Polyphosphate Hydrolysis within Acidic Vacuoles in Response to Amine-Induced Alkaline Stress in the Halotolerant Alga Dunaliella salina

The location and mobilization of polyphosphates in response to an amine-induced alkaline stress were studied in the halotolerant alga Dunaliella salina. The following observations suggest that polyphosphates accumulate in acidic vacuoles: (a) Accumulation of large amounts of polyphosphates is manifested as intravacuolar dense osmiophilic bodies in electron micrographs. (b) Uptake of amines into the vacuoles induces massive hydrolysis of polyphosphates, demonstrated by in vivo ³¹P-nuclear magnetic resonance, and by analysis of hydrolytic products on thin layer chromatograms. The analysis indicates that: (a) Polyphosphate hydrolysis is kinetically correlated with amine accumulation and with the recovery of cytoplasmic pH. (b) The major hydrolytic product is tripolyphosphate. (c) The peak position of the tripolyphosphate terminal phosphate in nuclear magnetic resonance spectra is progressively shifted as the cells recover, indicating that the pH inside the vacuoles increases while the pH in the cytoplasm decreases. (d) In lysed cell preparations, in which vacuoles become exposed to the external pH, mild alkalinization in the absence of amines induces polyphosphate hydrolysis to tripolyphosphates. It is suggested that amine accumulation within vacuoles activates a specific phosphatase, which hydrolyzes long-chain polyphosphates to tripolyphosphates. The hydrolysis increases the capacity of the vacuoles to sequester amines from the cytoplasm probably by releasing protons required to buffer the amine, and leads to recovery of cytoplasmic pH. Thus, polyphosphate hydrolysis provides a high-capacity buffering system that sustains amine compartmentation into vacuoles and protects cytoplasmic pH.     

Hydrolysis of polyphosphates and permeability changes in response to osmotic shocks in cells of the halotolerant alga dunaliella

The effects of osmotic shocks on polyphosphates and on the vacuolar fluorescent indicator atebrin have been investigated to test whether acidic vacuoles in the halotolerant alga Dunaliella salina have a role in osmoregulation. Upshocks and downshocks induce different patterns of polyphosphate hydrolysis. Upshocks induce rapid formation of new components, tentatively identified as 5 or 6 linear polyphosphates, formed only after upshocks with NaCl and not with glycerol, indicative of compartmentation of Na⁺ into the vacuoles. Conversely, downshocks induce a slower transient accumulation of tripolyphosphates, indicating activation of a different hydrolytic process within the vacuoles. Osmotic shocks do not lead to release of atebrin from acidic vacuoles, indicating that they do not induce a major intravacuolar alkalinization. However, osmotic shocks induce transient permeability changes measured by amine-induced atebrin release from vacuoles. Hypoosmotic shocks transiently increase the permeability (up to 20-fold), whereas hyperosmotic shocks induce a rapid drop in permeability. Electron micrographs of osmotically shocked cells also reveal transient changes in the surface and internal organelles of D. salina cells. It is suggested that hyperosmotic and hypoosmotic shocks induce different changes within acidic vacuoles and in the organization and/or composition of the plasma membrane in Dunaliella.     

Uptake of the fluorescent indicator atebrin into acidic vacuoles in the halotolerant alga Dunaliella satina

The fluorescent indicator atebrin (3-chloro-9-(4-diethylamino-1-methylbutyl)-7-methyoxy-acridine) is taken up by Dunaliella salina cells at alkaline external pH and accumulates in acidic vacuoles. The uptake is unaffected by light, by photosynthetic inhibitors, by protonophores or by ionophores; however, the dye can be released by amines, indicating that it is specifically accumulating in acidic vacuoles. Amines induce a biphasic enhancement of atebrin fluorescence — a fast phase, accompanied by redistribution within the cell, consistent with release of the dye from the vacuoles to the cytoplasm, and a slow phase, correlated with release of atebrin from the cells. These results are interpreted to indicate a slow equilibration of atebrin across the plasma membrane and a fast equilibration across the vacuolar membrane. Part of the dye cannot be released by the amines, and appears to be internally bound. Atebrin uptake is inhibited by cholesteryl hemisuccinate and is stimulated by lysophosphatidylcholine, indicating that modification of the lipid composition of the plasma membrane affects the permeability to atebrin. Analysis of the pH dependence of atebrin uptake indicates that the dye enters the cells by fluid-phase permeation. Different stresses enhance the rate of atebrin uptake and release, indicating that they modify plasma-membrane structure or composition. Atebrin may serve as a specific marker for acidic vacuoles, as an indicator for amine uptake, and as a probe for subtle changes in the permeability of the plasma membrane.Abbreviations Atebrin 3-chloro-9-(4-diethylamino-1-methylbutyl)-7-methoxy-acridine - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethyl-urea - SF-6847 3,5-ditertbutyl-4-hydroxybenzylidenemalonitrile     

Time-dependent resistance to alkaline pH of oxalate-supported calcium uptake by sarcoplasmic reticulum

Both oxalate-supported Ca²⁺ uptake and Ca²⁺-stimulated ATPase activity of the sarcoplasmic reticulum are sensitive to the pH of the assay medium. Ca²⁺ uptake is optimal at relatively acidic pH (6.2–6.6); whereas, Ca²⁺-stimulated ATPase activity is optimal at a more alkaline pH (7.4–8.0). Following the addition of ATP, Ca²⁺ uptake demonstrates a time-dependent resistance to the inhibition by an alkaline pH. Once the linear phase of Ca²⁺ uptake is reached, alkalinization thereafter does not alter the rate established at the acidic pH. A similar time-dependent resistance is observed to the inhibition of Ca²⁺ uptake by the cation ionophore, X537A. In contrast, acidification of the alkaline medium after Ca²⁺ uptake is initiated by ATP has no such resistance to change. Acidification results in a prompt acceleration of the rate of Ca²⁺ uptake identical to that observed under control conditions at the acidic pH. Ca²⁺-stimulated ATPase activity, however, increases with alkalinization and decreased with acidification, regardless of time, in a manner expected from the rates observed under conditions when the pH is constant from the time of ATP addition. The results suggest that there is a time-dependent, pH-sensitive factor of oxalate-supported Ca²⁺ uptake. This factor can be activated by acidification at any time after ATP addition and, thus, does not represent a destruction of membrane function. In contrast, Ca²⁺-stimulated ATPase activity demonstrates no time-dependent resistance to pH change.     

Phosphate Uptake by Excised Maize Root Tips Studied by in VivoP Nuclear Magnetic Resonance Spectroscopy

The extent of phosphate uptake measured by the relative changes in cytoplasmic Pi, vacuolar Pi, ATP, glucose-6-phosphate, and UDPG was determined using in vivo³¹P nuclear magnetic resonance spectroscopy. Maize (Zea mays) root tips were perfused with a solution containing 0.5 or 1.0 millimolar phosphate at pH ~6.5 under different conditions. In the aerated state, phosphate uptake resulted in a significant increase (>80%) in vacuolar Pi, but cytoplasmic Pi only transiently increased by 10%. Under N₂, the cytoplasmic Pi increased ~150% which could be attributed to a large extent to the breakdown of ATP, sugar phosphates and UDPG. Vacuolar Pi increased but only to the extent of ~10% of that seen under aerobic conditions. 2-deoxyglucose pretreatment was utilized to decrease the level of cytoplasmic Pi. When pretreated with the 2-deoxyglucose, the excised maize roots absorbed phosphate from the perfusate with a significant increase in the cytoplasmic Pi. The increase could only be traced to external phosphate since the concentrations of other phosphorus containing species remained constant during the uptake period. With 2-deoxyglucose pretreatment, phosphate uptake under anaerobic conditions was substantially inhibited with only the vacuolar phosphate showing a slight increase. When roots were treated with carbonyl cyanide m-chlorophenyl hydrazone, no detectable Pi uptake was found. These results were used to propose a H⁺-ATPase related transport mechanism for phosphate uptake and compartmentation in corn root cells.     

Detection and characterization of acidic compartments (vacuoles) in Chlorella vulgaris 11h cells by 31P-in vivo NMR spectroscopy and cytochemical techniques

Acidic inorganic phosphate (Pi) pool (pH around 6) was detected besides the cytoplasmic pool in intact cells of Chlorella vulgaris 11h by ³¹P-in vivo nuclear magnetic resonance (NMR) spectroscopy. It was characterized as acidic compartments (vacuoles) in combination with the cytochemical technique; staining the cells with neutral red and chloroquine which are known as basic reagents specifically accumulated in acidic compartments. Under various conditions, the results obtained with the cytochemical methods were well correlated with those obtained from in vivo NMR spectra; the vacuoles were well developed in the cells at the stationary growth phase where the acidic Pi signal was detected. In contrast, cells at the logarithmic phase in which no acidic Pi signal was detected contained only smaller vesicles that accumulated these basic reagents. No acidic compartment was detected by both cytochemical technique and ³¹P-NMR spectroscopy when the cells were treated with NH₄OH. The vacuolar pH was lowered by the anaerobic treatment of the cells in the presence of glucose, while it was not affected by the external pH during the preincubation ranging from 3 to 10. Possible vacuolar functions in unicellular algae especially with respect to intracellular pH regulation are discussed.Non-standard abbreviations EDTA ethylenediaminetetraacetic acid - HEPES N-2-hydroxyethylpiperazine-N-2-ethanesulfonic acid - MDP methylene diphosphonic acid - NMR nuelear magnetic resonance - PCA perchloric acid - PCV packed cell volume - Pi inorganic phosphate - Pic sytoplasmic inorganic phosphate - Piv vacuolar inorganic phosphate - ppm parts per million - SP sugar phosphates - TCA trichloroacetic acid     

Quinacrine is not a vital fluorescent probe for vesicular ATP storage

Quinacrine, a fluorescent amphipathic amine, has been used as a vital fluorescent probe to visualize vesicular storage of ATP in the field of purinergic signaling. However, the mechanism(s) by which quinacrine represents vesicular ATP storage remains to be clarified. The present study investigated the validity of the use of quinacrine as a vial fluorescent probe for ATP-storing organelles. Vesicular nucleotide transporter (VNUT), an essential component for vesicular storage and ATP release, is present in very low density lipoprotein (VLDL)-containing secretory vesicles in hepatocytes. VNUT gene knockout (Vnut^−/−) or clodronate treatment, a VNUT inhibitor, disappeared vesicular ATP release (Tatsushima et al., Biochim Biophys Acta Molecular Basis of Disease 2021, e166013). Upon incubation of mice’s primary hepatocytes, quinacrine accumulates in a granular pattern into the cytoplasm, sensitive to 0.1-μM bafilomycin A₁, a vacuolar ATPase (V-ATPase) inhibitor. Neither Vnut^−/− nor treatment of clodronate affected quinacrine granular accumulation. In vitro, quinacrine is accumulated into liposomes upon imposing inside acidic transmembranous pH gradient (∆pH) irrespective of the presence or absence of ATP. Neither ATP binding on VNUT nor VNUT-mediated uptake of ATP was affected by quinacrine. Consistently, VNUT-mediated uptake of quinacrine was negligible or under the detection limit. From these results, it is concluded that vesicular quinacrine accumulation is not due to a consequence of its interaction with ATP but due to ∆pH-driven concentration across the membranes as an amphipathic amine. Thus, quinacrine is not a vital fluorescent probe for vesicular ATP storage.     

Estimating the chemical compositions of soil solutions by obtaining saturation extracts or specific 1:2 by volume extracts

The aluminium tolerance of several tree species was studied in a cloud forest in Northern Venezuela, growing on a very acid soil and rich in soluble Al. The Al-accumulator species (>1000 ppm in leaves) were compared to non-accumulator ones in relation to total Al concentration in xylem sap, pH and Al concentration in vacuoles, and rhizosphere alkalinization capacity. The Al³⁺ concentration in the soil solution and the xylem sap were also measured. The results show that in the Al-accumulator plant Richeria grandis, xylem sap is relatively rich in Al and about 35% of it is present in ionic form. In the non-accumulator plant studied (Guapira olfersiana) there is no Al detectable in xylem sap. The pH of vacuolar sap of several Al-accumulator species studied was very acidic and ranged between 2.6–4.8, but the presence of Al in vacuoles was not correlated with the acidity of the vacuolar sap. Both Al-accumulator and non accumulator plants had the capacity to reduce acidity of the rhizosphere and increased the pH of the nutrient solution by one unit within the first 24 hours. Trees growing in natural, high acidity-high Al³⁺ environment show a series of tolerance mechanisms, such as deposition of Al in vacuoles, Al chelation and rhizosphere alkalinization. These partially ameliorate the toxic effects of this element, but they probably impose a high ecological cost in terms of photosynthate allocation and growth rate.     

Proton Gradient-Driven Nickel Uptake by Vacuolar Membrane Vesicles of Saccharomyces cerevisiae

A vacuolar H⁺-ATPase-negative mutant of Saccharomyces cerevisiae was highly sensitive to nickel ion. Accumulation of nickel ion in the cells of this mutant of less than 60% of the value for the parent strain arrested growth, suggesting a role for this ATPase in sequestering nickel ion into vacuoles. An artificially imposed pH gradient (interior acid) induced transient nickel ion uptake by vacuolar membrane vesicles, which was inhibited by collapse of the pH difference but not of the membrane potential. Nickel ion transport into vacuoles in a pH gradient-dependent manner is thus important for its detoxification in yeast.     

Transport and subcellular localization of polyamines in carrot protoplasts and vacuoles

Putrescine and spermidine uptake in carrot (Daucus carota L., cv “Tip top”) protoplasts and isolated vacuoles was studied. Protoplasts and vacuoles accumulated polyamines very quickly, with maximum absorption within 1 to 2 minutes. The insertion of a washing layer containing 100 millimolar unlabeled putrescine or spermidine did not change this pattern, but strongly reduced the uptake of putrescine and spermidine in protoplasts and in vacuoles. The dependence of spermidine uptake on the external concentration was linear up to the highest concentrations tested in protoplasts, while that in vacuoles showed saturation kinetics below 1 millimolar (K_m = 61.8 micromolar) and a linear component from 1 to 50 millimolar. Spermidine uptake in protoplasts increased linearly between pH 5.5 and 7.0, while there was a distinct optimum at pH 7.0 for vacuoles. Preincubation of protoplasts with 1 millimolar Ca²⁺ affected only surface binding but not transport into the cells. Nonpermeant polycations such as La³⁺ and polylysine inhibited spermidine uptake into protoplasts. Compartmentation studies showed that putrescine and spermidine were partly vacuolar in location and that exogenously applied spermidine could be recovered inside the cells. The characteristics of the protoplast and vacuolar uptake system induce us to put forward the hypothesis of a passive influx of polyamines through the plasmalemma and of the presence of a carrier-mediated transport system localized in the tonoplast.     

Regulation of Vacuolar pH of Plant Cells: II. A P NMR Study of the Modifications of Vacuolar pH in Isolated Vacuoles Induced by Proton Pumping and Cation/H Exchanges

The vacuolar pH and the trans-tonoplast ΔpH modifications induced by the activity of the two proton pumps H⁺-ATPase and H⁺-PPase and by the proton exchanges catalyzed by the Na⁺/H⁺ and Ca²⁺/H⁺ antiports at the tonoplast of isolated intact vacuoles prepared from Catharanthus roseus cells enriched in inorganic phosphate (Y Mathieu et al 1988 Plant Physiol [in press]) were measured using the ³¹P NMR technique. The H⁺-ATPase induced an intravacuolar acidification as large as 0.8 pH unit, building a trans-tonoplast ΔpH up to 2.2 pH units. The hydrolysis of the phosphorylated substrate and the vacuolar acidification were monitored simultaneously to estimate kinetically the apparent stoichiometry between the vectorial proton pumping and the hydrolytic activity of the H⁺-ATPase. A ratio of H⁺ translocated/ATP hydrolyzed of 1.97 ± 0.06 (mean ± standard error) was calculated. Pyrophosphate-treated vacuoles were also acidified to a significant extent. The H⁺-PPase at 2 millimolar PPi displayed hydrolytic and vectorial activities comparable to those of the H⁺-ATPase, building a steady state ΔpH of 2.1 pH units. Vacuoles incubated in the presence of 10 millimolar Na⁺ were alkalinized by 0.4 to 0.8 pH unit. It has been shown by using ²³Na NMR that sodium uptake was coupled to the H⁺ efflux and occurred against rather large concentration gradients. For the first time, the activity of the Ca²⁺/H⁺ antiport has been measured on isolated intact vacuoles. Ca²⁺ uptake was strongly inhibited by NH₄Cl or gramicidin. Vacuoles incubated with 1 millimolar Ca²⁺ were alkalinized by about 0.6 pH unit and this H⁺ efflux was associated to a Ca²⁺ uptake as demonstrated by measuring the external Ca²⁺ concentration with a calcium specific electrode. Steady state accumulation ratios of Ca²⁺ as high as 100 were reached for steady state external concentrations about 200 micromolar. The rate of Ca²⁺ uptake appeared markedly amplified in intact vacuoles when compared to tonoplast vesicles but the antiport displayed a much lower affinity for calcium. The different behavior of intact vacuoles compared to vesicles appears mainly to be due to differences in the surface to volume ratio and in the rates of dissipation of the pH gradient. Despite its low affinity, the Ca²⁺/H⁺ antiport has a high potential capacity to regulate cytoplasmic concentration of calcium.     

Salt Stress-Induced Cytoplasmic Acidification and Vacuolar Alkalization in Nitellopsis obtusa Cells : In VivoP-Nuclear Magnetic Resonance Study

Time courses of cytoplasmic and vacuolar pH changes under salt stress were monitored by in vivo³¹P-nuclear magnetic resonance spectroscopy in intact cells of Nitellopsis obtusa. When cells were treated with 100 millimolar NaCl for 2 hours, the cytoplasmic pH deceased from 7.2 to 7.0, while the vacuolar pH increased from 4.9 to 5.2. This salt-induced breakdown of the pH gradient between the cytoplasm and the vacuole was also confirmed through direct measurements of change in vacuolar pH with a micro-pH electrode. We speculate that the intracellular pH changes induced by the salt stress mainly results from the inhibition of the H⁺-translocating pyrophosphatase in the vacuolar membrane, since this H⁺-translocating system is sensitive to salt-induced increase in the cytoplasmic [Na⁺] and a simultaneous decrease in the cytoplasmic [K⁺]. Since disturbance of the cytoplasmic pH value should have serious consequences on the homeostasis of living cells, we propose that the salt-induced intracellular pH changes are one of initial and important steps that lead to cell death.     

The Fab1/PIKfyve Phosphoinositide Phosphate Kinase Is Not Necessary to Maintain the pH of Lysosomes and of the Yeast Vacuole

Lysosomes and the yeast vacuole are degradative and acidic organelles. Phosphatidylinositol 3,5-bisphosphate (PtdIns(3,5)P₂), a master architect of endolysosome and vacuole identity, is thought to be necessary for vacuolar acidification in yeast. There is also evidence that PtdIns(3,5)P₂ may play a role in lysosomal acidification in higher eukaryotes. Nevertheless, these conclusions rely on qualitative assays of lysosome/vacuole pH. For example, quinacrine, an acidotropic fluorescent base, does not accumulate in the vacuoles of fab1Δ yeast. Fab1, along with its mammalian ortholog PIKfyve, is the lipid kinase responsible for synthesizing PtdIns(3,5)P₂. In this study, we employed several assays that quantitatively assessed the lysosomal and vacuolar pH in PtdIns(3,5)P₂-depleted cells. Using ratiometric imaging, we conclude that lysosomes retain a pH < 5 in PIKfyve-inhibited mammalian cells. In addition, quantitative fluorescence microscopy of vacuole-targeted pHluorin, a pH-sensitive GFP variant, indicates that fab1Δ vacuoles are as acidic as wild-type yeast. Importantly, we also employed fluorimetry of vacuoles loaded with cDCFDA, a pH-sensitive dye, to show that both wild-type and fab1Δ vacuoles have a pH < 5.0. In comparison, the vacuolar pH of the V-ATPase mutant vph1Δ or vph1Δ fab1Δ double mutant was 6.1. Although the steady-state vacuolar pH is not affected by PtdIns(3,5)P₂ depletion, it may have a role in stabilizing the vacuolar pH during salt shock. Overall, we propose a model in which PtdIns(3,5)P₂ does not govern the steady-state pH of vacuoles or lysosomes.     

Regulation of intracellular pH values in higher plant cells. Carbon-13 and phosphorus-31 nuclear magnetic resonance studies.

The regulation of the cytoplasmic and vacuolar pH values (pHc and pHv) in sycamore (Acer pseudoplatanus L.) cells was analyzed using 31P and 13C nuclear magnetic resonance spectroscopy. Suspension-cultured cells were compressed in the NMR tube and perfused with the help of an original arrangement enabling a tight control of the pH (external pH, pHe) of the carefully oxygenated circulating nutrient medium. Intracellular pH values were measured from the chemical shifts of: CH2-linked carboxyl groups of citric acid below pH 5.7; orthophosphate between pH 5.7 and 8.0; 13C-enriched bicarbonate over pH 8.0. pHc and pHv were independent of pHe over the range 4.5-7.5. In contrast intracellular pH values decreased rapidly below pHe 4.5 and increased progressively at pHe over 7.5. There was an acceleration in the rate of O2 consumption accompanied with a decrease in cytoplasmic ATP concentration as pHe decreased. When the rate of O2 consumption was approaching the uncoupled O2 uptake rate, a loss of pHc control was observed. It is concluded that as pHe decreased, the plasma membrane ATPase consumed more and more ATP to reject the invading H+ ions in order to maintain pHc at a constant value. Below pHe 4.5 the efficiency of the H+ pump to react to back leakage of H+ ions became insufficient, leading to an acidification of pHc and to an alkalinization of pHe. On the other hand, over pHe 7.5 a passive influx of OH- ions was observed, and pHc increased proportionally to the increase of pHe. Simultaneously appreciable amounts of organic acids (malate and citrate) were synthesized by cells during the course of the alkalinization of the cytoplasmic compartment. The synthesis of organic acids which partially counteract the alkalinization of the cytoplasmic compartment may result from a marked activation of the cytoplasmic phosphoenolpyruvate carboxylase induced by an increase in cytoplasmic bicarbonate concentration. The fluctuations of pHv followed a similar course to that of pHc. It is concluded that the vacuole, which represents a potentially large H+ ions reservoir, can counteract H+ (or OH-) ion invasion observed at acidic (or alkaline) pHe contributing to the homeostasis of pHc.     

Effects of growth state and amines on cytoplasmic and vocuolar pH, phosphate and polyphosphate levels in Saccharomyces cerevisiae: a P-nuclear magnetic resonance study

The vacuoles of logarithmic and stationary stage cells were compared by ³¹P-NMR with regard to pH, orthophosphate (P_i) content and average size of polyphosphate. The vacuoles of stationary cells had lower pH higher P_i content, and polyphosphates of longer average chain lenght, although total polyphosphate content was about the same as in logarithmic cells. The lower vacuolar pH in stationary cells was the major cause of a larger cytoplasmic-vacuolar pH gradient. Addition of NH₄Cl, (NH₄)₂SO₄, methylamine or amantadine at pH 8 to cells in either stage caused an icnrease in both cytoplasmic and vacuolar pH, with little or no change in the cytoplasmic-vacuolar pH gradient. However, the administration of ammonium salts to the cells at pH 8.0 resulted in rapid hydrolysis of the intravacuolar polyphosphate to tripolyphosphate and P_i, with attendant redistribution of P_i between the vacuolar and cytoplasmic compartments.     

Effects of growth state and amines on cytoplasmic and vocuolar pH,phosphate and polyphosphate levels in Saccharomyces cerevisiae: a 31P-nuclear magnetic resonance study

The vacuoles of logarithmic and stationary stage cells were compared by ³¹P-NMR with regard to pH, orthophosphate (P_i) content and average size of polyphosphate. The vacuoles of stationary cells had lower pH higher P_i content, and polyphosphates of longer average chain lenght, although total polyphosphate content was about the same as in logarithmic cells. The lower vacuolar pH in stationary cells was the major cause of a larger cytoplasmic-vacuolar pH gradient. Addition of NH₄Cl, (NH₄)₂SO₄, methylamine or amantadine at pH 8 to cells in either stage caused an icnrease in both cytoplasmic and vacuolar pH, with little or no change in the cytoplasmic-vacuolar pH gradient. However, the administration of ammonium salts to the cells at pH 8.0 resulted in rapid hydrolysis of the intravacuolar polyphosphate to tripolyphosphate and P_i, with attendant redistribution of P_i between the vacuolar and cytoplasmic compartments.     

Phycomyces: discovery of the aiming error in the avoidance response

Vacuoles were prepared from germinating castor bean endosperm (Ricinus communis var Hale) and purified by filtration through a cotton layer under physiological osmolarity. The purity of vacuoles prepared by this method was comparable with that prepared by a sucrose step gradient centrifugation reported in a previous paper (Nishimura, Beevers 1978 Plant Physiol 62: 44-48). It was shown by assays of marker enzymes that the final preparation contained trace contamination of other organelles (glyoxysomes, mitochondria, and endoplasmic reticulum) and the cytosol. The isolated vacuoles were stained with neutral red, indicating that the intravacuolar pH is acidic. Intravacuolar pH of isolated vacuoles was determined by measuring the distribution of [¹⁴C]methylamine in the vacuoles and by directly measuring the pH of vacuolar extracts. The pH of isolated vacuolar extracts was 5.7 to 5.9. Similar values were obtained by the methylamine method and it was shown that intravacuolar pH increased as the pH of the medium was increased.     

Acid release,cytoplasmic alkalinization,and chromosome condensation during sea urchin fertilization and amine-lnduced parthenogenesis

We have studied the relationship between acid release, cytoplasmic alkalinization, and the extent of chromosome condensation during parthenogenetic activation of sea urchin eggs. The relative rate of acid release in Strongylocentrotus purpuratus eggs was determined from pH measurements of egg suspensions. Acid release in inseminated eggs began after a lag of 0.4 min and the relative rate increased 108-fold, declined, and release was essentially complete by 8-min postinsemination. An average of 3.8 ± 0.23 × 10^?12moles H⁺ cell^? was released as determined by backtitration with NaOH. Acid release characteristics of eggs parthenogenetically activated with either NH₄C1, methylamine ethylamine, n-propylamine, n-butylamine, or benzylamine were qualitatively similar. There was no detectable lag peroid and the increase in relative rate of acid release was directly proportional to the carbon number of the amine used, eg, from 8.3-fold methylamine to 470-fold with benzylamine. The total equivalents of acid released ranged from 0.50–8.2 × 10^?12 moles H⁺·cell^? in direct proportion to the concentration of amine used. The degree fo cytoplasmic alkalinization induced as a function of methylamine and benzylamine concentration was determined by pH measurements fo egg homogenates; egg cultures were also prepared for microscopic examination of chromosome condensation. None of the eggs had condensed chromosomes at 0.5-mM methylamine whereas a cytoplasmic alkalinization of 0.6 pH units was observed. Increased methylamine levels up to 10mM resulted in chromiosome condensation in only 20% of the eggs. A similar result was found with benzylamine. We conclude that acid release and cytoplasmic alkalinization during chemical parthenogenesis are insufficient to mimic sperm induction of chromiosome condensation and suggest that an additional factor(s) is required for chromosome condensation by low concentration of amines.     

Citrate Uptake into Tonoplast Vesicles from Acid Lime (Citrus aurantifolia) Juice Cells

Citrate transport into the vacuoles of acid lime juice cells was investigated using isolated tonoplast vesicles. ATP stimulated citrate uptake in the presence or in the absence of a ΔμH⁺. Energization of the vesicles only by an artificial K⁺ gradient (establishing an inside-positive Δψ) also resulted in citrate uptake as was the case of a ΔpH dominated ΔμH⁺. Addition of inhibitors to endomembrane ATPases showed no direct correlation between the inhibition to the tonoplast bound H⁺/ATPase and citrate uptake. The data indicated that, although some citrate uptake can be accounted for by Δψ and by a direct primary active transport mechanism involving ATP, under in vivo conditions of vacuolar pH of 2.0, citrate uptake is driven by ΔpH. Received: 27 April 1998/Revised: 8 September 1998     

Regulation of Vacuolar pH of Plant Cells: I. Isolation and Properties of Vacuoles Suitable for P NMR Studies

For the first time, the ³¹P nuclear magnetic resonance technique has been used to study the properties of isolated vacuoles of plant cells, namely the vacuolar pH and the inorganic phosphate content. Catharanthus roseus cells incubated for 15 hours on a culture medium enriched with 10 millimolar inorganic phosphate accumulated large amounts of inorganic phosphate in their vacuoles. Vacuolar phosphate ions were largely retained in the vacuoles when protoplasts were prepared from the cells and vacuoles isolated from the protoplasts. Vacuolar inorganic phosphate concentrations up to 150 millimolar were routinely obtained. Suspensions prepared with 2 to 3 × 10⁶ vacuoles per milliliter from the enriched C. roseus cells have an internal pH value of 5.50 ± 0.06 and a mean trans-tonoplast ΔpH of 1.56 ± 0.07. Reliable determinations of vacuolar and external pH could be made by using accumulation times as low as 2 minutes. These conditions are suitable to follow the kinetics of H⁺ exchanges at the tonoplast. The ³¹P nuclear magnetic resonance technique also offered the possibility of monitoring simultaneously the stability of the trans-tonoplast pH and phosphate gradients. Both appeared to be reasonably stable over several hours. The buffering capacity of the vacuolar sap around pH 5.5 has been estimated by several procedures to be 36 ± 2 microequivalents per milliliter per pH unit. The increase of the buffering capacity due to the accumulation of phosphate in the vacuoles is, in large part, compensated by a decrease of the intravacuolar malate content.