Differential effects of Na+, Mg2+, K+, Ca2+ and osmotic stress on the wild type and the NaCl-tolerant mutants stl1 and stl2 of Ceratopteris richardii

In order to identify physiological components that contribute to salinity tolerance, we compared the effects of Na⁺, Mg²⁺ and K⁺ salts (NaCl, Na₂SO₄, MgCl₂, MgSO₄, KCl and K₂SO₄), Ca₂₊ (CaSO₄), mannitol and melibiose on the wild type and the single-gene NaCl-tolerant mutants stl1 and stl2 of Ceratopteris richardii. Compared with gametophytic growth of the wild type, stl2 showed a low level of tolerance that was restricted to Na⁺ salts and osmotic stress. stl2 exhibited high tolerance to both Na⁺ and Mg²⁺ salts, as well as to osmotic stress. In response to short-term exposure (3 d) to NaCl, accumulation of K⁺ and Na⁺ was similar in the wild type and stl1. In contrast, stl2 accumulated higher levels of K⁺ and lower levels of Na⁺. Ca²⁺ supplementation (1.0 mol m^?3) ameliorated growth inhibition by Na⁺ and Mg²⁺ stress in wild type and stll, but not in stl2. In addition, under Na⁺ stress (175 mol m^?3) wild-type, stll and stl2 gametopbytes maintained higher tissue levels of K⁺ and lower levels of Na⁺ when supplemented with Ca²⁺ (1.0 mol m^?3). stl2 gametophytes were extremely sensitive to K⁺ supplementation. Growth of stl2 was greater than or equal to that of the wild type at trace concentrations of K⁺ but decreased substantially with increasing K⁺ concentration. Supplementation with K⁺ from 0 to 1.85 mol m^?3 alleviated some of the inhibition by 75 mol m^?3 NaCl in the wild type and in stl1. In stl2, growth at 75 mol m^?3 NaCl was similar at 0 and 1.85 mol m^?3 K⁺ supplementation. Although K⁺ supplementation above 1.85 mol m^?3 did not alleviate inhibition of growth by Na⁺ in any genotype, stl2 maintained greater relative tolerance to NaCl at all K⁺ concentrations tested.     

Rapid calcium exchange for protons and potassium in cell walls of Chara

Net fluxes of Ca²⁺, H⁺ and K⁺ were measured from intact Chara australis cells and from isolated cell walls, using ion-selective microelectrodes. In both systems, a stimulation in Ca²⁺ efflux (up to 100 nmol m^?2 s^?1, from an influx of ～40 nmol m^?2 s^?1) was detected as the H⁺ or K⁺ concentration was progressively increased in the bathing solution (pH 7.0 to 4.6 or K⁺ 0.2 to 10mol m^?3, respectively). A Ca²⁺ influx of similar size occurred following the reverse changes. These fluxes decayed exponentially with a time constant of about 10 min. The threshold pH for Ca²⁺ efflux (pH 5.2) is similar to a reported pH threshold for acid-induced wall extensibility in a closely related characean species. Application of NH₄⁺ to intact cells caused prolonged H⁺ efflux and also transient Ca²⁺ efflux. We attribute all these net Ca²⁺ fluxes to exchange in the wall with H⁺ or K⁺. A theoretical treatment of the cell wall ion exchanges, using the ‘weak acid Donnan Manning’ (WADM) model, is given and it agrees well with the data. The role of Ca²⁺ in the cell wall and the effect of Ca²⁺ exchanges on the measured fluxes of other ions, including bathing medium acidification by H⁺ efflux, are discussed.     

SO2-dependent cation competition and compartmentalization in Norway spruce needles

Ion contents in needles from Norway spruce trees [Picea abies (L.) Karst.] growing in Würzburg and in the SO₂-polluted Erzgebirge mountains were analysed to quantify cations which accumulate together with sulphate. In Würzburg there was a positive correlation of potassium (0.680 ± 0.300 Eq Eq^?1 SO₄^?2), magnesium (0.415 ± 0.111 Eq Eq^?1 SO₄^?2) and zinc (0.059 ± 0.006 Eq Eq^?1 SO₄^2?). In the Erzgebirge, potassium was also the stoichiometrically most important cation (0–887 ± 0–180 Eq K⁺ Eq^?1 SO₄^2?). All other correlations examined were weak or statistically non-significant. At both sites the calcium content of spruce needles did not depend on the sulphate content. The lack of a role for Ca²⁺ in neutralizing sulphate is a consequence of the presence of free oxalic acid in needles. Soluble oxalic acid precipitates Ca²⁺, which thereby becomes unavailable as a counterion for SO₄^2?. The activity coefficients of Ca²⁺ and oxalate^2?, and the solubility product of Ca-oxalate, were determined from in vivo data. It is concluded that the chronic accumulation of atmospheric sulphate in spruce needle vacuoles depletes available potassium and thereby strongly interferes with spruce growth and canopy turnover. This leads to impaired spruce vitality, even at sites where acute SO₂ disease symptoms are absent.     

The effect of divalent cations on Na+ tolerance in Charophytes. I: Char a buckellii

Abstract The comparative Na⁺ tolerance of Chora buckellii cultured in freshwater (FW) or artificial Waldsea water (AWW, which contains about 110 mol m^?3 each Na ⁺, Mg²⁺, Cl^? and SO^2-₄ was tested with respect to the external Na⁺ to Ca²⁺ ratio (Na: Ca). Fifty per cent of FW cells subjected to 70 mol m^?3 NaCl, which raised Na:Ca from 10: 1 to 700: 1 and the external osmotic pressure from 0.024 to 0.402 MPa, died within 6 d. Death was associated with the loss of Na/K selectivity, H⁺ -pump activity and turgor. Restoration of Na:Ca to 10:1 in high Na⁺ medium with CaCl₂ ensured 100% survival and maintained H⁺-pump activity and Na/K selectivity of FW cells. Turgor was regulated within 3 d with net uptake of Na ⁺, K⁺ and Cl^? in the vacuolc. Mg²⁺ was not as effective as Ca²⁺ in enhancing survival or maintaining H⁺ -pump activity and Na/K selectivity of FW cells in the presence of elevated Na⁺. However, turgor was regulated within 3 d by accumulation of Cl^? and an unknown cation in the vacuole. All AWW cells subjected to an increase of 70 mol m ^?3 NaCl, which raised Na: Ca from 16:1 to 25: 1 and the external osmotic pressure from 0.915 to 1.22 MPa, survived and maintained H ⁺ -pump activity. Turgor was regulated within 6d by accumulating Na ⁺, K⁺ and Cl^? in the vacuole. All AWW cells subjected to 70molm^?3 NaCl in a medium in which Na:Ca was equal to 700:1 survived and maintained H ⁺ -pump activity, but showed loss of Na/K selectivity. Turgor was regulated with an unknown osmoticum(a) within 6 d.     

Ionic processes underlying the decrease in osmotic potential of Chara L-cell fragments in dilute electrolyte solutions

Movements of ions are considered to be governed by the electroneutrality rule. Therefore, a cation moving across the cell membrane into the cell either passively or actively should move together with its counterion, an anion, in equal amounts of charge or in exchange for another cation inside the cell. This means that the net influx of the cation in question should be affected by the permeability of its counterion and/or another cation inside the cell. To examine osmotic and ionic regulation in Chara cells, cell fragments of Chara having a lower osmotic pressure than normal (L-cell fragments) were prepared. The L-cell fragments were individually put into various dilute electrolyte solutions and their osmotic potentials were measured with a turgor balance. Concentrations of K⁺, Na⁺, Ca²⁺, Mg²⁺, Cl^?, NO^?₃. and SO^2?₄. in the external electrolyte solutions in which L-cells had been incubated were also analysed by ion chromatography. The results showed that in 0.5 mM KCL + 0.1 mM CaCl₂ solution, Chara L-cell fragments absorbed K⁺ and Cl^? to maintain electroneutrality and then regained their osmotic potential very rapidly. When the anion was Cl, the cation absorbed at the highest rate was K⁺ On the other hand, when the cation was K, the anion absorbed at the highest rate was Cl, Other ions Ca²⁺, SO^2?₄ and NO^?₃ showed much less permeability than K⁺ and Cl ^?for the Chara plasma membrane. The conclusion from these findings was that due to the constraint of electroneutral transport, the uptake rate of a salt into L-cells is limited by the permeability of the least permeable ion.     

Alkalinity and acidity cycling and fluxes in an intermediate fen peatland in northern Ontario

Peatlands are important to global carbon (C) sequestration and surface water acid–base status, both of which are affected by peatland alkalinity and acidity cycling. Relationships among sulfate (SO₄ ^2?), nitrate (NO₃ ^?), organic acids (OA^?), base cations (i.e., Ca²⁺, Mg²⁺, K⁺, and Na⁺), proton (H⁺) acidity, and bicarbonate (HCO₃ ^?) alkalinity were investigated in an intermediate fen peatland in northern Ontario during 2004 (an average precipitation year) and 2005 (a dry summer). Potential evapotranspiration was higher and the water table, groundwater input from the uplands, and runoff were lower during 2005. Net inputs of base cations, HCO₃ ^?, SO₄ ^2?, and OA^?, and to a lesser degree NO₃ ^?, were lower during the drier year, mainly due to lower groundwater transfer to the fen. Fen porewater HCO₃ ^? concentration and net output were also lower in the drier year, whereas Ca²⁺, Mg²⁺, and SO₄ ^2? concentrations and net output were higher. During the climatically average year, N immobilization, carbonic acid (H₂CO₃) dissociation, and OA dissociation were equally important H⁺-producing reactions. Peat cation exchange accounted for 50% of the H⁺ sink, while SO₄ ^2? reduction and denitrification accounted for an additional 20 and 25% of the H⁺ sink, respectively. During the dry year, S oxidation accounted for 55% of the H⁺ net production, while that for H₂CO₃ dissociation was 70% lower than that during the climatically average year. Peat cation exchange consumed three times the acidity, and accounted for 92% of the H⁺ consumption during the dry year compared to the climatically average year. This was consistent with a three-fold higher net base cation export from the fen during the dry year. Based on the study results, a conceptual model was developed that describes the role of acidity formation and its implications to intermediate fen acidification.     

Sodium transport measured in plasma membrane vesicles isolated from wheat genotypes with differing K+/Na+ discrimination traits

Right-side-out plasma membrane vesicles were isolated from wheat roots using an aqueous polymer two-phase system. The purity and orientation of the vesicles were confirmed by marker enzyme analysis. Membrane potential (Ψ)-dependent ²²Na⁺ influx and sodium/proton (Na⁺/ H⁺) antiport-mediated efflux across the plasma membrane were studied using these vesicles. Membrane potentials were imposed on the vesicles using either K⁺ gradients in the presence of valinomycin or H⁺ gradients. The ΔΨ was quantified by the uptake of the lipophilic cation tetraphenylphosphonium. Uptake of Na⁺ into the vesicles was stimulated by a negative ΔΨ and had a K_m for extrav-esicular Na⁺ of 34.8 ± 5.9 mol m³. The ΔΨ-dependent uptake of Na⁺ was similar in vesicles from roots of hexaploid (cv. Troy) and tetraploid (cv. Langdon) wheat differing in a K⁺/Na⁺ discrimination trait, and was also unaffected by growth in 50 mol m^?3 NaCl. Inhibition of ΔΨ-dependent Na⁺ uptake by Ca²⁺ was greater in the hexaploid than in the tetraploid. Sodium/proton antiport was measured as Na⁺-dependent, amiloride-inhibited pH gradient formation in the vesicles. Acidification of the vesicle interior was measured by the uptake of ¹⁴C-methylamine. The Na⁺/H⁺ antiport had a K_m, for intravesicular Na⁺ of between 13 and 19 mol m^?3. In the hexaploid, Na⁺/H⁺ antiport activity was greater when roots were grown in the presence of 50 mol m^?3NaCl, and was also greater than the activity in salt-grown tetraploid wheat roots. Antiport activity was not increased in a Langdon 4D chromosome substitution line which carries a trait for K⁺/Na⁺ discrimination. It is concluded that neither of the transport processes measured is responsible for the Na⁺/K⁺ discrimination trait located on the 4D chromosome of wheat.     

Daily Patterns under the Life Cycle of a Maize Crop

Together with photosynthesis, transpiration and respiration, the daily uptake of NO₃^?, NH₄⁺, H₂PO₄^?, K⁺, Ca²⁺, Mg²⁺, SO₄^2?, the root respiration, root volume increase and root excretions have been studied by daily measurements during the growth period of whole maize plants (Zea mays L. cv. INRA F7 × F2) raised until complete maturity on nutrient solution. The uptake patterns show a maximum absorption of NO₃^?, K⁺ and Ca²⁺ during the vegetative growth phase. The absorption of these ions declines during maturation while that of H₂PO₄^? reaches a maximum. Root respiration and particularly the uptake of NO₃^? and K⁺ are well correlated with the rate of root growth. Root excretion is more notable in young plants than in the old. It represents less than 0.2% of the net assimilation of adult plants.     

The influence of monovalent cations upon influx and efflux of Ca2+ in barley roots

The effects of monovalent cations, inhibitors of metabolism dinitrophenol (DNP), carbonyl cyanide-p-trifluoromethoxyphenylhydrazone (FCCP), and KCN and temperature variations upon Ca²⁺ fluxes in intact roots of barley (Hordeum vulgare L. cv. Fergus and Herta) seedlings were investigated. ⁴⁵Ca²⁺ influx was depressed in CaSO₄-grown (low-salt) plants by the presence of NH₄⁺, K⁺, or Na⁺ in the uptake medium. In contrast Ca²⁺ influx was slightly increased by Li⁺. In low-salt roots pretreated with KCN and in roots preloaded with K⁺ (high-K⁺ plants), the presence of K⁺ in the medium had no significant effect on Ca²⁺ influx, while in roots preloaded with Na⁺, the presence of K⁺ in the medium depressed Ca²⁺ influx. In absolute terms, Ca²⁺ influx was significantly greater in high-salt (both K⁺ or Na⁺ preloaded) than in low-salt roots.Patterns of ⁴⁵Ca²⁺ efflux in the absence and in the presence of K⁺, NH₄⁺, or Li⁺ in the external medium showed that these monovalent cations caused stimulation of ⁴⁵Ca²⁺ efflux both from the cytoplasmic and vacuolar phases.It was noted that these modifications of Ca²⁺ fluxes by monovalent cations are transient and characteristic of a transitional stage of cation uptake by low-salt roots. We conclude that, together with stimulated active H⁺ efflux (another characteristic of this transitional stage), modifications of Ca²⁺ fluxes during monovalent cation uptake by low-salt roots is a response directed towards the maintenance of electrical neutrality.Determination of net fluxes revealed that the plants were close to Ca²⁺ flux equilibrium in the growth medium (0.5 mM CaSO₄). Transfer of these plants to 0.5 mM CaSO₄ + 0.25 mM K₂SO₄ caused a net release of CA²⁺ into the external medium.     

披针叶黄华试管苗适应盐胁迫的渗透调节机制

以披针叶黄华(Thermopsis lanceolata)试管苗为材料,通过组培方法研究其在0、0.2%、0.4%、0.6%、0.8%和1.0%NaCl和Na2SO4胁迫30d后的生长、有机渗透调节物质和无机渗透调节物质(Na+、K+和Ca2+)含量的变化,以探讨其耐盐性机制。结果显示:(1)随NaCl和Na2SO4胁迫浓度的增加,披针叶黄华试管苗叶片脯氨酸和可溶性糖含量均显著持续增加,且NaCl胁迫下脯氨酸上升的幅度均大于相同浓度Na2SO4胁迫下的增幅,而可溶性糖上升的幅度却小于相同浓度Na2SO4胁迫下的幅度;可溶性蛋白含量随NaCl浓度的增大呈先升高后降低的趋势,但随Na2SO4浓度的增加呈持续上升的趋势。(2)随NaCl和Na2SO4浓度的增加,披针叶黄华试管苗Na+含量呈增加趋势且各处理均显著高于对照,Ca2+含量和叶片K+含量却呈逐渐减少趋势且各处理均显著低于对照,而根系K+含量呈先降后升的趋势;Na2SO4胁迫下披针叶黄华试管苗叶片Na+含量上升幅度以及K+和Ca2+含量下降幅度均明显低于相同浓度NaCl胁迫组;而Na+/K+和Na+/Ca2+比值随NaCl和Na2SO4浓度增加而升高;NaCl胁迫下,叶片Na+/K+和Na+/Ca2+高于相同浓度Na2SO4胁迫下的比值,而根系Na+/K+和Na+/Ca2+却低于相同浓度Na2SO4胁迫下的比值。研究表明,盐胁迫下,披针叶黄华试管苗通过抑制叶片中Na+积累并增加可溶性糖和可溶性蛋白含量,在根系中维持较高K+和Ca2+含量以及较低水平Na+/K+和Na+/Ca2+比,以降低披针叶黄华细胞渗透势来适应盐渍环境;披针叶黄华对NaCl胁迫的调节能力弱于Na2SO4。     

Transmembrane potential-mediated coupling between H+ pump operation and K+ fluxes in Elodea densa leaves hyperpolarized by fusicoccin, light or acid load

In isolated Elodea densa leaves, the relationships between H⁺ extrusion (-ΔH⁺), K⁺ fluxes and membrane potential (E_m) were investigated for two different conditions of activation of the ATP-dependent H⁺ pump. The ‘basal condition’ (darkness, no pump activator present) was characterized by low values of-ΔH⁺ and K⁺ uptake (ΔK⁺), wide variability of the ?ΔH⁺/ΔK⁺ ratio, relatively low membrane polarization and E_m values more positive than EK for external K⁺ concentrations (|K⁺]_o of up to 2mol m^?3. A net K⁺ uptake was seen already at [K⁺]_o below 1 mol m^?3, suggesting that K⁺ influx in this condition was a thermodynamically uphill process involving an active mechanism. When the H⁺ pump was stimulated by fusicoccin (FC), by cytosol acidification, or by light (the ‘high polarization condition’), K⁺ influx largely dominated K⁺ and C^? efflux, and the ?ΔH⁺/ΔK⁺ ratio approached unity. In the range 50 mmol m^?3?5 mol m^?3 [K⁺]₀, E_m was consistently more negative than E_K. The curve of K⁺ influx at [K⁺]₀ ranging from 50 to 5000mmol m^?3 fitted a monophasic, hyperbolic curve, with an apparent half saturation value = 0–2 mol m^?3. Increasing |K⁺]₀ progressively depolarized E_m, counteracting the strong hyperpolarizing effect of FC. The effects of K⁺ in depolarizing E_m were well correlated with the effects on both K⁺ influx and ?ΔH⁺, suggesting a cause-effect chain: K⁺₀ influx → depolarization → activation of H⁺ extrusion. Cs⁺ competitively inhibited K⁺ influx much more strongly in the ‘high polarization’ than in the ‘basal’ condition (50% inhibition at [Cs⁺]/[K⁺]₀ ratios of 1:14 and 1:2, respectively) thus confirming the involvement of different K⁺ uptake systems in the two conditions. These results suggest that in E. densa leaves two distinct modes of interactions rule the relationships between H⁺ pump, membrane polarization and K⁺ transport. At low membrane polarization, corresponding to a low state of activation of the PM H⁺-ATP^ase and to E_m values more positive than E_K, K⁺ influx would mainly     

Cation pretreatment effects on nitrate uptake, xylem exudate, and malate levels in wheat seedlings

Week-old wheat seedlings absorbed at least 40% NO₃⁻ from NaNO₃ when preloaded with K⁺ than when preloaded with Na⁺ or Ca²⁺. Cultures of Triticum vulgare L. cv. Arthur were grown for 5 days on 0.2 mm CaSO₄, pretreated for 48 hours with either 1 mm CaSO₄, K₂SO₄, or Na₂SO₄, and then transferred to 1 mm NaNO₃. All solutions contained 0.2 mm CaSO₄. Shoots of K⁺-preloaded plants accumulated three times more NO₃⁻ than shoots of the other two treatments. Initially, the K⁺-preloaded plants contained 10-fold more malate than either Na⁺- or Ca²⁺-preloaded seedlings. During the 48-hour treatment with NaNO₃, malate in both roots and shoots of the K⁺-preloaded seedlings decreased. Seedlings preloaded with K⁺ reduced 25% more NO₃⁻ than those preloaded with either Na⁺ or Ca²⁺. These experiments indicate that K⁺ enhanced NO₃⁻ uptake and reduction even though the absorption of K⁺ and NO₃⁻ were separated in time. Xylem exudate of K⁺-pretreated plants contained roughly equivalent concentrations of K⁺ and NO₃⁻, but exudate from Na⁺ and Ca²⁺-pretreated plants contained two to four times more NO₃⁻ than K⁺. Therefore K⁺ is not an obligatory counterion for NO₃⁻ transport in xylem.     

Changes in growth and water-soluble solute concentrations in Sorghum bicolor stressed with sodium and potassium salts

Sorghum bicolor L. Moench, RS 610, was grown in liquid media salinized with NaCl, KCl, Na₂SO₄, K₂SO₄ or with variable mixtures of either NaCl/KCl or Na₂SO₄/K₂SO₄ at osmotic potentials ranging from 0 to -0.8 MPa. The purpose was to study the effects of different types and degrees of salinity in growth media on growth and solute accumulation. In 14-day-old plants the severity of leaf growth inhibition at any one level of osmotic potential in the medium increased according to the following order: NaCl < Na₂SO₄ < KCl = K₂SO₄. Inhibition of growth by mixtures of Na⁺ and K⁺ salts was the same as by K⁺ salts alone. Roots responded differently. Root growth was not affected by Na⁺ salts in the range of 0 to -0.2 MPa while it was stimulated by K⁺ salts. The major cation of leaves was K⁺ because S. bicolor is a Na⁺-excluder, while Na⁺ was the major cation in roots except at low Na⁺/K⁺ ratios in media. Anions increased in tissues linearly in relation to total monovalent cation, but not with a constant anion/cation ratio. This ratio increased as the cation concentrations in tissues increased. Sucrose in leaf tissue increased 75 fold in Chloride-plants (plants growing in media in which the only anion of the salinizing salts was Cl^?) and 50 fold in Sulphate-plants (the only anion of the salinizing salts was SO₄^2-). Proline increased 60 and 18 fold in Chloride- and Sulphate-plants, respectively, as growth media potentials decreased from 0 to -0.8 MPa. The concentrations of both sucrose and proline were directly proportional to the amount of total monovalent cation in the tissue. Sucrose concentrations began increasing when total monovalent cations exceeded 100 μmol (g fresh weight)^?1 (the monovalent cation level in non-stressed plants), but proline did not start accumulating until monovalent cation concentrations exceeded 200 μmol (g fresh weight)^?1. Therefore, sucrose seemed to be the solute used for osmotic adjustment under mild conditions of saline stress while proline was involved in osmotic adjustment under more severe conditions of stress. Concentrations of inorganic phosphate, glucose, fructose, total amino acids and malic acid fluctuated in both roots and leaves in patterns that could be somewhat correlated with saline stress and, sometimes, with particular salts in growth media. However, the changes measured were too small (at most a 2–3 fold increase) to be of importance in osmotic adjustment.     

Time and charge/pH-dependent activation of K+ channel-mediated K+ influx and K+/H+ exchange in guinea pig heart isolated mitochondria; role in bioenergetic stability

Mitochondria play an important role not only in producing energy for the cell but also for regulating mitochondrial and cell function depending on the cell's needs and environment. Uptake of cations, anions, and substrates requires a stable, polarized transmembrane charge potential (ΔΨ_m). Chemiosmosis requires ion exchangers to remove Na⁺, K⁺, Ca²⁺, PO₄^3?, and other charged species that enter mitochondria. Knowledge of the kinetics of mitochondrial (m) cation channels and exchangers is important in understanding their roles in regulating mitochondrial chemiosmosis and bioenergetics. The influx/efflux of K⁺, the most abundant mitochondrial cation, alters mitochondrial volume and shape by bringing in anions and H₂O by osmosis. The effects of K⁺ uptake through ligand-specific mK⁺ channels stimulated/inhibited by agonists/antagonists on mitochondrial volume (swelling/contraction) are well known. However, a more important role for K⁺ influx is likely its effects on H⁺ cycling and bioenergetics facilitated by mitochondrial (m) K⁺/H⁺ exchange (mKHE), though the kinetics and consequences of K⁺ efflux by KHE are not well described. We hypothesized that a major role of K⁺ influx/efflux is stimulation of respiration via the influx of H⁺ by KHE. We proposed to modulate KHE activity by energizing guinea pig heart isolated mitochondria and by altering the mK⁺ cycle to capture changes in mitochondrial volume, pH_m, ΔΨ_m, and respiration that would reflect a role for H⁺ influx via KHE to regulate bioenergetics. To test this, mitochondria were suspended in a 150 mM K⁺ buffer at pH 6.9, or in a 140 mM Cs⁺ buffer at pH 7.6 or 6.9 with added 10 mM K⁺, minimal Ca²⁺ and free of Na⁺. O₂ content was measured by a Clark electrode, and pH_m, ΔΨ_m, and volume, were measured by fluorescence spectrophotometry and light-scattering. Adding pyruvic acid (PA) alone caused increases in volume and respiration and a rapid decrease in the transmembrane pH gradient (ΔpH_m = pH_in–pH_ext) at pH_ext 6.9> > 7.6, so that ΔΨ_m was charged and maintained. BK_Ca agonist NS1619 and antagonist paxilline modified these effects, and KHE inhibitor quinine and K⁺ ionophore valinomycin depolarized ΔΨ_m. We postulate that K⁺ efflux-induced H⁺ influx via KHE causes an inward H⁺ leak that stimulates respiration, but at buffer pH 6.9 also utilizes the energy of ΔpH_m, the smaller component of the overall proton motive force, ΔμH⁺. Thus ΔpH_m establishes and maintains the ΔΨ_m required for utilization of substrates, entry of all cations, and for oxidative phosphorylation. Thus, K⁺ influx/efflux appears to play a pivotal role in regulating energetics while maintaining mitochondrial ionic balance and volume homeostasis.     

Calcium-salinity interactions affect ion transport in Chara corallina

Detached internodes of Chara corallina survived in solutions containing 100 mol m^?3 NaCl when the external concentration of Ca²⁺ was greater than 1 mol m^?3. Na⁺ influx was roughly proportional to external Na⁺ up to 100 mol m^?3 NaCl. Na⁺ influx involved two components: a Ca²⁺-insensitive influx which allowed the passage of Na⁺ independently of external Ca²⁺; and a Ca²⁺-inhibitable mechanism where Na⁺ influx was inversely proportional to external Ca²⁺. The Ca²⁺-inhibitable Na⁺ influx was similar to the Ca²⁺-inhibitable K⁺ influx. Mg²⁺ and Ba²⁺ were able to substitute for Ca²⁺ in partially inhibiting Na⁺ influx in the absence of external Ca²⁺. The effect of Ca²⁺ appears specific to Na⁺ and K⁺ influx since the effects of a Ca²⁺-free solution on the influx of some other cations, anions and neutral compounds is small. It is suggested that Na⁺ influx via the Ca²⁺-inhibitable mechanism represents Na⁺ leakage through K⁺ channels and that cell death at high salinity occurs due to a cytotoxic Na⁺ influx via this mechanism.     

A Mg2+-stimulated ATPase in platelet alpha-granule membranes: possible involvement in proton translocation

Isolated porcine platelet α granules display a Mg²⁺-stimulated ATPase activity. The enzyme is membrane bound and several criteria suggest that it is intrinsic to the α granules, rather than arising from contamination with other structures. Characterization of the ATPase revealed an apparent K_m for ATP of 198 μm. Other nucleotides are also hydrolyzed by the enzyme, though at a slower rate. The enzyme has an absolute requirement for divalent cations, and both Mg²⁺ (apparent K_m 0.93 mm) and Ca²⁺ (apparent K_m 0.95 mm) can activate it. Maximal hydrolysis rates are higher with Mg²⁺ than with Ca²⁺. Micromolar Ca²⁺ in the presence of maximally stimulating Mg²⁺ concentrations produces a small additional enhancement of activity. The Mg²⁺ ATPase has a broad activity maximum between pH 6.5 and 8.5, and an activation energy of 11.8 Kcal/mol. Several independent observations suggest that the ATPase could be involved in H⁺ translocation across the granule membrane: (a) the activity is stimulated upon disrupting membrane continuity by either hypotonic lysis or addition of nondenaturing detergents; (b) proton ionophores enhance the activity in intact but not in disrupted α granules; (c) permeating anions stimulate the ATPase more than slowly permeant or impermeant ones; (d) addition of NH₃ (as either NH₄Cl or (NH₄)₂SO₄) activates enzyme activity; (e) silicotungstate and disulfonic stilbene derivatives, which are inhibitors of other H⁺-transporting ATPases, also inhibit the α-granule enzyme. These findings are compared with the reported properties of H⁺ pumps of other storage and secretory organelles.     

Kinetics and ion specificity of Na/Ca exchange mediated by the reconstituted beef heart mitochondrial Na/Ca antiporter

The Na⁺/Ca²⁺ antiporter was purified from beef heart mitochondria and reconstituted into liposomes containing fluorescent probes selective for Na⁺ or Ca²⁺. Na⁺/Ca²⁺ exchange was strongly inhibited at alkaline pH, a property that is relevant to rapid Ca²⁺ oscillations in mitochondria. The effect of pH was mediated entirely via an effect on the K_m for Ca²⁺. When present on the same side as Ca²⁺, K⁺ activated exchange by lowering the K_m for Ca²⁺ from 2  to 0.9 μM. The K_m for Na⁺ was 8 mM. In the absence of Ca²⁺, the exchanger catalyzed high rates of Na⁺/Li⁺ and Na⁺/K⁺ exchange. Diltiazem and tetraphenylphosphonium cation inhibited both Na⁺/Ca²⁺ and Na⁺/K⁺ exchange with IC₅₀ values of 10 and 0.6 μM, respectively. The V_max for Na⁺/Ca²⁺ exchange was increased about fourfold by bovine serum albumin, an effect that may reflect unmasking of an autoregulatory domain in the carrier protein.     

Mitochondrial cation transport: A progress report

This report summarizes recent work in our laboratory aimed at understanding protein-mediated mitochondrial cation transport. We are studying three distinct cation cycles that contain porters catalyzing influx and efflux of cations between cytosol and mitochondrial matrix. Each of these cation cycles plays a major physiological role in the overall energy economy. The K⁺ cycle maintains the integrity of the vesicular structure and includes the K⁺/H⁺ antiporter, the K_ATP channel, and K⁺ leak driven by the high membrane potential. The Ca²⁺ cycle relays the signals calling for modulation of ATP production and includes the Ca²⁺ channel, the Na⁺/Ca²⁺ antiporter, and the Na⁺/H⁺ antiporter. The H⁺ cycle of brown adipose tissue mitochondria provides heat to hibernating and newborn mammals and consists of the uncoupling protein, which catalyzes regulated H⁺ influx.     

Ecophysiological investigations of Chara vulgaris L. grown in a brackish water lake: ionic changes and accumulation of sucrose in the vacuolar sap during sexual reproduction

Abstract Chara vulgaris L. growing in a brackish water lake was investigated in a field study during the main growth season (May to October 1985). Sucrose content and the ionic concentrations of the cations Na⁺, K⁺, Mg²⁺ and Ca²⁺ and the anions Cl^? and SO₄^2- of the vacuolar sap were estimated. Sucrose concentration in the vacuolar sap of vegetative growing plants was negligible, but with the beginning of the sexual reproduction period (fructification) the sucrose content increased from about 2 mol m^?3 to 110 mol m^?3. This level remained constant until the end of the fructification period. In spite of the increase of the sucrose concentration the osmotic potential of the vacuolar sap was constant. This was achieved by changing the ionic concentrations accordingly; in old or vegetative growing plants the ionic content accounted for about 80% of the vacuolar osmotic potential, but was about 63% during fructification. Sucrose is considered as a major photosynthate to supply the developing antheridia and oogonia and to serve as a precursor for the starch stored in the eggs.     

High salinity tolerance in the stl2 mutation of Ceratopteris richardii is associated with enhanced K+ influx and loss

The roles of K⁺ uptake and loss in the salinity response of the wild type and the salt-tolerant mutant stl2 of Ceratopteris richardii were studied by measuring Rb⁺ influx and loss and the effects of Na⁺, Mg²⁺, Ca²⁺ and K⁺-transport inhibitors. In addition, electrophysiological responses were measured for both K⁺ and Rb⁺ and for the effects of Na⁺ and NH₄⁺ on subsequent K⁺-induced depolarizations. stl2 had a 26–40% higher uptake rate for Rb⁺ than the wild type at 0.5–10 mol m^?3 RbCl. Similarly, membrane depolarizations induced by both RbCl and KCl were consistently greater in stl2. In the presence of 0–180 mol m^?3 NaCl, stl2 maintained a consistently greater Rb⁺ influx than the wild type. stl2 retained a greater capacity for subsequent KCl-induced depolarization following exposure to NaCl. Five mol m^?3 Mg²⁺ decreased Rb⁺ uptake in stl2; however, additional Mg²⁺ up to 40 mol m^?3 did not affect Rb⁺ uptake further. Ca²⁺ supplementation resulted in a very minor decrease of Rb⁺ uptake that was similar in the two genotypes. Tetraethylammonium chloride and CsCl gave similar inhibition of Rb⁺ uptake in both genotypes, but NH₄Cl gave substantially greater inhibition in the wild type than in stl2. NH₄Cl resulted in a greater membrane depolarization in the wild type and the capacity for subsequent depolarization by KCl was markedly reduced. stl2 exhibited a higher Independent loss of Rb⁺ than the wild type, but, in the absence of external K⁺, loss of Rb⁺ was equivalent in the two genotypes. Since constitutive K⁺ contents are nearly identical, we conclude that high K⁺ influx and loss exact a metabolic cost that is reflected in the inhibition of gametophytic growth. Growth inhibition can be alleviated by reduced supplemental K⁺ or by treatments that slightly reduce K⁺ influx, such as moderate concentrations of Na⁺ or Mg²⁺. We propose that high throughput of K⁺ allows maintenance of cytosolic K⁺ under salt stress and that a high uptake rate for K⁺ results in a reduced capacity for the entrance and accumulation of alternative cations such as Na⁺ in the cytosol.