The osmotically sensitive potassium and sodium compartments of synaptosomes

1. Synaptosomes are pinched-off nerve terminals whose components can be liberated by osmotic `shock'. A synaptosome preparation run through a Sephadex column that was eluted with an iso-osmotic solution retained its small ions, whereas when the column was eluted hypo-osmotically the small ions were lost. In this way the osmotically sensitive Na<sup>+</sup> and K<sup>+</sup> of synaptosomes were measured. Measurements of the lactate dehydrogenase occluded within the synaptosome were also made. The release of osmotically sensitive Na<sup>+</sup> and K<sup>+</sup> and occluded lactate dehydrogenase had similar characteristics with respect to the degree of osmotic `shock' necessary and the action of lytic agents. 2. The distribution of osmotically sensitive Na⁺, K⁺ and occluded lactate dehydrogenase in the subfractions of a crude mitochondrial preparation was examined. The synaptosome fraction was the richest source of these constituents. 3. On standing at 5° in iso-osmotic solution Na⁺ and K⁺ were lost from synaptosomes, whereas the amount of occluded lactate dehydrogenase remained stable, suggesting that the synaptosome membrane retained its integrity but that Na⁺ and K⁺ diffused through it out of the osmotically sensitive compartment. 4. The uptake of Na⁺ and K⁺ into the osmotically sensitive compartment was examined. At 5° the rates of uptake of Na⁺ and K⁺ were found to be equal to the rates of loss of these ions when correction to a uniform concentration gradient had been made. K⁺ travelled across the membrane slightly faster than Na⁺, the rate of K⁺ movement being about 1·0μμequiv.cm.⁻²sec.⁻¹ under a concentration gradient of 0·1m. Active transport is not thought to contribute to the ion movements under the conditions used. 5. The amount of K⁺ taken up into the osmotically sensitive compartment as a function of the external concentration was examined. Since the uncharged molecule d-[¹⁴C]galactose distributes across the synaptosome membrane similarly to K⁺ there is not thought to be a synaptosomal trans-membrane potential. The volume of the osmotically sensitive compartment was measured by this method and found to agree with estimates of the synaptosomal volume made from morphological studies. In media of low ionic strength synaptosomes exhibit a Donnan effect. 6. It is concluded from these studies that the osmotically sensitive compartment represents the inner volume of the synaptosome, which is completely separated from the outside environment by a diffusion barrier having many of the general properties of a biological membrane.     

Solvent Water for Electrolytes in the Muscle Fiber of the Giant Barnacle

Seven experiments are described which permit estimation of the "solvent water" or the "osmotically active water" of the dissected fiber from the giant barnacle, Balanus nubilus. Each of the first four experiments includes the measurement of a free ion activity in the myoplasm by means of a Na⁺, K⁺, or Cl^- ion-specific microelectrode. The fifth experiment makes use of a membrane potential vs. [K]_o curve. The last two experiments measured fiber water and fiber volume as bath osmolarity was changed. The seven independent estimations of solvent water ranged from 0.64 to 0.72 of fiber water with a mean of 0.68. Since the extracellular space of single fibers was about 7% of fiber water, it was concluded that 25% of analyzable water was not acting as solvent for the osmotically active solutes in the myoplasm.     

MAINTENANCE OF IONS,PROTEINS AND WATER IN LENS FIBER CELLS BEFORE AND AFTER TREATMENT WITH NON-IONIC DETERGENTS

If the plasma membrane and its associated transport proteins are solely responsible for maintenance of the asymmetric solute distribution then disruption of the plasma membrane would quickly lead to the symmetric distribution of all unattached inorganic ions between the cell and the extracellular environment. To test this hypothesis fresh pig lenses were incubated in Hanks ’ balanced salt solution in either absence or presence of non-ionic detergents (0.2 % Triton X-100 or 0.2 % Brij 58). Both detergents caused permeabilization of every lens fiber cell as shown by electron microscopy. The flux kinetics of K⁺, Mg^{2 +}, Na⁺, Ca^{2 +}, water and protein out of and into the permeabilized lens fiber cells was measured. Triton X-100 caused a faster flux rate of all solutes than did Brij 58. The Triton X-100 induced flux of solutes and water was associated with a decrease in lens ATP. Incubation of untreated lenses in solutions of different osmotic pressures at 0 °C demonstrated that the major fraction of lens water was osmotically unresponsive. Thus the asymmetric distribution of solutes in lens fiber cells is dependent on an intact plasma membrane and on a co-operative ATP-dependent association between K⁺, Mg^{2 +}, water and cytomatrix proteins.     

Solute Accumulation in Tobacco Cells Adapted to NaCl

Cells of Nicotiana tabacum L. var Wisconsin 38 adapted to NaCl (up to 428 millimolar) which have undergone extensive osmotic adjustment accumulated Na⁺ and Cl⁻ as principal solutes for this adjustment. Although the intracellular concentrations of Na⁺ and Cl⁻ correlated well with the level of adaptation, these ions apparently did not contribute to the osmotic adjustment which occurred during a culture growth cycle, because the concentrations of Na⁺ and Cl⁻ did not increase during the period of most active osmotic adjustment. The average intracellular concentrations of soluble sugars and total free amino acids increased as a function of the level of adaptation; however, the levels of these solutes did not approach those observed for Na⁺ and Cl⁻. The concentration of proline was positively correlated with cell osmotic potential, accumulating to an average concentration of 129 millimolar in cells adapted to 428 millimolar NaCl and representing about 80% of the total free amino acid pool as compared to an average of 0.29 millimolar and about 4% of the pool in unadapted cells. These results indicate that although Na⁺ and Cl⁻ are principal components of osmotic adjustment, organic solutes also may make significant contributions.     

Solute Transport Process in Intestinal Epithelial Cells

In rat small intestine, the active transport of organic solutes results in significant depolarization of the membrane potential measured in an epithelial cell with respect to a grounded mucosal solution and in an increase in the transepithelial potential difference. According to the analysis with an equivalent circuit model for the epithelium, the changes in emf's of mucosal and serosal membranes induced by active solute transport were calculated using the measured conductive parameters. The result indicates that the mucosal cell membrane depolarizes while the serosal cell membrane remarkably hyperpolarizes on the active solute transport. Corresponding results are derived from the calculations of emf's in a variety of intestines, using the data that have hitherto been reported. The hyperpolarization of serosal membrane induced by the active solute transport might be ascribed to activation of the serosal electrogenic sodium pump. In an attempt to determine the causative factors in mucosal membrane depolarization during active solute transport, cell water contents and ion concentrations were measured. The cell water content remarkably increased and, at the same time, intracellular monovalent ion concentrations significantly decreased with glucose transport. Net gain of glucose within the cell was estimated from the restraint of osmotic balance between intracellular and extracellular fluids. In contrast to the apparent decreases in intracellular Na⁺ and K⁺ concentrations, significant gains of Na⁺ and K⁺ occurred with glucose transport. The quantitative relationships among net gains of Na⁺, K⁺ and glucose during active glucose transport suggest that the coupling ratio between glucose and Na⁺ entry by the carrier mechanism on the mucosal membrane is approximately 1:1 and the coupling ratio between Na⁺-efflux and K⁺-influx of the serosal electrogenic sodium pump is approximately 4:3 in rat small intestine. In addition to the electrogenic ternary complex inflow across the mucosal cell membrane, the decreases in intracellular monovalent ion concentrations, the temporary formation of an osmotic pressure gradient across the cell membrane and the streaming potential induced by water inflow through negatively charged pores of the cell membrane in the course of an active solute transport in intestinal epithelial cells are apparently all possible causes of mucosal membrane depolarization.     

Osmotic properties of ehrlich ascites tumor cells during the cell cycle

Ehrlich ascites tumor cells were grown and maintained in continuous spinner culture. The population of dividing cells was synchronized by a double thymidine block technique. Cell cycle phases were determined graphically by plotting mitotic index, cell number, and DNA synthesis against time. Changes in the osmotic properties of Ehrlich ascites tumor cells during the cell cycle are described. Permeability to water is highest at the initiation of S and progressively decreases to its lowest value just after mitosis. Heats of activation for water permeability vary during the cell cycle, ranging from 9–14 kcal/mole. Results may imply changes in the state of water in the membrane during the cycle. The volume of osmotically active cell water is highest during S and early G2 and decreases during the mitotic phase, as cells undergo division. Total water content remains stable at 82% (w/w) during the cycle. Total concentration of the three major ions (Na, K, Cl), expressed as mEq/liter total cell volume, does not change. The fraction of total cell water which is osmotically active (Ponder's R) decreased gradually from 0.75 at S to about 0.56 following mitosis. Findings suggest that a fraction of the total water within the cell exists in a “bound” form and is, therefore, incapable of being shifted under the driving force of osmotic pressure. This fraction of bound water increases during the cell cycle. Possible alterations in membrane fluidity and the state of water in the cell are discussed.     

On the osmoregulation in Atriplex hymenelytra (Torr.) Wats. (Chenopodiaceae)

Summary Aspects of osmoregulation were studied in leaves of irrigated and nonirrigated plants of Atriplex hymenelytra (Torr.) Wats. (Chenopodiaceae) from their natural habitat in Death Valley, California. Using a set of several data concentrations of inorganic electrolytes (Na⁺, K⁺, Cl^-) and of oxalate in the mesophyll of this salt secreting species were calculated. The osmotic potential resulting from these solutes (under consideration of an empirically estimated osmotic coefficient) is in good agreement with field measurements of the overall osmotic potential in the leaf mesophyll as determined by pressure-volume curves. This indicates that these 4 electrolytes are the main osmotically active solutes. Oxalate is present in comparably high concentrations and is used to achieve ion balance.Organic solutes analyzed include soluble carbohydrates (mono-, di- and oligosaccharides), amino- and organic acids as well as glycinebetaine. Of these, organic- and amino acids (including proline) contribute only little to osmoregulation. Soluble carbohydrates and especially glycinebetaine exhibit concentrations high enough for generating considerable osmotic potentials, at least if these compounds are regarded to be restricted to the cytoplasm acting as compatible solutes.     

An attempt to use isolated vacuoles to determine the distribution of sodium and potassium in cells of storage roots of red beet (Beta vulgaris L.)

Vacuoles isolated from red beet (Beta vulgaris L.) storage roots contain Na⁺ and K⁺ but their analysis does not give reliable information about the size of vacuolar pools of these ions in vivo. Analyses of isolated vacuoles indicated that between 53% and 90% of the Na⁺ was located in the vacuole and that the vacuolar concentrations of Na⁺ ranged between 4 and 45 mol m^-3. Calculated concentrations of K⁺ in the vacuoles varied between 32 and 72 mol m^-3 but, in contrast to Na⁺, only about 50% of the K⁺ was located in the vacuole. Considerations of the likely cytoplasmic concentrations of Na⁺ and K⁺ suggest that if these results indicate conditions in vivo a large proportion of these ions must be located in the extracellular space, where they would exert considerable osmotic pressure. To test this, the effect of washing on cell turgor (measured directly with a pressure probe) and on loss of Na⁺ and K⁺ was determined. Washing caused an increase in turgor of 5 bar but losses of Na⁺ and K⁺ were less than predicted by the experiments with isolated vacuoles. It is concluded that beet vacuoles leak Na⁺ and K⁺ when isolated resulting in an underestimation of the size of vacuolar pools of these cations in vivo. Nonetheless, the turgor measurements provide evidence for the presence of osmotically active solute in the extracellular space. The possible contribution of extracellular Na⁺ and K⁺ to the observed turgor reduction is calculated and the physiological importance of the accumulation of extracellular solutes is discussed.     

Effects of PCMBS on the water and small solute permeabilities in frog urinary bladder

Summary It has been reported that PCMBS (p-chloromercuribenzene sulfonate) blocks the water permeability of red cells and of the tubular kidney membranes. In this study we compare the effects of this mercurial compound on the permeability of water and other small solutes in the frog urinary bladder.We observed that: (i) 5mm PCMBS applied at pH 5.0 to the mucosal side inhibited the net and unidirectional water fluxes induced by oxytocin without changing the P _f/P _d ratio. (ii) The oxytocin-induced urea and Na⁺ influxes were also inhibited by PCMBS. (iii) The unidirectional Cl^– movement was first reduced and then increased during the course of PCMBS treatment. (iv) The short-circuit measured at low mucosal Na⁺ concentration (10mm), diminished continuously, whereas the transepithelial resistance first increased and then diminished. (v) Mannitol, raffinose, -methyl-glucose, antipyrine, caffeine and Rb⁺ movements were not changed significantly during the first 26 min of the water permeability inhibition. In conclusion: (i) The ADH-sensitive water, urea and Na⁺ transport systems were inhibited by PCMBS, (ii) PCMBS did not induce a nonspecific and general effect on the permeability of the membrane during the development of the water permeability inhibition, and (iii) in terms of water channels, the inhibition of water transport with the maintenance of a highP _f/P _d ratio suggests that PCMBS closes the water channels in an all or none manner, reducing their operative number in the apical border of frog bladder.     

NaCl-stimulated proton efflux and cell expansion in sugar-beet leaf discs

The expansion of illuminated sugar-beet leaf discs floating on aqueous solutions is stimulated by 10 mM NaCl. During expansion, protons are pumped out of the cell and NaCl increases this proton flux by about 40%. The nett flux of K⁺ and Na⁺ into the discs was also evaluated. During the expansion period K⁺ decreases while Na⁺ increases markedly. The results indicate the existence of a sodium-stimulated proton pump which is active during cell enlargement.Abbreviations IAA indole-3-acetic acid - PEG polyethylene glycol     

Sodium chloride toxicity and the cellular basis of salt tolerance in halophytes

Background Halophytes are the flora of saline soils. They adjust osmotically to soil salinity by accumulating ions and sequestering the vast majority of these (generally Na⁺ and Cl⁻) in vacuoles, while in the cytoplasm organic solutes are accumulated to prevent adverse effects on metabolism. At high salinities, however, growth is inhibited. Possible causes are: toxicity to metabolism of Na⁺ and/or Cl⁻ in the cytoplasm; insufficient osmotic adjustment resulting in reduced net photosynthesis because of stomatal closure; reduced turgor for expansion growth; adverse cellular water relations if ions build up in the apoplast (cell walls) of leaves; diversion of energy needed to maintain solute homeostasis; sub-optimal levels of K⁺ (or other mineral nutrients) required for maintaining enzyme activities; possible damage from reactive oxygen species; or changes in hormonal concentrations.Scope This review discusses the evidence for Na⁺ and Cl⁻ toxicity and the concept of tissue tolerance in relation to halophytes.Conclusions The data reviewed here suggest that halophytes tolerate cytoplasmic Na⁺ and Cl⁻ concentrations of 100–200 mm, but whether these ions ever reach toxic concentrations that inhibit metabolism in the cytoplasm or cause death is unknown. Measurements of ion concentrations in the cytosol of various cell types for contrasting species and growth conditions are needed. Future work should also focus on the properties of the tonoplast that enable ion accumulation and prevent ion leakage, such as the special properties of ion transporters and of the lipids that determine membrane permeability.     

Volume changes of mammalian cells subjected to hypotonic solutions in vitro: evidence for the requirement of a sodium pump for the shrinking phase

A Coulter-orifice pulse-height analyzer system was used to measure volume spectra of mammalian cells in suspension at different times after the addition of an equal volume of water. In appropriate hypotonic medium, cultured mammalian cells rapidly increase in volume and then shrink, more slowly, approaching their initial volumes within 20 to 30 minutes at 37.5°C. The shrinking phase was found to be reversibly inhibited by ouabain and inhibited in both K⁺-free and Na⁺-free solutions; neither choline⁺ nor Li⁺ could substitute for extracellular Na⁺ in supporting the shrinking phenomenon but Rb⁺ and Cs⁺ were fairly good substitutes for K⁺. Under conditions similar to those with which the shrinking phenomenon was observed with cultured cells, it was not found with either human or mouse red blood cells. Two methods were used to determine intracellular Na⁺ and K⁺ content in osmotically shocked cells and in unshocked controls. An isotope equilibration method was employed with L5178-Y mouse lymphoblasts and a chemical determination by flame photometry was used with Ehrlich ascites tumor cells. The K⁺ content was significantly reduced and the Na⁺ content was unchanged or somewhat increased in cells which had returned to their original volumes in hypotonic medium. The K⁺ content was even more reduced but the Na⁺ content was greatly increased in cells which were osmotically shocked in the presence of ouabain.     

Monitoring of Na<Superscript>+</Superscript>/K<Superscript>+</Superscript>-ATPase mRNA expression in the cinnamon clownfish, <Emphasis Type="Italic">Amphiprion melanopus</Emphasis>, exposed to an osmotic stress environment: profiles on the effects of exogenous hormone

We examined changes in the expression of Na⁺/K⁺-ATPase mRNA in the gills of the cinnamon clownfish using quantitative real-time PCR in an osmotically changing environment [seawater (35 psu; practical salinity unit, 1 psu ≈ 1‰) → brackish water (17.5 psu) and brackish water with prolactin]. The expression of Na⁺/K⁺-ATPase mRNA in gills was increased after the transfer to brackish water, and the expression was repressed by prolactin treatment. Also, activities of gill Na⁺/K⁺-ATPase and plasma cortisol levels increased after the transfer to brackish water and were repressed in brackish water with prolactin treatment. Na⁺/K⁺-ATPase-immunoreactive cells were almost consistently observed in the gill filaments, but absent from the lamella epithelia. The plasma osmolality level decreased in brackish water, but the level of this parameter increased in brackish water with prolactin treatment during salinity change. These results suggest that the Na⁺/K⁺-ATPase gene plays an important role in osmoregulation in gills, and prolactin improves the hyperosmoregulatory ability of cinnamon clownfish in a brackish water (hypoosmotic) environment.     

Simultaneous net accumulation of both K+ and Na+ by lymphocytes at 0°C

Human lymphocytes at 0°C in low Na⁺ medium accumulate both K⁺ and Na⁺ to levels higher than in the external medium. This is not due to an impermeable compartment or a Donnan equilibrium, and is incompatible with the membrane Na⁺-pump concept. In contrast, it supports prior evidence that ion exchange in lymphocytes is mediated by adsorption onto and desorption from fixed anionic sites within the cell. Additional aspects of ion and water contents of cells in low Na⁺ medium are described and are explained by this concept.     

Sodium and Potassium Compartmentation and Transport across the Roots of Intact Spergularia marina

The Na⁺ and K⁺ transport characteristics of Spergularia marina (L.) Griseb. were considered in order to compare the systems by which these two physiologically different cations are managed during initial acquisition and subsequent partitioning in midvegetative plants. Uptake of ²²Na⁺ and ⁴²K⁺ and redistribution of labels in pulse-chase studies were compared under steady state growth conditions or with the concentration of one of the ions elevated. At high external concentrations, the initial ⁴²K⁺ accumulation and transport to the shoot was associated with a small, rapidly exchanging, cellular compartment similar to that previously indicated for Na⁺ (D Lazof, JM Cheeseman 1986 Plant Physiol 81: 742-747). At 1 mol m⁻³, K⁺ was conducted to the shoot through a root compartment, the specific activity of which rose much more slowly than the rapidly exchanging compartment. After a lag of approximately 5 minutes, ⁴²K⁺ translocation approached a constant rate with a half-time of 14 minutes compared to 5 minutes for ²²Na⁺ or for ⁴²K⁺ at higher external levels. At all external levels, prolonged translocation of ⁴²K⁺ was measured when a 10 minute pulse was followed by an unlabeled chase, again suggesting a conducting compartment distinct from that for Na⁺. It is suggested that the K⁺ conducting compartment, possibly the `bulk cytoplasm,' is associated with the active K⁺ transport system generally found in higher plants.     

Elver Invasion, Population Structure and Growth of Marbled eels Anguilla marmorata in a Tropical River on Réunion Island in the Indian Ocean

Winter skates, Leucoraja ocellata, exposed to 80% and 50% seawater (SW) exhibited rapid and significant weight gains followed by a slight recovery to new steady state levels within 8 days. Skates were acclimated at each salinity (100% SW [N = 16], 80% SW [N = 8], 50% SW [N = 8]), anesthetized (MS222) and bled from the caudal vein. In 100% SW, skate plasma (930mOsm/kg) was slightly hyperosmotic to the external medium (922mOsm/kg). Plasma osmolality decreased with seawater dilution, but became increasingly hyperosmotic to the bathing media. The environmental dilutions resulted in significant, but disproportionate changes in plasma Cl^–, P^–, Na⁺, Ca⁺, Mg⁺, trimethylamine oxide (TMAO) and urea concentrations. Mean corpuscular [Hb] and milliliter RBC water measurements suggest that skate red cells swelled less at each dilution than predicted for a passive erythrocyte osmometer. Concentrations of the major RBC solutes K⁺, urea, TMAO and Cl^– decreased by 8, 25, 5 and 21%, respectively in 80% SW. In 50% SW, K⁺, urea, TMAO and Cl^– concentrations decreased by 9, 47, 36 and 15%, respectively. Quantitatively, the other measured intracellular electrolytes (Mg⁺, Na⁺, P^– and Ca⁺) also exhibited disproportionate changes in concentration. Our results indicate that L. ocellata is a euryhaline elasmobranch that can tolerate significant reduction in the external salinity through the release of both ions and urea from the extracellular compartments while retaining electrolytes at the expense of urea in the intracellular compartment.     

Na movements and their oscillations during fertilization and the cell cycle in sea urchin eggs

We have analysed in detail the Na⁺ content and Na⁺ influx during fertilization and first divisions of the sea urchin egg (Paracentrotus lividus) using a filtration technique devised to eliminate rapidly contamination by the Na⁺ of external sea water. In the first 5 min following fertilization the egg fills up with Na⁺ (+ 30%). Thereafter Na⁺ is extruded and the Na⁺ content stabilizes at about 60% of the unfertilized egg level by the second cleavage (2 h). The initial increase in Na⁺ content is due to a large increase in Na⁺ influx already detected at 20 sec. The Na⁺ influx reaches its maximum at 1 min and its minimum at 5 min. H⁺ excretion follows the same kinetics. A second increase in Na⁺ influx is noted 5–10 min after fertilization; it reaches its maximum at prophase metaphase (30 min) and its minimum during cleavage (60 min). These oscillations in Na⁺ influx were observed for the first three divisions. Fertilization also immediately stimulates the Na⁺ efflux which remains elevated throughout the cell cycle and is responsible for the depletion of the Na⁺ content of the embryos. Activation of the eggs by weak amine bases (5 mM NH₄Cl) which bypasses the early cortical reaction produces only a depletion in the Na⁺ content of the egg similar to that produced by fertilization. NH₄Cl also increases the Na⁺ influx soon after fertilization, although no transient variations are noted.     

Method for determining solutes in the cell walls of leaves

A perfusion method is described whereby large discs of amphistomatous leaves are vacuum-perfused with water so that either successive fractions of perfusate may be analyzed for solutes or the infused water may be displaced and collected after equilibration with the leaf cells. With castor bean leaves, estimates of electrolyte concentration in cell wall water by the two methods were similar. Total electrolytes in leaf cell wall water of castor beans (Ricinus communis), sunflower (Helianthus annuus), and cabbage (Brassica oleracea capitata) from nonsaline cultures were about 2, 2, and 10 milliequivalents per liter, respectively, increasing to 4, 10, and 30 milliequivalents per liter under saline conditions. Electrolytes recovered in successive fractions were similar in composition, and continuous perfusion resulted in a steady release of solutes, the concentration in the perfusate varying inversely with the perfusion rate. Diffusional release of solutes from cells was less than expected at low perfusion rates, suggesting that solute reabsorption may increase as solute concentration in the perfusate increases with decreased perfusion rates. Perfusate concentration and composition were essentially unaffected by temperature (2 and 23 C) or by perfusing with 0.5 mm CaSO₄ rather than with water. Electrolytes in perfusates on an equivalent basis were Ca²⁺, 30%; Mg²⁺, 10%; and Na⁺ + K⁺, 60%, the proportions of sodium increasing from 10 to 50% in leaves (cabbage) that accumulated sodium under saline conditions. Salinity (added NaCl) of the root culture medium caused a 3- to 5-fold increase in total cell wall electrolyte concentration, but this amounted to an increase from less than 1 or a few per cent to no more than 7% (in cabbage) of the cell sap electrolyte concentrations. Solutes in the cell wall appear to be in dynamic equilibrium with intracellular solutes.     

Solute distribution between vacuole and cytosol of sugarcane suspension cells: Sucrose is not accumulated in the vacuole

The compartmentation of solutes in suspension cells of Saccharum sp. during different growth phases in batch culture was determined using CuCl₂ to permeabilize the plasma membrane of the cells. The efflux of cytosolic and vacuolar pools of sugars, cations and phosphate was monitored, and the efflux data for phosphate were compared and corrected using data from compartmentation analysis of phosphate as determined by ³¹P-nuclear magnetic resonance spectroscopy. The results show that sucrose is not accumulated in the vacuoles at any phase of the growth cycle. On the other hand, glucose and fructose are usually accumulated in the vacuole, except at the end of the cell-culture cycle when equal distribution of glucose and fructose between the cytosol and the vacuole is found. Both Na⁺ and Mg²⁺ are preferentially located in the vacuoles, but follow the same tendency as glucose and fructose with almost complete location in the vacuole in the early culture phases and increasing cytosolic concentration with increasing age of the cell culture. Potassium ions are always clearly accumulated in the cytosol at a concentration of about 80 mM; only about 20% of the cellular K⁺ is located inside the vacuole. Cytosolic phosphate is little changed during the cell cycle, whereas the vacuolar phosphate pool changes according to total cellular phosphate. In general there are two different modes of solute compartmentation in sugarcane cells. Some solutes, fructose, glucose, Mg²⁺ and Na⁺, show high vacuolar compartmentation when the total cellular content of the respective solute is low, whereas in the case of ample supply the cytosolic pools increase. For other solutes, phosphate and K⁺, the cytosolic concentration tends to be kept constant, and only excess solute is stored in the vacuole and remobilized under starvation conditions. The behaviour of sucrose is somewhat intermediate and it appears to equilibrate easily between cytosol and vacuole.Abbreviation NMR nuclear magnetic resonance The very cooperative help by Dr. J. Reiner with the ³¹P-NMR measurements and the technical assistance by D. Keis are gratefully acknowledged. This research was supported by the Deutsche Forschungsgemeinschaft and by Fonds der Chemischen Industrie.     

Na<Superscript>+</Superscript> Modulates Anion Permeation and Block of P2X<Subscript>7</Subscript> Receptors from Mouse Parotid Glands

Experiments were conducted to test the hypothesis that aliphatic hydrocarbons bind to pockets/crevices of sodium (Na⁺) channels to cause action potential (AP) block. Aliphatic solutes exhibiting successively greater octanol/water partitition coefficients (K _ow) were studied. Each solute blocked Na⁺ channels. The 50% effective concentration (EC₅₀) to block APs could be mathematically predicted as a function of the solute’s properties. The solutes studied were methyl ethyl ketone (MEK), cyclohexanone, dichloromethane, chloroform and triethylamine (TriEA); the K _ow increased from MEK to TriEA. APs were recorded from frog nerves, and test solutes were added to Ringer’s solution bathing the nerve. When combined with EC₅₀s for solutes with log K _ows < 0.29 obtained previously, the solute EC₅₀s could be predicted as a function of the fractional molar volume (dV/dm = [dV/dn]/100), polarity (P) and the hydrogen bond acceptor basicity (β) by the following equation: Fluidity changes cannot explain the EC₅₀s. Each of the solutes blocks Na⁺ channels with little or no change in kinetics. Na⁺ channel block explains much of the EC₅₀ data. EC₅₀s are produced by a combination of effects including ion channel block, fluidity changes and osmotically induced structural changes. As the solute log K _ow increases to values near 1 or greater, Na⁺ channel block dominates in determining the EC₅₀. The results are consistent with the hypothesis that the solutes bind to channel crevices to cause Na⁺ channel and AP block.