Monensin Inhibition of Na+-Dependent HCO3- Transport Distinguishes It from Na+-Independent HCO3- Transport and Provides Evidence for Na+/HCO3- Symport in the Cyanobacterium Synechococcus UTEX 625

The effect of monensin, an ionophore that mediates Na+/H+ exchange, on the activity of the inorganic carbon transport systems of the cyanobacterium Synechococcus UTEX 625 was investigated using transport assays based on the measurement of chlorophyll a fluorescence emission or 14C uptake. In Synechococcus cells grown in standing culture at about 20 [mu]M CO2 + HCO3-, 50 [mu]M monensin transiently inhibited active CO2 and Na+-independent HCO3- transport, intracellular CO2 and HCO3- accumulation, and photosynthesis in the presence but not in the absence of 25 mM Na+. These activities returned to near-normal levels within 15 min. Transient inhibition was attributed to monensin-mediated intracellular alkalinization, whereas recovery may have been facilitated by cellular mechanisms involved in pH homeostasis or by monensin-mediated H+ uptake with concomitant K+ efflux. In air-grown cells grown at 200 [mu]M CO2 + HCO3- and standing culture cells, Na+-dependent HCO3- transport, intracellular HCO3- accumulation, and photosynthesis were also inhibited by monensin, but there was little recovery in activity over time. However, normal photosynthetic activity could be restored to air-grown cells by the addition of carbonic anhydrase, which increased the rate of CO2 supply to the cells. This observation indicated that of all the processes required to support photosynthesis only Na+-dependent HCO3- transport was significantly inhibited by monensin. Monensin-mediated dissipation of the Na+ chemical gradient between the medium and the cells largely accounted for the decline in the HCO3- accumulation ratio from 751 to 55. The two HCO3- transport systems were further distinguished in that Na+-dependent HCO3- transport was inhibited by Li+, whereas Na+-independent HCO3- transport was not. It is suggested that Na+-dependent HCO3- transport involves an Na+/HCO3- symport mechanism that is energized by the Na+ electrochemical potential.     

Ethoxyzolamide Differentially Inhibits CO2 Uptake and Na+-Independent and Na+-Dependent HCO3- Uptake in the Cyanobacterium Synechococcus sp. UTEX 625

The effects of ethoxyzolamide (EZ), a carbonic anhydrase inhibitor, on the active CO2 and Na+-independent and Na+-dependent HCO3- transport systems of the unicellular cyanobacterium Synechococcus sp. UTEX 625 were examined. Measurements of transport and accumulation using radiochemical, fluorometric, and mass spectrometric assays indicated that active CO2 transport and active Na+-independent HCO3- transport were inhibited by EZ. However, Na+-independent HCO3- transport was about 1 order of magnitude more sensitive to EZ inhibition than was CO2 transport (50% inhibition = 12 [mu]M versus 80 [mu]M). The data suggest that both the active CO2 (G.D. Price, M.R. Badger [1989] Plant Physiol 89: 37-43) and the Na+ -independent HCO3 - transport systems possessed carbonic anhydrase-like activity as part of their mechanism of action. In contrast, Na+-dependent HCO3- transport was only partially (50% inhibition = 230 [mu]M) and noncompetitively inhibited by EZ. The collective evidence suggested that EZ inhibition of Na+ -dependent HCO3- transport was an indirect consequence of the action of EZ on the CO2 transport system, rather than a direct effect on HCO3- transport. A model is presented in which the core of the inorganic carbon translocating system is formed by Na+-dependent HCO3- transport and the CO2 transport system. It is argued that the Na+-independent HCO3 - utilizing system was not directly involved in translocation, but converted HCO3- to CO2 for use in CO2 transport.     

Cation specificity and modes of the Na+:CO3(2-):HCO3- cotransporter in renal basolateral membrane vesicles

The cation specificity and possible exchange modes of the Na+:CO3(2-):HCO3- cotransporter were evaluated by use of basolateral membrane vesicles isolated from rabbit renal cortex. External Li+ inhibited HCO3- gradient-stimulated 22Na uptake, indicating that Li+ interacts with the Na+:CO3(2-):HCO3- cotransporter. No interaction with K+, choline, Rb+, Cs+, or NH4+ could be similarly detected. Imposing an outward Li+ gradient caused quenching of acridine orange fluorescence in the presence but not in the absence of HCO3-, suggesting that Li+:base cotransport takes place via the Na+:CO3(2-):HCO3- cotransporter. Imposing an outward gradient of unlabeled Na+ stimulated the initial rate of 22Na uptake and induced its transient uphill accumulation, indicating Na(+)-Na+ exchange. Na(+)-Na+ exchange was observed in the presence but not in the absence of HCO3- and was inhibited by 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid (DIDS), suggesting that it occurs via the Na+:CO3(2-):HCO3- cotransporter. Similarly, an outward Li+ gradient stimulated uphill 22Na accumulation, indicating Na(+)-Li+ exchange. Na(+)-Li+ exchange was observed in the presence but not in the absence of HCO3-, and was inhibited by DIDS, suggesting that it also occurs via the Na+:CO3(2-):HCO3- cotransporter. Both Na(+)-Na+ and Li(+)-Na+ exchange modes were sensitive to inhibition by harmaline but not by amiloride. We conclude that Li+ is an alternative substrate for the renal Na+:CO3(2-):HCO3- cotransporter. Transport modes of the system include cation:base cotransport and HCO3-dependent cation-cation exchange.     

pH sensitivity of the Na+:HCO3- cotransporter in basolateral membrane vesicles isolated from rabbit kidney cortex.

HCO3- exit across the basolateral membrane of the kidney proximal tubule cell is mediated via an electrogenic Na+:HCO3- cotransporter. We have studied the effect of pH on the activity of this cotransport system in basolateral membrane vesicles isolated from rabbit renal cortex. At constant internal pH 6.0, increasing the external pH and [HCO3-] increased the rate of 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid-sensitive 22Na+ influx into the vesicles. To determine the role of internal pH on the activity of the Na+:HCO3- cotransport system, the influx of 22Na+ via HCO3-dependent Na(+)-Na+ exchange was measured in the absence of an initial pH and [HCO3-] gradient (pH(i) = pH(o), 5% CO2). Increasing the pH from 6.8 to 7.2 increased whereas, increasing the pH from 7.4 to 8.0 decreased the rate of 22Na+ influx via this exchange. Increasing pH at constant [HCO3-] (pH(i) = pH(o) = 8.0, 1.5% CO2 versus pH(i) = pH(o) = 7.2, 10% CO2) reduced the influx of 22Na+ via HCO3-dependent Na(+)-Na+ exchange. Increasing pH at constant [CO3(2-)](pH(i) = pH(o) = 8.0, 1.5% CO2 versus pH(i) = pH(o) = 7.2, 60% CO2) was associated with reduced 22Na+ uptake. Decreasing the pH (pH(i) = pH(o) = 6.3, 60% CO2 versus pH(i) = pH(o) = 7.2, 5% CO2) was associated with a reduced rate of HCO3(-)-dependent Na(+)-Na+ exchange. We conclude that the Na+:HCO3- cotransporter displays a significant pH sensitivity profile with the cotransporter being more functional at pH 7.0-7.4 and less active at more acid or alkaline pH. In addition, the results suggest that the pH sensitivity arises at the inner surface of the basolateral membrane.     

Induction of CO2 and Bicarbonate Transport in the Green Alga Chlorella ellipsoidea (II. Evidence for Induction in Response to External CO2 Concentration)

The critical species and concentrations of dissolved inorganic carbon (DIC) required for the induction of DIC transport during adaptation to low CO2 were determined for the green alga Chlorella ellipsoidea. The concentration of dissolved CO2 needed for the induction of both CO2 and HCO3- transport was independent of pH during adaptation, whereas the total DIC concentration required increased at alkaline pH. At pH 7.5, the minimum equilibrium DIC concentration at which high CO2 characteristics were maintained, i.e. transport was repressed, was 2100 [mu]M, whereas the maximum equilibrium DIC concentration below which DIC transport was fully induced (DICIND) was 500 [mu]M. Intracellular DIC concentration during adaptation to DICIND decreased temporarily after 2 h to 60% of the maximum level but recovered after 3 h of adaptation. After 3 h of adaptation to DICIND, cells exhibited maximum O2 evolution rate at DICIND. When cells partially adapted to DICIND were returned to high CO2, there was an immediate halt to the induction of transport and a gradual decrease in transport capacity over 23 h. The capacity for the induction of transport was unaffected by the absence of light. These results indicate that changes in the internal DIC pool during adaptation to low CO2 do not trigger the induction of DIC transport and that the induction is not light dependent. Induction of DIC transport in C. ellipsoidea appears to occur in response to the continuous exposure of cells to a critical CO2 concentration in the external medium.     

Na(+)-dependent Cl-HCO3 exchange in the squid axon. Dependence on extracellular pH.

Intracellular pH (pHi) in squid giant axons recovers from acid loads by means of a Na(+)-dependent Cl-HCO3 exchanger, the actual mechanism of which might be exchange of: (i) external Na+ and HCO3- for internal Cl- and H+, (ii) Na+ plus two HCO3- for Cl-, (iii) Na+ and CO3= for Cl-, or (iv) the NaCO3- ion pair for Cl-. Here we examine sensitivity of transport to changes of extracellular pH (pHo) in the range 7.1-8.6. We altered pHo in four ways, using: (i) classical "metabolic" disturbances in which we varied [HCO3-]o, [NaCO3-]o, and [CO3=]o at a fixed [CO2]o; (ii) classical "respiratory" disturbances in which we varied [CO2]o, [NaCO3-]o, and [CO3=]o at a fixed [HCO3-]o; (iii) novel mixed-type acid-base disturbances in which we varied [HCO3-]o and [CO2]o at a fixed [CO3=]o and [NaCO3-]o; and (iv) a second series of novel mixed-type disturbances in which we varied [CO2]o, [CO3=]o, and [Na+]o at a fixed [HCO3-]o and [NaCO3-]o. Axons (initial pHi approximately 7.4) were internally dialyzed with a pH 6.5 solution containing 400 mM Cl- but no Na+. After pHi, measured with a glass microelectrode, had fallen to approximately 6.6, dialysis was halted. The equivalent acid extrusion rate (JH) was computed from the rate of pHi recovery (i.e., increase) in the presence of Na+ and HCO3-. When pHo was varied by method (i), which produced the greatest range of [CO3=]o and [NaCO3-]o values, JH increased with pHo in a sigmoidal fashion; the relation was fitted by a pH titration curve with a pK of approximately 7.7 and a Hill coefficient of approximately 3.0. With method (ii), which produced smaller changes in [CO3=]o and [NaCO3-]o, JH also increased with pHo, though less steeply. With method (iii), which involved changes in neither [CO3=]o nor [NaCO3-]o, JH was insensitive to pHo changes. Finally, with method (iv), which involved changes in neither [HCO3-] nor [NaCO3-]o, but reciprocal changes in [CO3=]o and [Na+]o, JH also was insensitive to pHo changes. We found that decreasing pHo from 8.6 to 7.1 caused the apparent Km for external HCO3- ([Na+]o = 425 mM) to increase from 1.0 to 26.7 mM, whereas Jmax was relatively stable. Decreasing pHo from 8.6 to 7.4 caused the apparent Km values for external Na+ ([HCO3-]o = 48 mM) to increase from 8.6 to 81 mM, whereas Jmax was relatively stable.(ABSTRACT TRUNCATED AT 400 WORDS)     

CO2-stimulated NaCl absorption in the mouse renal cortical thick ascending limb of Henle. Evidence for synchronous Na +/H+ and Cl-/HCO3- exchange in apical plasma membranes

These experiments evaluated salt transport processes in isolated cortical thick limbs of Henle (cTALH) obtained from mouse kidney. When the external solutions consisted of Krebs-Ringer bicarbonate (KRB), pH 7.4, and a 95% O2-5% CO2 gas phase, the spontaneous transepithelial voltage (Ve, mV, lumen-to-bath) was approximately mV; the net rate of Cl- absorption (JnetCl) was approximately 3,600 pmols s-1 cm-2; the net rate of osmotic solute absorption Jnetosm was twice JnetCl; and the net rate of total CO2 transport (JnetCO2) was indistinguishable from zero. Thus, net Cl- absorption was accompanied by the net absorption of a monovalent cation, presumably Na+, and net HCO3- absorption was negligible. This salt transport process was stimulated by (CO2 + HCO3- ): omission of CO2 from the gas phase and HCO3- from external solutions reduced JnetCl, Jnetosm, and Ve by 50%. Furthermore, 10(-4) M luminal furosemide abolished JnetCl and Ve entirely. The lipophilic carbonic anhydrase inhibitor ethoxzolamide (10(-4) M, either luminal or peritubular) inhibited (CO2 + HCO3-)-stimulated JnetCl, Jnetosm, and Ve by approximately 50%; however, when the combination (CO2 + HCO3-) was absent, ethoxzolamide had no detectable effect on salt transport. Ve was reduced or abolished entirely by omission of either Na+ or Cl- from external solutions, by peritubular K+ removal, by 10(-3) M peritubular ouabain, and by 10(-4) M luminal SITS. However, Ve was unaffected by 10(-3) M peritubular SITS, or by the hydrophilic carbonic anhydrase inhibitor acetazolamide (2.2 x 10(-4) M, lumen plus bath). We interpret these data to indicate that (CO2 + HCO3-)-stimulated NaCl absorption in the cTALH involved two synchronous apical membrane antiport processes: one exchanging luminal Na+ for cellular H+; and the other exchanging luminal Cl- for cellular HCO3- or OH-, operating in parallel with a (CO2+ HCO3-)-independent apical membrane NaCl cotransport mechanism.     

Na+/HCO3-co-transport in basolateral membrane vesicles isolated from rabbit renal cortex

Recent studies suggest that the major pathway for exit of HCO3- across the basolateral membrane of the proximal tubule cell is electrogenic Na+/HCO3- co-transport. We therefore evaluated the possible presence of Na+/HCO3- co-transport in basolateral membrane vesicles isolated from the rabbit renal cortex. Imposing an inward HCO3- gradient induced the transient uphill accumulation of Na+, and imposing an outward Na+ gradient caused HCO3- -dependent generation of an inside-acid pH gradient as monitored by quenching of acridine orange fluorescence, findings consistent with the presence of Na+/HCO3- co-transport. In the absence of other driving forces, generating an inside-positive membrane potential by imposing an inward K+ gradient in the presence of valinomycin caused net Na+ uptake via a HCO3- -dependent pathway, indicating that Na+/HCO3- co-transport is electrogenic and associated with a flow of negative charge. Imposing transmembrane Cl- gradients did not appreciably affect HCO3- gradient-stimulated Na+ influx, suggesting that Na+/HCO3- co-transport is not Cl- -dependent. The rate of HCO3- gradient-stimulated Na+ influx was a simple, saturable function of the Na+ concentration (Km = 9.7 mM, Vmax = 160 nmol/min/mg of protein), was inhibited by 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid (I50 = 100 microM), but was inhibited less than 10% by up to 1 mM amiloride. We could not demonstrate a HCO3- -dependent or 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid-sensitive component of Na+ influx in microvillus membrane vesicles. This study thus indicates the presence of a transport system mediating electrogenic Na+/HCO3- co-transport in basolateral, but not luminal, membrane vesicles isolated from the rabbit renal cortex. Analogous to the use of renal microvillus membrane vesicles to study Na+/H+ exchange, renal basolateral membrane vesicles may be a useful model system for examining the kinetics and possible regulation of Na+/HCO3- co-transport.     

Active transport of CO(2) and bicarbonate is induced in response to external CO(2) concentration in the green alga Chlorella kessleri

The time-course of induction of CO(2) and HCO(3)- transport has been investigated during the acclimation of high CO(2)-grown Chlorella kessleri cells to dissolved inorganic carbon (DIC)-limited conditions. The rate of photosynthesis of the cells in excess of the uncatalysed supply rate of CO(2) from HCO(3)- was taken as an indicator of HCO(3)- transport, while a stimulation of photosynthesis on the addition of bovine carbonic anhydrase was used as an indicator of CO(2) transport. The maximum rate of photosynthesis (Pmax) was similar for high CO(2)-grown and low CO(2)-grown cells, but the apparent whole cell affinity for DIC and CO(2) of high CO(2)-grown cells was found to be about 30-fold greater than in air-grown cells, which indicates a lower affinity for DIC and CO(2). It was found that HCO(3)- and CO(2) transport were induced in 5.5 h in cells acclimating to air in the light and in the presence and absence of 21% O(2), which indicates that a change in the CO(2)/O(2) ratio in the acclimating medium does not trigger induction of DIC transport. No active DIC transport was detected in high CO(2)-grown cells maintained on high CO(2) for 5.5 h in the presence of 5 mM aminooxyacetate, an aminotransferase inhibitor. These results indicate no involvement of photorespiration in triggering induction. Active DIC transport induction was inhibited in cells treated with 5 microgram ml(-1) cycloheximide, but was unaffected by chloramphenicol treatment, indicating that the induction process requires de novo cytoplasmic protein synthesis. The total DIC concentration eliciting the induction and repression of CO(2) and HCO(3)- transport was higher at pH 7.5 than at pH 6.6. The concentrations of external CO(2) required for the induction and repression of DIC transport were 0 and 120 microM, respectively, and was independent of the pH of the acclimation medium. Prolonged exposure to a critical external CO(2) concentration elicits the induction of DIC transport in C. kessleri.     

Induction of CO2 and Bicarbonate Transport in the Green Alga Chlorella ellipsoidea (I. Time Course of Induction of the Two Systems)

Changes in the physiological properties of the green alga Chlorella ellipsoidea (UTEX 20) were determined during adaptation from high CO2 to air. Cells of C. ellipsoidea, grown in high CO2, had an extremely low affinity for dissolved inorganic carbon (DIC). However, high-affinity DIC transport was induced rapidly after switching to air, which caused a massive decrease in the DIC concentration in the medium. Rates of O2 evolution without added carbonic anhydrase (CA) were compared with calculated rates of uncatalyzed CO2 formation in the medium as a measure of active HCO3-uptake. Cells were found to be able to use HCO3- after 5 h of adaptation and this capacity increased during the next 17 h. The stimulation of O2 evolution upon CA addition was used as a measurement of active CO2 transport: such stimulation occurred 2 h after transfer and increased during the next 5 h. Increases in O2 evolution rates were correlated closely with an increasing capacity to accumulate intracellular pools of acid-labile DIC and with decreases in K1/2(CO2) and CO2-compensation point of the cells. Treatment of cells with cycloheximide (5 [mu]g mL-1) during adaptation completely inhibited DIC transport induction, whereas treatment with chloramphenicol (400 [mu]g mL-1) had no effect, indicating the requirement for cytoplasmic protein synthesis in the induction. These results suggest that both CO2 and HCO3- transport are induced upon transfer of cells from high CO2 to air and that there is a temporal separation between the induction of the two systems.     

Physiological characterization and light response of the CO2-concentrating mechanism in the filamentous cyanobacterium Leptolyngbya sp. CPCC 696

We studied the interactions of the CO(2)-concentrating mechanism and variable light in the filamentous cyanobacterium Leptolyngbya sp. CPCC 696 acclimated to low light (15 μmol m(-2) s(-1) PPFD) and low inorganic carbon (50 μM Ci). Mass spectrometric and polarographic analysis revealed that mediated CO(2) uptake along with both active Na(+)-independent and Na(+)-dependent HCO(3)(-) transport, likely through Na(+)/HCO(3)(-) symport, were employed to concentrate Ci internally. Combined transport of CO(2) and HCO(3)(-) required about 30 kJ mol(-1) of energy from photosynthetic electron transport to support an intracellular Ci accumulation 550-fold greater than the external Ci. Initially, Leptolyngbya rapidly induced oxygen evolution and Ci transport to reach 40-50% of maximum values by 50 μmol m(-2) s(-1) PPFD. Thereafter, photosynthesis and Ci transport increased gradually to saturation around 1,800 μmol m(-2) s(-1) PPFD. Leptolyngbya showed a low intrinsic susceptibility to photoinhibition of oxygen evolution up to PPFD of 3,000 μmol m(-2) s(-1). Intracellular Ci accumulation showed a lag under low light but then peaked at about 500 μmol photons m(-2) s(-1) and remained high thereafter. Ci influx was accompanied by a simultaneous, light-dependent, outward flux of CO(2) and by internal CO(2)/HCO(3)(-) cycling. The high-affinity and high-capacity CCM of Leptolyngbya responded dynamically to fluctuating PPFD and used excitation energy in excess of the needs of CO(2) fixation by increasing Ci transport, accumulation and Ci cycling. This capacity may allow Leptolyngbya to tolerate periodic exposure to excess high light by consuming electron equivalents and keeping PSII open.     

Intracellular pH regulation in cultured embryonic chick heart cells. Na(+)-dependent Cl-/HCO3- exchange

The contribution of Cl-/HCO3- exchange to intracellular pH (pHi) regulation in cultured chick heart cells was evaluated using ion-selective microelectrodes to monitor pHi, Na+ (aiNa), and Cl- (aiCl) activity. In (HCO3- + CO2)-buffered solution steady-state pHi was 7.12. Removing (HCO3- + CO2) buffer caused a SITS (0.1 mM)-sensitive alkalinization and countergradient increase in aiCl along with a transient DIDS-sensitive countergradient decrease in aiNa. SITS had no effect on the rate of pHi recovery from alkalinization. When (HCO3- + CO2) was reintroduced the cells rapidly acidified, aiNa increased, aiCl decreased, and pHi recovered. The decrease in aiCl and the pHi recovery were SITS sensitive. Cells exposed to 10 mM NH4Cl became transiently alkaline concomitant with an increase in aiCl and a decrease in aiNa. The intracellular acidification induced by NH4Cl removal was accompanied by a decrease in aiCl and an increase in aiNa that led to the recovery of pHi. In the presence of (HCO3- + CO2), addition of either amiloride (1 mM) or DIDS (1 mM) partially reduced pHi recovery, whereas application of amiloride plus DIDS completely inhibited the pHi recovery and the decrease in aiCl. Therefore, after an acid load pHi recovery is HCO3o- and Nao- dependent and DIDS sensitive (but not Ca2+o dependent). Furthermore, SITS inhibition of Na(+)-dependent Cl-/HCO3- exchange caused an increase in aiCl and a decrease in the 36Cl efflux rate constant and pHi. In (HCO3- + CO2)-free solution, amiloride completely blocked the pHi recovery from acidification that was induced by removal of NH4Cl. Thus, both Na+/H+ and Na(+)-dependent Cl-/HCO3- exchange are involved in pHi regulation from acidification. When the cells became alkaline upon removal of (HCO3- + CO2), a SITS-sensitive increase in pHi and aiCl was accompanied by a decrease of aiNa, suggesting that the HCO3- efflux, which can attenuate initial alkalinization, is via a Na(+)-dependent Cl-/HCO3- exchange. However, the mechanism involved in pHi regulation from alkalinization is yet to be established. In conclusion, in cultured chick heart cells the Na(+)-dependent Cl-/HCO3- exchange regulates pHi response to acidification and is involved in the steady-state maintenance of pHi.     

Changes in smooth muscle cell pH during hypoxic pulmonary vasoconstriction: a possible role for ion transporters

Hypoxic pulmonary vasoconstriction (HPV) occurs in smooth muscle cells (SMC) from small pulmonary arteries (SPA) and is accompanied by increases in free cytoplasmic calcium ([Ca2+]i) and cytoplasmic pH (pHi). SMC from large pulmonary arteries (LPA) relax during hypoxia, and [Ca2+]i and pHi decrease. Increases in pHi and [Ca2+]i in cat SPA SMC during hypoxia and the augmentation of hypoxic pulmonary vasoconstriction by alkalosis seen in isolated arteries and lungs suggest that cellular mechanisms, which regulate inward and outward movement of Ca2+ and H+, may participate in the generation of HPV. SMC transport systems that regulate pHi include the Na+ - H+ transporter which regulates intracellular Na+ and H+ and aids in recovery from acid loads, and the Na+ -dependent and Na+ -independent Cl-/HCO3- transporters which regulate intracellular chloride. The Na+ -dependent Cl-/HCO3- transporter also aids in recovery from acidosis in the presence of CO2 and HCO3-. The Na+ -independent Cl-/HCO3- transporter aids in recovery from cellular alkalosis. The Na+ - H+ transporter was present in SMC from SPA and LPA of the cat, but it seemed to have little if any role in regulating pHi in the presence of CO2 and HCO3-. Inhibiting the Cl-/HCO3- transporters reversed the normal direction of pHi change during hypoxia, suggesting a role for these transporters in the hypoxic response. Future studies to determine the interaction between pHi, [Ca2+]i and HPV should ascertain whether pHi and [Ca2+]i changes are linked and how they may interact to promote or inhibit SMC contraction.     

Driving Forces for Bicarbonate Transport in the Cyanobacterium Synechococcus R-2 (PCC 7942)

Air-grown Synechococcus R-2 (PCC 7942) cultures grown in BG-11 medium are very alkaline (outside pH is 10.0) and use HCO3- as their inorganic carbon source. The cells showed a dependence on Na+ for photosynthesis, but low Na+ conditions (1 mol m-3) were sufficient to support saturating photosynthesis. The intracellular dissolved inorganic carbon in the light was greater than 20 mol m-3 in both low-Na+ conditions and in BG-11 medium containing the usual [Na+] (24 mol m-3, designated high-Na+ conditions). The electrochemical potential for HCO3- in the light was in excess of 25 kJ mol-1, even in high-Na+ conditions. The Na+-motive force was greater than -12 kJ mol-1 under both Na+ conditions. On thermodynamic grounds, an Na+-driven co-port process would need to have a stoichiometry of 2 or greater ([greater than or equal to]2Na+ in/HCO3-1 in), but we show that Na+ or K+ fluxes cannot be linked to HCO3- transport. Na+ and K+ fluxes were unaffected by the presence or absence of dissolved inorganic carbon. In low-Na+ conditions, Na+ fluxes are too low to support the observed net 14C-carbon fixation rate. Active transport of HCO3- hyperpolarizes (not depolarizes) the membrane potential.     

HCO3- transport in basolateral membrane vesicles isolated from rat renal cortex

The mechanism of HCO3- translocation across the proximal tubule basolateral membrane was investigated by testing for Na+-HCO3- cotransport using isolated membrane vesicles purified from rat renal cortex. As indicated by 22Na+ uptake, imposing an inwardly directed HCO3- concentration gradient induced the transient concentrative accumulation of intravesicular Na+. The stimulation of basolateral membrane vesicle Na+ uptake was specifically HCO3(-)-dependent as only basolateral membrane-independent Na+ uptake was stimulated by an imposed hydroxyl gradient in the absence of HCO3-. No evidence for Na+-HCO3- cotransport was detected in brush border membrane vesicles. Charging the vesicle interior positive stimulated net intravesicular Na+ accumulation in the absence of other driving forces via a HCO3(-)-dependent pathway indicating the flow of negative charge accompanies the Na+-HCO3- cotransport event. Among the anion transport inhibitors tested, 4-4'-diisothiocyanostilbene-2,2'-disulfonic acid demonstrated the strongest inhibitor potency at 1 mM. The Na+-coupled transport inhibitor harmaline also markedly inhibited HCO3- gradient-driven Na+ influx. A role for carbonic anhydrase in the mechanism of Na+-HCO3- cotransport is suggested by the modest inhibition of HCO3- gradient driven Na+ influx caused by acetazolamide. The imposition of Cl- concentration gradients had a marked effect on HCO3- gradient-driven Na+ influx which was furosemide-sensitive and consistent with the operation of a Na+-HCO3- for Cl- exchange mechanism. The results of this study provide evidence for an electrogenic Na+-HCO3- cotransporter in basolateral but not microvillar membrane vesicles isolated from rat kidney cortex. The possible existence of an additional basolateral membrane HCO3(-)-translocating pathway mediating Na+-HCO3- for Cl- exchange is suggested.     

Evidence for K+-dependent HCO3- utilization in the marine diatom Phaeodactylum tricornutum

Photosynthetic utilization of inorganic carbon in the marine diatom Phaeodactylum tricornutum was investigated by the pH drift experiment, measurement of K(1/2) values of dissolved inorganic carbon (DIC) with pH change, and comparison of the rate of photosynthesis with the rate of the theoretical CO(2) formation from uncatalyzed HCO(3)(-) conversion in the medium. The higher pH compensation point (10.3) and insensitivity of the photosynthetic rate to acetazolamide indicate that the alga has good capacity for direct HCO(3)(-) utilization. The photosynthetic rate reached 150 times the theoretical CO(2) supply rate at 100 micromol L(-1) DIC (pH 9.0) in the presence of 10 mmol L(-1) K(+) and 46 times that in the absence of K(+), indicating that for pH 9.4-grown P. tricornutum, HCO(3)(-) in the medium is taken up through K(+)-dependent and -independent HCO(3)(-) transporters. The K(1/2) (CO(2)) values at pH 8.2 were about 4 times higher than those at pH 9.0, whereas the K(1/2) (HCO(3)(-)) values at pH 8.2 were slightly lower than those at pH 9.0 whether without or with K(+), providing further evidence for the presence of the two HCO(3)(-) transport patterns in this alga. Photosynthetic rate and affinity for HCO(3)(-) in the presence of K(+), respectively, were about 2- and 7-fold higher than those in the absence of K(+), indicating that K(+)-dependent HCO(3)(-) transport is a predominant pattern of HCO(3)(-) cellular uptake in low DIC concentration. However, as P. tricornutum was cultured at pH 7.2 or 8.0, photosynthetic affinities to HCO(3)(-) were not affected by K(+), implying that K(+)-dependent HCO(3)(-) transport is induced when P. tricornutum is cultured at high alkaline pH.     

Ionic mechanism of Na+-HCO3- cotransport in rabbit renal basolateral membrane vesicles

The exit of HCO3- across the basolateral membrane of the proximal tubule cell occurs via the electrogenic cotransport of 3 eq of base per Na+. We have used basolateral membrane vesicles isolated from rabbit renal cortex to identify the ionic species transported via this pathway. Media of varying pH and pCO2 were employed to evaluate the independent effects of HCO3- and CO3(2-) on 22Na transport. Na+ uptake was stimulated when [CO3(2-)] was increased at constant [HCO3-], indicating the existence of a transport site for CO3(2-). In the presence of HCO3-, Na+ influx was stimulated more than 3-fold by an inward SO3(2-) gradient. SO3(2-)-stimulated Na+ influx was stilbene-sensitive, confirming that it occurs via the Na+-HCO3- cotransport system. Na+-SO3(2-) cotransport was demonstrated and found to have a 1:1 stoichiometry. Increasing [CO3(2-)] at constant [HCO3-] reduced the stimulation of Na+ influx by SO3(2-), suggesting competition between SO3(2-) and CO3(2-) at a common divalent anion site. Additional divalent anions that were tested, such as SO4(2-), oxalate2-, and HPO4(2-), did not interact at this site. SO3(2-) stimulation of Na+ influx was absolutely HCO3-(-)dependent and was increased as a function of [HCO3-], indicating the presence of a separate HCO3- site. Lastly, we tested whether Na+ interacts via ion pair formation with CO3(2-) or binds to a distinct site. Na+, which has lower affinity than Li+ for ion pair formation with CO3(2-), was found to have greater than 5-fold higher affinity than Li+ for the Na+-HCO3- cotransport system. Moreover, when its inhibition was studied as a function of [Na+], harmaline was found to be a competitive inhibitor of Na+ influx, indicating the existence of a distinct cation site. Our data are compatible with a model in which base transport across the basolateral membrane of the proximal tubule cell takes place via 1:1:1 cotransport of CO3(2-), HCO3-, and Na+ on distinct sites.     

Electrogenic sodium-dependent bicarbonate secretion by glial cells of the leech central nervous system

The ability to move acid/base equivalents across the membrane of identified glial cells was investigated in isolated segmental ganglia of the leech Hirudo medicinalis. The intracellular pH (pHi) of the glial cells was measured with double-barreled, neutral-ligand, ion-sensitive microelectrodes during step changes of the external pH (pHo 7.4-7.0). The rate of intracellular acidification after the decrease in extracellular pH (pHo) was taken as a measure of the rate of acid/base transport across the glial membrane. Taking into account the total intracellular buffering power, the maximum rate of acid/base flux was 0.4 mM/min in CO2/HCO3-free saline, and 3.92 mM/min in the presence of 5% CO2/10 mM HCO-3, suggesting that the acid/base flux was dependent upon HCO3-. The rate of acid influx/base efflux increased both with the external HCO3- concentration and with increasing pHi (and hence HCO3-i). This suggested that the decrease in pHi was due to HCO3- efflux. The rapid decrease of pHi was accompanied by a HCO3--dependent depolarization of the glial membrane from -74 +/- 5 mV (n = 20) to -54 +/- 7 mV (n = 13). Both this depolarization and the rate of intracellular acidification were greatly reduced by the anion exchange inhibitor 4,4-diisothiocyanatostilbene-2,2'-disulfonic acid (DIDS; 0.3-0.5 mM), but were not affected by the removal of external Cl-. Reduction of the external Na+ concentration to one-tenth normal affected the rate of intracellular acidification only in the presence of CO2/HCO3-: the rate increased within the first 3-5 min after lowering external Na+; after longer exposures in low external Na+ the rate decreased, presumably due to depletion of intracellular Na+. Amiloride (1 mM), which inhibits the Na+-H+ exchange in these cells, had no effect on the rate of intracellular acidification. The intracellular Na activity (aNai) of the glial cells was measured to be 5.2 +/- 1.0 mM (n = 8) in CO2/HCO3-free saline; aNai increased to 7.3 +/- 2.2 mM (n = 8) after the addition of 5% CO2/24 mM HCO3-. Upon a change in pHo to 7.0 in the presence of CO2/HCO3-, aNai decreased by an average of 2 +/- 1.1 mM (n = 5); in CO2/HCO3--free saline external acidification produced a transient increase in aNai. It is concluded that, in the presence of CO2/HCO3-, the rate of intracellular acidification in glial cells is dominated by an outwardly directed, electrogenic Na+-HCO3-cotransport. Neurons, which do not possess this cotransporter, acidify at much lower rates under similar conditions.(ABSTRACT TRUNCATED AT 400 WORDS)     

Intracellular pH-regulating mechanism of the squid axon. Relation between the external Na+ and HCO-3 dependences

The intracellular pH-regulating mechanism of the squid axon was examined for its dependence on the concentrations of external Na+ and HCO3-, always at an external pH (pHo) of 8.0. Axons having an initial intracellular pH (pHi) of approximately 7.4 were internally dialyzed with a solution of pH 6.5 that contained 400 mM Cl- and no Na+. After pHi had fallen to approximately 6.6, dialysis was halted, thereby returning control of pHi to the axon. With external Na+ and HCO-3 present, intracellular pH (pHi) increased because of the activity of the pHi-regulating system. The acid extrusion rate (i.e., equivalent efflux of H+, JH) is the product of the pHi recovery rate, intracellular buffering power, and the volume-to-surface ratio. The [HCO3-]o dependence of JH was examined at three fixed levels of [Na+]o: 425, 212, and 106 mM. In all three cases, the apparent Jmax was approximately 19 pmol X cm-2 X s-1. However, the apparent Km (HCO3-) was approximately inversely proportional to [Na+]o, rising from 2.6 to 5.4 to 9.7 mM as [Na+]o was lowered from 425 to 212 to 106 mM, respectively. The [Na+]o dependence of JH was similarly examined at three fixed levels of [HCO3-]o: 12, 6, and 3 mM. The Jmax values did not vary significantly from those in the first series of experiments. The apparent Km (Na+), however, was approximately inversely related to [HCO3-]o, rising from 71 to 174 to 261 mM as [HCO3-]o was lowered from 12 to 6 to 3 mM, respectively. These results agree with the predictions of the ion-pair model of acid extrusion, which has external Na+ and CO3= combining to form the ion pair NaCO3-, which then exchanges for internal Cl-. When the JH data are replotted as a function of [NaCO3-]o, data from all six groups of experiments fall along the same Michaelis-Menten curve, with an apparent Km (NaCO3-) of 80 microM. The ordered and random binding of Na+ and CO3= cannot be ruled out as possible models, but are restricted in allowable combinations of rate constants.     

Polarized distribution of Na+/H+ antiport and Na+/HCO3- cotransport in primary cultures of renal inner medullary collecting duct cells.

Primary cultures of rat renal inner medullary collecting duct cells were grown to confluence on glass coverslips and treated permeant supports, and the pH-sensitive fluorescent probe 2,7-biscarboxyethyl-5,6-carboxyfluorescein was employed to delineate the nature of the transport pathways that allowed for recovery from an imposed acid load in a HCO3-/CO2-buffered solution. The H+ efflux rate of acid-loaded cells was 13.44 +/- 0.94 mM/min. Addition of amiloride, 10(-4) M, to the recovery solution reduced the H+ efflux rate to 4.06 +/- 0.63 mM/min. The amiloride-resistant pHi recovery mechanism displayed an absolute requirement for Na+ but was Cl(-)-independent. Studies performed on permeable supports demonstrated that the latter pathway was located primarily on the basolateral-equivalent (BE) cell surface and was inhibited by 50 microM 4,4'-diisothiocyanostilbene-2,2'-disulfonic acid (DIDS). In a Na(+)-replete solution containing DIDS (50 microM) and amiloride (10(-4) M), acid-loaded cells failed to return to basal pHi. To delineate further the amiloride-inhibitable component of pHi recovery, monolayers were studied in the nominal absence of HCO3-/CO2. In 70% of monolayers studied, Na(+)-dependent, amiloride-inhibitable H+ efflux was the sole mechanism whereby acid-loaded cells returned to basal pHi. A Na(+)-independent pathway was observed in 30% of monolayers examined and represented only a minor component of the pHi recovery process. In studies performed on permeable supports, the Na(+)-dependent amiloride-inhibitable pathway was found to be confined exclusively to the BE cell surface. In summary, confluent monolayers of rat renal inner medullary collecting duct cells in primary culture possess two major mechanisms that contribute toward recovery from an imposed acid load, namely, Na+/H+ antiport and Na+/HCO3- cotransport. Na(+)-independent pHi recovery mechanisms represent a minor component of the pHi recovery process in the cultured cell. Both the Na+/H+ antiporter and Na+/HCO3- cotransporter are located primarily on the BE cell surface.