Effect of SO32- on the activity of ribulose bisphosphate carboxylase from seedlings of Pinus silvestris

Abstract The effect of sulphite on ribulose bisphosphate carboxylase, extracted from needles of Pinus silvestris L., was studied in vitro at pH 8.15 and 25°C. 1 mM and higher concentrations of SO₃^2- inhibited the enzyme. The enzyme was activated either in the assay medium (2.5 – 20 mM HCO_3, 20 mM MgCl₂) or in 10 or 20 mM HCO₃^- and 20–25 mM MgCl₂. Linear reciprocal plots of the activity versus the substrate concentration were obtained, when the HCO₃^- concentration during activation was 4 mM or higher. When the enzyme was activated at high HCO₃^- and Mg²⁺ concentrations, the K_m(CO₂) was c. 27 μM. With respect to HCO₃^-. SO₃^2- inhibited the enzyme in a non-competitive fashion. The inhibition was similar, whether SO₃^2- was present during activation or not. Apparently. SO₃^2- did not interfere with the binding of CO₂ and Mg²⁺ at the activating site. The K₁ was 11–13 mM SO₃^2-. With respect to ribulose bisphosphate the inhibition was also noncompetitive. Similar results with respect to HCO₃^- were obtained for spinach, Spinacia oleracea L., which is contrary to earlier reports.     

CO2 and intracellular pH

Abstract The experimental determination of cytoplasmic and vacuolar pH values is discussed. Despite variation in these values evidence indicates that intracellular pH values are normally regulated within narrow limits. The regulatory mechanisms proposed involve the metabolic consumption of OH^& and the active efflux of H ⁺. The evidence for intracellular pH modification in response to CO₂ hydration and the production of HCO^?₃ and H⁺ is examined. Theoretical calculations and experimental data indicate that CO₂ concentrations as high as 5% will lower intracellular pH. Conversely, variation in CO₂ levels around atmospheric concentrations is unlikely to perturb intracellular pH. High CO₂ levels are found in bulky tissues, and flooded root systems. Evidence is presented that the slow diffusion of dissolved CO₂ compared to gaseous CO₂ results in its accumulation. It is proposed that the accumulation of respiratory CO₂ may reduce intracellular pH values when plant tissues, cells or protoplasts are maintained in a liquid culture medium. Finally, the possible role of dark CO₂ fixation and organic acid synthesis in the regulation of intracellular pH is examined.     

Quantification of the rate of CO2 formation in the periplasmic space of microalgae during photosynthesis. A comparison of whole-cell rate constants for CO2 and HCO3– uptake among three species of the green alga Chlorella

As previously described, the absolute rate of photosynthesis due to a limited concentration of dissolved inorganic carbon at alkaline pH, where the rate of CO₂ formation is strictly limited, plotted as a function of chlorophyll (Chl) concentration, will take the form of a rectangular hyperbola combined with a linear rate directly proportional to [Chl], which are, respectively, due to the contribution of CO₂ and HCO₃^– to photosynthesis. This model represents that the mathematical asymptote of absolute rate of photosynthesis versus cell density is described by the whole-cell rate constant for HCO₃^– uptake and the maximum rate of CO₂ formation in the extracellular space. This means that any trace modification of the CO₂ formation rate outside the cell will alter the photosynthetic rate and should be detectable experimentally. In air-grown Chlorella ellipsoidea and C. kessleri and in high CO₂-grown C. saccharophila, the graph of the absolute rate of photosynthesis against [Chl] clearly followed the mathematical model described above and the actual CO₂ formation rates outside the cells were not significantly different from the calculated rates. It also indicated that the whole-cell rate constants for CO₂ and HCO₃^– uptake in air-grown C. ellipsoidea and C. saccharophila were similar at ≈ 300 and 2·0 mm³μg^–1 Chl min^–1, respectively, whereas those in air-grown C. kessleri were ≈ 550 and 15 mm³μg^–1 Chl min^–1. These results indicate that no acidification of the periplasmic space occurs, and there is no trace activity of external carbonic anhydrase in these microalgae.     

Non-phytotoxicity of the aluminum sulfate ion, AlSO+4

Aluminum is a phytotoxic element in many soils and occurs in a variety of chemical species. In order to determine whether AlSO⁺₄ is toxic, seedlings of wheat (Triticum aestivum L. cv. Tyler) and red clover (Trifolium pratense L. cv. Kenland) were transferred to solutions containing controlled activities of Al³⁺, AlSO⁺₄, Na⁺ and Ca²⁺. Root elongation was inhibited by Al³⁺ (or mononuclear hydroxy-Al species that are in equilibrium with Al³⁺), but not by AlSO⁺₄. We assumed a formation constant (K_AlSO⁺₄= {AlSO⁺₄}/[{Al³⁺} {SO^2-₄}]; braces indicate activities} of 10^3.2 for AlSO⁺₄ in the computation of ionic activities, but use of K_AlSO⁺₄ values ranging from 10^2.8 to 10^3.6 had very little effect on the computed toxicities of Al³⁺ and AlSO⁺₄. Sulfate did not promote the formation of polynuclear Al complexes in our experiments. A practice in studies of Al phytotoxicity has been to attribute toxicity to mononuclear Al, but now it would seem advisable to exclude AlSO⁺₄. That AlSO⁺₄ is non-toxic, or is at least 10-fold less toxic than Al³⁺, has implications for the physiology of Al toxicity and for the use of sulfate salts in experimental work and in agriculture.     

Effects of Cations on (Ca2++ Mg2+)-Activated ATPase from Rat Brain

Abstract: With a partially purified, membrane-bound (Ca + Mg)-activated ATPase preparation from rat brain, the K_0.5 for activation by Ca²⁺ was 0.8 p μm in the presence of 3 mm -ATP, 6 mm -MgCl₂, 100 m_M-KCI, and a calcium EGTA buffer system. Optimal ATPase activity under these circumstances was with 6-100 μm -Ca²⁺, but marked inhibition occurred at higher concentrations. Free Mg²⁺ increased ATPase activity, with an estimated K_0.5, in the presence of 100 μm -CaCl₂, of 2.5 mm ; raising the MgCl₂ concentration diminished the inhibition due to millimolar concentrations of CaCl₂, but antagonized activation by submicromolar concentrations of Ca²⁺. Dimethylsulfoxide (10%, v/v) had no effect on the K_0.5 for activation by Ca²⁺, but decreased activation by free Mg²⁺ and increased the inhibition by millimolar CaCl₂. The monovalent cations K⁺, Na⁺, and TI⁺ stimulated ATPase activity; for K⁺ the K_0.5 was 8 mm , which was increased to 15 mm in the presence of dimethylsulfoxide. KCI did not affect the apparent affinity for Ca²⁺ as either activator or inhibitor. The preparation can be phosphorylated at 0°C by [γ-³²P]-ATP; on subsequent addition of a large excess of unlabeled ATP the calcium dependent level of phosphorylation declined, with a first-order rate constant of 0.12 s^?1. Adding 10 mm -KCI with the unlabeled ATP increased the rate constant to 0.20 s^?1, whereas adding 10 mm -NaCl did not affect it measurably. On the other hand, adding dimethyl-sulfoxide slowed the rate of loss, the constant decreasing to 0.06 s^?1. Orthovanadate was a potent inhibitor of this enzyme, and inhibition with 1 μm -vanadate was increased by both KCI and dimethylsulfoxide. Properties of the enzyme are thus reminiscent of the plasma membrane (Na + K)-ATPase and the sarcoplasmic reticulum (Ca + Mg)-ATPase, most notably in the K⁺ stimulation of both dephosphorylation and inhibition by vanadate.     

Role of Na+-Ca2+ Exchanger in Agonist-Induced Ca2+ Signaling in Cultured Rat Astrocytes

Abstract: We have previously demonstrated that activation of the Na⁺-Ca²⁺ exchanger in the reverse mode causes Ca²⁺ influx in astrocytes. In addition, we showed that the exchange activity was stimulated by nitric oxide (NO)/cyclic GMP and inhibited by ascorbic acid. The present study demonstrates that the Na⁺-Ca²⁺ exchanger is involved in agonist-induced Ca²⁺ signaling in cultured rat astrocytes. The astrocytic intracellular Ca²⁺ concentration ([Ca²⁺]_i) was increased by l -glutamate, noradrenaline (NA), and ATP, and the increases were all attenuated by the NO generator sodium nitroprusside (SNP). SNP also reduced the ionomycin-induced increase in [Ca²⁺]_i. The Na-induced Ca²⁺ signal was also attenuated by S-nitroso-l -cysteine and 8-bromo cyclic GMP, whereas it was enhanced by 3,4-dichlorobenzamil, an inhibitor of the Na⁺-Ca²⁺ exchanger. Treatment of astrocytes with antisense, but not sense, deoxynucleotides to the sequence encoding the Na⁺-Ca²⁺ exchanger enhanced the ionomycin-induced increase in [Ca²⁺]_i and blocked the effects of SNP and 8-bromo cyclic GMP in reducing the NA-induced Ca²⁺ signal. Furthermore, the ionomycin-induced Ca²⁺ signal was enhanced by removal of extracellular Na⁺ and pretreatment with ascorbic acid. These findings indicate that the Na⁺-Ca²⁺ exchanger is a target for NO modulation of elevated [Ca²⁺]_i and that the exchanger plays a role in Ca²⁺ efflux when [Ca²⁺]_i is raised above basal levels in astrocytes.     

Carbonate ions appear to neither inhibit nor stimulate use of bicarbonate ions in photosynthesis by Ulva lactuca

Rates of photosynthesis by the marine macroalga Ulva lactuca were measured in a factorial experiment at five concentrations of HCO₃^? and CO₃^2- between 0·20 and 1·26 mol m^?3, but very low concentrations of CO₂. The results demonstrated that HCO₃^? was available for use, but an analysis of variance showed that CO₃^2- had neither an inhibiting nor a stimulating effect on rates of photosynthesis over this concentration range. Over the experiment, pH varied from 8·46 to 10·06 and this also had no significant effect on rates of photosynthesis. The lack of a stimulatory effect of high concentrations of CO₃^2- on the rate of photosynthesis at low concentrations of HCO₃^? was taken as circumstantial evidence for direct uptake of HCO₃^? rather than proton extrusion and external production of CO₂. In the rockpools in which U. lactuca grows, pH values up to 10·35 have been recorded, and for much of the time, CO₃^2- was the major form of inorganic carbon available. The apparent lack of an ability to use CO₃^2- under these conditions suggests that direct use of CO₃^2- as a source of inorganic carbon for photosynthesis is unlikely to be widespread.     

Effects of Monovalent and Divalent Cations on Ca2+ Fluxes Across Chromaffin Secretory Membrane Vesicles

Abstract: Bovine chromaffin secretory vesicle ghosts loaded with Na⁺ were found to take up Ca²⁺ when incubated in K⁺ media or in sucrose media containing micromolar concentrations of free Ca²⁺. Li⁺- or choline⁺loaded ghosts did not take up Ca²⁺. The Ca²⁺ accumulated by Na⁺-loaded ghosts could be released by the Ca²⁺ ionophore A23187, but not by EGTA. Ca²⁺ uptake was inhibited by external Sr²⁺, Na ⁺, Li ⁺, or choline ⁺. All the ⁴⁵Ca²⁺ accumulated by Na⁺-dependent Ca²⁺ uptake could be released by external Na ⁺, indicating that both Ca²⁺ influx and efflux occur in a Na⁺-dependent manner. Na ⁺ -dependent Ca²⁺ uptake and release were only slightly inhibited by Mg²⁺. In the presence of the Na⁺ ionophore Monensin the Ca²⁺ uptake by Na ⁺-loaded ghosts was reduced. Ca²⁺ sequestered by the Na⁺-dependent mechanism could also be released by external Ca²⁺ or Sr²⁺ but not by Mg²⁺, indicating the presence of a Ca²⁺/Ca²⁺ exchange activity in secretory membrane vesicles. This Ca²⁺/Ca²⁺ exchange system is inhibited by Mg²⁺, but not by Sr²⁺. The Na ⁺ -dependent Ca²⁺ uptake system in the presence of Mg²⁺ is a saturable process with an apparent K_m of 0.28 μM and a V_max= 14.5 nmol min^?1 mg protein^?1. Ruthenium red inhibited neither the Na⁺/Ca²⁺ nor the Ca²⁺/Ca²⁺ exchange, even at high concentrations.     

Enhanced growth of the red algaPorphyra yezoensis Ueda in high CO2 concentrations

Leafy thalli of the red algaPorphyra yezoensis Ueda, initiated from conchospores released from free-living conchocelis, were cultured using aeration with high CO₂. It was found that the higher the CO₂ concentration, the faster the growth of the thalli. Aeration with elevated CO₂ lowered pH in dark, but raised pH remarkably in light with the thalli, because the photosynthetic conversion of HCO ₃ ^? to OH^? and CO₂ proceeded much faster than the dissociation of hydrated CO₂ releasing H⁺. Photosynthesis of the alga was found to be enhanced in the seawater of elevated dissolved inorganic carbon (DIC, CO₂ + HCO ₃ ^? + CO ₃ ^? ). It is concluded that the increased pH in the light resulted in the increase of DIC in the culture media, thus enhancing photosynthesis and growth. The relevance of the results to removal of atmospheric CO₂ by marine algae is discussed.     

Photosynthetic Uptake of Free CO2, by the Roots of Lobelia dortmanna

Lobelia dortmanna L. is probably unable to utilize HCO₃^?and uses only free CO₂ for photosynthesis as shown by the Winkler method. A ¹⁴C technique was used to show that if CO₂ is added to the water around roots, photosynthesis increases 3–5 times more than when the corresponding amount of CO₂ is added to the water surroundings the leaves. As the CO₂ content in lakes where Lobelia grows is very limited, Lobelia must absorb CO₂ from the sediment, and the carbon dioxide will have to diffuse from the roots up into the leaves through the intercellular system of the plant. In conjunction with Lobelia's CO₂ uptake from the sediment O₂ is liberated. The plant, therefore, acts as an oxygen pump, which oxidizes the sediment down to a depth of 20 cm.     

Space–time configurations of solute input and biological uptake in river systems traversing limestone uplands (Yorkshire Dales,northern England)

Solute concentrations, including major plant nutrients, are surveyed from sampling during 1985–89 in river systems variably influenced by upland Dinantian (Carboniferous) limestone. Concentrations of most ions generally increase downstream, but there are widespread dilution effects after rainy periods for major ions and local depletions of mostly biological origin for major plant nutrients. In the upper reaches, these depletions develop mainly under low flow from the influence of benthic algae and macrophytes; they affect inorganic C as HCO₃ ^- plus dissolved gaseous CO₂ and soluble reactive forms of Si, N and P. Inflow – outflow differences of an upland lake result from biological influence on these constituents and also Ca⁺ and K⁺. Experimental injections of NH₄-N, PO₄-P and K⁺were made to an acid headwater of the River Swale, together with Na⁺ and Cl^- as supposed conservative reference ions. Uptake is insignificant for K⁺ but marked for NH₄-N and PO₄-P; the residual percentage decreases exponentially with time. Relative rates of net uptake per unit time are greater for P than for NH₄-N and larger under conditions of higher flow velocity and benthic algal growth. Although limestone is lacking in some headwater regions, where atmospheric inputs appear to predominate, overall its chemical denudation as Ca²⁺ and HCO₃ ^-provides most of the solute flux downstream, as well as in some karstic headwaters where the highest values are limited by CaCO₃ saturation.     

The effect of Cd2+ on photosynthetic reactions of mesophyll protoplasts

Photosynthetic CO₂-fixation of mesophyll protoplasts of lambs lettuce [Valerianella locusta (L.) Betcke] was inhibited by short time exposure to Cd⁺. Inhibition was due to uptake of the metal ion into the protoplasts and increased with increasing Cd²⁺ concentrations and the time of preincubation. A 10 min pretreatment at 2 mM Cd²⁺ reduced CO₂-fixation by 40–60%. Inhibition of photosynthesis was independent of the light intensity to which the protoplasts were exposed. Measurement of the lightinduced electrochromic pigment absorption change at 518nm and chlorophyll fluorescence studies revealed that primary photochemical reactions associated with the thylakoid membranes were not affected by the metal ion. Also, light activation of the ribulose-1,5-bisphosphate carboxylase (EC 4.1.1.39) was not inhibited by Cd²⁺. Under rate-limiting CO₂ concentrations, inhibition of CO₂-fixation was smaller than at V_max of CO₂ reduction indicating that the carboxylation reaction of the Calvin cycle is not susceptible to Cd²⁺. Cd²⁺ treatment of protoplasts significantly extended the lagphase of CO₂-supported O₂-evolution and partly inhibited light activation of the glyceraldehyde-3-phosphate dehydrogenase (EC 1.2.1.13) and the ribulose-5-phosphate kinase (EC 2.7.1.19). Measurement of relative concentrations of [¹⁴C]-labeled Calvin cycle intermediates showed that Cd²⁺ caused a decrease in the 3-phosphoglycerate/triose phosphate ratio and an increase in the triose phosphate/ribulose-1,5-bisphosphate ratio. It is concluded that in protoplasts Cd²⁺ affects photosynthesis mainly at the level of dark reactions and that the site of inhibition may be localized in the regenerative phase of the Calvin cycle.     

Uptake of CO2 by aquatic vegetation

Abstract Photosynthesis by aquatic plants based on the supply of CO₂ from air-equilibrated solutions may be limited by the low diffusion coefficient of CO₂ in water. For plants in which the transport of CO₂ from the bulk medium is by diffusion, and the initial carboxylation uses RUBISCO, CO₂ supply can be increased by growth in habitats with fast water flow over the surface (reducing unstirred layer thickness), or with heterotrophically-augmented CO₂ levels, including the direct use of sediment CO₂. Many aquatic plants using RUBISCO as their initial carboxylase counter the limitations on CO₂ supply via the operation of biophysical CO₂ concentrating mechanisms which are based on active transport of HCO^?₃, CO₂ or H⁺ at the plasmalemma, and use bulk-phase HCO^?₃ or CO₂ as the C source. A final group of aquatic plants use biochemical CO₂ concentrating mechanisms based on auxiliary carboxylation by PEPc: C₄-like and Crassulacean Acid Metabolism–like processes are involved. These various mechanisms for increasing CO₂ supply to RUBISCO also help to offset the low specific reaction rate of aquatic plant RUBISCOs at low [CO₂] and low [CO₂]: [CO₂]. In addition to overcoming restrictions on CO₂ supply, the various methods of increasing inorganic C availability may also be important in alleviating shortages of nitrogen or photons.     

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.     

Regulation of the induction of bicarbonate uptake by dissolved CO2 in the marine diatom, Phaeodactylum tricornutum

Physiological properties of photosynthesis were determined in the marine diatom, Phaeodactylum tricornutum UTEX640, during acclimation from 5% CO₂ to air and related to H₂CO₃ dissociation kinetics and equilibria in artificial seawater. The concentration of dissolved inorganic carbon at half maximum rate of photosynthesis (K_0·5[DIC]) value in high CO₂‐grown cells was 1009 mmol m ^{? 3} but was reduced three‐fold by the addition of bovine carbonic anhydrase (CA), whereas in air‐grown cells K_0·5[DIC] was 71 mmol m ^{? 3}, irrespective of the presence of CA. The maximum rate of photosynthesis (P_max) values varied between 300 and 500 μ mol O₂ mg Chl ^{? 1} h ^{? 1} regardless of growth pCO₂. Bicarbonate dehydration kinetics in artificial seawater were re‐examined to evaluate the direct HCO₃ ^? uptake as a substrate for photosynthesis. The uncatalysed CO₂ formation rate in artificial seawater of 31·65°/_oo of salinity at pH 8·2 and 25 °C was found to be 0·6 mmol m ^{? 3} min ^{? 1} at 100 mmol m ^{? 3} DIC, which is 53·5 and 7·3 times slower than the rates of photosynthesis exhibited in air‐ and high CO₂‐grown cells, respectively. These data indicate that even high CO₂‐grown cells of P. tricornutum can take up both CO₂ and HCO₃ ^? as substrates for photosynthesis and HCO₃ ^? use improves dramatically when the cells are grown in air. Detailed time courses were obtained of changes in affinity for DIC during the acclimation of high CO₂‐grown cells to air. The development of high‐affinity photosynthesis started after a 2–5 h lag period, followed by a steady increase over the next 15 h. This acclimation time course is the slowest to be described so far. High CO₂‐grown cells were transferred to controlled DIC conditions, at which the concentrations of each DIC species could be defined, and were allowed to acclimate for more than 36 h. The K_0·5[DIC] values in acclimated cells appeared to be correlated only with [CO_2(aq)] in the medium but not to HCO₃ ^? , CO₃^{2 ?} , total [DIC] or the pH of the medium and indicate that the critical signal regulating the affinity of cells for DIC in the marine diatom, P. tricornutum, is [CO_2(aq)] in the medium.     

CO2 uptake and transport in leaf mesophyll cells

Abstract The acquisition of inorganic carbon for photosynthetic assimilation by leaf mesophyll cells and chloroplasts is discussed with particular reference to membrane permeation of CO₂ and HCO^?₃. Experimental evidence indicates that at the apoplast pH normally experienced by leaf mesophyll cells (pH 6–7) CO₂ is the principal species of inorganic carbon taken up. Uptake of HCO^?₃ may also occur under certain circumstances (i.e. pH 8.5), but its contribution to the net flux of inorganic carbon is small and HCO^?₃ uptake does not function as a CO₂-concentrating mechanism. Similarly, CO₂ rather than HCO^?₃ appears to be the species of inorganic carbon which permeates the chloroplast envelope. In contrast to many C₃ aquatic plants and C₄ plants, C₃ terrestrial plants lack specialized mechanisms for the acquisition and transport of inorganic carbon from the intercellular environment to the site of photosynthetic carboxylation, but rely upon the diffusive uptake of CO₂.     

HCO3− and CO2 leakage from Synechococcus UTEX 625

The leakage of various inorganic carbon species from air-grown cells of Synechococcus UTEX 625 was investigated after a light to dark transition or during a light period using a mass spectrometer under a wide variety of experimental conditions. Total inorganic carbon efflux and CO₂ efflux during the initial period of darkness were measured with or without carbonic anhydrase in the reaction medium respectively. The HCO₃^? efflux after a light to dark transition was estimated by difference. Carbon dioxide efflux in the light was measured by inhibiting CO₂ transport with either Na₂S or COS₃ or quenching the ¹³C inorganic carbon transport by the addition of ¹²C inorganic carbon in excess. In cells in which CO₂ fixation was inhibited, when only the HCO₃^? transport system was fully operative, CO₂ effluxed continuously during the light period at a rate equal to about 25% of that in darkness. When only the CO₂ transport system was operative, HCO₃^? effluxed during the light period. The difference between the light and dark efflux rates was consistent with a 0.6 unit decrease in the intracellular pH upon darkening the cells. The permeabilities of the cell for CO₂ (2.94 ± 0.14 ± 10^?8ms^?1; mean ± SE, n=137) and HCO₃^? (1.4–1.7 ± 10^?9 ms^?1) were calculated.     

Characterization of Exchange Inhibitory Peptide Effects on Na+/Ca2+ Exchange in Rat and Human Brain Plasma Membrane Vesicles

Abstract: The inhibitory effects of Na⁺/Ca²⁺ exchange inhibitory peptide (XIP), which corresponds to residues 219–238 of the Na⁺/Ca²⁺ exchange protein from canine heart, were studied in both rat and human brain plasma membrane vesicles. XIP had very high potency with respect to the inhibition of the initial velocity of intravesicular Na⁺-dependent Ca²⁺ uptake in both rat brain [IC₅₀ = 3.05 ± 0.69 µM (mean ± SE)] and human brain (IC₅₀ = 3.58 ± 0.58 µM). The maximal inhibition seen in rat brain vesicles was ～80%, whereas human brain vesicles were inhibited 100%. XIP also inhibited extravesicular Na⁺-dependent Ca²⁺ release, and the inhibitory effect was enhanced by increasing the extravesicular Na⁺ concentration. In contrast, the inhibitory effect of bepridil was competitive with respect to extravesicular Na⁺. When XIP was added at steady state (5 min after the initiation of intravesicular Na⁺-dependent Ca²⁺ uptake), it was found that the intravesicular Ca²⁺ content declined with time. Analysis of unidirectional fluxes for Ca²⁺ at steady state showed that 50 µM XIP inhibited Ca²⁺ influx and efflux ～85 and 70%, respectively. This result suggested that XIP inhibited both Na⁺/Ca²⁺ exchange and Ca²⁺/Ca²⁺ exchange but had no effect on the passive release pathway for Ca²⁺. The results suggest structural homology among cardiac, rat, and human brain exchangers in the XIP binding domain and that the binding of Na⁺ or other monovalent cations, e.g., K⁺, is required for XIP to have its inhibitory effect on Ca²⁺ transport.     

The Occurrence,Sources and Spatial Characteristics of Soil Salt and Assessment of Soil Salinization Risk in Yanqi Basin,Northwest China

In order to evaluate the soil salinization risk of the oases in arid land of northwest China, we chose a typical oasis-the Yanqi basin as the research area. Then, we collected soil samples from the area and made comprehensive assessment for soil salinization risk in this area. The result showed that: (1) In all soil samples, high variation was found for the amount of Ca²⁺ and K⁺, while the other soil salt properties had moderate levels of variation. (2) The land use types and the soil parent material had a significant influence on the amount of salt ions within the soil. (3) Principle component (PC) analysis determined that all the salt ion values, potential of hydrogen (pHs) and ECs fell into four PCs. Among them, PC1 (C1^-, Na⁺, SO₄ ^2-, EC, and pH) and PC2 (Ca²⁺, K⁺, Mg²⁺and total amount of salts) are considered to be mainly influenced by artificial sources, while PC3 and PC4 (CO₃ ^- and HCO₃ ^2-) are mainly influenced by natural sources. (4) From a geo-statistical point of view, it was ascertained that the pH and soil salt ions, such as Ca²⁺, Mg²⁺ and HCO₃ ^-, had a strong spatial dependency. Meanwhile, Na⁺ and Cl^- had only a weak spatial dependency in the soil. (5) Soil salinization indicators suggested that the entire area had a low risk of soil salinization, where the risk was mainly due to anthropogenic activities and climate variation. This study can be considered an early warning of soil salinization and alkalization in the Yanqi basin. It can also provide a reference for environmental protection policies and rational utilization of land resources in the arid region of Xinjiang, northwest China, as well as for other oases of arid regions in the world.