Specificity and sodium dependence of the active nucleoside transport system in choroid plexus

The transport of [3H]deoxyuridine by the active nucleoside transport system into the isolated rabbit choroid plexus was measured in vitro under various conditions. Choroid plexuses were incubated in artificial CSF containing 1 microM [3H]deoxyuridine and 1 microM nitrobenzylthioinosine for 5 min under 95% O2-5% CO2 at 37 degrees C and the accumulation of [3H]deoxyuridine measured. Nitrobenzylthioinosine was added to the artificial CSF at a concentration (1 microM) that did not inhibit the active nucleoside transport system but did inhibit the separate, saturable nucleoside efflux system. The active transport of deoxyuridine into the choroid plexus depended on Na+ in the medium, as ouabain, substitution of Li+ and choline for Na+, and poly-L-lysine all inhibited deoxyuridine transport. Thiocyanate in place of chloride and penetrating sulfhydryl reagents also inhibited the active transport of deoxyuridine into choroid plexus. The active transport of deoxyuridine into choroid plexus, which is inhibited by naturally occurring ribo- and deoxyribonucleosides (IC50 = 7-21 microM), was not inhibited (IC50 much greater than 150 microM) by nucleosides with certain alterations on the 2', 3', or 5' positions in D-ribose or 2-deoxy-D-ribose (e.g., adenine arabinoside, 3'-deoxyadenosine, xylosyladenosine); or the pyrimidine or purine rings (e.g., 6-azauridine, xanthosine, 7-methylinosine, or 8-bromoadenosine). Other analogues were effective (IC50 = 8-26 microM; e.g., 5-substituted pyrimidine nucleosides, 7-deazaadenosine, 6-mercaptoguanosine) or less effective (IC50 = 46-145 microM; e.g., 5-azacytidine, 3-deazauridine) inhibitors of deoxyuridine transport into the isolated choroid plexus.     

Characterization, development, and localization of the deoxycytidine phosphorylating systems in mammalian brain

The accumulation of deoxycytidine by rabbit and mouse brain was studied in vitro. Brain slices from brain stem, cerebellum, and forebrain of rabbits of various ages (1 day to 2.5 years) and forebrain from adult mice were incubated for various times in artificial CSF containing 6 nM [3H]deoxycytidine at 37 degrees C under 95% O2/5% CO2. Rabbit and mouse brain slices of all ages accumulated [3H]deoxycytidine by a saturable system (IC50 = 4 microM) and converted it to [3H]deoxycytidine phosphates and [3H]DNA. When slices from all brain regions of 1-day-old rabbits were incubated in 6 nM [3H]deoxycytidine for 30 min, tissue-to-medium ratios of 3H were between 1.2 and 2.5 and declined with age, except in cortex; the percentages of total 3H in perchloric acid homogenates of brain slices as [3H]DNA were 10-24% and declined to low levels in middle age. However, at all ages and in all regions tested, 30-85% of the [3H]deoxycytidine within the slices was phosphorylated. After homogenization and subcellular fractionation of the brain slices incubated in [3H]deoxycytidine for 30 min, the highest percentage of [3H]deoxycytidine phosphates plus [3H]DNA was present in the nuclear and mitochondrial fractions of all brain regions. Deoxycytidine phosphates were synthesized from deoxycytidine in all brain regions tested into middle age.     

Deoxycytidine Transport and Metabolism in the Central Nervous System

Abstract: The mechanisms by which deoxycytidine enters and leaves brain, choroid plexus, and CSF were investigated by injecting [³H]deoxycytidine intraarterially, intravenously, and intraventricularly. After intracarotid injection of deoxycytidine (1.0 μM) into rats, deoxycytidine did not pass through the blood-brain barrier at a faster rate than sucrose. [³H]Deoxycytidine, either alone or together with unlabeled deoxycytidine, was infused at a constant rate into conscious adult rabbits. At 130 min, [³H]deoxycytidine readily entered CSF, choroid plexus, and brain. In brain, approx. 60% of the nonvolatile radioactivity was attributable to [³H]deoxycytidine phosphates. The addition of 0.22 mmol/kg unlabeled deoxycytidine to the infusion syringe decreased the phosphorylation of [³H]deoxycytidine in brain by approx. 50%; the addition of 2.2 mmol/kg of unlabeled deoxycytidine to the infusion syringe decreased the relative entry of [³H]deoxycytidine into CSF and brain by approx. 50 and 75%, respectively. Two hours after the intraventricular injection of [³H]deoxycytidine, [³H]deoxycytidine was rapidly cleared from CSF, in part, to brain, where approx. 65% of the [³H]deoxycytidine was converted to [³H]deoxycytidine phosphates. The intraventricular injection of unlabeled deoxycytidine with the [³H]deoxycytidine decreased the phosphorylation of [³H]deoxycytidine in the brain significantly and also decreased the clearance of [³H]deoxycytidine from the CSF. These results were interpreted as showing that the entry of deoxycytidine from blood into CSF occurs by a saturable transport system within the choroid plexus. Once within the CSF, the deoxycytidine can enter brain, undergo phosphorylation to deoxycytidine phosphates, and subsequently be incorporated into DNA.     

Effects of decreased atmospheric deposition on the sulfur budgets of two Dutch moorland pools

The chemical composition of surface waters of two Dutch moorland pools and of incident precipitation, was monitored from 1982 to 1990. For this period, sulfur and water budgets were calculated using a hydrochemical model developed for well-mixed non-stratifying lakes. Total atmospheric deposition of S decreased significantly after 1986 at both locations. A model describing the sulfur budget in terms of input, output and reduction/oxidation processes predicted a fast decrease of pool water SO₄ ²⁻ concentrations after a decrease of atmospheric input. However, SO₄ ²⁻ concentrations in the surface water was lowered only slightly or remained constant. Apparently a source within the lake caused the unexpectedly high SO₄ ²⁻ concentrations. The possible supply of SO₄ ²⁻ from the sediment through regulation by (K-)Al-SO₄ containing minerals or desorption of SO₄ ²⁻ from positively charged surfaces in the sediment was evaluated. Solubility calculations of pore water with respect to alunite, basaluminite and jurbanite indicated that SO₄ ²⁻ concentration was not regulated by these minerals. It is suggested here (1) that desorption of SO₄ ²⁻ from peaty sediments may account for the estimated SO₄ ²⁻ supply provided that the adsorption complex is periodically recharged by partial oxidation of the upper bottom sediments and (2) that because of exposure of a part of the pool bottom to the atmosphere during dry summers and subsequent oxidation of reduced S, the amount of SO₄ ²⁻ may be provided which complements the decreasing depositional SO₄ ²⁻ input. In future research these two mechanisms need to be investigated.     

Sulfate reduction and S-oxidation in a moorland pool sediment

In an oligotrophic moorland pool in The Netherlands, S cycling near the sediment/water boundary was investigated by measuring (1) SO₄ ^2– reduction rates in the sediment, (2) depletion of SO₄ ^2– in the overlying water column and (3) release of³⁵S from the sediment into the water column. Two locations differing in sediment type (highly organic and sandy) were compared, with respect to reduction rates and depletion of SO₄ ^2– in the overlying water.Sulfate reduction rates in sediments of an oligotrophic moorland pool were estimated by diagenetic modelling and whole core³⁵SO₄ ^2– injection. Rates of SO₄ ^2– consumption in the overlying water were estimated by changes in SO₄ ^2– concentration over time in in situ enclosures. Reduction rates ranged from 0.27–11.2 mmol m^–2 d^–1. Rates of SO₄ ^2– uptake from the enclosed water column varied from –0.5, –0.3 mmol m^–2 d^–1 (November) to 0.43–1.81 mmol m^–2 d^–1 (July, August and April). Maximum rates of oxidation to SO₄ ^2– in July 1990 estimated by combination of SO₄ ^2– reduction rates and rates of in situ SO₄ ^2– uptake in the enclosed water column were 10.3 and 10.5 mmol m^–2 d^–1 at an organic rich and at a sandy site respectively.Experiments with³⁵S^2– and³⁵SO₄ ^2– tracer suggested (1) a rapid formation of organically bound S from dissimilatory reduced SO₄ ^2– and (2) the presence of mainly non SO₄ ^2–-S derived from reduced S transported from the sediment into the overlying water. A³⁵S^2– tracer experiment showed that about 7% of³⁵S^2– injected at 1 cm depth in a sediment core was recovered in the overlying water column.Sulfate reduction rates in sediments with higher volumetric mass fraction of organic matter did not significantly differ from those in sediments with a lower mass fraction of organic matter.Corresponding author     

The Active and the Inactive Form of the hAT1 Receptor Have an Identical Ligand-Binding Environment: An MPA Study on a Constitutively Active Angiotensin II Receptor Mutant

Several models of activation mechanisms were proposed for G protein-coupled receptors (GPCRs), yet no direct methods exist for their elucidation. The availability of constitutively active mutants has given an opportunity to study active receptor conformations within acceptable limits using models such as the angiotensin II type 1 (AT₁)¹ receptor mutant N111G-hAT₁ which displays an important constitutive activity. Recently, by using methionine proximity assay, we showed for the hAT₁ receptor that TMD III, VI, and VII form the ligand-binding pocket of the C-terminal amino acid of an antagonistic AngII analogue. In the present contribution, we investigated whether the same residues would also constitute the ligand-binding contacts in constitutively activated mutant (CAM) receptors. For this purpose, the same Met mutagenesis strategy was carried out on the N111G double mutants. Analysis of 43 receptors mutants in the N111G-hAT₁ series, photolabeled and CNBr digested, showed that there were only subtle structural changes between the wt-receptor and its constitutively active form.     

Multifactorial diversity sustains microbial community stability

Maintenance of a high degree of biodiversity in homogeneous environments is poorly understood. A complex cheese starter culture with a long history of use was characterized as a model system to study simple microbial communities. Eight distinct genetic lineages were identified, encompassing two species: Lactococcus lactis and Leuconostoc mesenteroides. The genetic lineages were found to be collections of strains with variable plasmid content and phage sensitivities. Kill-the-winner hypothesis explaining the suppression of the fittest strains by density-dependent phage predation was operational at the strain level. This prevents the eradication of entire genetic lineages from the community during propagation regimes (back-slopping), stabilizing the genetic heterogeneity in the starter culture against environmental uncertainty.     

On the 13C/12C isotopic signal of day and night respiration at the mesocosm level

While there is currently intense effort to examine the ¹³C signal of CO₂ evolved in the dark, less is known on the isotope composition of day‐respired CO₂. This lack of knowledge stems from technical difficulties to measure the pure respiratory isotopic signal: day respiration is mixed up with photorespiration, and there is no obvious way to separate photosynthetic fractionation (pure c_i/c_a effect) from respiratory effect (production of CO₂ with a different δ¹³C value from that of net‐fixed CO₂) at the ecosystem level. Here, we took advantage of new simple equations, and applied them to sunflower canopies grown under low and high [CO₂]. We show that whole mesocosm‐respired CO₂ is slightly ¹³C depleted in the light at the mesocosm level (by 0.2–0.8‰), while it is slightly ¹³C enriched in darkness (by 1.5–3.2‰). The turnover of the respiratory carbon pool after labelling appears similar in the light and in the dark, and accordingly, a hierarchical clustering analysis shows a close correlation between the ¹³C abundance in day‐ and night‐evolved CO₂. We conclude that the carbon source for respiration is similar in the dark and in the light, but the metabolic pathways associated with CO₂ production may change, thereby explaining the different ¹²C/¹³C respiratory fractionations in the light and in the dark.