Interaction between dopamine influx and efflux in rat striatal synaptosomes

Exchange release has previously been proposed as the mechanism by which dopamine is transported over the synaptosomal membrane. An increase in carrier-mediated dopamine release should therefore result in an enhanced rate of synaptosomal dopamine uptake. In order to test this hypothesis, rat striatal synaptosomes were incubated with ¹⁴C-dopamine until equilibrium. Then, the ¹⁴C-dopamine concentration in the medium was reduced in order to elicit various rates of net dopamine efflux, while influx was monitored using tracer amounts of ³H-dopamine. Dopamine release was concentration dependent and saturable and thus may be carrier-mediated. In contrast to that expected for a mechanism of exchange release, dopamine influx was depressed as compared to equilibrium conditions. Furthermore, nomifensine, a specific inhibitor of dopamine influx, did not attenuate dopamine efflux. It is concluded that dopamine transport over the synaptosomal membrane may not be via a mechanism of strict exchange release.     

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.     

Sodium influx at the outer surface of frog skin

Summary The unidirectional sodium influx across the outside surface of the frog skin epithelium was measured. The method was identical to the one described by Biber and Curran [4] except that mannitol instead of inulin was used as the indicator for the amount of tracer containing test solution remaining on the surface of the skin after blotting. The space of distribution for³H-mannitol is about twice as large as the corresponding space for inulin after 32-sec exposure to the tracer. At a sodium concentration of 6.7mm the sodium influx determined with inulin as marker for the test solution is 0.146 Equiv hr^–1cm^–2 larger than the influx measured in the same preparation with mannitol. This difference increases in proportion to the sodium concentration and can be ascribed to diffusion of sodium into a space which is accessible to mannitol but not to inulin during a 30-sec interval. Hence, nearly two-thirds of the previously described linear component of the sodium influx proceeds, as was suspected previously, into a compartment which is not directly connected to net sodium transport across the skin. The nature of the remaining one-third of this linear compartment is not clear but previous experiments suggest that it is also not involved in net sodium transport.     

Calcium influx at the plasmalemma of Chara corallina

Influx of ⁴⁵Ca into internodal cells of Chara corallina has been measured, using short uptake times, and a wash in ice-cold La³⁺-containing pondwater after the labelling period to overcome the difficulty of distinguishing extracellular tracer from that in the cell. Over 5–15 min the uptake was linear with time, through the origin. The basal influx from 0.1 mM Ca²⁺ externally was 0.25–0.5 pmol·cm^-2·s^-1, but some batches of cells showed higher fluxes. The influx was markedly stimulated by depolarisation in pondwater containing 20 mM K⁺. In cells in which the control flux was less than about 0.5 pmol·cm^-2·s^-1 there was no effect of 50 M nifedipine. In cells in which the control flux was greater than about 0.5 pmol·cm^-2·s^-1 (whether by natural variability, pretreatment, or by depolarisation in 20 mM K⁺), the flux was reduced by 50 M nifedipine to a value in the range 0.25–0.59 pmol·cm^-2·s^-1. It is suggested that two types of Ca-channel are probably involved, both opening on depolarisation, but only one sensitive to nifedipine. The flux was inhibited by 10 M BAY K 8644, which in animal cells more commonly opens Ca-channels. The apparent influx measured over long uptake times was much reduced, and the kinetics indicated filling a pool of apparent size about 1.45 nmol·cm^-2 with a halftime of about 38 min, probably representing cytoplasmic stores. It is argued that in spite of the very small pool of (free+bound) cytoplasmic Ca²⁺ the measured influx is a reasonable estimate of the influx at the plasmalemma.Abbreviations 0.4K-APW6 artificial pondwater, pH 6, containing 0.4 mM KCl - 20 K-APW6 artificial pondwater, pH 6, containing 20 mM KCl - Ca_o external Ca²⁺     

Calcium influx in contracting and paralyzed frog twitch muscle fibers

Calcium uptake produced by a potassium contracture in isolated frog twitch fibers was 6.7 +/- 0.8 pmol in 0.7 cm of fiber (mean +/- SEM, 21 observations) in the presence of 30 microM D600. When potassium was applied to fibers paralyzed by the combination of 30 microM D600, cold, and a prior contracture, the calcium uptake fell to 3.0 +/- 0.7 pmol (11): the fibers were soaked in 45Ca in sodium Ringer for 3 min before 45Ca, in a potassium solution, was added for 2 min; each estimate of uptake was corrected for 5 min of resting influx, measured from the same fiber (average = 2.3 +/- 0.3 pmol). The calcium influx into paralyzed fibers is unrelated to contraction. This voltage-sensitive, slowly inactivating influx, which can be blocked by 4 mM nickel, has properties similar to the calcium current described by several laboratories. The paired difference in calcium uptake between contracting and paralyzed fibers, 2.9 +/- 0.8 pmol (16), is a component of influx related to contraction. Its size varies with contracture size and it occurs after tension production: 45Ca applied immediately after contracture is taken up in essentially the same amounts as 45Ca added before contraction. This delayed uptake is probably a "reflux" refilling a binding site on the cytoplasmic side of the T membrane, which had been emptied during the prior contracture, perhaps to initiate it. We detect no component of calcium uptake related to excitation-contraction coupling occurring before or during a contracture.     

Calcium influx determines the muscular response to electrotransfer

Cell membrane permeabilization by electric pulses (electropermeabilization), results in free exchange of ions across the cell membrane. The role of electrotransfer-mediated Ca(2+)-influx on muscle signaling pathways involved in degeneration (β-actin and MurF), inflammation (IL-6 and TNF-α), and regeneration (MyoD1, myogenin, and Myf5) was investigated, using pulse parameters of both electrochemotherapy (8 HV) and DNA delivery (HVLV). Three pulsing conditions were used: 8 high-voltage pulses (8 HV), resulting in large permeabilization and ion flux, and a combination of one high-voltage pulse and one low-voltage pulse (HVLV), either alone or in combination with injection of DNA. Mice and rats were anesthetized before pulsing. At the times given, animals were killed, and intact tibialis cranialis muscles were excised for analysis. Uptake of Ca(2+) was assessed using (45)Ca as a tracer. Using gene expression analyses and histology, we showed a clear association between Ca(2+) influx and muscular response. Moderate Ca(2+) influx induced by HVLV pulses results in activation of pathways involved in immediate repair and hypertrophy. This response could be attenuated by intramuscular injection of EGTA reducing Ca(2+) influx. Larger Ca(2+) influx as induced by 8-HV pulses leads to muscle damage and muscle fiber regeneration through recruitment of satellite cells. The extent of Ca(2+) influx determines the muscular response to electrotransfer and, thus, the success of a given application. In the case of electrochemotherapy, in which the objective is cell death, a large influx of Ca(2+) may be beneficial, whereas for DNA electrotransfer, muscle recovery should occur without myofiber loss to ensure preservation of plasmid DNA.     

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)     

Cold activation of Na influx through the Na-H exchange pathway in guinea pig red cells

Summary Previous work showed that amiloride partially inhibits the net gain of Na in cold-stored red cells of guinea pig and that the proportion of unidirectional Na influx sensitive to amiloride increases dramatically with cooling. This study shows that at 37°C amiloride-sensitive (AS) Na influx in guinea pig red blood cells is activated by cytoplasmic H⁺, hypertonic incubation, phorbol ester in the presence of extracellular Cat²⁺ and is correlated with cation-dependent H⁺ loss from acidified cells. Cytoplasmic acidification increases AS Na efflux into Na-free medium. These properties are consistent with the presence of a Na-H exchanger with a H⁺ regulatory site. Elevation of cytoplasmic free Mg^2– above 3 mm greatly increases AS Na influx: this correlates with a Na-dependent loss of Mg^2–, indicating the presence of a Na-Mg exchanger.At 20°C activators of Na-H exchange have little or no further stimulatory effect on the already elevated AS Na influx. AS Na influx is much larger than either Na-dependent H⁺ loss or AS Na efflux at 20°C. The affinity of the AS Na influx for cytoplasmic H⁺ is greater at 20°C than at 37°C. Depletion of cytoplasmic Mg²⁺ does not abolish the high AS Na influx at 20°C.Thus, elevation of AS Na influx with cooling appears to be due to increased activity of a Na-H exchanger (operating in a slippage mode) caused by greater sensitivity to H⁺ at a regulatory site.     

Calcium influx at the plasmalemma of isolated guard cells of Commelina communis

The influx of ⁴⁵Ca into isolated guard cells of Commelina communis L. has been measured, using short uptake times, and washing in ice-cold La³⁺-containing solutions to remove extracellular tracer after the loading period. Over 0.5–4 min the uptake was linear with time, through the origin. Over 20–200M external Ca²⁺ the influx measured with 10–20 mM external KCl was in the range 0.3–2.3 pmol·cm^-2·s^-1 (on the basis of estimated guard-cell area); with only 1 mM KCl externally the ⁴⁵Ca influx was significantly reduced, in the range 0.3–1.1 pmol·cm^-2·s^-1 for external Ca²⁺ of 50–100 M. The results indicate that the Ca-channel is voltage-sensitive, opening with depolarisation. No consistent effect of the addition of abscisic acid could be found. In different experiments, on the addition of 0.1 mM abscisic acid the Ca²⁺ influx was sometimes stimulated by 28–79%, was sometimes unaffected, and was sometimes inhibited by 16–29%. The results rule out a long-lasting stimulation of ⁴⁵Ca influx by ABA, but they do not rule out a transient stimulation followed by inhibition, perphaps as a consequence of down-regulation of Ca²⁺ influx by increasing cytoplasmic Ca²⁺. The hypothesis that ABA may act via an action on Ca²⁺ influx, increasing cytoplasmic Ca²⁺, with consequent effects on voltage-dependent and Ca²⁺-dependent ion channels in both plasmalemma and tonoplast, is neither proved nor disproved by these results.Abbreviations ABA abscisic acid - Ca_o, K_o external Ca and K concentrations     

Controls on na influx in corn roots

We have investigated the effects of hyperpolarization and depolarization, and the presence of K⁺ and/or Ca²⁺, on ²²Na⁺ influx into corn (Zea mays L.) root segments. In freshly excised root tissue which is injured, Na⁺ influx is unaffected by hyperpolarization with fusicoccin, or depolarization with uncoupler (protonophore), or by addition of K⁺. However, added Ca²⁺ suppresses Na⁺ influx by 60%. In washed tissue which has recovered, Na⁺ influx is doubled over that of freshly excised tissue, and the influx is increased by fusicoccin and suppressed by uncoupler. This energy-linked component of Na⁺ influx is completely eliminated by low concentrations of K⁺, leaving the same level and kind of Na⁺ influx seen in freshly excised roots. The K⁺-sensitive energy linkage appears to be by the carrier for active K⁺ influx. Calcium is equally inhibitory to Na⁺ influx in washed as in fresh tissue. Other divalent cations are only slightly less effective. Net Na⁺ uptake was about 25% of ²²Na⁺ influx, but proportionately the response to K⁺ and Ca²⁺ was about the same.

The constancy of K⁺-insensitive Na⁺ influx under conditions known to hyperpolarize and depolarize suggests that if Na⁺ transport is by means of a voltage-sensitive channel, the rise or fall of channel resistance must be proportional to the rise or fall in potential difference. The alternative is a passive electroneutral exchange of ²²Na⁺ for endogenous Na⁺. The data suggest that an inwardly directed Na⁺ current is largely offset by an efflux current, giving both a small net uptake and isotopic exchange.

     

Na-Ca exchanger as a calcium influx pathway in adrenal glomerulosa cells

When aequorin-loaded glomerulosa cells were incubated in isotonic Na2+-free medium containing N-methyl-D-glucamine instead of NaCl, there was an increase in cytoplasmic free calcium concentration, [Ca2+] c, which was not observed when extracellular calcium concentration was reduced to 1 microM. Upon removal of extracellular sodium, there was nearly five-fold increase in fractional efflux ratio of calcium. The reduction of extracellular sodium resulted in a stimulation of calcium influx rate, the magnitude of which was dependent on extracellular sodium concentration. Similar stimulation of calcium influx was observed when extracellular sodium was replaced with lithium. Nitrendipine did not affect the calcium influx induced by the reduction of extracellular sodium while a derivative of amiloride 3',4'-dichlorobenzamil, which inhibits Na-Ca exchange, attenuated calcium influx observed in sodium-free medium. These results indicate that removal of extracellular sodium leads to an increase in [Ca2+] c by stimulating calcium influx and that calcium enters the cell via Na-Ca exchanger.     

Calcium influx following fertilization of Urechis caupo eggs.

Measurements of ⁴⁵Ca flux into and out of Urechis eggs indicate that, during the first 10 min after insemination, the eggs take up 0.24 pmole of Ca/egg. Total egg Ca measured by atomic absorption (AA) spectroscopy increased by 0.23 pmole of Ca/egg (0.56, 0.79, and 0.76 pmole of Ca/egg for unfertilized, 10-min fertilized, and 60-min fertilized eggs, respectively). Thus, the total change in egg Ca is accounted for by the influx even though the rate of efflux, measured as a release of ⁴⁵Ca from preloaded eggs, increases to twice the unfertilized rate by 15 min. The fertilization influx follows saturation kinetics (K_a = 1.3 mM). It is competitively inhibited by procaine, but is not inhibited by dinitrophenol, mersalyl acid, or ruthenium red. Ten percent of the total Ca influx has occurred by 10 sec, and it is, therefore, the most rapid response to fertilization yet known in these eggs. The influx is also observed in eggs partially activated by insemination in pH 7 seawater (SW); the other fertilization responses, except sperm penetration, do not occur in pH 7 SW. Although Ca influx alone is insufficient to activate the eggs, it may be a prerequisite for cytoplasmic activation and development, inducing other secondary responses which are prevented by low external pH.     

Volume-sensitive K influx in human red cell ghosts

K influx into resealed human red cell ghosts increases when the ghosts are swollen. The influx demonstrates properties similar to volume-sensitive K fluxes present in other cells. The influx is, for the most part, insensitive to the nature of the major intracellular cation and therefore is not a K-K exchange. The influx is much greater when the major anion is Cl than when the major anion is NO3; Cl stimulates the flux and, at constant Cl, NO3 inhibits it. Increase in the influx rate is rapid when shrunken ghosts are swollen or when NO3 is replaced by Cl. The volume-sensitive K influx requires intracellular MgATP at low concentrations, and ATP cannot be replaced by nonhydrolyzable ATP analogues. The volume-sensitive influx is inhibited by Mg2+ and by high concentrations of vanadate, but is stimulated by low concentrations of vanadate. It is not modified by cAMP, the removal of Ca2+ by EGTA, substances that activate protein kinase C, or by inhibition of phosphatidylinositol kinase. The influx is inhibited by neomycin and by trifluoperazine.     

Orthophosphate influx and efflux rates of Chlorella fusca measured in a continuous turbidostat culture with 32P under various conditions

The main objective of the experiments with Chlorella fusca strain 211-8b was to measure, with adequate time resolution, the unidirectional influx rates of phosphate into non-phosphate-starved algae under different steady state conditions (light, temperature, 3-phosphoglycerate influence) or following the addition of several photosynthesis and phosphate transport inhibitors (phenylmercuric acetate, p-chloromercuribenzoate, arsenate). the algae were cultivated in a phosphate rich medium in a continuous turbidostat culture. The phosphate exchange experiments with carrier-free ³²PO ₄ ^3- were performed directly in the continuous culture. The sampling intervals after the tracer addition were 15 s.For a continuous steady state culture grown in the light (25° C) the unidirectional influx rate measured with ³²P is 260 times higher than the net uptake rate (=influx minus efflux rate) calculated from the mass balance using the data of this culture. In all experiments, except the control experiment with trichloroacetic acid killed cells, the specific activity of the intracellular inorganic orthophosphate compartment oscillates around a constant mean value which never reaches the specific activity of the nutrient medium within the duration of the short-term experiments (7.5 min). The inhibitors strongly affect the characteristics of the oscillations. The unidirectional influx rates are constant. Oscillating flushing rates with unlabelled phosphate from a storage compartment have been postulates to explain the oscillations. Oscillating rates from the individual cells are apparently synchronized by an unknown mechanism.     

Mathematical modeling of marker influx and efflux in cells

The tumor promoter, phorbol 12-myristate 13-acetate (PMA), affects the processing of fluid that enters a cell from the ambient medium. Previous work showed that marker accumulates to a higher level in PMA-treated than in untreated cells. Since PMA also affects the physical activity of the membrane and stimulates the normal process of taking up extracellular fluid, called endocytosis, it is important to learn whether the perturbations in fluid processing can be attributed entirely to a change in the cell’s limiting membrane. To this end, a model for fluid uptake and processing was developed and applied to experiments in which a marker for extracellular fluid was added to cells. From previous work on marker accumulation, it was deduced that there were at least two functional compartments involved in fluid movement. Compartment I is a rapidly filling and rapidly recycling compartment. Compartment II is a slowly filling and emptying compartment. Three routes of vesicle traffic must be considered, one mediating influx from the ambient medium into compartment I, a second, efflux from compartment I to the medium, and a third efflux from compartment I into compartment II. Using earlier models for processing, workers found it difficult to estimate rates of movement through either of the latter routes, as well as the volume of compartment I. The difficulty arises from the fact that only one kinetic constant can be estimated directly from data, namely the instantaneous uptake rate. The remaining data depend on measuring the total mass of marker in the cells. Since the concentration of marker in the cell changes continuously, it is advantageous to employ differential equations to simulate the tracer movement. By applying the model to experimental values, we found estimates for all three rates of fluid movement and the volume of compartment I. It is thought that the model will enable us to determine whether apparent alterations in the time course of uptake arise solely from altered properties of the limiting membrane. This revised version submitted December, 2000. Research supported in part by a grant from the National Institutes of Health, R15 CA78322-01.     

Role of Na+/H+ exchange in thrombin- and arachidonic acid-induced Ca2+ influx in platelets

Platelet activation is accompanied by an increase of cytosolic free Ca2+ concentration, [Ca2+]i, (due to both extracellular Ca2+ influx and Ca2+ movements from the dense tubular system) and an Na+ influx associated with H+ extrusion. The latter event is attributable to the activation of Na+/H+ exchange, which requires Na+ in the extracellular medium and is inhibited by amiloride and its analogs. The present study was carried out to determine whether a link exists between Ca2+ transients (measured by the quin2 method and the 45CaCl2 technique) and Na+/H+ exchange activation (studied with the pH-sensitive intracellular probe, 6-carboxyfluorescein) during platelet stimulation. Washed human platelets, stimulated with thrombin and arachidonic acid, showed: (1) a large and rapid [Ca2+]i rise, mostly due to a Ca2+ influx through the plasma membrane; (2) a marked intracellular alkalinization. Both phenomena were markedly inhibited in the absence of extracellular Na+ or in the presence of an amiloride analog (EIPA). Monensin, a cation exchanger which elicits Na+ influx and alkalinization, and NH4Cl, which induces alkalinization only, were able to evoke an increase in [Ca2+]i, mostly as an influx from the extracellular medium. Our results suggest that Ca2+ influx induced by thrombin and arachidonic acid in human platelets is strictly dependent on Na+/H+-exchange activation.     

Calcium influx: an intracellular message of the mitogenic action of insulin-like growth factor-I

When G0-arrested BALB/c 3T3 cells were treated sequentially with platelet-derived growth factor and epidermal growth factor, cells became responsive to insulin-like growth factor-I (IGF-I). In these primed competent cells, 1 nM IGF-I elicited an approximately 3-fold increase in the calcium influx rate. IGF-I-induced calcium influx was relatively slow in onset and continued for at least 2 h in the presence of IGF-I. When a single Ca2+ channel current was studied by the patch-clamp technique using the cell-attached mode, inward currents with unitary conductance of 19 pS were observed in the presence of 1 nM IGF-I in the patch pipette. IGF-I-sensitive inward current was independent of membrane potential and was activated by a high concentration of insulin. Accordingly, 1 nM IGF-I caused a gradual increase in cytoplasmic free calcium concentration measured by fura2. The action of IGF-I on calcium influx was dependent on extracellular calcium, and IGF-I did not stimulate calcium influx when extracellular calcium concentration was reduced to 10 microM. Both cobalt and tetramethrin blocked the action of IGF-I on calcium influx without affecting the binding of 125I-IGF-I. In primed competent cells, IGF-I-stimulated [3H]thymidine incorporation was dependent on extracellular calcium and was attenuated by cobalt and tetramethrin. When cell-bound 125I-IGF-I was cross-linked by use of disuccinimidyl suberate, a 130-kDa protein was radiolabeled. Affinity labeling of the 130-kDa protein, presumably the alpha-subunit of the IGF-I receptor, was blocked by excess amount of unlabeled IGF-I. These results suggest that relatively low concentrations of IGF-I stimulate calcium influx in primed competent BALB/c 3T3 cells by activating a calcium-permeable cation channel via the IGF-I receptor and that calcium influx may be a critical intracellular message of the progression activity of IGF-I.     

Calreticulin couples calcium release and calcium influx in integrin-mediated calcium signaling

The engagement of integrin alpha7 in E63 skeletal muscle cells by laminin or anti-alpha7 antibodies triggered transient elevations in the intracellular free Ca(2+) concentration that resulted from both inositol triphosphate-evoked Ca(2+) release from intracellular stores and extracellular Ca(2+) influx through voltage-gated, L-type Ca(2+) channels. The extracellular domain of integrin alpha7 was found to associate with both ectocalreticulin and dihydropyridine receptor on the cell surface. Calreticulin appears to also associate with cytoplasmic domain of integrin alpha7 in a manner highly dependent on the cytosolic Ca(2+) concentration. It appeared that intracellular Ca(2+) release was a prerequisite for Ca(2+) influx and that calreticulin associated with the integrin cytoplasmic domain mediated the coupling of between the Ca(2+) release and Ca(2+) influx. These findings suggest that calreticulin serves as a cytosolic activator of integrin and a signal transducer between integrins and Ca(2+) channels on the cell surface.     

Improved mathematical model for estimating H+ influx and H+ efflux in plant vacuolar vesicles acidified by ATPase or pyrophosphatase

To adapt to environmental changes, plant cells very likely possess a biochemical system, using vacuoles, for maintaining cytoplasmic pH homeostasis. A simple approach is to estimate the active H(+) influx and H(+) efflux of isolated vacuolar vesicles, although there is no good mathematical model to describe H(+) flux. To establish a new quantitative model, vacuolar vesicles were isolated from hypocotyls of mung bean (Vigna radiata L.), and pyrophosphate (PPi)- or ATP-dependent acidification was monitored using acridine orange. The change of pH inside the vesicles (pH(in)) was calculated using a pH calibration curve relating fluorescence quenching with DeltapH. After formation of a steady state DeltapH, passive H(+) efflux was monitored after terminating pumping with ethylenediaminetetraacetate, and the relative H(+) permeability coefficient (p(H+)) was calculated. The H(+) efflux simulated using the p(H+) corresponded to the H(+) efflux determined experimentally. H(+) influx was then calculated by subtracting the predicted H(+) efflux from the experimental net H(+) influx. H(+) influx into vesicles driven by H(+)-PPase or H(+)-ATPase decreased exponentially as the intravesicular pH(in) decreased, suggesting modulation of pumping by DeltapH, pH(in), or both. Finally, the PPi- or ATP-dependent H(+) accumulation determined experimentally was closely simulated by the predicted H(+) influx and H(+) efflux. The ability to predict H(+) flux under different conditions provides a powerful tool for studying pH homeostasis.     

Vacuolar Fluxes of Chloride and Bromide in Nitella translucens

The kinetics of halide-ion transfer to the vacuole of Nitellatranslucens have been further examined. The percentage of totaltracer found in the vacuole can be expressed as the sum of twocomponents, a fast component important at short times, and aslow component increasing as the level of tracer in the cytoplasmrises. In the individual cells in any given experiment the rate oftransfer to the vacuole in the fast component is a quantizedfraction of the total influx. This statement expresses the factthat in each experiment the cells can be divided into groups,each covering the whole range of influx values and having thesame mean influx, whose mean vacuolar percentages are in theratio 1:2:3 (with also a few cells having higher values of vacuolarpercentage). There appears therefore to be a process of quantizeddischarge to the vacuole from an internal cytoplasmic compartment. Double-labelling with ³⁶Cl and ⁸²Br was used to measure bothfast and slow components in the same cell. Although the bromideinflux was only one-third of the chloride influx from equalexternal concentrations of O.6 mM, the vacuolar percentagesfor bromide and chloride were equal in cells loaded for thesame time in bromide and chloride, whether the loading was fora short or a longer time. Therefore both slow and fast componentsare equal for the two ions, and in cells labelled for a shorttime in bromide and a longer time in chloride, the vacuolarpercentage for bromide can be used as a measure of the fastcomponent for chloride. The contribution of the slow componentto the vacuolar transfer increases with time, but the slopeof its time dependence is proportional to the influx in thecell. It is not quantized. Hence the rate of transfer to thevacuole can be specified only as a fraction of the total influx,and not as an absolute rate, and the exchange with the slowcytoplasmic compartment is very closely linked to the influx.The equality of the slow components of vacuole transfer forbromide and chloride (in spite of very different influxes) isconsistent with the hypothesis that the slow exchange reflectsexchange with pinocytotic vesicles, but is difficult to explainin terms which do not involve a common entry process for salt,in a unit involving both bromide and chloride. The significance of the quantized discharge, and the relationbetween the fast and slow components, are not yet understood.The increase in the slow component as the cell becomes labelledis very steep, and hence even the slow cytoplasmic compartmentcan represent only a part of the cytoplasm, in which the specificactivity is higher than the rest.