Evidence for tripeptide/H+ co-transport in rabbit renal brush-border membrane vesicles.

L-Phe-L-Pro-L-Ala is a tripeptide which is hydrolysable almost exclusively by dipeptidyl peptidase IV in rabbit renal brush-border membrane vesicles. In order to delineate the mechanism of the transport of an intact tripeptide across the brush-border membrane, we studied the characteristics of the uptake of [3H]Phe-Pro-Ala in membrane vesicles in which the activity of dipeptidylpeptidase IV was completely inhibited by treatment with di-isopropyl fluorophosphate. In these vesicles, uptake of radiolabel from the tripeptide was found to be Na(+)-independent, but was greatly stimulated by an inwardly directed H+ gradient. The H(+)-gradient-dependent radiolabel uptake appeared to be an active process, because the time course of uptake exhibited an overshoot phenomenon. The process was also electrogenic, being stimulated by an inside-negative membrane potential. Under the uptake-measurement conditions there was no detectable hydrolysis of [3H]Phe-Pro-Ala in the incubation medium when di-isopropyl fluorophosphate-treated membrane vesicles were used. Analysis of intravesicular contents revealed that the radiolabel inside the vesicles was predominantly (greater than 90%) in the form of intact tripeptide. These data indicate that the uptake of radiolabel from [3H]Phe-Pro-Ala in the presence of an inwardly directed H+ gradient represents almost exclusively uptake of intact tripeptide. Uphill transport of the tripeptide was also demonstrable in the presence of an inwardly directed Na+ or K+ gradient, but only if nigericin was added to the medium. Under these conditions, nigericin, an ionophore for Na+, K+ and H+, was expected to generate a transmembrane H+ gradient. Uptake of Phe-Pro-Ala in the presence of a H+ gradient was inhibited by di- and tri-peptides, but not by free amino acids. It is concluded that tripeptide/H+ co-transport is the mechanism of Phe-Pro-Ala uptake in rabbit renal brush-border membrane vesicles.     

Chloride transport across rat ileal basolateral membrane vesicles.

The present study was designed to investigate Cl- transport across rat ileal basolateral membranes. Basolateral membrane vesicles were prepared by a well-validated technique. The purity of the basolateral membrane vesicles was verified by marker enzyme studies and by studies of d-glucose and calcium uptake. Cl- uptake was studied by a rapid filtration technique. Neither an outwardly directed pH gradient, nor a HCO3- gradient, or their combination could elicit any stimulation of Cl- transport when compared with no gradient. 4,4-Diisothiocyanostilbene-2,2-disulfonic acid at 5 mM concentration did not inhibit Cl- uptake under gradient condition. Similarly, the presence of the combination of outwardly directed Na+ and HCO3- gradients did not stimulate Cl- uptake compared with the combination of K+ and HCO3- gradients or no HCO3- gradient. This is in contrast to our results in the brush border membranes, where an outwardly directed pH gradient caused an increase in Cl- uptake. Cl- uptake was stimulated in the presence of combined Na+ and K+ gradient. Bumetanide at 0.1 mM concentration inhibited the initial rate of Cl- uptake in the presence of combined Na+ and K+ gradients. Kinetic studies of bumetanide-sensitive Cl- uptake showed a Vmax of 5.6 +/- 0.7 nmol/mg protein/5 sec and a Km of 30 +/- 8.7 mM. Cl- uptake was stimulated by an inside positive membrane potential induced by the ionophore valinomycin in the setting of inwardly directed K+ gradient compared with voltage clamp condition. These studies demonstrate two processes for Cl- transport across the rat ileal basolateral membrane: one is driven by an electrogenic diffusive process and the second is a bumetanide-sensitive Na+/K+/2 Cl- process. Cl- uptake is not enhanced by pH gradient, HCO3- gradient, their combination, or outwardly directed HCO3- and Na+ gradients.     

Sodium gradient-dependent L-glutamate transport is localized to the canalicular domain of liver plasma membranes. Studies in rat liver sinusoidal and canalicular membrane vesicles

The driving forces for L-glutamate transport were determined in purified canalicular (cLPM) and basolateral (i.e. sinusoidal and lateral; blLPM) rat liver plasma membrane vesicles. Initial rates of L-glutamate uptake in cLPM vesicles were stimulated by a Na+ gradient (Na+o greater than Na+i), but not by a K+ gradient. Stimulation of L-glutamate uptake was specific for Na+, temperature sensitive, and independent of nonspecific binding. Sodium-dependent L-glutamate uptake into cLPM vesicles exhibited saturation kinetics with an apparent Km of 24 microM, and a Vmax of 21 pmol/mg X min at an extravesicular sodium concentration of 100 mM. Specific anionic amino acids inhibited L-[3H]glutamate uptake and accelerated the exchange diffusion of L-[3H]glutamate. An outwardly directed K+ gradient (K+i greater than K+o) further increased the Na+ gradient (Na+o greater than Na+i)-dependent uptake of L-glutamate in cLPM vesicles, resulting in a transient accumulation of L-glutamate above equilibrium values (overshoot). The K+ effect had an absolute requirement for Na+. In contrast, in blLPM the initial rates of L-glutamate uptake were only minimally stimulated by a Na+ gradient, an effect that could be accounted for by contamination of the blLPM vesicles with cLPM vesicles. These results indicate that hepatic Na+ gradient-dependent transport of L-glutamate occurs at the canalicular domain of the plasma membrane, whereas transport of L-glutamate across sinusoidal membranes results mainly from passive diffusion. These findings provide an explanation for the apparent discrepancy between the ability of various in vitro liver preparations to transport glutamate and suggest that a canalicular glutamate transport system may serve to reabsorb this amino acid from bile.     

Trans-stimulation and driving forces for GSH transport in sinusoidal membrane vesicles from rat liver

Sinusoidal membrane vesicles from rat liver were employed to study the characteristics of GSH transport. Saturable concentration dependent uptake was best described by the sum of a high and low Km transport. Preloading with GSH markedly stimulated the initial uptake of GSH. GSH transport was electrogenic; uptake was enhanced by an inwardly directed K+ gradient which could be blocked by the K+-channel blocker, Ba2+. The other cations such as Na+, Li+ were poor substitutes for K+. These results therefore show that net GSH transport involves movement of K+.     

Translocation of fatty acids across the basolateral rat liver plasma membrane is driven by an active potential-sensitive sodium-dependent transport system

In previous studies it was shown that hepatocellular uptake of fatty acids is mediated by a specific fatty acid binding membrane protein. To determine now directly the driving forces for their entry into hepatocytes, the uptake of a representative long chain fatty acid, [3H]oleate, by basolateral rat liver plasma membrane vesicles was examined. Influx of oleate was stimulated by increasing the Na+ concentration of the medium. In the presence of an inwardly directed Na+ gradient (NaSCN, NaNO3, NaCl) oleate was accumulated during the initial uptake phase (20 s) at a concentration of 1.4-1.9-fold that at equilibrium (overshoot). This activation of influx was not observed after replacement of Na+ by Li+, K+, or choline+. Na+-dependent oleate uptake was significantly stimulated by creation of a negative intravesicular potential, either by altering the accompanying anions or by valinomycin-induced K+ diffusion potentials, suggesting an electrogenic transport mechanism. Na+-dependent fatty acid uptake was temperature dependent, with maximal overshoots occurring at 37 degrees C, and revealed saturation kinetics with a Km of 83.1 nM and Vmax of 2.9 nmol X min-1 X mg protein-1. These studies demonstrate that the carrier-mediated hepatocellular uptake of fatty acids represents an active potential-sensitive Na+-fatty acid cotransport system.     

Characteristics of D-alanine transport by luminal membrane vesicles from pars convoluta and pars recta of rabbit proximal tubule

Uptake of D-alanine against a concentration gradient has been shown to occur with isolated luminal-membrane vesicles from pars convoluta or pars recta of rabbit proximal tubule. Renal D-alanine transport systems, displaying the following characteristics, were shown: (1) In vesicles from pars convoluta, the uptake of D-alanine was mediated by both Na+-dependent and Na+-independent transport processes. It was found that an inwardly directed H+-gradient could drive the transport of D-alanine into the vesicles both in the presence and absence of Na+. Thus, in addition to Na+, the transport of D-alanine is influenced by the H+-gradient. (2) In vesicles from pars recta, the transient accumulation of D-alanine was strictly dependent on Na+, since no 'overshoot' was ever observed in the absence of Na+. Although the Na+-dependent uptake of D-alanine was stimulated at acid pH, H+ did not substitute for Na+, as it apparently does in pars convoluta, but instead potentiated the Na+ effect. (3) Addition of L-alanine to vesicle preparations, both from pars convoluta and from pars recta, specifically inhibited renal uptake of D-alanine. A comparison between the transport characteristics of D- and L-alanine indicated that these two isomers of alanine probably share common transport systems located along the proximal tubule of rabbit kidney.     

Na+- and K+-dependent uridine transport in rat renal brush-border membrane vesicles

The transport of uridine into rat renal brush-border membrane vesicles was investigated using an inhibitor-stop filtration method. Uridine was not metabolized under these conditions. The rapid efflux of intravesicular uridine was prevented by adding 1 mM phloridzin to the ice-cold stop solution. In the presence of inwardly directed gradients of either Na+ or K+, zero-trans uridine uptake exhibited a transient overshoot phenomenon indicating active transport. The overshoot was much more pronounced with Na+ than K+ and it was not observed when either Na+ or K+ was at equilibrium across the membrane. The K+-induced overshoot was not due to the presence of a membrane potential alone, as an inwardly directed gradient of choline chloride failed to produce it. The amplitude of the overshoot was increased by raising either the Na+ or K+ concentration outside the membrane or by using more lipophilic anions (reactive order was NO3- greater than SCN- greater than Cl- greater than SO4(2-). Zero-trans efflux studies showed that the uridine transport is bidirectional. Li+ could substitute poorly for Na+ but not at all for K+. Stoichiometries of 1:1 and greater than 1:1 were observed for Na+: uridine and K+: uridine coupling, respectively. A preliminary analysis of the interactions between Na+ and K+ for uridine uptake showed complex interactions which can best be explained by the involvement of two different systems for nucleoside transport in the rat renal brush-border membrane, one requiring Na+ and the other K+ as transport coupler.     

Modulation of serotonin uptake kinetics by ions and ion gradients in human placental brush-border membrane vesicles

The modulation of serotonin uptake kinetics by Na+, Cl-, H+, and K+ was investigated in brush-border membrane vesicles prepared from normal human term placentas. The presence of Na+ and Cl- in the external medium was mandatory for the function of the serotonin transporter. In both cases, the initial uptake rate of serotonin was a hyperbolic function of the ion concentration, indicating involvement of one Na+ and one Cl- per transport of one serotonin molecule. The apparent dissociation constant for Na+ and Cl- was 145 and 79 mM, respectively. The external Na+ increased the Vmax of the transporter and also increased the affinity of the transporter for serotonin. The external Cl- also showed similar effects on the Vmax and the Kt, but its effect on the Kt was small compared to that of Na+. The presence of an inside-acidic pH, with or without a transmembrane pH gradient, stimulated the NaCl-dependent serotonin uptake. The effect of internal [H+] on the transport function was to increase the Vmax and decrease the affinity of the transporter for serotonin. The presence of K+ inside the vesicles also greatly stimulated the initial rates of serotonin uptake, and the stimulation was greater at pH 7.5 than at pH 6.5. This stimulation was a hyperbolic function of the internal K+ concentration at both pH values, indicating involvement of one K+ per transport of one serotonin molecule. The apparent dissociation constant for K+ was 5.6 mM at pH 6.5 and 4.0 mM at pH 7.5. The effects of internal [K+] on the uptake kinetics were similar to those of internal [H+].(ABSTRACT TRUNCATED AT 250 WORDS)     

HCO3- transport in basolateral membrane vesicles isolated from rat renal cortex

The mechanism of HCO3- translocation across the proximal tubule basolateral membrane was investigated by testing for Na+-HCO3- cotransport using isolated membrane vesicles purified from rat renal cortex. As indicated by 22Na+ uptake, imposing an inwardly directed HCO3- concentration gradient induced the transient concentrative accumulation of intravesicular Na+. The stimulation of basolateral membrane vesicle Na+ uptake was specifically HCO3(-)-dependent as only basolateral membrane-independent Na+ uptake was stimulated by an imposed hydroxyl gradient in the absence of HCO3-. No evidence for Na+-HCO3- cotransport was detected in brush border membrane vesicles. Charging the vesicle interior positive stimulated net intravesicular Na+ accumulation in the absence of other driving forces via a HCO3(-)-dependent pathway indicating the flow of negative charge accompanies the Na+-HCO3- cotransport event. Among the anion transport inhibitors tested, 4-4'-diisothiocyanostilbene-2,2'-disulfonic acid demonstrated the strongest inhibitor potency at 1 mM. The Na+-coupled transport inhibitor harmaline also markedly inhibited HCO3- gradient-driven Na+ influx. A role for carbonic anhydrase in the mechanism of Na+-HCO3- cotransport is suggested by the modest inhibition of HCO3- gradient driven Na+ influx caused by acetazolamide. The imposition of Cl- concentration gradients had a marked effect on HCO3- gradient-driven Na+ influx which was furosemide-sensitive and consistent with the operation of a Na+-HCO3- for Cl- exchange mechanism. The results of this study provide evidence for an electrogenic Na+-HCO3- cotransporter in basolateral but not microvillar membrane vesicles isolated from rat kidney cortex. The possible existence of an additional basolateral membrane HCO3(-)-translocating pathway mediating Na+-HCO3- for Cl- exchange is suggested.     

Modulation of salt permeabilities of intestinal brush-border membrane vesicles by micromolar levels of internal calcium

A possible modulation of ion permeabilities of rat intestinal brush-border membrane vesicles by Ca2+, a putative second messenger of salt secretion, was explored by three independent methods: (1) measurements of [3H]glucose accumulation driven by a Na+ gradient; (2) stopped-flow spectrophotometry of salt-induced osmotic swelling; (3) 86Rb+, 22Na+ and 36Cl- flux measurements. Cytoskeleton-deprived membrane vesicles were prepared from isolated brushborders by thiocyanate treatment. Intravescicular Ca2+ levels were varied by preincubating vesicles in Ca-EGTA buffers in the presence of the Ca2+-ionophore A23187. At Ca2+free greater than 10(-5) M, initial Na+-dependent glucose uptake in the presence of a 0.1 M NaSCN gradient (but not in its absence) was inhibited by about 50 per cent as compared to EGTA alone (ED50 approximately equal to 10(-6) M Ca2+). By contrast, initial rates of 22Na+ uptake and reswelling rates of vesicles exposed to a NaSCN gradient were increased at least 2-fold by 10(-5) M Ca2+free. Both observations are compatible with a Ca2+-induced increase of the Na+-permeability of the vesicle membrane. The modulation of ion transport was fully reversible and critically dependent on internal Ca2+, suggesting a localization of Ca2+-sensor sites at the inner surface of the microvillous membrane. As shown by radiotracer and osmotic swelling measurements, micromolar Ca2+ additionally increased the flux rate of K+, Rb+, Cl- and NO-3 but did not change the membrane permeability for small uncharged molecules, including glucose and mannitol. The effect of Ca2+ on ion permeabilities could be blocked by Ba2+ (10(-3) M) or Mg2+ (10(-2) M), but not by amiloride (10(-3) M), apamin (2 X 10(-7) M), trifluoperazine (10(-4) M) or quinine (5 X 10(-4) M). At present it is unclear whether Ca2+ activates a nonselective cation and anion channel or multiple highly selective channels in the vesicle membrane.     

Biotin uptake mechanisms in brush-border and basolateral membrane vesicles isolated from rabbit kidney cortex

Biotin transport was studied using brush-border and basolateral membrane vesicles isolated from rabbit kidney cortex. An inwardly directed Na+ gradient stimulated biotin uptake into brush-border membrane vesicles and a transient accumulation of the anion against its concentration gradient was observed. In contrast, uptake of biotin by basolateral membrane vesicles was found to be Na+-gradient insensitive. Generation of a negative intravesicular potential by valinomycin-induced K+ diffusion potentials or by the presence of Na+ salts of anions of different permeabilities enhanced biotin uptake by brush-border membrane vesicles, suggesting an electrogenic mechanism. The Na+ gradient-dependent uptake of biotin into brush-border membrane vesicles was saturable with an apparent Km of 28 microM. The Na+-dependent uptake of tracer biotin was significantly inhibited by 50 microM biotin, and thioctic acid but not by 50 microM L-lactate, D-glucose, or succinate. Finally, the existence in both types of membrane vesicles of a H+/biotin- cotransport system could not be demonstrated. These results are consistent with a model for biotin reabsorption in which the Na+/biotin- cotransporter in luminal membranes provides the driving force for uphill transport of this vitamin.     

Dicarboxylate transport in human placental brush-border membrane vesicles

Pathways for transport of dicarboxylic acid metabolites by human placental epithelia were investigated using apical membrane vesicles isolated by divalent cation precipitation. The presence of Na+/dicarboxylate cotransport was assessed directly by [14C]succinate tracer flux measurements and indirectly by fluorescence determinations of voltage sensitive dye responses. The imposition of an inwardly directed Na+ gradient stimulated vesicle uptake of succinate achieving levels approximately 5-fold greater than those observed at equilibrium. The increased succinate uptake was specific for Na+ as no stimulation was observed in the presence of Li+, K+ or choline+ gradients. In addition to concentrative accumulation of succinate, a direct coupling of Na+/succinate cotransport was suggested by the absence of a sizeable conductive pathway for succinate uptake and decreased succinate uptake levels associated with a more rapid decay of an imposed Na+ gradient. Na+ gradient-driven succinate uptake was not the result of parallel Na+/H+ and succinate/OH- exchange activities but was reduced by the Na+-coupled inhibitor harmaline. The voltage sensitivity of Na+ gradient-driven succinate uptake suggests Na+/succinate cotransport is electrogenic occurring with net transfer of positive charge. Substrate-specificity studies suggest the tricarboxylic acid cycle intermediates as candidates for transport by the Na+-coupled pathway. Decreasing pH increased the citrate-induced inhibition of succinate uptake suggesting divalent citrate as the preferred substrate for transport. Initial rate determinations of succinate uptake indicate succinate interacts with a single saturable site (Km 33 microM) with a maximal transport rate of 0.5 nmol/mg per min.     

Calcium transport mechanisms in basolateral plasma membrane-enriched vesicles from rat parotid gland.

Ca2+ transport was studied by using basolateral plasma membrane vesicles from rat parotid gland prepared by a Percoll gradient centrifugation method. In these membrane vesicles, there were two Ca2+ transport systems; Na+/Ca2+ exchange and ATP-dependent Ca2+ transport. An outwardly directed Na+ gradient increased Ca2+ uptake. Ca2+ efflux from Ca2+-preloaded vesicles was stimulated by an inwardly directed Na+ gradient. However, Na+/Ca2+ exchange did not show any 'uphill' transport of Ca2+ against its own gradient. ATP-dependent Ca2+ transport exhibited 'uphill' transport. An inwardly directed Na+ gradient also decreased Ca2+ accumulation by ATP-dependent Ca2+ uptake. The inhibition of Ca2+ accumulation was proportional to the external Na+ level. Na+/Ca2+ exchange was inhibited by monensin, tetracaine and chlorpromazine, whereas ATP-dependent Ca2+ transport was inhibited by orthovanadate, tetracaine and chlorpromazine. Oligomycin had no effect on either system. These results suggest that in the parotid gland cellular free Ca2+ is extruded mainly by an ATP-dependent Ca2+ transport system, and Na+/Ca2+ exchange may modify the efficacy of that system.     

Cl(-)-HCO3- exchange in rat renal basolateral membrane vesicles

Pathways for HCO3- transport across the basolateral membrane were investigated using membrane vesicles isolated from rat renal cortex. The presence of Cl(-)-HCO3- exchange was assessed directly by 36Cl- tracer flux measurements and indirectly by determinations of acridine orange absorbance changes. Under 10% CO2/90% N2 the imposition of an outwardly directed HCO3- concentration gradient (pHo 6/pHi 7.5) stimulated Cl- uptake compared to Cl- uptake under 100% N2 in the presence of a pH gradient alone. Mediated exchange of Cl- for HCO3- was suggested by the HCO3- gradient-induced concentrative accumulation of intravesicular Cl-. Maneuvers designed to offset the development of ion-gradient-induced diffusion potentials had no significant effect on the magnitude of HCO3- gradient-driven Cl- uptake further suggesting chemical as opposed to electrical Cl(-)-HCO3- exchange coupling. Although basolateral membrane vesicle Cl- uptake was observed to be voltage sensitive, the DIDS insensitivity of the Cl- conductive pathway served to distinguish this mode of Cl- translocation from HCO3- gradient-driven Cl- uptake. No evidence for K+/Cl- cotransport was obtained. As determined by acridine orange absorbance measurements in the presence of an imposed pH gradient (pHo 7.5/pHi 6), a HCO3- dependent increase in the rate of intravesicular alkalinization was observed in response to an outwardly directed Cl- concentration gradient. The basolateral membrane vesicle origin of the observed Cl(-)-HCO3- exchange activity was verified by experiments performed with purified brush-border membrane vesicles. In contrast to our previous observations of the effect of Cl- on HCO3- gradient-driven Na+ uptake suggesting a basolateral membrane Na+-HCO3- for Cl- exchange mechanism, no effect of Na+ on Cl-HCO3- exchange was observed in the present study.     

ATP-dependent and DCCD-insensitive Cl- uptake by membrane vesicles from the rat brain plasma membrane fractions

ATP-dependent Cl- uptake by membrane vesicles from the rat brain plasma membrane fractions was not affected by the addition of 40 mM of K+, Na+ or HCO3- to the assay medium. Na+ and K+ did not alter the uptake even in the presence of a K+ ionophore, valinomycin (10 microM), or a H+/K+ exchanger, nigericin (10 microM), whereas in the presence of both of these ionophores, K+, but not Na+, reduced the Cl- uptake. Inhibitors of proton pump activity, N,N'-dicyclohexylcarbodiimide (1 mM) and 5-(N,N-hexamethylene)amiloride (40 microM), however, did not affect the Cl- uptake. These findings suggest the presence of a primary Cl- transport system probably associated with passive H+ flux in the brain plasma membranes.     

Functional reconstitution of the gamma-aminobutyric acid transporter from synaptic vesicles using artificial ion gradients.

The gamma-aminobutyric acid transporter of rat brain synaptic vesicles was reconstituted in proteoliposomes, and its activity was studied in response to artificially created membrane potentials or proton gradients. Changes of the membrane potential were monitored using the dyes oxonol VI and 3,3'-diisopropylthiodicarbocyanine iodide, and changes of the H+ gradient were followed using acridine orange. An inside positive membrane potential was generated by the creation of an inwardly directed K+ gradient and the subsequent addition of valinomycin. Under these conditions, valinomycin evoked uptake of [3H]GABA which was saturable. Similarly, [3H]glutamate uptake was stimulated by valinomycin, indicating that both transporters can be driven by the membrane potential. Proton gradients were generated by the incubation of K(+)-loaded proteoliposomes in a buffer free of K+ or Na+ ions and the subsequent addition of nigericin. Proton gradients were also generated via the endogenous H+ ATPase by incubation of K(+)-loaded proteoliposomes in equimolar K+ buffer in the presence of valinomycin. These proton gradients evoked nonspecific, nonsaturable uptake of GABA and beta-alanine but not of glycine in proteoliposomes as well as protein-free liposomes. Therefore, transporter activity was monitored using glycine as an alternative substrate. Proton gradients generated by both methods elicited saturable glycine uptake in proteoliposomes. Together, our data confirm that the vesicular GABA transporter can be energized by both the membrane potential and the pH gradient and show that transport can be achieved by artificial gradients independently of the endogenous proton ATPase.     

The role of potassium and chloride ions on the Na+/acidic amino acid cotransport system in rat intestinal brush-border membrane vesicles

The Na+/L-glutamate (L-aspartate) cotransport system present at the level of rat intestinal brush-border membrane vesicles is specifically activated by the ions K+ and Cl-. The presence of 100 mM K+ inside the vesicles drastically enhances the uptake rate and the transient intravesicular accumulation (overshoot) of the two acidic amino acids. It has been demonstrated that the activation of the transport system depended only in the intravesicular K+ concentration and that in the absence of any sodium gradient, an outward K+ gradient was unable to influence the Na+/acidic amino acid transport system. It was also found that Cl- could specifically activate the Na+-dependent L-glutamate (L-aspartate) uptake either in the presence or in the absence of K+. Also the effect of Cl- was observed only in the presence of an inward Na+ gradient and it was noted to be higher when chloride ion was present on both sides of the membrane vesicles. No influence (activation or accumulation) was observed in the absence of the Na+ gradient and in the presence of chloride gradient. L-Glutamate uptake measured in the presence of an imposed diffusion potential and in the presence of K+ or Cl- did not show any translocation of net charge.     

Mechanisms of taurocholate transport in canalicular and basolateral rat liver plasma membrane vesicles. Evidence for an electrogenic canalicular organic anion carrier

The driving forces for taurocholate transport were determined in highly purified canalicular (cLPM) and basolateral rat liver plasma membrane (LPM) vesicles. Alanine transport was also examined for comparison. Inwardly directed Na+ but not K+ gradients transiently stimulated [3H]taurocholate (1 microM) and [3H]alanine (0.2 mM) uptake into basolateral LPM 3-4- fold above their respective equilibrium values (overshoots). Na+ also stimulated [3H]taurocholate countertransport and tracer exchange in basolateral LPM whereas valinomycin-induced inside negative K+ diffusion potentials stimulated alanine uptake but had no effect on taurocholate uptake. In contrast, in the "right-side out" oriented cLPM vesicles, [3H]taurocholate countertransport and tracer exchange were not dependent on Na+. Efflux of [3H]taurocholate from cLPM was also independent of Na+ and could be trans-stimulated by extra-vesicular taurocholate. Furthermore, an inside negative valinomycin-mediated K+ diffusion potential inhibited taurocholate uptake into and stimulated taurocholate efflux from the cLPM vesicles. These studies provide direct evidence for a "carrier mediated" and potential-sensitive conductive pathway for the canalicular excretion of taurocholate. In addition, they confirm the presence of a possibly electroneutral Na+-taurocholate cotransport system in basolateral membranes of the hepatocyte.     

Characterization of Na+-dependent phosphate transport in cardiac sarcolemmal vesicles

Pi uptake by purified bovine cardiac sarcolemmal vesicles was stimulated by an inwardly directed Na+ gradient, but not by such gradients of K+, Rb+, Li+, and choline. When Na+ was present both inside and outside the vesicles, or when Na+ gradient was dissipated by monensin, the Na+-dependent Pi uptake increased with time, reached a peak, and then declined approaching a steady state. The initial rate of Na+-dependent Pi uptake was a saturable function of Pi concentration (Km = 0.5 mM). These findings indicate the existence of a Na+,Pi-cotransporter in the sarcolemma. The Na+-activation curve of the Pi uptake exhibited positive cooperativity, suggesting the requirement for multiple Na+ binding to the functional unit of the carrier. The initial rate of Na+-dependent Pi uptake decreased as extra-vesicular pH increased in the range of 5.5-8.7. The uptake rate increased under conditions that are known or expected to generate an inside-negative membrane potential, indicating that Pi uptake is accompanied by the uptake of positive charge. These results suggest the electrogenic cotransports of two Na+ and one H2PO4-. We conclude that this cotransporter catalyzes the secondary active transport of Pi across the cardiac plasma membrane and regulates myocardial energy metabolism. We also suggest that the cotransporter may control intracellular Na+ and thus be involved in the regulation of trans-sarcolemmal Ca2+ movement and cardiac contractility.     

Effects of medium amino acids on ouabain-sensitive 86Rb+ -uptake and membrane-potential dependent [3H]tetraphenylphosphonium accumulation in Friend erythroleukemia cells

The effects of amino acids present in minimal essential medium were investigated on 86Rb+ -fluxes and on the membrane-potential dependent accumulation of the lipophilic cation [3H]tetraphenylphosphonium (TTP+) in logarithmically growing Friend erythroleukemia cells. The ouabain-sensitive 86Rb+ -uptake measured as well in complete growth medium as in Earle's balanced salt solution (EBSS) with amino acid composition present in growth medium, was 3 to 4-fold increased in comparison to the 86Rb+-uptake measured in pure EBSS only. The Na+,K+,2Cl- -cotransport measured as piretanide-sensitive 86Rb+-uptake was reduced in the presence of amino acids. Stimulation of the ouabain-sensitive 86Rb+ -uptake could be brought about by the addition of alanine alone or of the sodium ionophore monensin. In spite of the activation of the Na+,K+ -pump the membrane-potential dependent accumulation of [3H]TPP+ was about 40 per cent reduced in the presence of medium amino acids indicating a decreased membrane potential under these conditions. On the other hand, monensin which induces an electrically silent Na+ -influx via Na+/H+ -exchange was shown to hyperpolarize the membrane on the basis of [3H]TPP+-accumulation. These results suggest that the intensive uptake of neutral amino acids by Na+-cotransport in rapidly growing cells may be responsible for both stimulation of the Na+,K+ -pump and decrease in the transmembrane potential.