Erythrocyte antioxidant enzymes in hypertensive patients receiving lisinopril monotherapy or combined lisinopril plus simvastatin therapy

Statins and angiotensin-converting enzyme (ACE) inhibitors have beneficial impact on the serum cholesterol and blood pressure. It is supposed that statins and ACE inhibitors may modify the antioxidative status in erythrocytes. The study objective was to compare the effects of two treatments, lisinopril alone versus lisinopril plus simvastatin, on erythrocyte antioxidant enzyme activities. The study involved 32 patients with arterial hypertension, their initial serum total cholesterol, LDL-cholesterol and triglycerides were within the normal range. Patients of two groups, each of 16 subjects, were treated with lisinopril (10 mg/day) or with lisinopril (10 mg/day) plus simvastatin (20 mg/day). Before and after the ambulatory therapy for 3 and 6 months, activities of superoxide dismutase (SOD), catalase, glutathione peroxidase (GPx), glutathione reductase (GR) were determined in purified erythrocytes. All treated patients had significantly higher catalase activity (by 79.3–106.5%, p < 0.0001) and significantly lower GPx activity (by 20.7–30.6%, p < 0.001) as compared to the baselines. The same results were obtained in both groups (lisinopril and lisinopril + simvastatin), after both periods (3 and 6 month) of treatments. SOD activity increased only in the lisinopril group and only after 6 months (p = 0.0345). No changes of GR activity were observed under all conditions studied. Thus, the lisinopril monotherapy and combined lisinopril plus simvastatin therapy exhibit specific, pronounced and equipotent effects on antioxidant enzymes in human erythrocytes. Peroral administration of lisinopril or lisinopril plus simvastatin may protect erythrocytes and other tissues against oxidative damage.     

Copper modifies the activity of sodium-transporting systems in erythrocyte membrane in patients with essential hypertension

The aim of the study was to verify the hypothesis if copper could influence the activity of sodium-transporting systems in erythrocyte membrane that could be related to essential hypertension. The examined group of patients consisted of 15 men with hypertension. The control group was 11 healthy male volunteers. The Na⁺/H⁺ exchanger (NHE) activity in erythrocytes was determined according to Orlov et al. The activity of transporting systems (ATP-Na⁺/K⁺; co-Na⁺/K⁺/Cl⁻; ex-Na⁺/Li⁺; free Na⁺ and K⁺ outflow [Na⁺, K⁺-outflow]) was determined according to Garay's method. The concentration of copper in plasma was assessed using atomic absorption spectrometry. The activity of ATP-Na⁺/K⁺ (μmol/L red blood cells [RBCs]/h) in hypertensive patients was 2231.5±657.6 vs 1750.5±291 in the control (p<0.05), the activity of co-Na⁺/K⁺/Cl⁻ (μmol/L RBCs/h) in hypertensives was 171.3±77.9 vs 150.7±53.9 in the control (NS). Na⁺-outflow (μmol/L RBCs/h) in hypertensives was 118.3±51.6 vs 113.3±24.4 in the control (NS). The K⁺-outflow (μmol/L RBCs/h) in hypertensives was 1361.7±545.4 vs 1035.6±188.3 in the control (NS). The activity of ex-Na⁺/Li⁺ (μmol/L RBCs/h) in hypertensive patients was 266.1±76.1 vs 204.1±71.6 in the control (p<0.05). NHE activity (mmol/L RBCs/h) in hypertensives was 9.7±2.96 vs 7.7±1.33 in the control (p<0.05). In hypertensive patients, negative correlation was found between the activity of Na⁺/K⁺/Cl⁻ co-transport and plasma copper concentration (R _s=−0.579, p <0.05) and between the activity of ex-Na⁺/Li⁺ and plasma copper concentration (R _s=−0.508, p<0.05). Plasma copper concentration significantly influences the activity of sodium transporting systems in erythrocyte membrane. Copper supplementation could be expected to provide therapeutic benefits for hypertensive patients.     

Cumulative effect of nitrogen and sulphur on <Emphasis Type="Italic">Brassica juncea</Emphasis> L. genotypes under NaCl stress

In the present study, N and S assimilation, antioxidant enzymes activity, and yield were studied in N and S-treated plants of Brassica juncea (L.) Czern. & Coss. (cvs. Chuutki and Radha) under salt stress. The treatments were given as follows: (1) NaCl₉₀ mM+N₀S₀ mg kg^-1 sand (control), (2) NaCl₉₀ mM+N₆₀S₀ mg kg^-1 sand, (3) NaCl₉₀ mM+N₆₀S₂₀ mg kg^-1 sand, (4) NaCl₉₀ mM+N₆₀S₄₀ mg kg^-1 sand, and (5) NaCl₉₀ mM+N₆₀S₆₀ mg kg^-1 sand. The combined application of N (60 mg kg⁻¹ sand) and S (40 mg kg⁻¹ sand) proved beneficial in alleviating the adverse effect of salt stress on growth attributes (shoot length plant⁻¹, fresh weight plant⁻¹, dry weight plant⁻¹, and area leaf⁻¹), physio-biochemical parameters (carbonic anhydrase activity, total chlorophyll, adenosine triphosphate-sulphurylase activity, leaf N, K and Na content, K/Na ratio, activity of nitrate reductase, nitrite reductase, glutamine synthetase, glutamate synthase, catalase, superoxide dismutase, ascorbate peroxidase and glutathione reductase, and content of glutathione and ascorbate), and yield attributes (pods plant⁻¹, seeds pod⁻¹, and seed yield plant⁻¹). Therefore, it is concluded that combined application of N and S induced the physiological and biochemical mechanisms of Brassica. The stimulation of antioxidant enzymes activity and its synergy with N and S assimilation may be one of the important mechanisms that help the plants to tolerate the salinity stress and resulted in an improved yield.     

Effects of cortisol and fluoride on ion-transporting ATPase activities in cultured osteoblastlike cells

Summary Na⁺,K⁺-ATPase, HCO ₃ ⁻ -ATPase, Ca²⁺,Mg²⁺,-ATPase, Ca²⁺-ATPase, and alkaline phosphatase activities were measured in cultures of osteoblastlike cells treated with fluoride and cortisol separately and in combinations. Low concentrations of cortisol increased HCO ₃ ⁻ -ATPase (10⁻¹¹ to 10⁻¹⁸ M cortisol) and alkaline phosphatase (10⁻¹¹ to 10⁻⁹ M cortisol) activities, but higher cortisol concentrations reduced these activities. Na⁺,K⁺-ATPase, Ca²⁺,Mg²⁺-ATPase, and Ca²⁺-ATPase activities tended only to be reduced by cortisol. Fluoride (10⁻⁶ and 5×10⁻⁶ M) increased HCO ₃ ⁻ -ATPase and alkaline phosphatase activities, but these activities were similar to controls in the presence of 10⁻⁵ M fluoride. Ca²⁺,Mg²⁺-ATPase activity was decreased and Na⁺,K⁺-ATPase activity was increased as the concentration of fluoride increased (10⁻⁶ to 10⁻⁵ M). Preliminary experiments with fluoride indicated that lower concentrations (10⁻⁷ M) were without effect. Cortisol concentrations of 10⁻⁹ and 10⁻⁸ M were chosen for studies with combinations of cortisol and fluoride because the effects of these concentrations on alkaline phosphatase activity were opposite, i.e. 10⁻⁹ M increased whereas 10⁻⁸ M decreased activity. Fluoride concentrations of 10⁻⁶, 5×10⁻⁶, and 10⁻⁵ M were chosen because a peak of alkaline phosphatase activity occurred at 5×10⁻⁶ M fluoride. Higher (10⁻⁴ M) and lower (10⁻⁷ M) fluoride concentrations were without effect. The effects of combinations of cortisol and fluoride depend on the enzyme activity measured. Fluoride (10⁻⁶ M) combined with cortisol (10⁻⁹ M) produced a peak of Na⁺,K⁺-ATPase activity. The increased activity obtained with all concentrations of fluoride alone was preserved when fluoride was combined with 10⁻⁸ M cortisol, although the activity tended to be reduced at 5×10⁻⁶ and 10⁻⁵ M fluoride. HCO ₃ ⁻ -ATPase activity was increased by fluoride combined with 10⁻⁸ M cortisol and decreased by fluoride combined with 10⁻⁹ M cortisol compared to the activities obtained with fluoride alone. The decrease in Ca²⁺,Mg²⁺-ATPase activity caused by fluoride alone was prevented by 10⁻⁹ and enhanced by 10⁻⁸ M cortisol, although all treatments produced the same activity at 10⁻⁵ M fluoride. Ca²⁺-ATPase activity tended to be increased by combinations of fluoride and cortisol, but significantly so only at 10⁻⁵ M fluoride in combinations with 10⁻⁸ and 10⁻⁹ M cortisol. Alkaline phosphatase activity was increased by fluoride combined with 10⁻⁹ M cortisol and decreased by fluoride combined with 10⁻⁸ M cortisol compared to the activities obtained with fluoride alone. These results suggest that the abilities of bone cells to regulate ion transport (as reflected in their ion-transporting ATPase activities) are modulated by glucocorticoids and fluoride. Inasmuch as these cells may regulate the ionic composition and concentrations of the bone extracellular fluid (ECF) in vivo, the modulation of their activities by cortisol and fluoride may result in altered bone ECF composition. This work was supported by Grant NAG-2-108 from the National Aeronautics and Space Administration, D.C., and Grant PO1 NS15767 from the National Institute of Neurological and Communicative Disorders and Stroke, Bethesda, MD.     

Theoretical study of N<Subscript>4</Subscript>X (X = O,S, Se) systems

A series of N₄X (X = O, S, Se) compounds have been examined with ab initio and density functional theory (DFT) methods. To our knowledge, these compounds, except for the C_2v ring and the C_3v towerlike isomers of N₄O, are first reported here. The ring structures are the most energetically favored for N₄X (X = O and S) systems. For N₄Se, the cagelike structure is the most energetically favored. Several decomposition and isomerization pathways for the N₄X species have been investigated. The dissociation of C_2v ring N₄O and N₄S structures via ring breaking and the barrier height are only 1.1 and −0.2 kcal mol⁻¹ at the CCSD(T)/6-311+G*//MP2/6-311+G* level of theory. The dissociation of the cagelike N₄X species is at a cost of 12.1–16.2 kcal mol⁻¹. As for the towerlike and triangle bipyramidal isomers, their decomposition or isomerization barrier heights are all lower than 10.0 kcal mol⁻¹. Although the C_S cagelike N₄S isomer has a moderate isomerization barrier (18.3–29.1 kcal mol⁻¹), the low dissociation barrier (−1.0 kcal mol⁻¹) indicates that it will disappear when going to the higher CCSD(T) level. Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

Effect of L-carnitine against acute mitoxantrone toxicity in mice

Various experiments were performed in our laboratory to define a possible role for carnitine derivatives in mitoxantrone (MX) therapy. We report here the results of the effect of L-carnitine (LCAR) on the lethal toxicity of MX in mice. MX was administered intravenously at doses of 7, 9, 11, 13, 15 or 17 mg kg⁻¹ either alone or in combination with LCAR at a single intravenous dose of 200 mg kg⁻¹. The dependence of the probability of death on various doses was evaluated for the MX-LCAR combination compared to MX alone. From these experiments, the following lethal dose fifty (LD₅₀) values were calculated: LD₅₀ for MX alone was 15.2 mg kg⁻¹, whereas in combination with LCAR it increases to 21.8 mg kg⁻¹. The relative toxicity given as the ratio of the LD50 of both MX alone and the combination of MX-LCAR was 69.7%. The results of our experiments unequivocally show the effect of LCAR on acute toxic doses of MX.     

Influence of sodium fluoride and caffeine on the concentration of fluoride ions, glucose, and urea in blood serum and activity of protein metabolism enzymes in rat liver

The aim of the study was examining the effect of fluoride ions and caffeine administration on glucose and urea concentration in blood serum and the activity of protein metabolism enzymes and selected enzymes of the urea cycle in rat liver. The study was carried out using 18 male Sprague-Daowley rats (4.5 mo old). Rats were divided into three groups. Group I received distilled water ad libitum. Group II received 4.9 mg F⁻/kg body mass/d of sodium fluoride in the water, and group III received sodium fluoride (in the above-mentioned dose) and 3 mg/kg body mass/d of caffeine in the water. After 50 d, the rats were anesthetized with thiopental and fluoride ions, glucose, and urea concentration in blood serum were determined. Also determined were the activities of aspartate aminotransferase, alanine aminotransferase glutamate dehydrogenase, ornithine carbamoylotransferase and arginase in liver homogenates. Liver was taken for pathomorphological examinations. The applied doses of F⁻ (4.9 mg/kg body mass/d) and F⁻+ caffeine (4.9 mg F⁻/kg body mass/d+3 mg caffeine/kg body mass/d) resulted in a statistically significant increase of fluoride ion concentration in blood serum, a slight increase of the glucose concentration, and no changes in the concentration of urea in blood serum. This might testify to the absence of kidney lesions for the applied concentrations of F⁻. No change in the functioning of hepatocytes was observed; however, slight disturbances have been noted in the functioning of the liver, connected with the activation of urea cycle, increase of arginase activity, and accumulation of F⁻ in this organ. There was no observed significant influence of caffeine supplementation on the obtained results.     

The role of GA,IAA and BAP in the regulation of <Emphasis Type="Italic">in vitro</Emphasis> shoot growth and microtuberization in potato

The effect of auxin, GA and BAP on potato shoot growth and tuberization was investigated under in vitro condition. The shoot length of potato explants increased with the increasing of concentrations (0.5 – 10 mg dm⁻³) of IAA treatment especially with the addition of GA₃ (0.5 mg dm⁻³), but was inhibited by BAP (5 mg dm⁻³). The root number and root fresh weight of potato explants increased with the increasing of IAA levels either in the presence of GA₃ (treatment IAA+GA) or not (IAA alone). However, no root was observed in the treatment IAA+BAP, instead there were brown swollen calli formed around the basal cut surface of the explants. The addition of GA₃ remarkably increased the fresh weight and diameter of calli. Microtubers were formed in the treatments of IAA+BAP and IAA + GA + BAP but not observed in the treatments of IAA alone or IAA + GA. IAA of higher concentrations (2.5 – 10 mg dm⁻³) was helpful to form sessile tubers. With the increasing of IAA levels, the fresh weight and diameter of microtubers increased progressively. At 10 mg/L IAA, the fresh weight and diameter of microtubers in the treatment of IAA + GA + BAP were 409.6 % and 184.4 % of that in the treatment of IAA + BAP respectively, indicating the interaction effect of GA and IAA in potato microtuberization.     

Spatial and Temporal Variability in Sediment Denitrification Within an Agriculturally Influenced Reservoir

Reservoirs are intrinsically linked to the rivers that feed them, creating a river–reservoir continuum in which water and sediment inputs are a function of the surrounding watershed land use. We examined the spatial and temporal variability of sediment denitrification rates by sampling longitudinally along an agriculturally influenced river–reservoir continuum monthly for 13 months. Sediment denitrification rates ranged from 0 to 63 μg N₂O g ash free dry mass of sediments (AFDM)⁻¹ h⁻¹ or 0–2.7 μg N₂O g dry mass of sediments (DM)⁻¹ h⁻¹ at reservoir sites, vs. 0–12 μg N₂O gAFDM⁻¹ h⁻¹ or 0–0.27 μg N₂O gDM⁻¹ h⁻¹ at riverine sites. Temporally, highest denitrification activity traveled through the reservoir from upper reservoir sites to the dam, following the load of high nitrate (NO₃⁻-N) water associated with spring runoff. Annual mean sediment denitrification rates at different reservoir sites were consistently higher than at riverine sites, yet significant relationships among theses sites differed when denitrification rates were expressed per gDM vs. per gAFDM. There was a significant positive relationship between sediment denitrification rates and NO₃⁻-N concentration up to a threshold of 0.88 mg NO₃⁻ -N l⁻¹, above which it appeared NO₃⁻-N was no longer limiting. Denitrification assays were amended seasonally with NO₃⁻-N and an organic carbon source (glucose) to determine nutrient limitation of sediment denitrification. While organic carbon never limited sediment denitrification, all sites were significantly limited by NO₃⁻-N during fall and winter when ambient NO ₃⁻-N was low.     

Denitrification,dissimilatory nitrate reduction to ammonium,and nitrogen fixation along a nitrate concentration gradient in a created freshwater wetland

Wetlands are often highly effective nitrogen (N) sinks. In the Lake Waco Wetland (LWW), near Waco, Texas, USA, nitrate (NO₃⁻) concentrations are reduced by more than 90% in the first 500 m downstream of the inflow, creating a distinct gradient in NO₃⁻ concentration along the flow path of water. The relative importance of sediment denitrification (DNF), dissimilatory NO₃⁻ reduction to ammonium (DNRA), and N₂ fixation were examined along the NO₃⁻ concentration gradient in the LWW. “Potential DNF” (hereafter potDNF) was observed in all months and ranged from 54 to 278 μmol N m⁻² h⁻¹. “Potential DNRA” (hereafter potDNRA) was observed only in summer months and ranged from 1.3 to 33 μmol N m⁻² h⁻¹. Net N₂ flux ranged from 184 (net denitrification) to −270 (net N₂ fixation) μmol N m⁻² h⁻¹. Nitrogen fixation was variable, ranging from 0 to 426 μmol N m⁻² h⁻¹, but high rates ranked among the highest reported for aquatic sediments. On average, summer potDNRA comprised only 5% (±2% SE) of total NO₃⁻ loss through dissimilatory pathways, but was as high as 36% at one site where potDNF was consistently low. Potential DNRA was higher in sediments with higher sediment oxygen demand (r ² = 0.84), and was related to NO₃⁻ concentration in overlying water in one summer (r ² = 0.81). Sediments were a NO₃⁻ sink and accounted for 50% of wetland NO₃⁻ removal (r ² = 0.90). Sediments were an NH₄⁺ source, but the wetland was often a net NH₄⁺ sink. Although DNRA rates in freshwater wetlands may rival those observed in estuarine systems, the importance of DNRA in freshwater sediments appears to be minor relative to DNF. Furthermore, sediment N₂ fixation can be extremely high when NO₃⁻ in overlying water is consistently low. The data suggest that newly fixed N can support sustained N transformation processes such as DNF and DNRA when surface water inorganic N supply rates are low.     

Effects of the interaction between ozone and carbon dioxide on gas exchange,photosystem II and antioxidants in rice leaves

To understand the interactive effects of O₃ and CO₂ on rice leaves; gas exchange, chlorophyll (Chl) fluorescence, ascorbic acid and glutathione were examined under acute (5 h), combined exposures of O₃ (0, 0.1, or 0.3 cm³ m⁻³, expressed as O₀, O_0.1, or O_0.3, respectively), and CO₂ (400 or 800 cm³ m⁻³, expressed as C⁴⁰⁰ or C⁸⁰⁰, respectively) in natural-light gas-exposure chambers. The net photosynthetic rate (P _N), maximum (F_v/F_m) and operating (F_q′/F_m′) quantum efficiencies of photosystem II (PSII) in young (8^th) leaves decreased during O₃ exposure. However, these were ameliorated by C⁸⁰⁰ and fully recovered within 3 d in clean air (O⁰ + C⁴⁰⁰) except for the O^0.3 + C⁴⁰⁰ plants. The maximum PSII efficiency at 1,500 μmol m⁻² s⁻¹ PPFD (F_v′/F_m′) for the O^0.3 + C₄₀₀ plants decreased for all measurement times, likely because leaves with severely inhibited P _N also had a severely damaged PSII. The P _N of the flag (16^th) leaves at heading decreased under O₃ exposure, but the decline was smaller and the recovery was faster than that of the 8^th leaves. The F_q′/F_m′ of the flag leaves in the O^0.3 + C⁴⁰⁰ and O^0.3 + C⁸⁰⁰ plants decreased just after gas exposure, but the F_v/F_m was not affected. These effects indicate that elevated CO₂ interactively ameliorated the inhibition of photosynthesis induced by O₃ exposure. However, changes in antioxidant levels did not explain the above interaction.     

Seasonal variation in the nitrogenase activity of aPanicum maximum var.trichoglume pasture and identification of associated bacteria

Summary The influence of seasonal variation on nitrogenase (N₂-ase) activity of undisturbed soil-plant cores ofPanicum maximum var.trichoglume was measured using the C₂H₂ reduction assay. The largest N₂-ase activity in the field, 14.7 g N ha⁻¹ day⁻¹, occurred in spring when soil moisture was high, soil temperature was low and nitrogenous fertiliser influence was at a minimum. The potential N₂-ase activity of the cores, measured under controlled conditions, reached a maximum of 27.2 g N ha⁻¹ day⁻¹ and averaged 26.3 g N ha⁻¹ day⁻¹ over the 14 month sampling period. N₂-ase activity was positively correlated (P=0.05) with field soil moisture and negatively correlated with field soil temperature (r=0.59 and −0.78 respectively). Multiple regression showed that 69% of the variation of N₂-ase activity in the field was associated with the combined effects of soil moisture and soil temperature. Nitrogen fixing bacteria were isolated from the roots ofP. maximum and based upon morphology, biochemical tests and fluorescent antibody reaction, were found to be closely related toAzospirillum lipoferum.     

N2O, CH4 and CO2 emissions from seasonal tropical rainforests and a rubber plantation in Southwest China

The main focus of this study was to evaluate the effects of soil moisture and temperature on temporal variation of N₂O, CO₂ and CH₄ soil-atmosphere exchange at a primary seasonal tropical rainforest (PF) site in Southwest China and to compare these fluxes with fluxes from a secondary forest (SF) and a rubber plantation (RP) site. Agroforestry systems, such as rubber plantations, are increasingly replacing primary and secondary forest systems in tropical Southwest China and thus effect the N₂O emission in these regions on a landscape level. The mean N₂O emission at site PF was 6.0 ± 0.1 SE μg N m⁻² h⁻¹. Fluxes of N₂O increased from <5 μg N m⁻² h⁻¹ during dry season conditions to up to 24.5 μg N m⁻² h⁻¹ with re-wetting of the soil by the onset of first rainfall events. Comparable fluxes of N₂O were measured in the SF and RP sites, where mean N₂O emissions were 7.3 ± 0.7 SE μg N m⁻² h⁻¹ and 4.1 ± 0.5 SE μg N m⁻² h⁻¹, respectively. The dependency of N₂O fluxes on soil moisture levels was demonstrated in a watering experiment, however, artificial rainfall only influenced the timing of N₂O emission peaks, not the total amount of N₂O emitted. For all sites, significant positive correlations existed between N₂O emissions and both soil moisture and soil temperature. Mean CH₄ uptake rates were highest at the PF site (−29.5 ± 0.3 SE μg C m⁻² h⁻¹), slightly lower at the SF site (−25.6 ± 1.3 SE μg C m⁻² h⁻¹) and lowest for the RP site (−5.7 ± 0.5 SE μg C m⁻² h⁻¹). At all sites, CH₄ uptake rates were negatively correlated with soil moisture, which was also reflected in the lower uptake rates measured in the watering experiment. In contrast to N₂O emissions, CH₄ uptake did not significantly correlate with soil temperature at the SF and RP sites, and only weakly correlated at the PF site. Over the 2 month measurement period, CO₂ emissions at the PF site increased significantly from 50 mg C m⁻² h⁻¹ up to 100 mg C m⁻² h⁻¹ (mean value 68.8 ± 0.8 SE mg C m⁻² h⁻¹), whereas CO₂ emissions at the SF and RP site where quite stable and varied only slightly around mean values of 38.0 ± 1.8 SE mg C m⁻² h⁻¹ (SF) and 34.9 ± 1.1 SE mg C m⁻² h⁻¹ (RP). A dependency of soil CO₂ emissions on changes in soil water content could be demonstrated for all sites, thus, the watering experiment revealed significantly higher CO₂ emissions as compared to control chambers. Correlation of CO₂ emissions with soil temperature was significant at the PF site, but weak at the SF and not evident at the RP site. Even though we demonstrated that N and C trace gas fluxes significantly varied on subdaily and daily scales, weekly measurements would be sufficient if only the sink/ source strength of non-managed tropical forest sites needs to be identified.     

Relationship between synovial fluid and plasma manganese,arginase, and nitric oxide in patients with rheumatoid arthritis

Nitric oxide (NO) participates in the pathogenesis of inflammatory reactions in many autoimmune diseases such as rheumatoid arthritis (RA). There is a reciprocal pathway between arginase and nitric oxide synthese (NOS) for NO production, and Mn is required for arginase activity and stability. To investigate whether NO production related with the arginine-nitric oxide pathway in patients with RA, we measured synovial fluid and plasma nitrite (NO_x) levels, arginase activities, and its cofactor manganese (Mn) concentrations in 21 RA patients and 13 healthy control subjects. Plasma albumin levels were measured as an index of nutritional status. NO_x levels were determined after the reduction of nitrates to nitrites using the Griess reaction. Whereas, synovial fluid arginase activities and Mn levels were found to be significantly lower (p<0.001, p<0.001, respectively), plasma arginase activities and Mn levels were similar in patients with RA when compared to the control subjects. Plasma and synovial fluid NO levels were similar in patients with RA and in healthy subjects (p>0.05, p>0.05, respectively). There were significantly positive correlations between synovial fluid and plasma arginase activities vs Mn content (r=0.543, p=0.011; r=0.516, p=0.017, respectively) and significantly negative correlations between synovial fluid and plasma NO levels vs arginase activities (r=−0.497, p=0.022; r=−0.508, p=0.019 respectively) in the patients group. Our results indicate that the lower concentration of synovial fluid Mn could cause lower arginase activity and this could also upregulate NO production by increasing L-arginine content in patients with RA.     

Isotopic signature of nitrate in two contrasting watersheds of Brush Brook,Vermont, USA

We used the dual isotope method to study differences in nitrate export in two subwatersheds in Vermont, USA. Precipitation, soil water and streamwater samples were collected from two watersheds in Camels Hump State Forest, located within the Green Mountains of Vermont. These samples were analyzed for the δ¹⁵N and δ¹⁸O of NO₃⁻. The range of δ¹⁵N–NO₃⁻ values overlapped, with precipitation −4.5‰ to +2.0‰ (n = 14), soil solution −10.3‰ to +6.2‰ (n = 12) and streamwater +0.3‰ to +3.1‰ (n = 69). The δ¹⁸O of precipitation NO₃⁻ (mean 46.8 ± 11.5‰) was significantly different (P < 0.001) from that of the stream (mean 13.2 ± 4.3‰) and soil waters (mean 14.5 ± 4.2‰) even during snowmelt periods. Extracted soil solution and streamwater δ¹⁸O of NO₃⁻ were similar and within the established range of microbially produced NO₃⁻, demonstrating that NO₃⁻ was formed by microbial processes. The δ¹⁵N and δ¹⁸O of NO₃⁻ suggests that although the two tributaries have different seasonal NO₃⁻ concentrations, they have a similar NO₃⁻ source.     

Phytotoxic effects of Cu, Zn, Cd and Pb on in vitro regeneration and concomitant protein changes in Holarrhena antidysenterica

The nodal explants of in vitro shoots of Holarrhena antidysenterica L. were cultured on Murashige and Skoog's (MS) medium augmented with 15 μM N⁶-benzyladenine (BA) alone (control) or supplemented with different concentrations (1, 5, 10 and 20 mg dm⁻³) of CdCl₂, CuSO₄, Pb(NO₃)₂ and ZnSO₄. The maximum morphogenic response in terms of average shoot number (4.95 ± 0.17) was seen in control. ZnSO₄ proved to be less inhibitory in comparison to CuSO₄, Pb(NO₃)₂ and CdCl₂. None of the explants cultured on CdCl₂ containing medium induced multiple shoots. Maximum protein content [3.80 ± 0.04 mg g⁻¹(f.m.)] was observed in control and slightly less [3.50 ± 0.02 mg g⁻¹(f.m.)] in tissues exposed to 1 mg dm⁻³ of CuSO₄ and minimum [1.00 ± 0.02 mg g⁻¹(f.m.)] in Zn treated (20 mg dm⁻³) explants. SDS-PAGE analysis of the treated tissues revealed that two new polypeptides (29 and 20 kDa) in response to Cu and Zn treatment, respectively, have been synthesized.     

Catalysis on dinuclear Mn(II) centers: hydrolytic and redox activities of rat liver arginase

 Rat liver arginase contains a dinuclear Mn₂(II,II) center in each subunit having EPR properties similar to those observed in Mn-catalases. The principal physiologic role of arginase is catalyzing the hydrolytic cleavage of l-arginine to produce l-ornithine and urea. Here we demonstrate that arginase catalyzes the disproportionation of hydrogen peroxide by a redox mechanism analogous to Mn-catalases, but at rates that are 10^–5 to 10^–6 of k _cat for the Mn-catalases, and also exhibits peroxidase activity. The dinuclear Mn₂(II,II) center is essential for maximal catalase activity, since both the H101N and H126N mutant arginases containing only one Mn(II)/subunit have catalase activities that are <3% of that for the wild-type enzyme. Like the Mn-catalases, the catalase activity of arginase is not inhibited by millimolar concentrations of CN^–, the most potent inhibitor of heme catalases, or by EDTA, a chelator of free metal ions. The catalase activity of arginase is not significantly inhibited by Cl^– or F^–, in contrast to Mn-catalases, while potent inhibitors of the hydrolytic activity are also effective inhibitors of the catalase activity. These results suggest that lower affinity of hydrogen peroxide to the active site of arginase contributes to the lower catalase activity. EPR spectroscopy reveals that potent inhibitors of the hydrolytic reaction, including N ^ω-hydroxy-l-arginine, l-lysine, and l-valine, decouple the electronic interaction between the Mn²⁺ ions, most probably by removing a μ-bridging ligand or by increasing the intermanganese separation. The capacity for arginase to deliver a hydroxide ion to hydrolyze the l-arginine substrate is suggested to arise from a "dinuclear effect", wherein the two metal ions contribute more or less equivalently in deprotonation of metal-bound water molecule. Structure-reactivity analyses of these reactions will provide insights into the factors that control redox versus hydrolytic function in dimanganese clusters. Received: 18 November 1996 / Accepted: 7 April 1997     

Importance of point sources on regional nitrous oxide fluxes in semi-arid steppe of Inner Mongolia, China

The aim of the present work was to estimate the contribution of different point and diffuse sources to the regional N₂O emission strength of steppe in the Xilin river catchment, Inner Mongolia, People’s Republic of China. Transect studies showed that the topographic effect on N₂O emissions from upland soils was negligible and that upland steppe is only a very weak net source of N₂O during the growing season (0.8 ± 0.4 μg N₂O–N m⁻² h⁻¹). Slightly higher emissions were found for riparian areas (1.8 ± 0.3 μg N₂O–N m⁻² h⁻¹), which cover ∼4% of the landscape. Even faeces or urine additions stimulated N₂O emissions from steppe soils only weakly (<2.5 μg N₂O–N m⁻² h⁻¹ for a 5 days period). Due to low moisture contents, N₂O emissions from dung heaps were also rather low (6.2 ± 0.8 μg N₂O–N kg⁻¹ dry matter h⁻¹). In contrast, three orders of magnitude higher N₂O emissions were found at sheepfolds (2.45 mg N₂O–N m⁻² h⁻¹ on average). By calculating N₂O emissions on a landscape scale, we show that point sources, and especially sheepfolds, become the dominating regional N₂O source during the growing season if stocking rates are >1 sheep ha⁻¹. Our results indicate that the common grazing management in the Xilin river region leads to a translocation of nitrogen from large source areas towards defined spots. This finding is further supported by measurements of NH₃ concentrations at different sites. Since most of the nitrogen accumulated in these hot spots is finally lost through burning of the dried excrements by the farmers for heating and cooking purposes, the ecosystem faces a significant human perturbation of regional N cycling, which may contribute to an accelerated degradation of steppe in the Xilin river region. Responsible Editor: Per Ambus.     

Anion-selectivity of the Swelling-activated Osmolyte Channel in Eel Erythrocytes

Osmotic swelling of fish erythrocytes activates a broad-specificity permeation pathway that mediates the volume-regulatory efflux of taurine and other intracellular osmolytes. This pathway is blocked by inhibitors of the erythrocyte band 3 anion exchanger, raising the possibility that band 3 is involved in the volume-regulatory response. In this study of eel erythrocytes, a quantitative comparison of the pharmacology of swelling-activated taurine transport with that of band 3-mediated SO²⁻ ₄ transport showed there to be significant differences between them. N-ethylmaleimide and quinine were effective inhibitors of swelling-activated taurine transport but caused little, if any, inhibition of band 3. Conversely, DIDS was a more potent inhibitor of band 3-mediated SO²⁻ ₄ flux than of swelling-activated taurine transport. In cells in isotonic medium, pretreated then co-incubated with 0.1 mm DIDS, the band 3-mediated transport of SO²⁻ ₄ and Cl⁻ was reduced to a low level. Exposure of these cells to a hypotonic medium containing 0.1 mm DIDS was followed by the activation of a Cl⁻ permeation pathway showing the same inhibitor sensitivity as swelling-activated taurine transport. The data are consistent with swelling-activated transport of taurine and Cl⁻ being via a common pathway. A comparison of the swelling-activated transport rates for taurine and Cl⁻ with those for several other solutes was consistent with the hypothesis that this pathway is an anion-selective channel, similar to those that mediate the volume-regulatory efflux of Cl⁻ and organic osmolytes from mammalian cells. Received: 7 July 1995/Revised: 2 September 1995     

Metallopeptide-promoted inactivation of angiotensin-converting enzyme and endothelin-converting enzyme 1: toward dual-action therapeutics

A series of metallopeptides based on the amino terminal copper/nickel (ATCUN) binding motif have been evaluated as classical inhibitors and catalytic inactivators of both rabbit and human angiotensin-converting enzyme (hACE), and human endothelin-converting enzyme 1 (hECE-1). The cobalt complex [KGHK–Co(NH₃)₂]²⁺, where KGHK is lysylglycylhistidyllysine, displayed similar K _I and IC₅₀ values to those found for [KGHK–Cu]⁺, in spite of the enhanced charge, and so either the influence of charge is offset by the steric influence of the axially coordinated ammine ligands, or binding is dominated by contributions from the amino acid side chains, especially the C-terminal lysine that mimics the binding pattern observed for lisinopril. Moreover, the inhibition observed for [KGHK–Co(NH₃)₂]²⁺ contrasts with the activation of hACE by Co²⁺(aq), reflecting the stimulation of enzyme activity following replacement of the catalytic zinc cofactor by cobalt ion at each of the two active sites. Quantitative analysis of the dose-dependent stimulation of activity by Co²⁺(aq) yielded apparent affinities of 1.3 ± 0.2 and 56 ± 8 μM for the two sites in the presence of saturating Zn²⁺ (10 μM). Catalytic inactivation of hACE by [KGHK–Cu] ⁺ at subsaturating concentrations had previously been characterized, with k _obs = 2.9 ± 0.5 × 10⁻² min⁻¹. Under similar conditions, the same complex is found to catalytically inactivate hECE-1, with k _obs = 2.12 ± 0.16 × 10⁻² min⁻¹, demonstrating the potential for dual-action activity against two key drug targets in cardiovascular disease. Irreversible inactivation of a drug target represents a novel mechanism of drug action that complements existing classical inhibitor strategies that underlie current drug discovery efforts.Electronic Supplementary Material Supplementary material is available to authorized users in the online version of this article at .