Insulin Binding to Human Astrocytoma Cells and Its Effect on Uridine Incorporation into Nucleic Acid

Binding of [125I]monoiodoinsulin to human astrocytoma cells (U-373 MG) was time dependent, reaching equilibrium after 1 h at 22 degrees C with equilibrium binding corresponding to 2.2 fmol/mg protein: this represents approximately 2,000 occupied binding sites per cell. The t1/2 of 125I-insulin dissociation at 22 degrees C was 10 min; the dissociation rate constant of 1.1 X 10(-2) s-1 was unaffected by a high concentration of unlabeled insulin (16.7 microM). Porcine insulin competed for specific 125I-insulin binding in a dose-dependent manner and Scatchard analysis suggested multiple affinity binding sites (higher affinity Ka = 4.4 X 10(8) M-1 and lower affinity Ka = 7.4 X 10(6) M-1). Glucagon and somatostatin did not compete for specific insulin binding. Incubation of cells with insulin (0.5 microM) for 2 h at 37 degrees C increased [2-14C]uridine incorporation into nucleic acid by 62 +/- 2% (n = 3) above basal. Cyclic AMP, in the absence of insulin, also stimulated nucleoside incorporation into nucleic acid [65 +/- 1% (n = 3)] above basal. Preincubation with cyclic AMP followed by insulin had an additive effect on nucleoside incorporation [160 +/- 4% (n = 3) above basal]. Dipyridamole (50 microM), a nucleoside transport inhibitor, blocked both basal and stimulated uridine incorporation. These studies confirm that human astrocytoma cells possess specific insulin receptors with a demonstrable effect of ligand binding on uridine incorporation into nucleic acid.     

Characterization of sulfate transport in Desulfovibrio desulfuricans

Uptake of ³⁵S-labelled sulfate was studied with a new isolate of Desulfovibrio desulfuricans, strain CSN. Micromolar additions of sulfate (1–10 M or nmol/mg protein) to cell suspensions incubated in 150 mM KCl at-1°C were almost completely taken up and accumulated about 5,000-fold. Accumulation was not influenced by incubation in NaCl instead of KCl, by acidic pH (5.5) or by incubation under air for 10 min. In alkaline milieu (pH 8.5), after prolonged contact with air (2 h), or after growth with excess sulfate or thiosulfate as electron acceptor, the amount taken up was diminished approximately by half. Pasteurization inhibited sulfate uptake completely. With increasing concentrations of added sulfate (0.1 to 2.5 mM) the intracellular concentration increased only slowly up to 25 mM, and the accumulation factor decreased down to 8. Sulfate transport was reversible. Accumulated sulfate was rapidly lost from the cells after addition of excess non-labelled sulfate or after addition of the uncoupler carbonyl cyanide m-chlorophenylhydrazone (CCCP). The ATPase inhibitor dicyclohexylcarbodiimide (DCCD) specifically inhibited sulfate reduction but had no immediate influence on sulfate accumulation. Addition of the phosphate analogue arsenate (5 mM) was without effect. These results were not in favour of an ATP-dependent transport system. The K⁺-H⁺-antiporter nigericin (in 150 mM KCl) and the Na⁺-H⁺-antiporter monensin (in 150 mM NaCl) caused partial inhibition of sulfate accumulation, whereas the K⁺-transporter valinomycin (in 150 mM KCl) and the Na⁺-H⁺ exchange inhibitor amiloride (2 mM) were without effect. The permeant thiocyanate anion (150 mM) inhibited sulfate uptake by 60% at pH 7, and completely at pH 8.5. Although the effects of the different ionophores on the chemiosmotic gradients have not been studied so far, the results indicated that probably both, pH and drive sulfate accumulation and that sulfate is taken up electrogenically in symport with more than 2 protons. The structural sulfate analogues tungstate and molybdate (0.1 mM, each) did not affect sulfate accumulation, although molybdate inhibited sulfate reduction. Chromate completely blocked both of these activities. Sulfite and selenite caused little or no decrease of sulfate accumulation, whereas with thiosulfate and selenate significant inhibition was observed.Abbreviations CCCP carbonyl cyanide m-chlorophenylhydrazone - DCCD dicyclohexylcarbodiimide     

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     

Metabolism of l-alanine in Desulfotomaculum ruminis and two marine Desulfovibrio strains

The degradation of l-alanine by three strains of sulfate-reducing bacteria that can grow with l-alanine as an energy source was investigated. In Desulfotomaculum ruminis and most likely also in two marine Desulfovibrio strains alanine is converted to pyruvate via an NAD-dependent alanine dehydrogenase. D. ruminis contained high activities of soluble NADH and NADPH dehydrogenases. In the marine strains the activities were much lower and the NADH dehydrogenase was partly associated with the membrane fraction.     

Isolation and characterization of a thermophilic benzoate-degrading,sulfate-reducing bacterium,Desulfotomaculum thermobenzoicum sp. nov.

A new thermophilic sulfate-reducing bacterium, strain TSB, that was spore-forming, rod-shaped, slightly motile and gram-positive, was isolated from a butyrate-containing enrichment culture inoculated with sludge of a thermophilic methane fermentation reactor. This isolate could oxidize benzoate completely. Strain TSB also oxidized some fatty acids and alcohols. SO _inf4 ^sup2- , SO _inf3 ^sup2- , S₂O _inf3 ^sup2- and NO _inf3 ^sup- were utilized as electron acceptors. With pyruvate or lactate the isolate grew without an external electron acceptor and produced acetate. The optimum temperature for growth was 62°C. The G+C content of DNA was 52.8 mol%. This isolate is described as a new species, Desulfotomaculum thermobenzoicum.     

Sulfate reduction rates and some aspects of the limnology of four lakes and a fjord in the Vestfold Hills,Antarctica

Sulfate reduction rates were measured in waters and sediments from four antarctic lakes and an antarctic fjord basin by a radiometric technique. There was generally a linear correlation between the period of incubation and sulfate reduced; the average of the correlation coefficients was 0.76 ± 0.1. The rates at 6 °C were very low (0.0–1.1 µmol kg^–1 d^–1) when compared to most other marine and non-marine environments for which sulfate reduction rates have been reported. Lactate and acetate did not stimulate sulfate reduction. Temperatures of the sediments selected from the different sites varied from –0.4 to 4.5 °C and the chloride and sulfate concentrations of the sediments varied from 0.19 to 0.83 mol kg^–1 and 0.04 to 41.01 mmol kg^–1 respectively. Sulfate reduction rates did not correlate with the chlorosity of sediment porewaters.