cells. This cofactor was indistinguishable from thioredoxin in molecular weight but had a slightly different isoelectric point, allowing a separation of the two types of molecules by isoelectric focusing. Whereas electrons from nicotinamide adenine dinucleotide phosphate, reduced form, could be transferred via thioredoxin reductase or via glutathione and glutathione reductase to reduce thioredoxin in extracts of wild-type cells, electrons from nicotinamide adenine dinucleotide, reduced form, could only be transferred to the cofactor of the mutant via glutathione and glutathione reductase. All of the other available mutants blocked in sulfate reduction in E. coli contained normal levels of thioredoxin. The "PAPS reductase" mutant is shown to be blocked in the PAPS sulfotransferase reaction. We conclude that the cofactor found in mutant B tsnC*7004 is probably a mutated thioredoxin with an amino acid substitution that alters the isoelectric point and the reactivity with thioredoxin reductase.     

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.     

Assimilatory sulfur metabolism in marine microorganisms: Sulfur metabolism,growth, and protein synthesis of Pseudomonas halodurans and Alteromonas luteo-violaceus during sulfate limitation

Sulfate concentration in the growth medium exerted a strong influence on the sulfur content of protein in two marine bacteria, Pseudomonas halodurans and Alteromonasluteo-violaceus, but the distribution of sulfur in major biochemical fractions was not affected. 90% of the total cellular sulfur was contained in low molecular weight organic compounds and protein; inorganic sulfate was not an important component. The sulfur content of isolated protein and total cellular sulfur increased in proportion to the external sulfate concentration for both bacteria, reaching a maximum at about 100–250 M. The growth rate of P. halodurans only was dependent on the sulfate concentration.Sulfur starvation of cells labeled to equilibrium with ³⁵S-sulfate resulted in a rapid decrease in low molecular weight organic S with a concommitant increase in alcohol soluble (P. halodurans) or residue protein (A. luteo-violaceus). Although cell division was prevented, total protein increased in both bacteria, resulting in synthesis of sulfur-deficient protein. This effect was most pronounced in P. halodurans.Addition of ³⁵S-sulfate to sulfur-starved A. luteo-violaceus further demonstrated that sulfur metabolism was restricted primarily to the synthesis and utilization of sulfurcontaining protein precursors. The low molecular weight organic S pool was replenished rapidly, and the pool size per cell reached twice the normal value before cell division resumed. Incorporation into protein was very rapid.Abbreviations L.M.W. low molecular weight - TCA trichloroacetic acid     

Assimilatory sulfur metabolism in marine microorganisms: a novel sulfate transport system in Alteromonas luteo-violaceus.

The sulfate transport mechanism of a marine bacterium, Alteromonas luteo-violaceus, was unique among microorganisms in its extremely low affinity for the sulfate analog thiosulfate. Distinguishing characteristics included weak inhibition of sulfate transport by thiosulfate, inability to transport thiosulfate effectively, poor growth using thiosulfate as the sole source of sulfur, and a mild effect of the sulfhydryl reagent para-hydroxymercuribenzoate. In contrast, sulfate transport by a marine pseudomonad, Pseudomonas halodurans, was strongly inhibited by thiosulfate, and para-hydroxymercuribenzoate reversibly but completely blocked sulfate transport.     

Assimilatory sulfate reduction in chloroplasts: Evidence for the participation of both stromal and membrane-bound enzymes

The reduction of sulfate in osmotically shocked chloroplastswas investigated. Like intact (i.e., Class a) chloroplasts,this type carries out the complete sulfate reducing process.The conditions for formation of the intermediate bound sulfiteand bound sulfide were examined. The amount of bound sulfideand bound sulfide formed from sulfate was proportional to theamount of chlorophyll. The Km of the overall reaction from sulfateto bound sulfite was 1.53 mmoles (at 500 µg chlorophyll).ATP was saturated at 5 mM over a concentration of 0.25 to 0.5mg chlorophyll. At higher concentrations of chlorophyll, nosaturation by ATP was observed. Cysteine formation showed anoptimum concentration for O-acetyl serine at 4 mM. After separation of the osmotically ruptured chloroplasts intoa soluble "chloroplast extract" and a paniculate "chloroplastthylakoid fraction," bound sulfite was formed from sulfate bythe thylakoid fraction but not by the chloroplast extract. Fromthe chloroplast extract, a protein of low molecular weight waspurified. It increased the amount of bound sulfite formed whena NADPH₂-regenerating system was present. (Received June 6, 1975; )     

Assimilatory sulfur metabolism in Rhodopseudomonas sulfoviridis

Rhodopseudomonas sulfoviridis is unable to grow with sulfate as sole sulfur source. Radioactively labelled sulfate is not incorporated into the cells. Growth only occurs in the presence of reduced sulfur compounds, such as sulfide, thiosulfate, elemental sulfur and cysteine. ATP sulfurylase, adenylylsulfate kinase, O-acetylserine sulfhydrylase and cysteine desulfhydrase are present. Adenylylsulfate sulfotransferase and thiosulfonate reductase are lacking. The enzymes of the sulfate-activating system are not derepressed by O-acetylserine.Non common Abbreviations APS Adenosine 5-phosphosulfate - PAPS 3-phosphoadenosine 5-phosphosulfate     

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.     

Assimilatory sulfate reduction in C(3), C(3)-C(4), and C(4) species of Flaveria

The activity of the enzymes catalyzing the first two steps of sulfate assimilation, ATP sulfurylase and adenosine 5'-phosphosulfate reductase (APR), are confined to bundle sheath cells in several C(4) monocot species. With the aim to analyze the molecular basis of this distribution and to determine whether it was a prerequisite or a consequence of the C(4) photosynthetic mechanism, we compared the intercellular distribution of the activity and the mRNA of APR in C(3), C(3)-C(4), C(4)-like, and C(4) species of the dicot genus Flaveria. Measurements of APR activity, mRNA level, and protein accumulation in six Flaveria species revealed that APR activity, cysteine, and glutathione levels were significantly higher in C(4)-like and C(4) species than in C(3) and C(3)-C(4) species. ATP sulfurylase and APR mRNA were present at comparable levels in both mesophyll and bundle sheath cells of C(4) species Flaveria trinervia. Immunogold electron microscopy demonstrated the presence of APR protein in chloroplasts of both cell types. These findings, taken together with results from the literature, show that the localization of assimilatory sulfate reduction in the bundle sheath cells is not ubiquitous among C(4) plants and therefore is neither a prerequisite nor a consequence of C(4) photosynthesis.     

Assimilatory sulfate reduction in Escherichia coli: identification of the alternate cofactor for adenosine 3'-phosphate 5'-phosphosulfate reductase as glutaredoxin.

The alternate cofactor (7004 cofactor) for Escherichia coli adenosine 3'-phosphate 5'-phosphosulfate (PAPS) reductase originally discovered in an E. coli mutant (tsnC 7004) lacking thioredoxin activity has now been purified and characterized. The tryptic peptide map of the 7004 cofactor is totally different from that of thioredoxin, indicating that the two proteins are unrelated in their primary structure. The 7004 cofactor has an amino acid composition different from that of thioredoxin but similar to that of glutaredoxin, a protein required for the glutathione-dependent deoxyribonucleotide formation by ribonucleotide reductase. Thus, the 7004 cofactor could not be a mutated form of thioredoxin, as was suspected earlier. Thioredoxin but not glutaredoxin is a substrate for thioredoxin reductase, but both thioredoxin and glutaredoxin can catalyze the dithiothreitol- or glutathione-dependent reduction of PAPS. On a molar basis, the dithiothreitol-coupled cofactor activity of thioredoxin is three- to fourfold higher that that of glutaredoxin. Comparison of the cofactor activities in the glutathione-coupled and the dithiothreitol-coupled PAPS reductase reaction shows that the cofactor activity of thioredoxin in the glutathione-coupled reaction is only 23% of that observed in the dithiothreitol-coupled reaction. However, in the case of glutaredoxin, cofactor activities are approximately the same in both the dithiothreitol- and glutathione-coupled reactions.     

Sulphur metabolism in Thiorhodaceae I. Quantitative measurements on growing cells ofChromatium okenii

Growth experiments and short term experiments in a stirred cuvette showed thatChromatium okenii strain Ostrau is not able to oxidize any reduced sulphur compounds except sulphide and elementary sulphur; thiosulphate, sulphite, and thioglycolate can not be utilized as reducing agents for photosynthesis. The cells are not able to use H₂; hydrogenase could not be demonstrated. In the dark, sulphide is formed from intracellular sulphur and the carbon content of the cells decreases. Growth and turnover of sulphur compounds was followed in the light in the presence and absence of acetate as a second carbon source. Sulphide oxidation depends on the presence of CO₂ and on light intensity, i.e. sulphur metabolism is governed by the photosynthetic activity of the cells.     

Antiquity and evolutionary status of bacterial sulfate reduction: Sulfur isotope evidence

The presently available sedimentary sulfur isotope record for the Precambrian seems to allow the following conclusions: (1) In the Early Archaean, sedimentary ^{3 4} patterns attributable to bacteriogenic sulfate reduction are generally absent. In particular, the ^{3 4} spread observed in the Isua banded iron formation (3.7×10⁹ yr) is extremely narrow and coincides completely with the respective spreads yielded by contemporaneous rocks of assumed mantle derivation. Incipient minor differentiation of the isotope patterns notably of Archaean sulfates may be accounted for by photosynthetic sulfur bacteria rather than by sulfate reducers. (2) Isotopic evidence of dissimilatory sulfate reduction is first observed in the upper Archaean of the Aldan Shield, Siberia (3.0×10⁹ yr) and in the Michipicoten and Woman River banded iron formations of Canada (2.75×10⁹ yr). This narrows down the possible time of appearance of sulfate respirers to the interval 2.8–3.1×10⁹ yr. (3) Various lines of evidence indicate that photosynthesis is older than sulfate respiration, the SO ₄ ^2– utilized by the first sulfate reducers deriving most probably from oxidation of reduced sulfur compounds by photosynthetic sulfur bacteria. Sulfate respiration must, in turn, have antedated oxygen respiration as O₂-respiring multicellular eucaryotes appear late in the Precambrian. (4) With the bulk of sulfate in the Archaean oceans probably produced by photosynthetic sulfur bacteria, the accumulation of SO ₄ ^2– in the ancient seas must have preceded the buildup of appreciable steady state levels of free oxygen. Hence, the occurrence of sulfate evaporites in Archaean sediments does not necessarily provide testimony of oxidation weathering on the ancient continents and, consequently, of the existence of an atmospheric oxygen reservoir.Paper presented at the Fourth College Park Colloquium on Chemical Evolution, Limits of Life, October 18–20, 1978.     

The relationship between hydrogen metabolism,sulfate reduction and nitrogen fixation in sulfate reducers

Summary Hydrogenase and nitrogenase activities of sulfate-reducing bacteria allow their adaptation to different nutritional habits even under adverse conditions. These exceptional capabilities of adaptation are important factors in the understanding of their predominant role in problems related to anaerobic metal corrosion. Although the D₂–H⁺ exchange reaction indicated thatDesulfovibrio desulfuricans strain Berre-Sol andDesulfovibrio gigas hydrogenases were reversible, the predominant activity in vivo was hydrogen uptake. Hydrogen production was restricted to some particular conditions such as sulfate or nitrogen starvation. Under diazotrophic conditions, a transient hydrogen evolution was followed by uptake when dinitrogen was effectively fixed. In contrast, hydrogen evolution proceeded when acetylene was substituted as the nitrogenase substrate. Hydrogen can thus serve as an electron donor in sulfate reduction and nitrogen metabolism.