Uptake of Imidazole and its Effects on the Intracellular pH and Ionic Relations of Chara corallina

Ammonia (pK_a 9.25) and methylamine (pK_a, 10.65) increase cytoplasmicpH and stimulate Cl^– influx in Chara corallina, theseeffects being associated with influx of the amine cations ona specific porter. The weak base imidazole (pK_a 6.96) has similareffects but diffuses passively into the cell both as an unionizedbase and as a cation. When the external pH is greater than 6.0influx of the unionized species predominates. Imidazole accumulates to high concentrations in the vacuole,where it is protonated. Cytoplasmic pH and vacuolar pH riseby only 0.2–0.3 units, suggesting a large balancing protoninflux across the plasma membrane. Balance of electric chargeis partially maintained by net efflux of K⁺ and net influx ofCl^–. Calculation of vacuolar concentrations of imidazole(from (¹⁴C] imidazole uptake, assuming that there is no metabolism)plus K⁺ and Na⁺ indicates an excess of cations over inorganicanions (Cl^–). However, although the osmotic potentialof the cells increases, also indicating increased solute concentrations,the increase is less than that predicted by the calculated ionicconcentrations. This discrepancy remains to be resolved. Becausethe osmotic potential also increases when imidazole is absorbedfrom Cl^–-free solutions it is likely that maintenanceof charge-balance can also involve synthesis and vacuolar storageof organic or amino acids. Key words: Imidazole, potassium, intracellular pH, membrane transport, Chara     

Biophysical and Biochemical Regulation of Cytoplasmic pH in Chara corallina during Acid Loads

The contribution of membrane transport to regulation of cytoplasmicpH in Chara corallina has been measured during proton-loadingby uptake of butyric acid. In the short-term (i.e. up to 20min) uptake of butyric acid is not affected by removal of externalK⁺, Na⁺ or Cl^– but over longer periods uptake is decreased(by 20–50% in different experiments) in the absence ofexternal Na⁺ or, sometimes, K⁺. Influxes of both Na⁺ and K⁺increase temporarily after addition of butyrate, Na⁺ immediatelyand K⁺ after a lag. Effects on Cl^– influx are small butCl^– efflux increases enormously after a short lag. Anapproximate comparison of internal butyrate with changes inthe concentration of K⁺, Na⁺, and Cl^– suggests that initially(i.e. for a few min) cytoplasmic pH is determined by bufferingand possibly by some decarboxylation of organic acids (biochemicalpH regulation), and that biophysical pH regulation involvingefflux of H⁺ balanced by influxes of K⁺, Na⁺ and especiallyefflux of Cl^– progressively becomes dominant. When butyric acid is washed out of the cells, cytoplasmic pHis restored completely or partially (depending on the butyrateconcentration used) and this is independent of the presenceor absence of external Cl^–. Where Cl^– is present,its influx is relatively small. It is suggested that cytoplasmicpH is then controlled biochemically, involving the synthesisof an (unidentified) organic acid and the accumulation of acidicanions in place of butyurate lost from the cell. During thesecond application of butyrate, net Cl^– efflux is small:it is suggested that control of cytoplasmic pH then involvesdecarboxylation of the organic acid anions. The questions of the source of Cl^– lost from the cell(cytoplasm or vacuole) and of possible cytoplasmic swellingassociated with the accumulation of butyrate are discussed. Key words: Chara corallina, butyric acid, cytoplasmic pH, membrane transport     

Chloride Transport in Chara: I. KINETICS AND CURRENT-VOLTAGE CURVES FOR A PROBABLE PROTON SYMPORT

Chara cells show an inward positive electric current acrossthe plasmalemma when exposed to Cl^– under voltage-clampconditions. The rapid rise of this current suggests that itis directly associated with the inward transport of Cl^–.The dependence of the current on Cl^– concentration showssaturation, the data fitting the Michaelis-Menten equation withV_m up to 100 nmol m^–2 s^–1 (for Cl^–starvedcells) with K_M 10–20 µM, and with some allowancefor an unstirred layer of water adjacent to the membrane. Theeffects on the current of clamp potential, illumination, withdrawalof alkali metal cations, and addition of amine were also investigated.These results suggest that the mechanism is the symport of 2H⁺ with each Cl^–, and that the actions of light, externalK⁺, and amine in stimulating Cl^–, influx are indirect.     

Control of Plasma Membrane Cl- Fluxes in Chara corallina by External Cl- and Light

The efflux of Cl^– at the plasma membrane of Chara wasstudied in relation to two treatments known to affect the flux:that of removal of external Cl^– and of light. It is shownthat although removal of external Cl^– results in a rapidreduction in Cl^– efflux (consistent with a direct effectof external Cl^– on the transport system) the magnitudeof this reduction in the dark is greater than the measured darkinflux. Therefore, in the dark at least, it is proposed that1:1 exchange diffusion cannot account for the trans-stimulationof efflux by external Cl^–. Light induces an inhibition of efflux and a concomitant stimulationof Cl^– influx at 20 °C, but at 10 °C the responsesto light of the two fluxes can be separated temporally. It istherefore suggested that the fluxes are not reciprocally dependenton the same factor which mediates in the light response. Furtherconsiderations show that it is unlikely that the cytoplasmicCl^– concentration mediates in the light response of eitherflux, but that changes in cytoplasmic pH may do so.     

Effects of Ammonia and Methylamine on Cl- Transport and on the pH Changes and Circulating Electric Currents Associated with HCO3- Assimilation in Chara corallina

Low concentrations of ammonia and methylamine greatly increaseCl^– influx into Chara corallina. Both amines have theirmaximum effect at pH 6.5–7.5. The amine stimulation ofCl^– influx is small below about pH 5.5. Above pH 8.5 theremay be inhibition of influx by amines. Concentrations of 10–25µM ammonia are sufficient to cause the maximum stimulationof Cl^– influx; the corresponding methylamine concentrationsare 0.1–0.2 mM. It is concluded that entry of amine cations(NH₄^$ and CH₃NH₃^$), rather than unionized bases (NH₃ and CH₃NH₂),causes Cl^– transport to be increased. Increases in rates of Cl^– transport are not necessarilyaccompanied by effects on HCO₃^$ assimilation and OH^– efflux.Measurements of localized pH differences at the cell surfaceand of circulating electric currents in the bathing solutionshow that these phenomena are only significantly affected byammonia at or above 50 µM and by methylamine at or above1.0 mM. The significance of the effects of amines is assessedin relation to current ideas about transport of Cl^–, HCO₃^–,and OH^–.     

Chloride Transport in Chara corallina and the Electrochemical Potential Difference for Hydrogen Ions

The pH of the cytoplasm of Chara corallina cells has been measuredwith the weak acid 5,5-dimethyloxazolidine-2,4-dione (DM0).Over an external pH range 4·5–9·5 the resultsfit the regression equation pH_cytoplasm=6·28+0·22pH_out. Using measured values of the electric potential difference acrossthe plasmalemma we have calculated the electrochemical potentialdifference across this membrane for H⁺ and Cl^–. Thesedata are used to test the hypothesis that the inward transportof Cl^– is coupled to the inthix of H⁺ or, which comesto the same thing, efflux of OH^–. One-for-one couplingwill not give net Cl^– uptake from solutions with pH greaterthan about 7·2, unless the cytoplasmic Cl^– concentrationis lower than 10 mM, or the pH just outside the membrane islower than that in the bulk solution. It is shown that net Cl^–uptake proceeds from solutions with pH up to 9. The alternative possibility is that Cl^– transport is broughtabout by co-transport of two H⁺ for each Cl^–; this isnot ruled out by the results reported. Such a mechanism mightbe detectable by its electrogenic effect: although such effectshave not been detected, it is shown that they would be smallunder most conditions. Other possible mechanisms are discussed.     

The Hyperpolarization of the Chara Membrane at High pH: Effects of External Potassium, Internal pH, and DCCD

At high external pH, the Chara membrane is known to switch toa new state in which the membrane potential is highly negative;it has been characterized as a passive diffusion potential forH⁺ (or 0H^–). DCCD is shown to inhibit the increased conductanceand the highly negative membrane potential associated with thisstate. DCCD also inhibits the plasmalemma H⁺-ATPase, as wellas cytoplasmic streaming. The alkaline state of the membraneis shown to involve a decreased permeability to K⁺; this enhancesthe selectivity for H⁺ (or OH^–) which results from theincreased permeability to H⁺ (or OH^–). Altering the cytoplasmicpH affects the membrane potential at both neutral and alkalinepH. It can also affect the ability of the cell to make the transitionto the alkaline state.     

Inhibition of Cl- Channel Activation in Chara corallina Membrane by Lanthanum Ion

We examined a role of Ca²⁺ in the activation of the two majorion channels, i.e., Cl^– and K⁺ channels at the excitationof the characean plasmalemma. The current-voltage relation (I-Vcurve) of the Chara membrane was compared under the ramp voltageclamp condition before and after external application of 20µMof La³⁺ (a Ca²⁺ channel blocker). The transient inward currentcomponent, which is carried mainly by the efflux of Cl^–,disappeared almost completely in about 30 min with La³⁺ treatment.On the other hand, no effect was observed on the late largeoutward current, which is mainly carried by the efflux of K⁺in a large depolarization region (less negative than –50mV). These results suggest that the Cl^– channel in theChara plasmalemma is activated by Ca²⁺ influx, while the K⁺channel is simply activated by depolarization. (Received April 7, 1986; Accepted June 6, 1986)     

Short-term Measurements of the Cytoplasmic pH of Chara corallina Derived from the Intracellular Equilibration of 5,5-Dimethyloxazolidine-2,4-Dione (DMO)

Smith, F. A. 1986. Short-term measurements of the cytoplasmicpH of Chara corallina derived from the intracellular equilibrationof 5,5-dimethyloxazolidine-2,4-dione (DMO).—J. exp. Bot.37: 1733–1745. Measurements of the time-course of influx of ¹⁴C-labelled 5,5-dimethyloxazolidine-2,4-dione(DMO) into the cytoplasm and vacuole of internodal cells ofChara corallina, and of efflux of DMO into non-radioactive solutions,have shown that exchange of DMO across the tonoplast is veryrapid compared with exchange across the plasma membrane. Thishas made possible calculations of cytoplasmic pH from distributionof DMO between cytoplasm and vacuole over short periods (5 or10 min) even when intracellular DMO is not at flux equilibriumwith external DMO. Using this new method, estimates have beenmade of the rates and magnitude of: (i) acidification of thecytoplasm caused by acidic growth regulators (IAA and NAA) andby metabolic inhibitors (azide, DNP, CCCP and DCMU), and (ii)alkalinization caused by uptake of ammonium and methylammoniumions. The potential application of the method to future studiesof membrane transport in charophyte cells is assessed. Key words: Charophyles, cytoplasmic pH.     

Proton Transport and pH Control in Sinapis alba Root Hairs: A Study carried out with Double-Barrelled pH Micro-electrodes

Continuous measurements of cytoplasmic pH (pH_c) in Sinapis roothairs have been carried out with double-barrelled pH-micro-electrodesin order to gain information on translocation of protons acrossthe plasmalemma and cytoplasmic pH control. (i) The cytoplasmicpH of Sinapis (7–33 ? 0–12, standard conditions)changes no more than 0.1 pH_c, per pH_o-unit, regardless of whethercyanide is present or not. (ii) Weak acids rapidly acidify pH_cand hyperpolarize, while weak bases alkalize pH_c and depolarizethe cells, (iii) 1.0 mol M,³ NaCN acidifies the cytoplasm by0.4 to 0.7 pH-units, but alkalizes the vacuole. (iv) 20 mmolm^–3 CCCP has no significant effect on pH_c, if added atpH 9.6 or 7.2, but acidifies pH_c by 1.3 units at pH 4.3. Inthe presence of CCCP, cyanide acidifies the cytoplasm, (v) Chloridetransiently acidifies pH_c, while K⁺, Na⁺, and have no significant effects, (vi) Cytoplasmic buffer capacityforms a bell-shaped curve versus pH_c with an optimum of about50 mol m^–3 H⁺pH_c-unit. The modes of proton re-entry and the effects of active and passiveproton transport on cellular pH control are critically discussed.It is suggested that the proton leak, consisting of H⁺-cotransport(e.g. H⁺/Cl^–) rather than H⁺-uniport, is no threat topH_c. The proton export pump, although itself reacting to changesin pH_c, influences pH_c only to a minor extent. It is concludedthat buffer capacity and membrane transport play moderate rolesin pH_c control in Sinapis, while the interlocked H⁺-producingand -consuming reactions of cellular metabolism are the mainregulating factors. This makes pH control in Sinapis quite differentfrom bacterial and animal cells. Key words: Cytoplasmic pH, double-barrelled pH micro-electrode, pH control, proton transport, Sinapis     

Comparison of Cytoplasmic pH and Cl- Influx in Cells of Chora corallina Following 'C1- Starvation'

Cytoplasmic pH and C1– influx in cells of Chara corallinahave been measured following pretreatment in C1– freesolutions (‘C1– starvation’) or in controlsolutions containing C1–. Influx of C1– was greatlyincreased following starvation for 3—24 h, but significantchanges in cytoplasmic pH were only detected after 23—24h. It is thus unlikely that increased cytoplasmic pH controlsCl-influx in the early stages of Cl—starvation. Additionof NH⁺⁴ also increased Cl- influx, both in non-starved cellsand (sometimes) in Cl-starved cells, and this effect was accompaniedby an increase in cytoplasmic pH. The possible significanceof the cytoplasmic pH and CI- concentration as factors controllingCI- influx in Chara are assessed.     

Entry of Methylammonium and Ammonium Ions into Chara Internodal Cells

Low concentrations of ammonia and methylamine greatly affectmembrane transport by, and the electrical properties of, cellsof Chara corallina (=C. australis). In the presence of theseamines, influx of Cl^– and efflux of K⁺ increase and alarge depolarizing current flows through the cell membrane. Measurements with [¹⁴C]methylamine show that methylamine isabsorbed rapidly over a wide pH range, and that the absorptionisotherm is complex. Methylamine influx is not affected by presenceor absence of Cl^–, K⁺, or Na⁺, but is decreased by additionof . The depolarizing current is associated with a small increase in membrane conductance, except at highpH, and both these effects are reversible. The current showssaturation with increasing amine concentration; when methylamineis 10–12 times more concentrated than ammonia, it producesa current of the same magnitude. The results show that the amines enter the cells as cations( or CH₃) except where external pH is high, and that a specific, selective electrogenicporter is involved. There is no need to invoke active transport,as there is no evidence that internal amine concentrations exceedthe equilibrium (Nernst) concentrations.     

Malate Accumulates in the Vacuole of Chara australis During Uptake of Ammonium From Chloride-free Solution

Internodal cells of Chara australis can accumulate ammoniumto high concentrations (10 to 70 mol m^–3) in their vacuoles.When Cl^– is included in the bathing solution, changesin the cellular concentrations of ammonium, K⁺, Cl^– andNa⁺ have been shown to meet the requirements for electroneutralityand to account for the changes in vacuolar osmotic pressureassociated with ammonium uptake. If accumulation occurs in theabsence of external Cl^–, however; changes in the inorganicions do not meet these criteria. Malate is found in the vacuolesof cells accumulating amine in the absence of external Cl^–and its presence (at 0·5 to 8·5 mol m^–3)allows us to account for electroneutrality and for changes inthe osmotic potential. Key words: Malate, Chara, electroneutrality, ammonium     

Salinity-induced Malate Accumulation in Chara

Ion absorption by Chara corallina from solutions containingpredominantly KC1 or RbCl at up to 100 mol m^–3 resultedin accumulation of salts and turgor regulation. Turgor regulationdid not occur in solutions containing Na⁺ or Li⁺salts. Duringion absorption from various salts of K⁺ and Rb⁺ vacuolar cationconcentration exceeded Cl^– concentration. This differencewas shown to be balanced by the synthesis and accumulation ofmalate. Vacuolar malate concentration reached 48 mol m₃^–,with accumulation occurring at rates of up to 0.45 mol m^–3h^–1. Malate accumulation was inhibited by low externalpH and was dependent upon external HCO₃^– concentration.The synthesis of malic acid and its subsequent dissociationimposed a severe acid load on the cell. Biophysical regulationof cellular pH was achieved by a H⁺efflux at a rate of about40 nmol m^–2 s^–1from the cell. The results presentedargue against cytoplasmic Cl^–, HCO₃^– or pH regulatingmalate accumulation in Chara and it is suggested that malatetransport across the tonoplast may regulate malate accumulation. Key words: Malate, Chara corallina, pH regulation, salinity     

Effects of Cations on the Cytoplasmic pH of Chara corallina

Smith, F. A. and Gibson, J.–L. 1985. Effects of cationson the cytoplasmic pH of Chara corallina.—J.exp. Bot.36: 1331–1340 Removal of external Ca²⁺ from cells of Chara corallina lowersthe cytoplasmic pH, as determined by the intracellular distributionof the weak acid 5,5–dimethyloxazolidine2–,4–dione(DM0), when the external pH is below about 60. This effect isreversed, at least partially, by addition of the following cationsto Ca²⁺-free solutions: tetraethylammonium (TEA⁺) and Na⁺ at5 or 10 mol m^-3, Li⁺ and Cs⁺ (10 mol m^-3), or Mg²⁺, Mn²⁺ andLa³⁺ (02 or 05 mol m^-3). Under the same conditions, increasesin pH sometimes, but not always, occur in the presence of 10mol m^-3 K⁺ or Rb⁺ The results are discussed in relation to the major transportprocesses that determine pH and the electric potential differenceacross the plasma membrane, namely fluxes of H⁺ and of K⁺. Thesimplest explanation of the effects of the various cations testedin this study is that they primarily affect pHi_c via changesin influx of H⁺ but direct effects on the H⁺ pump or on K⁺ fluxesmay also be involved Key words: Chara corallina, cytoplasmic pH, cations, H⁺transport     

Nitrate Transport into Chara corallina Cells using as an Analogue for Nitrate: III. INTERACTIONS BETWEEN CHLORIDE AND NITRATE TRANSPORT PROCESSES

The effects of Cl^– and pretreatment on ³⁶Cl^–influx and influx into Characorallina cells were examined. Both treatments reduced ³⁶Cl^–influx into C. corallina cells in the acid pH range (4.5–7.0). pretreatment stimulated influx into C. corallina cells, but Cl^– pretreatment hadno effect. There was a direct inhibitory effect of CI on influx into C. corallina cells, but no apparenteffect on net NO uptake. The time course of ³⁶Cl accumulation into cytoplasmic and vacuolarcompartments during incubation of the cells with showed that significant radioactivity appeared in the vacuolarsap after 30 min. There was a linear increase in the percentageof total ³⁶CI which crossed the tonoplast (_c-v). There was noeffect of Cl^– or pretreatment on accumulation of radioactivity in the vacuole. Thin layer chromatography ofthe vacuolar sap showed that after 2 h only one component waspresent which had an R_F which was similar to ³⁶CI^–. Therate of accumulation of ³⁶C1^– in the vacuole could beused to estimate rates of reduction. Key words: Chloride, Chlorate, Chara, Nitrate     

Proton-Chloride Symport in Barley Roots

An increase in the acidity of the incubation medium from pH6 5 to pH 4.0 increased Cl- flux into ATP-depleted Hordeum vulgareL roots more than three times This pH-dependent Cl^– fluxwas inhibited by p-chloromercuriphenyl sulphonic acid. The effectof pH on Cl- influx was eliminated when the pH gradient wasdissipated by addition of salts of permeable weak acids, andin K-loaded roots in the presence of a protonophore togetherwith valinomycin The results support the assumption that a H⁺-Cl^–symportsystem is present in barley root cells Hordeum vulgare L., barley, excised roots, ion transport, proton-chloride symport     

Ion Effluxes during Excitation of Characeae

Ion effluxes during excitation of Chara and Nitellopsis measuredby conductometry method were compared with results obtainedby two other analytical methods, Ag-AgCl method for Cl^–and ion chromatography method for K⁺. In both species, the averageefflux measured by the conductometry method was very close tothose of K⁺ and Cl^–. (Received May 12, 1986; Accepted June 25, 1986)     

Nitrate Transport into Chara corallina Cells using 36ClO-3 as an Analogue for Nitrate: I. INTERACTION BETWEEN 36ClO-3 AND NO-3 AND CHARACTERIZATION OF 36CIO-3/NO-3 INFLUX

The use of chlorate as an analogue for NO^–₃ during nitrateuptake into Chara corallina cells has been investigated. NO^–₃inhibits ³⁶C1O^–₃ influx into Chara over the concentrationrange 0–1000 mmol m^–3. Lineweaver-Burke plots ofthe data are characteristic of competitive inhibition by NO^–3in the low concentration range (0–300 mmol m^–3 ClO^–₃)and apparent K_INO3 is 140 mmol m^–3 which is of a similarorder of magnitude as apparent K_mCIO3- 180 mmol m^–3. Athigher substrate concentrations the inhibition by NO^–₃was not characteristic of competitive or uncompetitive inhibition. ³⁶C1O^–₃/NO^–₃ influx was dependent on K⁺ and Ca²⁺in the external medium and inhibited by FCCP. NO^–₃ pretreatmentor N starvation increased subsequent ³⁶C1O^–₃/NO^–₃influx into Chara. A comparison between rates of net NO^–₃uptake and ³⁶C1O^–₃/NO^–₃ influx supported the previoushypothesis that NO^–₃ efflux is an important componentin the determination of overall uptake rates. Key words: Nitrate, Chara, ³⁶CIO^–₃     

Uptake of Methylamine by Ulva rigida: Transport of Cations and Diffusion of Free Base

Methylamine¹ is taken up rapidly by disks cut from fronds ofUlva rigida (‘Ulva lactuca’) and can be accumulatedat concentrations several hundred times greater than those inthe bathing medium. At pH 8.0 (the pH of sea-water) the relationshipbetween influx and concentration is normally linear up to 0.1–0.3mM, followed by a second, less steep linear phase, the slopeof which decreases or increases with decreasing or increasingexternal pH. When pH is greater than 9.0, however, net uptakesoon ceases. Methylamine influx is greatly reduced at low temperature,by low concentrations of ammonia and, depending on the lengthof storage of the material, by darkness. Influx is also greatlyreduced when disks are pretreated in solutions containing ammoniaand to a much lesser extent when they are pretreated in methylamine,imidazol or nitrate. Methylamine influx lowers intracellularK⁺, increases Cl^– and has no effect on Na⁺. We suggestthat the first linear phase of influx versus concentration reflectsthe operation of an amine cation porter that is rate-limitedby diffusion of CH₃NH₃⁺ through the external unstirred layer,and that the second phase is due to diffusion of CH₃NH₂ intothe tissue.