An S-Type Anion Channel SLAC1 Is Involved in Cryptogein-Induced Ion Fluxes and Modulates Hypersensitive Responses in Tobacco BY-2 Cells

Pharmacological evidence suggests that anion channel-mediated plasma membrane anion effluxes are crucial in early defense signaling to induce immune responses and hypersensitive cell death in plants. However, their molecular bases and regulation remain largely unknown. We overexpressed Arabidopsis SLAC1, an S-type anion channel involved in stomatal closure, in cultured tobacco BY-2 cells and analyzed the effect on cryptogein-induced defense responses including fluxes of Cl⁻ and other ions, production of reactive oxygen species (ROS), gene expression and hypersensitive responses. The SLAC1-GFP fusion protein was localized at the plasma membrane in BY-2 cells. Overexpression of SLAC1 enhanced cryptogein-induced Cl⁻ efflux and extracellular alkalinization as well as rapid/transient and slow/prolonged phases of NADPH oxidase-mediated ROS production, which was suppressed by an anion channel inhibitor, DIDS. The overexpressor also showed enhanced sensitivity to cryptogein to induce downstream immune responses, including the induction of defense marker genes and the hypersensitive cell death. These results suggest that SLAC1 expressed in BY-2 cells mediates cryptogein-induced plasma membrane Cl⁻ efflux to positively modulate the elicitor-triggered activation of other ion fluxes, ROS as well as a wide range of defense signaling pathways. These findings shed light on the possible involvement of the SLAC/SLAH family anion channels in cryptogein signaling to trigger the plasma membrane ion channel cascade in the plant defense signal transduction network.     

Influence of the level of nitrate nutrition on ion uptake and assimilation, organic Acid accumulation, and cation-anion balance in whole tomato plants

Tomato plants (Lycopersicon esculentum L. var. Ailsa Craig) were grown in water culture in nutrient solution in a series of 10 increasing levels of nitrate nutrition. Using whole plant data derived from analytical and yield data of individual plant parts, the fate of anion charge arising from increased NO₃ assimilation was followed in its distribution between organic anion accumulation in the plant and OH⁻ efflux into the nutrient solution as calculated by excess anion over cation uptake. With increasing NO₃ nutrition the bulk of the anion charge appeared as organic anion accumulation in the plants. OH⁻ efflux at a maximum accounted for only 20% of the anion charge shift. The major organic anion accumulated in response to nitrate assimilation was malate. The increase in organic anion accumulation was paralleled by an increase in cation concentration (K⁺, Ca²⁺, Mg²⁺, Na⁺). Total inorganic anion levels (NO₃⁻, SO₄²⁻, H₂PO₄⁻, Cl⁻) were relatively constant. The effect of increasing NO₃ nutrition in stimulating organic anion accumulation was much more pronounced in the tops than in the roots.     

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.     

Nitrate Uptake into Barley (Hordeum vulgare) Plants : A New Approach Using ClO(3) as an Analog for NO(3)

Evidence is presented that chlorate is an extremely good analog for nitrate during nitrate uptake by intact barley (Hordeum vulgare cv. Fergus) roots. The depletion of ClO₃⁻ or NO₃⁻ from uptake media over 2 to 6 hours by seedlings was found to be dependent on combined NO₃⁻ plus ClO₃⁻ concentrations, and total anion uptake was equivalent at different NO₃⁻/ClO₃⁻ ratios. After loading barley seedlings with ³⁶ClO₃⁻ for 6 hours, kinetic parameters were derived from the analysis of efflux of [³⁶Cl] chlorate into unlabeled solution. On the basis of this analysis, the half times for exchange for the cytoplasmic and vacuolar phases were 17 minutes and 20 hours, respectively.     

Nitrate uptake by roots as regulated by nitrate assimilation in the shoot of castor oil plants

Ricinus communis was used to test the Ben Zioni-Dijkshoorn hypothesis that NO₃ uptake by roots can be regulated by NO₃ assimilation in the shoot. The rate of the anion charge from assimilated NO₃⁻ (and SO₄²⁻) was followed in its distribution between organic acid anion accumulation and HCO₃⁻ efflux into the nutrient solution. In plants adequately supplied with NO₃⁻, HCO₃⁻ efflux accounted for between 56 and 63% of the anion charge. When the plants were subjected to a low NO₃ regime HCO₃⁻ excretion accounted for only 23% of the charge. A comparison of mature plants growing for a 10-day period at the two levels of NO₃ nutrition revealed that the uptake of NO₃⁻ at the higher level was increased 3-fold, whereas K uptake was unaltered. To trace ion movement within the plant, the ionic constituents of xylem and phloem sap were determined. In xylem sap these constituents were found to be predominantly K⁺, Ca²⁺, and NO₃⁻, whereas in the phloem sap they were mainly K⁺ and organic acid anions. Results have been obtained which may be interpreted as providing direct evidence of NO₃ uptake by roots regulated by NO₃ reduction in the tops, the process being facilitated by the recirculation of K⁺ in the plant.     

Decrease of pH Gradients in Tonoplast Vesicles by NO(3) and Cl: Evidence for H-Coupled Anion Transport

Chloride or nitrate decreased a pH gradient (measured as [¹⁴C]methylamine accumulation) in tonoplast-enriched vesicles. The ΔpH decrease was dependent on the anion concentration. These effects are independent of the anion-sensitive H⁺-ATPase of the tonoplast, since the pH gradient (acid inside) was imposed artificially using a pH jump or a K⁺ gradient and nigericin. 4,4′-Diisothiocyano-2,2′-stilbene disulfonic acid partially prevented the decrease in pH gradient induced by Cl⁻. Two possible models to account for this anion-dependent decrease of ΔpH are: (a) H⁺ loss is accompanied by Cl⁻ or NO₃⁻ efflux from the vesicles via H⁺/anion symport systems on the tonoplast and (b) H⁺ loss is accompanied by Cl⁻ or NO₃⁻ uptake into the vesicles via H⁺/anion antiport systems. Depending on the requirements and conditions of the cell, these two systems would serve to either mobilize Cl⁻ and NO₃⁻ stored in the vacuole for use in the cytoplasm or to drive anions into the vacuole. Chloride or nitrate also decreased a pH gradient in fractions containing plasma membrane and Golgi, implying that these membranes may have similar H⁺-coupled anion transport systems.     

Simultaneous Influx and Efflux of Nitrate during Uptake by Perennial Ryegrass

Experiments with intact plants of Lolium perenne previously grown with ¹⁴NO₃⁻ revealed significant efflux of this isotopic species when the plants were transferred to solutions of highly enriched ¹⁵NO₃⁻. The exuded ¹⁴NO₃⁻ was subsequently reabsorbed when the ambient solutions were not replaced. When they were frequently replaced, continual efflux of the ¹⁴NO₃⁻ was observed. Influx of ¹⁵NO₃⁻ was significantly greater than influx of ¹⁴NO₃⁻ from solutions of identical NO₃⁻ concentration. Transferring plants to ¹⁴NO₃⁻ solutions after a six-hour period in ¹⁵NO₃⁻ resulted in efflux of the latter. Presence of Mg²⁺, rather than Ca²⁺, in the ambient ¹⁵NO₃⁻ solution resulted in a decidedly increased rate of ¹⁴NO₃⁻ efflux and a slight but significant increase in ¹⁵NO₃⁻ influx. Accordingly, net NO₃⁻ influx was slightly depressed. A model in accordance with these observations is presented; its essential features include a passive bidirectional pathway, an active uptake mechanism, and a pathway for recycling of endogenous NO₃⁻ within unstirred layers from the passive pathway to the active uptake site.     

Nitrate efflux is an essential component of the cryptogein signaling pathway leading to defense responses and hypersensitive cell death in tobacco

There is much interest in the transduction pathways by which avirulent pathogens or derived elicitors activate plant defense responses. However, little is known about anion channel functions in this process. The aim of this study was to reveal the contribution of anion channels in the defense response triggered in tobacco by the elicitor cryptogein. Cryptogein induced a fast nitrate (NO(3)(-)) efflux that was sensitive to anion channel blockers and regulated by phosphorylation events and Ca(2+) influx. Using a pharmacological approach, we provide evidence that NO(3)(-) efflux acts upstream of the cryptogein-induced oxidative burst and a 40-kD protein kinase whose activation seems to be controlled by the duration and intensity of anion efflux. Moreover, NO(3)(-) efflux inhibitors reduced and delayed the hypersensitive cell death triggered by cryptogein in tobacco plants. This was accompanied by a delay or a complete suppression of the induction of several defense-related genes, including hsr203J, a gene whose expression is correlated strongly with programmed cell death in plants. Our results indicate that anion channels are involved intimately in mediating defense responses and hypersensitive cell death.     

Involvement of putative glutamate receptors in plant defence signaling and NO production

Ionotropic glutamate receptors (iGluRs) are non-selective cation channels permeable to calcium, present in animals and plants. In mammals, glutamate is a well-known neurotransmitter and recently has been recognized as an immunomodulator. As animals and plants share common mechanisms that govern innate immunity with calcium playing a key role in plant defence activation, we have checked the involvement of putative iGluRs in plant defence signaling. Using tobacco cells, we first provide evidence supporting the activity of iGluRs as calcium channels and their involvement in NO production as reported in animals. Thereafter, iGluRs were shown to be activated in response to cryptogein, a well studied elicitor of defence response, and partly responsible for cryptogein-induced NO production. However, other cryptogein-induced calcium-dependent events including anion efflux, H₂O₂ production, MAPK activation and hypersensitive response (HR) did not depend on iGluRs indicating that different calcium channels regulate different processes at the cell level. We have also demonstrated that cryptogein induces efflux of glutamate in the apoplast by exocytosis. Taken together, our results demonstrate for the first time, an involvement of a putative iGluR in plant defence signaling and NO production, by mechanisms that show homology with glutamate mode of action in mammals.     

Short Term Studies of Nitrate Uptake into Barley Plants Using Ion-Specific Electrodes and ClO(3): II. Regulation of NO(3) Efflux by NH(4)

The influence of NH₄⁺, in the external medium, on fluxes of NO₃⁻ and K⁺ were investigated using barley (Hordeum vulgare cv Betzes) plants. NH₄⁺ was without effect on NO₃⁻ (³⁶ClO₃⁻) influx whereas inhibition of net uptake appeared to be a function of previous NO₃⁻ provision. Plants grown at 10 micromolar NO₃⁻ were sensitive to external NH₄⁺ when uptake was measured in 100 micromolar NO₃⁻. By contrast, NO₃⁻ uptake (from 100 micromolar NO₃⁻) by plants previously grown at this concentration was not reduced by NH₄⁺ treatment. Plants pretreated for 2 days with 5 millimolar NO₃⁻ showed net efflux of NO₃⁻ when roots were transferred to 100 micromolar NO₃⁻. This efflux was stimulated in the presence of NH₄⁺. NH₄⁺ also stimulated NO₃⁻ efflux from plants pretreated with relatively low nitrate concentrations. It is proposed that short term effects on net uptake of NO₃⁻ occur via effects upon efflux. By contrast to the situation for NO₃⁻, net K⁺ uptake and influx of ³⁶Rb⁺-labeled K⁺ was inhibited by NH₄⁺ regardless of the nutrient history of the plants. Inhibition of net K⁺ uptake reached its maximum value within 2 minutes of NH₄⁺ addition. It is concluded that the latter ion exerts a direct effect upon K⁺ influx.     

Transport of anions in isolated barley vacuoles : I. Permeability to anions and evidence for a cl-uptake system

The anion contents of young barley leaves and of mesophyll protoplasts from the leaves was compared. Anion loss from the protoplasts during isolation was small. Although only about 60% of the leaf cells were mesophyll cells, phosphate and sulfate contents of the mesophyll cells accounted for almost 90% of the leaf contents. Chloride accumulated in the leaf epidermis. The rapid isolation of vacuoles from mesophyll protoplasts permitted the determination of vacuolar ion concentrations. Sodium and nitrate levels were very low in the cytoplasm, and much higher in the vacuole. When barley plants were grown in the presence of low NaCl levels, chloride concentrations were comparable in cytoplasm and vacuole, and similar observations were made with sulfate. Cytoplasmic phosphate concentrations were close to 30 millimolar and potassium concentrations 100 millimolar. During a 30 minute incubation period at room temperature, anion contents of isolated vacuoles decreased considerably. Efflux of NO₃⁻ was faster than that of Cl⁻. Phosphate and sulfate crossed the tonoplast only slowly. 4,4′-Diisothiocyano-2,2′-stilbenedisulfonic acid partially inhibited the efflux of nitrate and, to a lesser extent, that of chloride. Decreased efflux was also observed in the presence of MgATP. In remarkable contrast, p-chloromercuribenzene sulfonate and HgCl₂ stimulated the efflux of nitrate and chloride, but not of phosphate. Labeled chloride was taken up by isolated vacuoles. The apparent K_m for chloride uptake at low chloride concentrations was 2.3 millimolar. At elevated chloride concentrations, chloride did not display saturation characteristics but, rather, characteristics of a diffusional process. Uptake was stimulated by ATP.     

Microelectrode Measurements on Red Beet Vacuole : Biological Effect of Na OR NO(3) Ions, Diffusing from the Microelectrode

Glass microelectrodes filled with 3 molar KCl are widely used to measure intracellular potentials and it is usual to try to minimize their electrolyte loss. In these experiments we have used the ionic leak of our microelectrodes, filled with various salt solutions, to introduce a given ion into the red beet vacuole. This allowed us to show that NO₃⁻ ions reduce the magnitude of the current spectral density while they do not change the resistance of the tonoplast. This is true when NO₃⁻ is either added to the external medium or used as the microelectrode filling solution. This can be interpreted by a NO₃⁻ effect on the vacuolar side of the tonoplast, resulting in an inhibition of the ion transporting ATPase. Replacing K⁺ by Na⁺ ions in the medium has no effect on tonoplast resistance (R_s). On the contrary, when ions leaking from the microelectrode are H⁺, Li⁺ or K⁺, R_s is close to 4 kilohm square centimeter, whereas R_s is of the order of 30KΩ square centimeter when Na⁺ are the leaking ions. We also found a possible correlation between the presence of a Lorentzian in the current spectral density (cut-off frequency = 2 hertz) and a Cl⁻ efflux from the vacuole. This could be explained by the existence of Cl⁻ channels on the tonoplast.     

Effect of exogenous and endogenous nitrate concentration on nitrate utilization by dwarf bean

The effect of the exogenous and endogenous NO₃⁻ concentration on net uptake, influx, and efflux of NO₃⁻ and on nitrate reductase activity (NRA) in roots was studied in Phaseolus vulgaris L. cv. Witte Krombek. After exposure to NO₃⁻, an apparent induction period of about 6 hours occurred regardless of the exogenous NO₃⁻ level. A double reciprocal plot of the net uptake rate of induced plants versus exogenous NO₃⁻ concentration yielded four distinct phases, each with simple Michaelis-Menten kinetics, and separated by sharp breaks at about 45, 80, and 480 micromoles per cubic decimeter.

Influx was estimated as the accumulation of ¹⁵N after 1 hour exposure to ¹⁵NO₃⁻. The isotherms for influx and net uptake were similar and corresponded to those for alkali cations and Cl⁻. Efflux of NO₃⁻ was a constant proportion of net uptake during initial NO₃⁻ supply and increased with exogenous NO₃⁻ concentration. No efflux occurred to a NO₃⁻-free medium.

The net uptake rate was negatively correlated with the NO₃⁻ content of roots. Nitrate efflux, but not influx, was influenced by endogenous NO₃⁻. Variations between experiments, e.g. in NO₃⁻ status, affected the values of K_m and V_max in the various concentration phases. The concentrations at which phase transitions occurred, however, were constant both for influx and net uptake. The findings corroborate the contention that separate sites are responsible for uptake and transitions between phases.

Beyond 100 micromoles per cubic decimeter, root NRA was not affected by exogenous NO₃⁻ indicating that NO₃⁻ uptake was not coupled to root NRA, at least not at high concentrations.

     

Intracellular pH Regulation during NO(3) Assimilation in Shoot and Roots of Ricinus communis

Ricinus communis L. was used to test the Dijkshoorn-Ben Zioni hypothesis that NO₃⁻ uptake by roots is regulated by NO₃⁻ assimilation in the shoot. The fate of the electronegative charge arising from total assimilated NO₃⁻ (and SO₄²⁻) was followed in its distribution between organic anion accumulation and HCO₃⁻ excretion into the nutrient solution. In plants adequately supplied with NO₃⁻, HCO₃⁻ excretion accounted for about 47% of the anion charge, reflecting an excess nutrient anion over cation uptake. In vivo nitrate reductase assays revealed that the roots represented the site of about 44% of the total NO₃⁻ reduction in the plants. To trace vascular transport of ionic and nitrogenous constituents within the plant, the composition of both xylem and phloem saps was thoroughly investigated. Detailed dry tissue and sap analyses revealed that only between 19 and 24% of the HCO₃⁻ excretion could be accounted for from oxidative decarboxylation of shoot-borne organic anions produced in the NO₃⁻ reduction process. The results obtained in this investigation may be interpreted as providing direct evidence for a minor importance of phloem transport of cation-organate for the regulation of intracellular pH and electroneutrality, thus practically eliminating the necessity for the Dijkshoorn-Ben Zioni recycling process.     

Role of Nitrate and Nitrite in the Induction of Nitrite Reductase in Leaves of Barley Seedlings

The role of NO₃⁻ and NO₂⁻ in the induction of nitrite reductase (NiR) activity in detached leaves of 8-day-old barley (Hordeum vulgare L.) seedlings was investigated. Barley leaves contained 6 to 8 micromoles NO₂⁻/gram fresh weight × hour of endogenous NiR activity when grown in N-free solutions. Supply of both NO₂⁻ and NO₃⁻ induced the enzyme activity above the endogenous levels (5 and 10 times, respectively at 10 millimolar NO₂⁻ and NO₃⁻ over a 24 hour period). In NO₃⁻-supplied leaves, NiR induction occurred at an ambient NO₃⁻ concentration of as low as 0.05 millimolar; however, no NiR induction was found in leaves supplied with NO₂⁻ until the ambient NO₂⁻ concentration was 0.5 millimolar. Nitrate accumulated in NO₂⁻-fed leaves. The amount of NO₃⁻ accumulating in NO₂⁻-fed leaves induced similar levels of NiR as did equivalent amounts of NO₃⁻ accumulating in NO₃⁻-fed leaves. Induction of NiR in NO₂⁻-fed leaves was not seen until NO₃⁻ was detectable (30 nanomoles/gram fresh weight) in the leaves. The internal concentrations of NO₃⁻, irrespective of N source, were highly correlated with the levels of NiR induced. When the reduction of NO₃⁻ to NO₂⁻ was inhibited by WO₄²⁻, the induction of NiR was inhibited only partially. The results indicate that in barley leaves NiR is induced by NO₃⁻ directly, i.e. without being reduced to NO₂⁻, and that absorbed NO₂⁻ induces the enzyme activity indirectly after being oxidized to NO₃⁻ within the leaf.     

Short Term Studies of Nitrate Uptake into Barley Plants Using Ion-Specific Electrodes and ClO(3): I. Control of Net Uptake by NO(3) Efflux

A computer-controlled multichannel data acquisition system was employed to obtain continuous measurements of net nitrate or chlorate uptake by roots of intact barley plants (Hordeum vulgare cv Betzes) using nitrate-specific electrodes. Plants, previously grown in solutions maintained at 10 or 200 micromolar NO₃⁻ (low N or high N conditions, respectively), were provided with 200 micromolar NO₃⁻ or ClO₃⁻ during the uptake period. Initial rates of NO₃⁻ uptake were several times higher in low N plants than in high N plants. Within 10 min, uptake in the former plants declined to a new steady rate which was sustained for the remainder of the experiment. No such time-dependent changes were evident in the high N plants. Rates and patterns of net chlorate uptake exhibited almost identical dependence upon previous nitrate provision. NO₃⁻ (³⁶ClO₃⁻) influx, by contrast, appeared to be independent of NO₃⁻ pretreatment prior to influx determination. Nitrate efflux, estimated by several different methods, was strongly correlated with internal nitrate concentration of the roots.     

Regulation of NO(3) Influx in Barley : Studies Using NO(3)

Short-term (10 minutes) measurements of plasmalemma NO₃⁻ influx (_oc) into roots of intact barley plants were obtained using ¹³NO₃⁻. In plants grown for 4 days at various NO₃⁻ levels (0.1, 0.2, 0.5 millimolar), _oc was found to be independent of the level of NO₃⁻ pretreatment. Similarly, pretreatment with Cl⁻ had no effect upon plasmalemma ¹³NO₃⁻ influx. Plants grown in the complete absence of ¹³NO₃⁻ (in CaSO₄ solutions) subsequently revealed influx values which were more than 50% lower than for plants grown in NO₃⁻. Based upon the documented effects of NO₃⁻ or Cl⁻ pretreatments on net uptake of NO₃⁻, these observations suggest that negative feedback from vacuolar NO₃⁻ and/or Cl⁻ acts at the tonoplast but not at the plasmalemma. When included in the influx medium, 0.5 millimolar Cl⁻ was without effect upon ¹³NO₃⁻ influx, but NH₄⁺ caused approximately 50% reduction of influx at this concentration.     

The Influence of Nitrate and Chloride Uptake on Expressed Sap pH, Organic Acid Synthesis, and Potassium Accumulation in Higher Plants

The influence of NO₃⁻ uptake and reduction on ionic balance in barley seedlings (Hordeum vulgare, cv. Compana) was studied. KNO₃ and KCl treatment solutions were used for comparison of cation and anion uptake. The rate of Cl⁻ uptake was more rapid than the rate of NO₃⁻ uptake during the first 2 to 4 hours of treatment. There was an acceleration in rate of NO₃⁻ uptake after 4 hours resulting in a sustained rate of NO₃⁻ uptake which exceeded the rate of Cl⁻ uptake. The initial (2 to 4 hours) rate of K⁺ uptake appeared to be independent of the rate of anion uptake. After 4 hours the rate of K⁺ uptake was greater with the KNO₃ treatment than with the KCl treatment, and the solution pH, cell sap pH, and organic acid levels with KNO₃ increased, relative to those with the KCl treatment. When absorption experiments were conducted in darkness, K⁺ uptake from KNO₃ did not exceed K⁺ uptake from KCl. We suggest that the greater uptake and accumulation of K⁺ in NO₃⁻-treated plants resulted from (a) a more rapid, sustained uptake and transport of NO₃⁻ providing a mobile counteranion for K⁺ transport, and (b) the synthesis of organic acids in response to NO₃⁻ reduction increasing the capacity for K⁺ accumulation by providing a source of nondiffusible organic anions.     

Studies of the uptake of nitrate in barley : v. Estimation of root cytoplasmic nitrate concentration using nitrate reductase activity-implications for nitrate influx

The cytoplasmic NO₃⁻ concentration ([NO₃⁻]_c) was estimated for roots of barley (Hordeum vulgare L. cv Klondike) using a technique based on measurement of in vivo nitrate reductase activity. At zero external NO₃⁻ concentration ([NO₃⁻]_o), [NO₃⁻]_c was estimated to be 0.66 mm for plants previously grown in 100 μm NO₃⁻. It increased linearly with [NO₃⁻]_o between 2 and 20 mm, up to 3.9 mm at 20 mm [NO₃⁻]_o. The values obtained are much lower than previous estimates from compartmental analysis of barley roots. These observations support the suggestion (MY Siddiqi, ADM Glass, TJ Ruth [1991] J Exp Bot 42: 1455-1463) that the nitrate reductase-based technique and compartmental analysis determine [NO₃⁻]_c for two separate pools; an active, nitrate reductase-containing pool (possibly located in the epidermal cells) and a larger, slowly metabolized storage pool (possibly in the cortical cells), respectively. Given the values obtained for [NO₃⁻]_c and cell membrane potentials of −200 to −300 mV (ADM Glass, JE Schaff, LV Kochian [1992] Plant Physiol 99: 456-463), it is very unlikely that passive influx of NO₃⁻ is possible via the high-concentration, low-affinity transport system for NO₃⁻. This conclusion is consistent with the suggestion by Glass et al. that this system is thermodynamically active and capable of transporting NO₃⁻ against its electrochemical potential gradient.     

NO3 ?-induced pH Changes in Mammalian Cells : Evidence for an NO3?-H+ Cotransporter

The effect of NO₃ ⁻ on intracellular pH (pH_i) was assessed microfluorimetrically in mammalian cells in culture. In cells of human, hamster, and murine origin addition of extracellular NO₃ ⁻ induced an intracellular acidification. This acidification was eliminated when the cytosolic pH was clamped using ionophores or by perfusing the cytosol with highly buffered solutions using patch-pipettes, ruling out spectroscopic artifacts. The NO₃ ⁻- induced pH change was not due to modulation of Na⁺/H⁺ exchange, since it was also observed in Na⁺/H⁺ antiport-deficient mutants. Though NO₃ ⁻ is known to inhibit vacuolar-type (V) H⁺-ATPases, this effect was not responsible for the acidification since it persisted in the presence of the potent V-ATPase inhibitor bafilomycin A₁. NO₃ ⁻/HCO₃ ⁻ exchange as the underlying mechanism was ruled out because acidification occurred despite nominal removal of HCO₃ ⁻, despite inhibition of the anion exchanger with disulfonic stilbenes and in HEK 293 cells, which seemingly lack anion exchangers (Lee, B.S., R.B. Gunn, and R.R. Kopito. 1991. J. Biol. Chem. 266:11448– 11454). Accumulation of intracellular NO₃ ⁻, measured by the Greiss method after reduction to NO₂ ⁻, indicated that the anion is translocated into the cells along with the movement of acid equivalents. The simplest model to explain these observations is the cotransport of NO₃ ⁻ with H⁺ (or the equivalent counter-transport of NO₃ ⁻ for OH⁻). The transporter appears to be bi-directional, operating in the forward as well as reverse directions. A rough estimate of the fluxes of NO₃ ⁻ and acid equivalents suggests a one-to-one stoichiometry. Accordingly, the rate of transport was unaffected by sizable changes in transmembrane potential. The cytosolic acidification was a saturable function of the extracellular concentration of NO₃ ⁻ and was accentuated by acidification of the extracellular space. The putative NO₃ ⁻-H⁺ cotransport was inhibited markedly by ethacrynic acid and by α-cyano-4-hydroxycinnamate, but only marginally by 4,4′-diisothiocyanostilbene-2,2′ disulfonate or by p-chloromercuribenzene sulfonate. The transporter responsible for NO₃ ⁻-induced pH changes in mammalian cells may be related, though not identical, to the NO₃ ⁻-H⁺ cotransporter described in Arabidopsis and Aspergillus. The mammalian cotransporter may be important in eliminating the products of NO metabolism, particularly in cells that generate vast amounts of this messenger. By cotransporting NO₃ ⁻ with H⁺ the cells would additionally eliminate acid equivalents from activated cells that are metabolizing actively, without added energetic investment and with minimal disruption of the transmembrane potential, inasmuch as the cotransporter is likely electroneutral.