Cercospora beticola Toxins (X. Inhibition of Plasma Membrane H+-ATPase by Beticolin-1)

Influxes of 13NH4+ across the root plasmalemma were measured in intact seedlings of Picea glauca (Moench) Voss. Two kinetically distinct uptake systems for NH4+ were identified. In N-deprived plants, a Michaelis-Menten-type high-affinity transport system (HATS) operated in a 2.5 to 350 [mu]M range of external NH4+ concentration ([NH4 +]o). The Vmax of this HATS was 1.9 to 2.4 [mu]mol g-1 h-1, and the Km was 20 to40 [mu]M. At [NH4+]o from 500 [mu]M to 50 mM, a linear low-affinity system (LATS) was apparent. Both HATS and LATS were constitutive. A time-dependence study of NH4+ influx in previously N-deprived seedlings revealed a small transient increase of NH4+ influx after 24 h of exposure to 100 [mu]M [NH4+]o. This was followed by a decline of influx to a steady-state value after 4 d. In seedlings exposed to 100 [mu]M external NO3- concentration for 3 d, the Vmax for NH4+ uptake by HATS was increased approximately 30% compared to that found in N-deprived seedlings, whereas LATS was down-regulated. The present study defines the much higher uptake capacity for NH4+ than for N03- in seedlings of this species.     

Characterization and regulation of ammonium transport systems in Citrus plants

We have investigated both the kinetics and regulation of 15NH4+ influx in roots of 3-month-old hydroponically grown Citrus (Citrus sinensis L. Osbeck x Poncirus trifoliata Blanco) seedlings. The 15NH4+ influx is saturable below an external ammonium concentration of 1 mM, indicating the action of a high-affinity transport system (HATS). The HATS is under feedback repression by the N status of the plant, being down-regulated in plants adequately supplied with N during growth, and up-regulated by N-starvation. When assayed between 1 and 50 mM [15NH4+]0, the 15NH4+ influx showed a linear response typical of a low-affinity transport system (LATS). The activity of the LATS increased in plants supplied with NH4+ as compared with plants grown on an N-free medium. Transfer of the plants to N-free solution resulted in a marked decrease in the LATS-mediated 15NH4+ influx. Accordingly, resupply of NH4+ after N-starvation triggered a dramatic stimulation of the activity of the LATS. These data provide evidence that in Citrus plants, the LATS or at least one of its components is inducible by NH4+. Even when up-regulated, both the HATS and the LATS displayed a limited capacity, as compared with that usually found in herbaceous species. The use of various metabolic uncouplers or inhibitors indicated that 15NH4+ influx mediated by the HATS is strongly dependent on energy metabolism and H+ transmembrane electrochemical gradient. By contrast, the LATS is not affected by protonophores or inhibitors of the H(+)-ATPase, suggesting that its activity is mostly driven by the NH4+/NH3 transmembrane gradient. In agreement with these hypotheses, the HATS-mediated 15NH4+ influx was strongly inhibited when the solution pH was raised from 4 to 7, whereas influx mediated by the LATS was slightly stimulated.     

Potassium Fluxes in Chlamydomonas reinhardtii (I.Kinetics and Electrical Potentials)

Potassium influx and cellular [K+] were measured in the unicellular green alga Chlamydomonas reinhardtii after pretreatment in either 10 or 0 mM external K+ ([K]0). K+ (42K+ or 86Rb+) influx was mediated by a saturable, high-affinity transport system (HATS) at low [K+]0 and a linear, low-affinity transport system at high [K+]o. The HATS was typically more sensitive to metabolic inhibition (and darkness) than the low-affinity transport system. Membrane electrical potentials were determined by measuring the equilibrium distribution of tetraphenylphosphonium. These values, together with estimates of cytoplasmic [K+] (B. Malhotra and A.D.M. Glass [1995] Plant Physiol 108: 1537-1545), demonstrated that at 0.1 mM [K+]0 K+ uptake must be active. At higher [K+]0 (>0.3 mM) K+ influx appeared to be passive and possibly channel mediated. When cells were deprived of K+ for 24 h, the Vmax for the HATS increased from 50 x 10-6 to 85 x 10-6 nmol h-1 cell-1 and the Km value decreased from 0.25 to 0.162 mM. Meanwhile, cellular [K+] declined from 24 x 10-6 to 9 x 10-6 nmol cell-1. During this period influx increased exponentially, reaching its peak value after 18 h of K+ deprivation. This increase of K+ influx was not expressed when cells were exposed to inhibitors of protein synthesis. The use of 42K+ and 86Rb+ in parallel experiments demonstrated that Chlamydomonas discriminated in favor of K+ over Rb+, and this effect increased with the duration of K+ deprivation.     

Kinetics of NH 4 + uptake by the arbuscular mycorrhizal fungus Rhizophagus irregularis

The kinetics and energetics of (15)NH (4) (+) uptake by the extraradical mycelium of the arbuscular mycorrhizal fungus Rhizophagus irregularis were investigated. (15)NH (4) (+) uptake increased with increasing substrate concentration over the concentration range of 0.002 to 25?mM. Eadie-Hofstee plots showed that ammonium (NH (4) (+) ) uptake over this range was biphasic. At concentrations below 100?μM, NH (4) (+) uptake fits a Michaelis-Menten curve, typical of the activity of a saturable high-affinity transport system (HATS). At concentrations above 1?mM, NH (4) (+) influx showed a linear response typical of a nonsaturable low-affinity transport system (LATS). Both transport systems were dependent on external pH. The HATS and, to a lesser extent, the LATS were inhibited by the ionophore carbonylcyanide m-chlorophenylhydrazone (CCCP) and the ATP-synthesis inhibitor 2,4-dinitrophenol. These data indicate that the two NH (4) (+) transport systems of R. irregularis are dependent on metabolic energy and on the electrochemical H(+) gradient. The HATS- and the LATS-mediated (15)NH (4) (+) influxes were also regulated by acetate. This first report of the existence of active high- and low-affinity NH4(+) transport systems in the extraradical mycelium of an arbuscular mycorrhizal fungus and provides novel information on the mechanisms underlying mycosymbiont uptake of nitrogen from the soil environment.     

Elevated [Cl-]i, and [Na+]i inhibit Na+, K+, Cl- cotransport by different mechanisms in squid giant axons

Bumetanide-sensitive (BS) unidirectional fluxes of (36)Cl- or (22)Na+ were measured in internally dialyzed squid giant axons while varying the intra- or extracellular concentrations of Na+ and/or Cl-. Raising either [Cl-]i or [Na+]i resulted in a concentration-dependent reduction of the BS influx of both (36)Cl- and (22)Na+. Raising [Cl-]i above 200 mM completely blocked BS influxes. However, raising [Na+]i to 290 mM resulted in saturable but incomplete inhibition of both BS Na+ influx and BS Cl- influx. The consequences of varying intracellular Cl- on cotransporter effluxes were complex. At lower [Cl-]i values (below 100 mM) intracellular Cl- activated cotransporter effluxes. Surprisingly, however, raising [Cl-]i levels > 125 mM resulted in a [Cl-]i-dependent inhibition of BS effluxes of both Na+ and Cl-. On the other hand, raising [Na+]i resulted only in the activation of the BS Na+ efflux; intracellular Na+ did not inhibit BS efflux even at 290 mM. The inhibitory effects of intracellular Na+ on cotransporter-mediated influxes, and lack of inhibitory effects on BS effluxes, are consistent with the trans-side inhibition expected for an ordered binding/release model of cotransporter operation. However, the inhibitory effects of intracellular Cl- on both influxes and effluxes are not explained by such a model. These data suggest that Cl may interact with an intracellular site (or sites), which does not mediate Cl transport, but does modulate the transport activity of the Na+, K+, Cl- cotransporter.     

Alleviation of rapid, futile ammonium cycling at the plasma membrane by potassium reveals K+-sensitive and -insensitive components of NH4+ transport

Futile plasma membrane cycling of ammonium (NH4+) is characteristic of low-affinity NH4+ transport, and has been proposed to be a critical factor in NH4+ toxicity. Using unidirectional flux analysis with the positron-emitting tracer 13N in intact seedlings of barley (Hordeum vulgare L.), it is shown that rapid, futile NH4+ cycling is alleviated by elevated K+ supply, and that low-affinity NH4+ transport is mediated by a K+-sensitive component, and by a second component that is independent of K+. At low external [K+] (0.1 mM), NH4+ influx (at an external [NH4+] of 10 mM) of 92 micromol g(-1) h(-1) was observed, with an efflux:influx ratio of 0.75, indicative of rapid, futile NH4+ cycling. Elevating K+ supply into the low-affinity K+ transport range (1.5-40 mM) reduced both influx and efflux of NH4+ by as much as 75%, and substantially reduced the efflux:influx ratio. The reduction of NH4+ fluxes was achieved rapidly upon exposure to elevated K+, within 1 min for influx and within 5 min for efflux. The channel inhibitor La3+ decreased high-capacity NH4+ influx only at low K+ concentrations, suggesting that the K+-sensitive component of NH4+ influx may be mediated by non-selective cation channels. Using respiratory measurements and current models of ion flux energetics, the energy cost of concomitant NH4+ and K+ transport at the root plasma membrane, and its consequences for plant growth are discussed. The study presents the first demonstration of the parallel operation of K+-sensitive and -insensitive NH4+ flux mechanisms in plants.     

The face value of ion fluxes: the challenge of determining influx in the low-affinity transport range

The existence of distinct high- and low-affinity transport systems (HATS and LATS) is well established for major nutrient ions. However, influx mediated by these systems is usually estimated using uniformly simple tracer protocols. Two (42)K radiotracer methods to measure potassium influxes in the HATS and LATS ranges in intact barley (Hordeum vulgare L.) roots are compared here: a direct influx (DI) method, and an integrated flux analysis (IFA), which is designed to account for tracer efflux from labelled roots and differential tracer accumulation along the plant axis. Methods showed only minor discrepancies for influx values in the HATS range, but large discrepancies in the LATS range, revealing striking distinctions in the cellular exchange properties dominated by the operation of the two transport systems. It is shown that accepted DI protocols are associated with very large errors in the high-conductance LATS range, underestimating influx at least 6-fold due to four characteristics of this transport mode: (i) accelerated cellular (42)K exchange; (ii) a greatly increased ratio of efflux to influx; (iii) increased (42)K loss during the removal of water from roots in preweighing centrifugation or blotting protocols; and (iv) increased (42)K retention at the root-shoot interface, a region of the plant frequently disregarded in DI determinations. The findings warrant a re-evaluation of a large body of literature reporting influx in the LATS range, and are of fundamental importance to ion flux experimentation in plant physiology.     

Ammonium Uptake by Rice Roots (I. Fluxes and Subcellular Distribution of 13NH4+)

The time course of 13NH4+ uptake and the distribution of 13NH4+ among plant parts and subcellular compartments was determined for 3-week-old rice (Oryza sativa L. cv M202) plants grown hydroponically in modified Johnson's nutrient solution containing 2,100, or 1000 [mu]M NH4+ (referred to hereafter as G2, G100, or G1000 plants, respectively). At steady state, the influx of 13NH4+ was determined to be 1.31, 5.78, and 10.11 [mu]mol g-1 fresh weight h-1, respectively, for G2, G100, and G1000 plants; efflux was 11, 20, and 29%, respectively, of influx. The NH4+ flux to the vacuole was calculated to be between 1 and 1.4 [mu]mol g-1 fresh weight h-1. By means of 13NH4+ efflux analysis, three kinetically distinct phases (superficial, cell wall, and cytoplasm) were identified, with t1/2 for 13NH4+ exchange of approximately 3 s and 1 and 8 min, respectively. Cytoplasmic [NH4+] was estimated to be 3.72, 20.55, and 38.08 mM for G2, G100, and G1000 plants, respectively. These concentrations were higher than vacuolar [NH4+], yet 72 to 92% of total root NH4+ was located in the vacuole. Distributions of newly absorbed 13NH4+ between plant parts and among the compartments were also examined. During a 30-min period G100 plants metabolized 19% of the influxed 13NH4+. The remainder (81%) was partitioned among the vacuole (20%), cytoplasm (41%), and efflux (20%). Of the metabolized 13N, roughly one-half was translocated to the shoots.     

Analysis of 13NH4+ Efflux in Spruce Roots (A Test Case for Phase Identification in Compartmental Analysis)

13NH4+-efflux analyses were conducted with roots of intact Picea glauca (Moench) Voss. seedlings at external NH4+ concentrations of 100 [mu]M and 1.5 mM. Three kinetically distinct phases were identified with half-lives of exchange of approximately 2 s, 30 s, and 14 min. The presumed identities of the subcellular compartments corresponding to these phases were confirmed by several techniques, including pretreatment of roots (a) at 75[deg]C or with SDS, (b) with [alpha]-keto-glutarate or L-methionine-DL-sulfoximine, (c) at elevated levels of Ca2+, and (d) at low pH or with Al3+ at low pH. Treatments a and b selectively influenced phase III without affecting phases I and II. Similarly, treatment c selectively perturbed phase II, and treatment d affected phases II and III. Based on these findings and the assumption of an in-series arrangement of root cell compartments, it was concluded that phase III corresponded to the cytoplasm, phase II corresponded to the Donnan free space, and phase I corresponded to a film of solution adhering to the root surface.     

Glucose-induced increase in cytoplasmic pH in pancreatic beta-cells is mediated by Na+/H+ exchange, an effect not dependent on protein kinase C.

Glucose-induced changes in cytoplasmic pH (pHi) were investigated using pancreatic beta-cells isolated from obese hyperglycemic mice. Glucose, at concentrations above 3-5 mM, depolarized the beta-cell and increased pHi, cytoplasmic free Ca2+ ([Ca2+]i), and insulin release. This increase in pHi was dependent on the presence of extracellular Na+ and was inhibited by 5-(N-ethyl-N-isopropyl) amiloride, a blocker of Na+/H+ exchange. Stimulation of protein kinase C with phorbol ester also induced an alkalinization. However, when protein kinase C activity was down-regulated, glucose stimulation still induced alkalinization. At 20 mM glucose, 10 mM NH4Cl induced a marked rise in pHi, paralleled by repolarization, inhibition of electrical activity, and decreases in both [Ca2+]i and insulin release. Reduction in [Ca2+]i was prevented by 200 microM tolbutamide, but not by 10 mM tetraethylammonium. At 4 mM glucose, NH4Cl induced a transient increase in insulin release, without changing [Ca2+]i. Exposure of beta-cells to 10 mM sodium acetate caused a persistent decrease in pHi, an effect paralleled by a small transient increase in [Ca2+]i. Acidification per se did not change the beta-cell sensitivity to glucose, not excluding that the activity of the ATP-regulated K+ channels may be modulated by changes in pHi.     

Ammonium Uptake by Rice Roots (III. Electrophysiology)

The transmembrane electrical potential differences ([delta][psi]) were measured in epidermal and cortical cells of intact roots of 3-week-old rice (Oryza sativa L. cv M202) seedlings grown in 2 or 100 [mu]M NH4+ (G2 or G100 plants, respectively). In modified Johnson's nutrient solution containing no nitrogen, [delta][psi] was in the range of -120 to -140 mV. Introducing NH4+ to the bathing medium caused a rapid depolarization. At the steady state, average [delta][psi] of G2 and G100 plants were -116 and -89 mV, respectively. This depolarization exhibited a biphasic response to external NH4+ concentration similar to that reported for 13NH4+ influx isotherms (M.Y. Wang, M.Y. Siddiqi, T.J. Ruth, A.D.M. Glass [1993] Plant Physiol 103: 1259-1267). Plots of membrane depolarization versus 13NH4+ influx were also biphasic, indicating distinct coupling processes for the two transport systems, with a breakpoint between two concentration ranges around 1 mM NH4+. The extent of depolarization was also influenced by nitrogen status, which was larger for G2 plants than for G100 plants. Depolarization of [delta][psi] due to NH4+ uptake was eliminated by a protonophore (carboxylcyanide-m-chlorophenylhydrazone), inhibitors of ATP synthesis (sodium cyanide plus salicylhydroxamic acid), or an ATPase inhibitor (diethylstilbestrol). The results of these observations are discussed in the context of the mechanisms of NH4+ uptake by high- and low-affinity transport systems operating across the plasma membranes of root cells.     

Methylammonium as a Transport Analog for Ammonium in Tomato (Lycopersicon esculentum L.)

Methylammonium (CH3NH3+) has been widely used as an analog of ammonium (NH4+) for examining transport in bacteria and fungi. We compared the kinetics of root CH3NH3+ and NH4+ uptake from solution culture in intact tomato (Lycopersicon esculentum cv T5) plants. Efflux of NH4+ and CH3NH3+ was negligible. The apparent maximum rate of absorption (apparent Vmax) was similar for NH4+ and CH3NH3+, but the apparent affinity (apparent Km) was about 10-fold greater for NH4+ than for CH3NH3+. In characterizing the interaction between NH4+ and CH3NH3+ transport, we used [15N]NH4+ and [14C]CH3NH3+ as well as improved methods for analysis of nonisotopic CH3NH3+ and NH4+. CH3NH3+ acted as an inhibitor of NH4+ influx. Relatively low concentrations of NH4+ strongly inhibited CH3NH3+ influx. Treatments with 1 mM methionine sulfoximine that blocked NH4+ assimilation had little influence on NH4+ inhibition of CH3NH3+ influx. These results suggest that the two ions share a common transport system in tomato, but because this transport system has a much greater affinity for NH4+, CH3NH3+ may be used as a transport analog only when ambient concentrations of NH4+ are very low.     

NO3- and ClO3- fluxes in the chl1-5 mutant of Arabidopsis thaliana. Does the CHL1-5 gene encode a low-affinity NO3- transporter?

The CHL1 gene is considered to encode a low-affinity transport system (LATS) for NO3- in Arabidopsis thaliana (Y.-F. Tsay, J.I. Schroeder, K.A. Feldmann, N.M. Crawford [1993] Cell 72: 705-713). However, the anticipated reduced NO3- uptake by the LATS associated with loss of CHL1 gene activity in chl1-5 deletion mutants was evident only when plants were grown on NH4NO3. When KNO3 was the sole N source, NO3- accumulation and short-term tracer influx (using 13NO3- and 15NO3-) in leaves and roots of wild-type and mutant plants were essentially identical. Nevertheless, root uptake of 36CIO3- by the LATS and CIO3- accumulation in roots and shoots of mutant plants were significantly lower than in wild-type plants when grown on KNO3. One explanation for these results is that a second LATS is able to compensate for the chl1-5 deficiency in KNO3-grown plants. Growth on NH4NO3 may down-regulate the second LATS enough that the anticipated difference in NO3- uptake becomes apparent.     

A comparative kinetic analysis of nitrate and ammonium influx in two early-successional tree species of temperate and boreal forest ecosystems

Root NO₃ ^? and NH₄ ⁺ influx systems of two early‐successional species of temperate (trembling aspen: Populus tremuloides Michx.) and boreal (lodgepole pine: Pinus contorta Dougl. ex Loud. var. latifolia Engelm.) forest ecosystems were characterized. NO₃ ^? and NH₄ ⁺ influxes were biphasic, consisting of saturable high‐affinity (HATS) and constitutive non‐saturable low‐affinity transport systems (LATS) that were evident at low and relatively high N concentrations, respectively. NO₃ ^? influx via HATS was inducible (IHATS); nitrate pre‐treatment resulted in 8–10‐fold increases in the V_max for influx in both species. By contrast, HATS for NH₄ ⁺ were entirely constitutive. In both species, V_max values for NH₄ ⁺ influx were higher than those for NO₃ ^? uptake; the differences were larger in pine (6‐fold) than aspen (1·8‐fold). In aspen, the K_m for NH₄ ⁺ influx by HATS was approximately 3‐fold higher than for IHATS NO₃ ^? influx, while in pine the K_m for IHATS NO₃ ^? influx was approximately 3‐fold higher than for NH₄ ⁺ influx. The aspen IHATS for NO₃ ^? influx appeared to be more efficient than that of pine (V_max values for aspen being approximately 10‐fold higher and K_m values being approximately 13‐fold lower than for pine). By contrast, only small differences in values for the NH₄ ⁺ HATS were evident between the two species. The kinetic parameters observed here probably result from adaptations to the N availabilities in their respective natural habitats; these may contribute to the distribution and niche separation of these species.     

Potassium uptake supporting plant growth in the absence of AKT1 channel activity: Inhibition by ammonium and stimulation by sodium.

A transferred-DNA insertion mutant of Arabidopsis that lacks AKT1 inward-rectifying K+ channel activity in root cells was obtained previously by a reverse-genetic strategy, enabling a dissection of the K+-uptake apparatus of the root into AKT1 and non-AKT1 components. Membrane potential measurements in root cells demonstrated that the AKT1 component of the wild-type K+ permeability was between 55 and 63% when external [K+] was between 10 and 1,000 microM, and NH4+ was absent. NH4+ specifically inhibited the non-AKT1 component, apparently by competing for K+ binding sites on the transporter(s). This inhibition by NH4+ had significant consequences for akt1 plants: K+ permeability, 86Rb+ fluxes into roots, seed germination, and seedling growth rate of the mutant were each similarly inhibited by NH4+. Wild-type plants were much more resistant to NH4+. Thus, AKT1 channels conduct the K+ influx necessary for the growth of Arabidopsis embryos and seedlings in conditions that block the non-AKT1 mechanism. In contrast to the effects of NH4+, Na+ and H+ significantly stimulated the non-AKT1 portion of the K+ permeability. Stimulation of akt1 growth rate by Na+, a predicted consequence of the previous result, was observed when external [K+] was 10 microM. Collectively, these results indicate that the AKT1 channel is an important component of the K+ uptake apparatus supporting growth, even in the "high-affinity" range of K+ concentrations. In the absence of AKT1 channel activity, an NH4+-sensitive, Na+/H+-stimulated mechanism can suffice.     

Cytosolic potassium homeostasis revisited: <Superscript>42</Superscript>K-tracer analysis in<Emphasis Type="Italic"> Hordeum vulgare</Emphasis> L. reveals set-point variations in [K<Superscript>+</Superscript>]

Current models of potassium acquisition and cytochemical processes in plants assume that potassium concentrations in the cytosol ([K+]cyt) are maintained homeostatically at approximately 100 mM. Here, we use 42K radiotracer data in the model plant species Hordeum vulgare L. (barley) to show that this assumption is incorrect. Our study reveals that [K+]cyt in root cells of intact barley seedlings is held at a minimum of two physiological set points, coinciding with two fundamentally distinct modes of K+ transport, each of which is characterized by a unique network of fluxes to and from the cytosol, and reflects variations in mechanisms and energetics of K+ transport, cytosolic K+ turnover, flux partitioning, and sensitivity to NH4+. Increased external potassium or ammonium concentrations caused a substantial drop in [K+]cyt, as well as a switch from a transport mode dominated by high-affinity, energy-dependent, influx to a mode dominated by channel-mediated fluxes in both directions across the plasma membrane. Our study provides the first subcellular demonstration of the flexibility, rather than strict homeostasis, of cellular K+ maintenance, and of the dynamic interaction between plant membrane fluxes of the two major nutrient cations K+ and NH4+.     

Further characterization of the mechanisms mediating the rise in cytosolic free Na+ in thrombin-stimulated platelets. Evidence for inhibition of the Na+,K(+)-ATPase and for Na+ entry via a Ca2+ influx pathway.

Human platelets were loaded with the fluorescent Na(+)-sensitive dye sodium-binding benzofuran isophtalate (SBFI), and changes in the fluorescence excited at 345 and 385 nm were analyzed after manipulations that evoked predictable changes in the cytosolic Na+ concentration ([Na+]i). Raising [Na+]i by either gramicidin D or monensin specifically increased the fluorescence excited at 345 nm and decreased that excited at 385 nm. Hence, calculation of changes in the 345/385 nm excitation ratio yields an estimate of actual changes in [Na+]i. A transient activation of Na+/H+ exchange evoked by addition of acidified platelets to buffer, pH 7.4, evoked a transient rise in [Na+]i. The re-establishment of basal [Na+]i could be prevented by ouabain, indicating an involvement of the Na+,K(+)-ATPase. Upon stimulation by 0.5 unit/ml of thrombin, [Na+]i immediately increased by 16 +/- 4 mM and this rise continued for at least 60 min after addition of agonist, albeit at a lower rate. This latter sustained rise could not be curtailed by scavenging thrombin by means of hirudin. Addition of ouabain or the phorbol ester 12-O-tetradecanoylphorbol-13-acetate induced a comparable slow rise in the 345/385 excitation ratio. This may indicate a protein kinase C-mediated inhibition by thrombin of the Na+,K(+)-ATPase. In the absence of extracellular Ca2+ (Ca2+o), the [Na+]i gain was augmented to 38 +/- 9 mM. This additional uptake of Na+ was prevented by (i) Mn2+ ions, (ii) La3+ ions, (iii) the blocker of receptor-mediated Ca2+ entry (1-[beta[3-(4-methoxyphenyl)propoxyl]-4-methoxyphenethyl]-1H-im ida zole hydrochloride), and (iv) by hirudin which reversed receptor occupancy by thrombin. These findings suggest that the additional thrombin-induced [Na+]i gain in the absence of Ca2+o is due to Na+ influx through a Ca2+ entry pathway. The increase in [Na+]i in the presence of Ca2+o results from Na+ influx via Na+/H+ exchange.     

Pressure dependence of equilibria and kinetics of Escherichia coli ribosomal subunit association

Equilibria and rates were observed over the ranges 1-1600 atm, 3-10 mM Mg2+, at 60 mM NH4Cl, pH 7.5, 20 degrees C, by light scattering. The main reaction is accurately represented at all conditions by the following phenomenological equations. 30 S + 50 S = 70 S, KA70 = ka/kd = [70 S]/[30 S][50 S] The equilibrium constants obey simple rules: the volume of association, delta VA0, has the constant value 242 +/- 9 ml/mol, independent of pressure, at all Mg2+ concentrations; the derived values of log KA70 at 1 atm increase linearly with log [Mg2+] at a slope of 7.5. In contrast, the rate constants show a clear break at 6 mM Mg2+: below 6 mM, log ka decreases with pressure with a delta Va of 105 +/- 9 ml/mol and increases with log [Mg2+] at a slope of 4.9; above 6 mM, these values are halved; a split can actually be seen at 6 mM Mg2+, near 500 atm. The usual two-step mechanism for second order reactions in solution, which would insert a 70 S' species, either an encounter complex or a true low concentration steady state intermediate, into the above equation can accommodate these results: as [Mg2+] increases, the rate of transformation of 70 S' into 70 S finally predominates over the rate of dissociation of 70 S' into subunits. The bulk of the pressure effects and all of the [Mg2+] dependence arise from the progressive increase in delta GA0 (electrostatic) that occurs when 30, 50, and 70 S particles all lose equivalent fractions of their internal Mg2+ in response to increases in pressure or decreases in [Mg2+].     

Kinetics and stoichiometry of coupled Na efflux and Ca influx (Na/Ca exchange) in barnacle muscle cells

Coupled Na+ exit/Ca2+ entry (Na/Ca exchange operating in the Ca2+ influx mode) was studied in giant barnacle muscle cells by measuring 22Na+ efflux and 45Ca2+ influx in internally perfused, ATP-fueled cells in which the Na+ pump was poisoned by 0.1 mM ouabain. Internal free Ca2+, [Ca2+]i, was controlled with a Ca-EGTA buffering system containing 8 mM EGTA and varying amounts of Ca2+. Ca2+ sequestration in internal stores was inhibited with caffeine and a mitochondrial uncoupler (FCCP). To maximize conditions for Ca2+ influx mode Na/Ca exchange, and to eliminate tracer Na/Na exchange, all of the external Na+ in the standard Na+ sea water (NaSW) was replaced by Tris or Li+ (Tris-SW or LiSW, respectively). In both Na-free solutions an external Ca2+ (Cao)-dependent Na+ efflux was observed when [Ca2+]i was increased above 10(-8) M; this efflux was half-maximally activated by [Ca2+]i = 0.3 microM (LiSW) to 0.7 microM (Tris-SW). The Cao-dependent Na+ efflux was half-maximally activated by [Ca2+]o = 2.0 mM in LiSW and 7.2 mM in Tris-SW; at saturating [Ca2+]o, [Ca2+]i, and [Na+]i the maximal (calculated) Cao-dependent Na+ efflux was approximately 75 pmol#cm2.s. This efflux was inhibited by external Na+ and La3+ with IC50's of approximately 125 and 0.4 mM, respectively. A Nai-dependent Ca2+ influx was also observed in Tris-SW. This Ca2+ influx also required [Ca2+]i greater than 10(-8) M. Internal Ca2+ activated a Nai-independent Ca2+ influx from LiSW (tracer Ca/Ca exchange), but in Tris-SW virtually all of the Cai-activated Ca2+ influx was Nai-dependent (Na/Ca exchange). Half-maximal activation was observed with [Na+]i = 30 mM. The fact that internal Ca2+ activates both a Cao-dependent Na+ efflux and a Nai-dependent Ca2+ influx in Tris-SW implies that these two fluxes are coupled; the activating (intracellular) Ca2+ does not appear to be transported by the exchanger. The maximal (calculated) Nai-dependent Ca2+ influx was -25 pmol/cm2.s. At various [Na+]i between 6 and 106 mM, the ratio of the Cao-dependent Na+ efflux to the Nai-dependent Ca2+ influx was 2.8-3.2:1 (mean = 3.1:1); this directly demonstrates that the stoichiometry (coupling ratio) of the Na/Ca exchange is 3:1. These observations on the coupling ratio and kinetics of the Na/Ca exchanger imply that in resting cells the exchanger turns over at a low rate because of the low [Ca2+]i; much of the Ca2+ extrusion at rest (approximately 1 pmol/cm2.s) is thus mediated by an ATP-driven Ca2+ pump.(ABSTRACT TRUNCATED AT 400 WORDS)