Cations and Anions as Modifiers of Ryanodine Binding to the Skeletal Muscle Calcium Release Channel

Rate and equilibrium measurements of ryanodine binding to terminal cysternae fractions of heavy sarcoplasmic reticulum vesicles demonstrate that its activation by high concentrations of monovalent salts is based on neither elevated osmolarity nor ionic strength. The effect of the ions specifically depends on their chemical nature following the Hofmeister ion series for cations (Li⁺ < NH⁺ ₄ < K⁻∼ Cs⁺≤ Na⁺) and anions (gluconate⁻ < Cl⁻ < NO₃ ⁻∼ ClO₄ ⁻∼ SCN⁻) respectively, indicating that both are involved in the formation of the salt-protein complex that can react with ryanodine. Activation by rising salt concentrations exhibits saturation kinetics with different dissociation constants (25–11 m) and different degrees of cooperativity (n= 1.5–4.0) for the respective salts. Maximal second order binding rates between 40,000 and 80,000 (m ⁻¹· sec⁻¹) were obtained for chlorides and nitrates of 1a group alkali ions with the exception of lithium supporting only rates of maximally 10,000 (M⁻¹· sec⁻¹). The nitrogen bases, NH⁺ ₄ and Tris⁺, in combination with chloride or nitrate, behave divergently. High maximal binding rates were achieved only with NH₄NO₃. The dissociation constants for the ryanodine–protein complexes obtained by measurements at equilibrium proved to depend differently on salt concentration, yet, converging to 1–3 nm for the applied salts at saturating concentrations. The salts do not affect dissociation of the ryanodine protein complex proving that the effect of salts on the protein's affinity for ryanodine is determined by their effect on the on-rate of ryanodine binding. ATP and its analogues modify salt action resulting in elevated maximal binding rates and reduction or abolition of binding cooperativity. Linear relations have been obtained by comparing the rates of ryanodine binding at different salt concentrations with the rates or the initial amplitudes (15 sec) of salt induced calcium release from actively loaded heavy vesicles indicating that the various salts promote specifically and concentration dependently channel opening and its reaction with ryanodine. Received: 9 February 1998/Revised: 24 April 1998     

NH4 + induces antioxidant cellular machinery and provides resistance to salt stress in citrus plants

Key message

NH ₄ ⁺ acts as a mild oxidative stressor, which triggers antioxidant cellular machinery and provide resistance to salinity.

Abstract

NH₄ ⁺ nutrition in Carrizo citrange (Citrus sinensis L. Osbeck × Poncirus trifoliata L) plants acts as an inducer of resistance against salinity conditions. NH₄ ⁺ treatment triggers mild chronic stress that primes plant defence responses by stress imprinting and confers protection against subsequent salt stress. In this work, we studied the influence of NH₄ ⁺ nutrition on antioxidant enzymatic activities and metabolites involved in detoxification of reactive oxygen species (ROS) to clarify their involvement in NH₄ ⁺-mediated salt resistance. Our results showed that NH₄ ⁺ nutrition induces in citrus plants high levels of H₂O₂, strongly inhibits superoxide dismutase (SOD) and glutathione reductase (GR) activities, and leads to higher content of oxidised glutathione (GSSG) than in control plants in the absence of salt, thus providing evidence to confirm mild stress induced by NH₄ ⁺ nutrition. However, upon salinity, plants grown with NH₄ ⁺ (N-NH₄ ⁺ plants) showed a reduction of H₂O₂ levels in parallel to an increase of catalase (CAT), SOD, and GR activities compared with the control plants. Moreover, N-NH₄ ⁺ plants were able to keep high levels of reduced glutathione (GSH) upon salinity and were able to induce glutathione-S-transferase (GST) and phospholipid hydroperoxide glutathione peroxidise (PHGPx) mRNA accumulation. Based on this evidence, we confirm that sublethal concentrations of NH₄ ⁺ might act as a mild oxidative stressor, which triggers antioxidant cellular machinery that can provide resistance to subsequent salt stress.     

Enhancement of cyanobacterial salt tolerance by combined nitrogen

Presence of certain nitrogenous compounds in the growth medium significantly enhanced the salt tolerance of the fresh-water cyanobacterium Anabaena sp. strain L-31 as well as the brackish water cyanobacterium Anabaena torulosa. Among these, nitrate, ammonium, and glutamine were most effective followed by glutamate and aspartate. These nitrogenous compounds also inhibited Na⁺ influx in both Anabaena spp. with the same order of effectiveness as that observed for protection against salt stress. The inhibition of Na⁺ influx on addition of the nitrogenous substances was rapid; nitrate and ammonium inhibited Na⁺ influx competitively. Proline and glycine did not affect Na⁺ influx and also had no influence on the salt tolerance of either Anabaena sp. The observed protection was not consequent to a stimulatory effect of combined nitrogen on growth per se. Uptake of NO₃⁻ and NH₄⁺ increased during salt stress but was not correlated with growth. Intracellular levels of NO₃⁻ and NH₄⁺ were found to be inadequate to constitute a major component of the internal osmoticum. The results suggest that inhibition of Na⁺ influx by combined nitrogen is a major mechanism for protection of cyanobacteria against salt stress.     

The kinetics and mechanism of the reaction of 2′-deoxy-5′-guanosinemonophosphoric acid and the diaqua form of cis-platin

2′-Deoxy-5′-guanosinemonosphoric acid (B) reacts with cis-[Pt(NH₃)₂(OH₂)₂]²⁺ in two steps to form the cis-[Pt(NH₃)₂B₂]^y+ ion. In the first step 2′-d-5′- GMPH₂ reacts some ten times faster than 5′-GMPH₂ does. Rate constants, ΔH^#, ΔS^# and ΔV^# are very similar for the two bases in the second reaction. It is proposed that the product in the first step contains no water and is cis-[Pt(NH₃)₂B]^x+ in which the nucleobase is bidentate bonding through both N(7) of guanine and an oxygen atom of the phosphate group.     

Effects of hydroxylamine and silicomolybdate on the decay in delayed light emission in the 6–100 μs range after a single 10 ns flash in pea thylakoids

Measurements are reported on μs delayed light emission, following a single 10 ns excitation flash, in Alaska pea thylakoids treated with hydroxylamine (NH₂OH) or with silicomolybdate.

1. In thylakoids treated with 2 mM NH₂OH in the light, or in the dark, the quantum yield of delayed light emission is considerably enhanced. A 10 μs lifetime component of delayed light emission is not significantly changed, whereas a 50–70 μs lifetime component is increased. MnCl₂ and diphenylcarbazide are unable to reverse the above effects of NH₂OH treatment. Thus Mn²⁺ and diphenylcarbazide must not donate electrons directly to reaction center II but on the oxygen-evolution side of the NH₂OH block.
2. When the closed form of photosystem II reaction centers (P₆₈₀Q^-), where P₆₈₀ is the reaction center chlorophyll and Q is a ‘stable’ electron acceptor, is generated by preillumination of NH₂OH-treated thylakoids with diuron present, the μs delayed light emission is inhibited, but a low level residual delayed light emission remains. Possible origins of this emission are discussed. It is believed that the best explanation for residual DLE is the existence of another acceptor besides Q that partakes in charge separation and rapid dissipative recombination when the reaction center is in the P₆₈₀Q^- state.
3. The quantum yield of delayed light emission from ‘closed’ reaction centers (P₆₈₀ ⁺Q^-) that have all charge stabilization reactions (i.e., flow of electrons to P₆₈₀ ⁺ and out of Q^-) blocked by NH₂OH treatment and addition of diuron is 1.1×10^-3 for components measured in a range from 6 to 400 μs and extrapolated to zero time.
4. The addition of silicomolybdate, which accepts electron from Q^-, causes delayed light emission in the μs range to be greatly inhibited.

     

The effect of environmental ammonia concentrations on the ion-exchange of shore crabs,Carcinus maenas (L.)

1. Ion exchange characteristics (ion-permeability, net, passive and active ion fluxes) of adult shore crabs were studied in relation to experimentally-increased external ammonia concentrations.2. Moderately-elevated ammonia concentrations (up to about 1 mmol/1 NH₄⁺) induce an increase in the ion permeability and the salt fluxes across the body wall of Carcinus maenas. At still higher NH₄⁺ concentrations, ion-permeability and ion fluxes are reduced again.3. Active salt influx generally follows the same pattern as observed for whole animal permeability, probably because both parameters are strongly related to gill perfusion and gill ventilation.4. Prolonged exposure to elevated ammonia concentrations in the environment is unfavourable, not because of the NH₄⁺ toxicity, but because of the higher energy requirements associated with the higher salt fluxes.     

THE PENETRATION OF THE MEMBRANE OF BRAIN MITOCHONDRIA BY ANIONS

The permeability of the membrane of rat brain non-synaptosomal mitochondria, towards inorganic and substrate anions, was assessed by measuring the rate of swelling that occurred when mitochondria were suspended in an iso-osmotic solution of a permeant anion, in the presence of a permeant cation such as NH⁺₄ or K⁺ in the presence or absence of valinomycin. In NH⁺₄-phosphate swelling was higher than it was in KCI or K⁺-phosphate, which showed the prevalence of the mechanism of phosphate transport previously demonstrated in liver mitochondria. The entry of succinate and L-malate seemed to require the presence in the inner mitochondrial membrane of specific carriers. as previously postulated for liver mitochondria, but the rate of swelling of brain mitochondria was lower than that of liver organelles. In K⁺-succinate, in the presence of antimycin, added ATP induced swelling and this was attributable to the simultaneous permeation both of the anion and the cation. Fumarate did not penetrate into brain mitochondria. Practically no swelling was recorded in NH⁺₄ or K⁺-citrate, which indicated that this anion penetrated poorly into the isolated brain mitochondria even in the presence of malate. Swelling occurred in NH⁺₄-L-glutamate in the presence of rotenone, and the entry of this anion seemed to follow a gradient of concentration although the presence of a specific translocator in the inner mitochondrial membrane might be concerned. The entry of glutamate was independent of that of phosphate and N-ethylmaleimide appeared to be a specific inhibitor of this entry. Swelling in K⁺-L-glutamate, in the presence of rotenone, was enhanced by the addition of valinomycin or ATP but in the latter case when osmotic equilibrium was reached swelling was not reversed by oligomycin. In conclusion, the lesser extent of swelling of isolated brain mitochondria compared with liver mitochondria could be attributed to the heterogeneity of the populations of these organelles, each population possessing its own characteristics of membrane permeability. Observations of electron micrographs of brain mitochondria incubated in iso-osmotic substrate anions confirmed the heterogeneous rate of swelling of these particles.     

Glutamate dehydrogenase in developing endosperm, chloroplasts, and roots of castor bean

All the glutamate dehydrogenase activity in developing castor bean endosperm is shown to be located in the mitochondria. The enzyme can not be detected in the plastids, and this is probably not due to the inactivation of an unstable enzyme, since a stable enzyme can be isolated from castor bean leaf chloroplasts. The endosperm mitochondrial glutamate dehydrogenase consists of a series of differently charged forms which stain on polyacrylamide gel electrophoresis with both NAD⁺ and NADP⁺. The chloroplast and root enzymes differ from the endosperm enzyme on polyacrylamide gel electrophoresis. The amination reaction of all the enzymes is affected by high salt concentrations. For the endosperm enzyme, the ratio of activity with NADH to that with NADPH is 6.3 at 250 millimolar NH₄Cl and 1.5 at 12.5 millimolar NH₄Cl. K_m values for NH₄⁺ and NAD(P)H are reduced at low salt concentrations. The low K_m values for the nucleotides may favor a role for glutamate dehydrogenase in ammonia assimilation in some situations.     

Demonstration of Both a Photosynthetic and a Nonphotosynthetic CO(2) Requirement for NH(4) Assimilation in the Green Alga Selenastrum minutum

Nitrogen-limited and nitrogen-sufficient cell cultures of Selenastrum minutum (Naeg.) Collins (Chlorophyta) were used to investigate the dependence of NH₄⁺ assimilation on exogenous CO₂. N-sufficient cells were only able to assimilate NH₄⁺ maximally in the presence of CO₂ and light. Inhibition of photosynthesis with 3-(3,4-dichlorophenyl)-1,1-dimethylurea, diuron also inhibited NH₄⁺ assimilation. These results indicate that NH₄⁺ assimilation by N-sufficient cells exhibited a strict requirement for photosynthetic CO₂ fixation. N-limited cells assimilated NH₄⁺ both in the dark and in the light in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea, diuron, indicating that photosynthetic CO₂ fixation was not required for NH₄⁺ assimilation. Using CO₂ removal techniques reported previously in the literature, we were unable to demonstrate CO₂-dependent NH₄⁺ assimilation in N-limited cells. However, employing more stringent CO₂ removal techniques we were able to show a CO₂ dependence of NH₄⁺ assimilation in both the light and dark, which was independent of photosynthesis. The results indicate two independent CO₂ requirements for NH₄⁺ assimilation. The first is as a substrate for photosynthetic CO₂ fixation, whereas the second is a nonphoto-synthetic requirement, presumably as a substrate for the anaplerotic reaction catalyzed by phosphoenolpyruvate carboxylase.     

Influence of inorganic nitrogen sources on K+/Na+ homeostasis and salt tolerance in sorghum plants

This work aimed to study the regulation of K⁺/Na⁺ homeostasis and the physiological responses of salt-treated sorghum plants [Sorghum bicolor (L.) Moench] grown with different inorganic nitrogen (N) sources. Four days after sowing (DAS), the plants were transferred to complete nutrient solutions containing 0.75 mM K⁺ and 5 mM N, supplied as either NO₃ ^? or NH₄ ⁺. Twelve DAS, the plants were subjected to salt stress with 75 mM NaCl, which was applied in two doses of 37.5 mM. The plants were harvested on the third and seventh days after the exposure to NaCl. Under the salt stress conditions, the reduction of K⁺ concentrations in the shoot and roots was higher in the culture with NO₃ ^? than with NH₄ ⁺. However, the more conspicuous effect of N was on the Na⁺ accumulation, which was severely limited in the presence of NH₄ ⁺. This ionic regulation had a positive influence on the K⁺/Na⁺ ratio and the selective absorption and transport of K⁺ in the plants grown with NH₄ ⁺. Under control and salt stress conditions, higher accumulation of free amino acids and soluble proteins was promoted in NH₄ ⁺ grown roots than NO₃ ^? grown roots at both harvesting time, whereas higher accumulation of soluble sugars was observed only at 7 days of salt stress exposure. Unlike the NH₄ ⁺ grown plants, the gas exchanges of the NO₃ ^? grown plants were reduced after 7 days of salt stress. These results suggest that external NH₄ ⁺ may limit Na⁺ accumulation in sorghum, which could contribute to improving its physiological and metabolic responses to salt stress.     

Glycine transport by hemolysed and restored pigeon red cells effects of a domnan-induced electrical potential on entry and exit kinetics

The influence of a Donnan effect on the transport of glycine by hemolysed and restored pigeon red cells was examined. The Donnan effect was produced by replacing Cl^? with 2,4-toluenedisulfonate or glutamate. The effects of the associated membrane potential and inside-outside pH difference on glycine entry and exit rates were examined. The effects of pH on entry and exit rates in the absence of a Donnan effect were also examined.In the absence of a Donnan effect, Na⁺-dependent glycine entry requires the protonated form of a group with a pK_app of 7.9 and the depronated form of another group with a pK_app of 6.8. Neither of these are required for exit but the deprotonated form of a group(s) with a pK_app of 6.2 is required. The pK 7.9 group and pK 6.2 group probably react with H⁺ at the inner face of the membrane and the pK 6.8 group probably reacts at the outer face.The V for glycine entry was determined for cells with their Cl^? largely replaced by toluenedisulfonate and without such replacement. Between pH 6.1 and 7, the ratio of the respective V values, V_T/V_Cl, was 1.5–1.7. V_T/V_Cl rose above pH 7 to near 4 at pH 8.3. At pH 6.9, with glutamate replacing cell Cl^?, the analogous ratio (V_Glu/V_Cl) was 1.7. The increase of V_T/V_Cl above pH 7 could be quantitatively accounted for by the increase in cell [H⁺]/medium [H⁺] caused by the Donnan effect together with the assumption that the pK 7.9 group reacts with H⁺ at the inner face of the membrane.When cell Cl^? was replaced by toluenedisulfonate or glutamate there was a drop in the term in the glycine K_m describing Na⁺ dependence of glycine entry. When cell Cl^? was replaced by toluenedisulfonate there was a rise in the Na⁺-independent term in the glycine entry K_m. By replacing varying amounts of cell Cl^? with either toluenedisulfonate or glutamate, plots were obtained of entry rates vs. the cell [Cl^?]/medium [Cl^?] ratio consistent with the assumption that the Donnan-induced membrane potential acts on a “moving” charge. Glycine exit was only slightly accelerated by trans-toluenedisulfonate. The ratio, exit rate into toluenedisulfonate medium/exit rate into Cl^? medium rose with decreasing pH. This rise could be accounted for by a Donnan-induced inside-outside pH difference which affects a pK_app 6.2 group reacting with internal H⁺.The observed influences of the Donnan effect on V(glycine entry), on both components of K_m(glycine entry), on the shape of the plot of glycine entry rate vs. the cell [Cl^?]/medium [Cl^?] ratio and on glycine exit all fit the assumptions that when the empty porter reorients, one unit of negative charge accompanies it “across” the membrane and that no other steps involve charge movement.The properties of the system seem inconsistent with a translational (“ferry boar”) mobile carrier.     

Heterotrophic Carbon Dioxide Fixation Products of Euglena: EFFECTS OF AMMONIUM

The metabolic products of heterotrophic (dark) CO₂ fixation by Euglena gracilis Klebs strain Z Pringsheim were separated and identified. They consisted of amino acids, phosphorylated compounds, tricarboxylic acid cycle intermediates, and nucleotides. Exposure of the cells to NH₄⁺ after a period of NH₄⁺ deprivation stimulated heterotrophic CO₂ fixation almost 4-fold, modifying the spectrum of the fixation products. In particular, the NH₄⁺ treatment stimulated fixation of CO₂ into glutamine, glycine, alanine, and serine.     

Influence of Nitrate and Ammonium Nutrition on the Uptake, Assimilation, and Distribution of Nutrients in Ricinus communis

Ricinus communis L. plants were grown in nutrient solutions in which N was supplied as NO₃⁻ or NH₄⁺, the solutions being maintained at pH 5.5. In NO₃⁻-fed plants excess nutrient anion over cation uptake was equivalent to net OH⁻ efflux, and the total charge from NO₃⁻ and SO₄²⁻ reduction equated to the sum of organic anion accumulation plus net OH⁻ efflux. In NH₄⁺-fed plants a large H⁺ efflux was recorded in close agreement with excess cation over anion uptake. This H⁺ efflux equated to the sum of net cation (NH₄⁺ minus SO₄²⁻) assimilation plus organic anion accumulation. In vivo nitrate reductase assays revealed that the roots may have the capacity to reduce just under half of the total NO₃⁻ that is taken up and reduced in NO₃⁻-fed plants. Organic anion concentration in these plants was much higher in the shoots than in the roots. In NH₄⁺-fed plants absorbed NH₄⁺ was almost exclusively assimilated in the roots. These plants were considerably lower in organic anions than NO₃⁻-fed plants, but had equal concentrations in shoots and roots. Xylem and phloem saps were collected from plants exposed to both N sources and analyzed for all major contributing ionic and nitrogenous compounds. The results obtained were used to assist in interpreting the ion uptake, assimilation, and accumulation data in terms of shoot/root pH regulation and cycling of nutrients.     

The effect of land use on dissolved organic carbon and nitrogen uptake in streams

1. Agricultural and urban land use may increase dissolved inorganic nitrogen (DIN) concentrations in streams and saturate biotic nutrient demand, but less is known about their impacts on the cycling of organic nutrients. To assess these impacts we compared the uptake of DIN (as ammonium, NH₄⁺), dissolved organic carbon (DOC, as acetate), and dissolved organic nitrogen (DON, as glycine) in 18 low‐gradient headwater streams in southwest Michigan draining forested, agricultural, or urban land‐use types. Over 3 years, we quantified uptake in two streams in each of the three land‐use types during three seasons (spring, summer and autumn). 2. We found significantly higher NH₄⁺ demand (expressed as uptake velocity, V_f) in urban compared to forested streams and NH₄⁺V_f was greater in spring compared to summer and autumn. Acetate V_f was significantly higher than NH₄⁺ and glycine V_f, but neither acetate nor glycine V_f were influenced by land‐use type or season. 3. We examined the interaction between NH₄⁺ and acetate demand by comparing simultaneous short‐term releases of both solutes to releases of each solute individually. Acetate V_f did not change during the simultaneous release with NH₄⁺, but NH₄⁺V_f was significantly higher with increased acetate. Thus, labile DOC V_f was not limited by the availability of NH₄⁺, but NH₄⁺V_f was limited by the availability of labile DOC. In contrast, neither glycine nor NH₄⁺V_f changed when released simultaneously indicating either that overall N‐uptake was saturated or that glycine and NH₄⁺ uptake were controlled by different factors. 4. Our results suggest that labile DOC and DON uptake can be equivalent to, or even higher than NH₄⁺ uptake, a solute known to be highly bioreactive, but unlike NH₄⁺ uptake, may not differ among land‐use types and seasons. Moreover, downstream export of nitrogen may be exacerbated by limitation of NH₄⁺ uptake by the availability of labile DOC in headwater streams from the agricultural Midwestern United States. Further research is needed to identify the factors that influence cycling of DOC and DON in streams.     

THE RELATIVE IMPORTANCE OF WATER MOTION ON NITROGEN UPTAKE BY THE SUBTIDAL MACROALGA ADAMSIELLA CHAUVINII (RHODOPHYTA) IN WINTER AND SUMMER1

The influence of seawater velocity (1.5–12 cm · s^?1) on inorganic nitrogen (N) uptake by the soft‐sediment perennial macroalga Adamsiella chauvinii (Harv.) L. E. Phillips et W. A. Nelson (Rhodophyta) was determined seasonally by measuring uptake rate in a laboratory flume. Regardless of N tissue content, water velocity had no influence on NO₃^? uptake in either winter or summer, indicating that NO₃^?‐uptake rate was biologically limited. However, when thalli were N limited, increasing water velocity increased NH₄⁺ uptake, suggesting that mass‐transfer limitation of NH₄⁺ is likely during summer for natural populations. Uptake kinetics (V_max, K_s) were similar among three populations of A. chauvinii at sites with different mean flow speeds; however, uptake rates of NO₃^? and NH₄⁺ were lower in summer (when N status was generally low) than in winter. Our results highlight how N uptake can be affected by seasonal changes in the physiology of a macroalga and that further investigation of N uptake of different macroalgae (red, brown, and green) during different seasons is important in determining the relative influence of water velocity on nutrient uptake.     

Kinetics of cyanide binding to chloroperoxidase in the presence of nitrate: detection of the influence of a heme-linked acid group by shift in the appa

The kinetics of the binding of cyanide to ferric chloroperoxidase have been studied at 25°C and ionic strength 0.11 M using a stopped-flow apparatus. The dissociation constant (K_CN) of the peroxidase-cyanide complex and both forward (k₊) and reverse (k_?) rate constants are independent of the H⁺ concentration over the pH range 2.7 to 7.1. The values obtained are k_cn = (9.5 ± 1.0) × 10^-5 M, k₊. = (5.2 ± 0.5) × 10⁴ M^?1 sec^?1 and k_- = (5.0± 1.4) sec^-1. In the presence of 0 06 M potassium nitrate the affinity of cyanide for chloroperoxidase decreases due to the inhibition of the forward reaction. The dissociation rate is not affected. The nitrate anion exerts its influence by binding to a protonated form of the enzyme, whereas the cyanide binds to the unprotonated form. Binding of nitrate results in an apparent shift towards higher pK_a values of the ionization of a crucial heme-linked acid group. Hence the influence of this group can be detected in the accessible pH range. Extrapolation to zero nitrate concentration yields a value of 3.1±0.3 for the pK_a of the heme-linked acid group.     

The effect of anions on the reaction catalyzed by lupine-nodule glutamate dehydrogenase

The kinetics of the reductive amination reaction of lupine-nodule glutamate dehydrogenase (l-glutamate:NAD oxidoreductase (deaminating), EC 1.4.1.2) were found to vary with the identity of the ammonium salt which was used as a substrate. Normal Michaelis-Menten kinetics were obtained with (NH₄)₂SO₄ but when NH₄Cl or NH₄-acetate was varied apparent substrate inhibition was observed. Linear double-reciprocal plots were obtained with NH₄Cl and NH₄-acetate, however, if the concentration of Cl^? or acetate was maintained constant by adding KCl or K-acetate. Chloride and acetate were subsequently found to cause linear noncompetitive inhibition with respect to NH₄⁺ and the apparent substrate inhibition by NH₄Cl and NH₄-acetate can be explained as the result varying a substrate and a noncompetitive inhibitor in constant ratio. Other anions were also found to be inhibitors of the glutamate dehydrogenase reaction; I^? caused parabolic noncompetitive inhibition with respect to NH₄⁺ and NO₃^? caused slope-parabolic noncompetitive inhibition with respect to all three substrates of the reductive amination reaction. For the oxidation deamination reaction, Cl^? was a linear competitive inhibitor with respect to both NAD and l-glutamate whereas NO₃^? caused parabolic competitive inhibition with respect to these reactants. To explain the results, it is proposed that anions bind to an allosteric site and cause a change in some of the rate constants of the reaction. Specifically, the results are consistent with anions causing decreases in the rates of association of NADH and 2-oxoglutarate with the enzyme and an increase in the rate of dissociation of NAD.     

Effects of monovalent cations on the catalytic activity of pig liver phosphofructokinase.

The monovalent cations NH₄⁺, K⁺, and Rb⁺ activate pig liver phosphofructokinase by increasing the maximal velocity. In the presence of these cations the enzyme retains sigmoid kinetics with respect to fructose-6-phosphate. However, these cations bring about a decrease in the [S]_0.5 for fructose-6-phosphate to an extent directly proportional to their ionic volumes. The apparent dissociation constants of NH₄⁺, K⁺, and Rb⁺ for the enzyme at 0.5 mM ATP and 4 mM Fru6P are 0.2 mM, 8 mM, and 15 mM, respectively. The maximal velocity of the enzyme in the presence of saturating concentrations of Rb⁺ is about 70% of that seen with NH₄⁺ or K⁺. The monovalent cations Li⁺, Na⁺, and Cs⁺ inhibit the enzyme at high concentrations (> 50 mM) by decreasing the maximal velocity. Although the efficiency of inhibition by these cations qualitatively increases with decreasing size, there is no obvious quantitative relationship between efficiency of inhibition and any parameter of ionic size.     

Effective charge measurements reveal selective and preferential accumulation of anions, but not cations, at the protein surface in dilute salt solutions

Specific-ion effects are ubiquitous in nature; however, their underlying mechanisms remain elusive. Although Hofmeister-ion effects on proteins are observed at higher (>0.3M) salt concentrations, in dilute (<0.1M) salt solutions nonspecific electrostatic screening is considered to be dominant. Here, using effective charge (Q*) measurements of hen-egg white lysozyme (HEWL) as a direct and differential measure of ion-association, we experimentally show that anions selectively and preferentially accumulate at the protein surface even at low (<100 mM) salt concentrations. At a given ion normality (50 mN), the HEWL Q* was dependent on anion, but not cation (Li⁺, Na⁺, K⁺, Rb⁺, Cs⁺, GdnH⁺, and Ca²⁺), identity. The Q* decreased in the order F⁻ > Cl⁻ > Br⁻ > NO₃⁻ ∼ I⁻ > SCN⁻ > ClO₄⁻ ≫ SO₄²⁻, demonstrating progressively greater binding of the monovalent anions to HEWL and also show that the SO₄²⁻ anion, despite being strongly hydrated, interacts directly with the HEWL surface. Under our experimental conditions, we observe a remarkable asymmetry between anions and cations in their interactions with the HEWL surface.