Na-Independent HCO(3) Transport and Accumulation in the Cyanobacterium Synechococcus UTEX 625

The active transport and intracellular accumulation of HCO₃⁻ by air-grown cells of the cyanobacterium Synechococcus UTEX 625 (PCC 6301) was strongly promoted by 25 millimolar Na⁺.Na⁺-dependent HCO₃⁻ accumulation also resulted in a characteristic enhancement in the rate of photosynthetic O₂ evolution and CO₂ fixation. However, when Synechococcus was grown in standing culture, high rates of HCO₃⁻ transport and photosynthesis were observed in the absence of added Na⁺. The internal HCO₃⁻ pool reached levels up to 50 millimolar, and an accumulation ratio as high as 970 was observed. Sodium enhanced HCO₃⁻ transport and accumulation in standing culture cells by about 25 to 30% compared with the five- to eightfold enhancement observed with air-grown cells. The ability of standing culture cells to utilize HCO₃⁻ from the medium in the absence of Na⁺ was lost within 16 hours after transfer to air-grown culture and was reacquired during subsequent growth in standing culture. Studies using a mass spectrometer indicated that standing culture cells were also capable of active CO₂ transport involving a high-affinity transport system which was reversibly inhibited by H₂S, as in the case for air-grown cells. The data are interpreted to indicate that Synechococcus possesses a constitutive CO₂ transport system, whereas Na⁺-dependent and Na⁺-independent HCO₃⁻ transport are inducible, depending upon the conditions of growth. Intracellular accumulation of HCO₃⁻ was always accompanied by a quenching of chlorophyll a fluorescence which was independent of CO₂ fixation. The extent of fluorescence quenching was highly dependent upon the size of the internal pool of HCO₃⁻ + CO₂. The pattern of fluorescence quenching observed in response to added HCO₃⁻ and Na⁺ in air-grown and standing culture cells was highly characteristic for Na⁺-dependent and Na⁺-independent HCO₃⁻ accumulation. It was concluded that measurements of fluorescence quenching provide an indirect means for following HCO₃⁻ transport and the dynamics of intracellular HCO₃⁻ accumulation and dissipation.     

Characterization of the na-requirement in cyanobacterial photosynthesis

The Na⁺ requirement for photosynthesis and its relationship to dissolved inorganic carbon (DIC) concentration and Li⁺ concentration was examined in air-grown cells of the cyanobacterium Synechococcus leopoliensis UTEX 625 at pH 8. Analysis of the rate of photosynthesis (O₂ evolution) as a function of Na⁺ concentration, at fixed DIC concentration, revealed two distinct regions to the response curve, for which half-saturation values for Na⁺ (K_½[Na⁺]) were calculated. The value of both the low and the high K_½(Na⁺) was dependent upon extracellular DIC concentration. The low K_½(Na⁺) decreased from 1000 micromolar at 5 micromolar DIC to 200 micromolar at 140 micromolar DIC whereas over the same DIC concentration range the high K_½(Na⁺) decreased from 10 millimolar to 1 millimolar. The most significant increases in photosynthesis occurred in the 1 to 20 millimolar range. A fraction of total photosynthesis, however, was independent of added Na⁺ and this fraction increased with increased DIC concentration. A number of factors were identified as contributing to the complexity of interaction between Na⁺ and DIC concentration in the photosynthesis of Synechococcus. First, as revealed by transport studies and mass spectrometry, both CO₂ and HCO₃⁻ transport contributed to the intracellular supply of DIC and hence to photosynthesis. Second, both the CO₂ and HCO₃⁻ transport systems required Na⁺, directly or indirectly, for full activity. However, micromolar levels of Na⁺ were required for CO₂ transport while millimolar levels were required for HCO₃⁻ transport. These levels corresponded to those found for the low and high K_½(Na⁺) for photosynthesis. Third, the contribution of each transport system to intracellular DIC was dependent on extracellular DIC concentration, where the contribution from CO₂ transport increased with increased DIC concentration relative to HCO₃⁻ transport. This change was reflected in a decrease in the Na⁺ concentration required for maximum photosynthesis, in accord with the lower Na⁺-requirement for CO₂ transport. Lithium competitively inhibited Na⁺-stimulated photosynthesis by blocking the cells' ability to form an intracellular DIC pool through Na⁺-dependent HCO₃⁻ transport. Lithium had little effect on CO₂ transport and only a small effect on the size of the pool it generated. Thus, CO₂ transport did not require a functional HCO₃⁻ transport system for full activity. Based on these observations and the differential requirement for Na⁺ in the CO₂ and HCO₃⁻ transport system, it was proposed that CO₂ and HCO₃⁻ were transported across the membrane by different transport systems.     

Na-Stimulation of Photosynthesis in the Cyanobacterium Synechococcus UTEX 625 Grown on High Levels of Inorganic Carbon

Photosynthesis of washed cells of Synechococcus UTEX 625 grown on 5% CO₂ was markedly stimulated (647 ± 50%) at pH 8.0 by the addition of low concentrations of NaCl (concentration required for half-maximal response, K_½, = 18 micromolar). Studies with KCl and Na₂SO₄ showed that the stimulation was due to Na⁺. Photosynthesis at pH 6.1 was only slightly stimulated by Na⁺. The response of photosynthesis at pH 8.0 to [Na⁺] was strongly sigmoidal for dissolved inorganic carbon ([DIC] ≤ 500 micromolar). Cells grown with high total [DIC], but air-levels of CO₂, at pH 9.6 showed the same response to low [Na⁺]. The absence of Na⁺ could be partially, but not completely overcome, by higher [DIC]. Various methods for examining CO₂ or HCO₃⁻ use (K_½^CO₂ determination; isotopic disequilibrium; and consideration of HCO₃⁻ dehydration rate) were consistent with CO₂ use by the cells, but HCO₃⁻ use could not be ruled out. Isotopic disequilibrium studies showed that CO₂ use was stimulated by Na⁺. Cells grown on 5% CO₂ accumulated DIC against a concentration gradient by a process (or processes) dependent on Na⁺. No evidence for uptake of Na⁺ concomitant with DIC uptake could be found. The lack of O₂ evolution during the initial and most rapid period of DIC accumulation suggested that the required energy was obtained from cyclic photophosphorylation.     

Simultaneous Transport of CO(2) and HCO(3) by the Cyanobacterium Synechococcus UTEX 625

A mass spectrometer was used to simultaneously follow the time course of photosynthetic O₂ evolution and CO₂ depletion of the medium by cells of the cyanobacterium Synechococcus leopoliensis UTEX 625. Analysis of the data indicated that both CO₂ and HCO₃⁻ were simultaneously and continuously transported by the cells as a source of substrate for photosynthesis. Initiation of HCO₃⁻ transport by Na⁺ addition had no effect on ongoing CO₂ transport. This result is interpreted to indicate that the CO₂ and HCO₃⁻ transport systems are separate and distinctly different transport systems. Measurement of CO₂-dependent photosynthesis indicated that CO₂ uptake involved active transport and that diffusion played only a minor role in CO₂ acquisition in cyanobacteria.     

Inorganic Carbon Uptake by Chlamydomonas reinhardtii

The rates of CO₂-dependent O₂ evolution by Chlamydomonas reinhardtii, grown with either air levels of CO₂ or air with 5% CO₂, were measured at varying external pH. Over a pH range of 4.5 to 8.5, the external concentration of CO₂ required for half-maximal rates of photosynthesis was constant, averaging 25 micromolar for cells grown with 5% CO₂. This is consistent with the hypothesis that these cells take up CO₂ but not HCO₃⁻ from the medium and that their CO₂ requirement for photosynthesis reflects the K_m(CO₂) of ribulose bisphosphate carboxylase. Over a pH range of 4.5 to 9.5, cells grown with air required an external CO₂ concentration of only 0.4 to 3 micromolar for half-maximal rates of photosynthesis, consistent with a mechanism to accumulate external inorganic carbon in these cells. Air-grown cells can utilize external inorganic carbon efficiently even at pH 4.5 where the HCO₃⁻ concentration is very low (40 nanomolar). However, at high external pH, where HCO₃⁻ predominates, these cells cannot accumulate inorganic carbon as efficiently and require higher concentrations of NaHCO₃ to maintain their photosynthetic activity. These results imply that, at the plasma membrane, CO₂ is the permeant inorganic carbon species in air-grown cells as well as in cells grown on 5% CO₂. If active HCO₃⁻ accumulation is a step in CO₂ concentration by air-grown Chlamydomonas, it probably takes place in internal compartments of the cell and not at the plasmalemma.     

Photosynthesis and Inorganic Carbon Usage by the Marine Cyanobacterium, Synechococcus sp

The marine cyanobacterium, Synechococcus sp. Nägeli (strain RRIMP N1) changes its affinity for external inorganic carbon used in photosynthesis, depending on the concentration of CO₂ provided during growth. The high affinity for CO₂ + HCO₃⁻ of air-grown cells (K_½ < 80 nanomoles [pH 8.2]) would seem to be the result of the presence of an inducible mechanism which concentrates inorganic carbon (and thus CO₂) within the cells. Silicone-oil centrifugation experiments indicate that the inorganic carbon concentration inside suitably induced cells may be in excess of 1,000-fold greater than that in the surrounding medium, and that this accumulation is dependent upon light energy. The quantum requirements for O₂ evolution appear to be some 2-fold greater for low CO₂-grown cells, compared with high CO₂-grown cells. This presumably is due to the diversion of greater amounts of light energy into inorganic carbon transport in these cells.

A number of experimental approaches to the question of whether CO₂ or HCO₃⁻ is primarily utilized by the inorganic carbon transport system in these cells show that in fact both species are capable of acting as substrate. CO₂, however, is more readily taken up when provided at an equivalent concentration to HCO₃⁻. This discovery suggests that the mechanistic basis for the inorganic carbon concentrating system may not be a simple HCO₃⁻ pump as has been suggested. It is clear, however, that during steady-state photosynthesis in seawater equilibrated with air, HCO₃⁻ uptake into the cell is the primary source of internal inorganic carbon.

     

Photosynthetic Adaptation by Synechococcus leopoliensis in Response to Exogenous Dissolved Inorganic Carbon

Synechococcus leopoliensis was grown over a wide range of dissolved inorganic carbon (DIC) concentrations (4-25,000 micromolar) which were obtained by varying culture pH (6.2-9.6) and the CO₂ concentration of the gas stream (36-50,000 microliters per liter). The [DIC] required to half-saturate photosynthesis (K_½^DIC) was found to vary depending upon the ambient DIC concentration at which the cells were grown. Low [DIC] grown cells exhibited low values of K_½^DIC (4.7 micromolar) whereas cells grown at high [DIC] exhibited high values of K_½^DIC (1-2.5 millimolar). Intermediate concentrations of DIC produced intermediate values. Changes in K_½^DIC appeared to be solely a function of [DIC] and were independent of both culture pH and CO₂ concentration. As changes in K_½^DIC occur in response to DIC concentrations commonly found in natural systems we suggest this adaptation may be of ecological significance.     

Effect of Photon Fluence Rate on Oxygen Evolution and Uptake by Chlamydomonas reinhardtii Suspensions Grown in Ambient and CO(2)-Enriched Air

A closed system consisting of an assimilation chamber furnished with a membrane inlet from the liquid phase connected to a mass spectrometer was used to measure O₂ evolution and uptake by Chlamydomonas reinhardtii cells grown in ambient (0.034% CO₂) or CO₂-enriched (5% CO₂) air. At pH = 6.9, 28°C and concentrations of dissolved inorganic carbon (DIC) saturating for photosynthesis, O₂ uptake in the light (U_o) equaled O₂ production (E_o) at the light compensation point (15 micromoles photons per square meter per second). E_o and U_o increased with increasing photon fluence rate (PFR) but were not rate saturated at 600 micromoles photons per square meter per second, while net O₂ exchange reached a saturation level near 500 micromoles photons per square meter per second which was nearly the same for both, CO₂-grown and air-grown cells. Comparison of the U_o/E_o ratios between air-grown and CO₂-grown C. reinhardtii showed higher values for air-grown cells at light intensities higher than light compensation. For both, air-grown and CO₂-grown algae the rates of mitochondrial O₂ uptake in the dark measured immediately before and 5 minutes after illumination were much lower than U_o at PFR saturating for net photosynthesis. We conclude that noncyclic electron flow from water to NADP⁺ and pseudocyclic electron flow via photosystem I to O₂ both significantly contribute to O₂ exchange in the light. In contrast, mitochondrial respiration and photosynthetic carbon oxidation cycle are regarded as minor O₂ consuming reactions in the light in both, air-grown and CO₂-grown cells. It is suggested that the “extra” O₂ uptake by air-grown algae provides ATP required for the energy dependent CO₂/HCO₃⁻ concentrating mechanism known to be present in these cells.     

Active Transport of CO(2) by the Cyanobacterium Synechococcus UTEX 625 : Measurement by Mass Spectrometry

Mass spectrometry has been used to confirm the presence of an active transport system for CO₂ in Synechococcus UTEX 625. Cells were incubated at pH 8.0 in 100 micromolar KHCO₃ in the absence of Na⁺ (to prevent HCO₃⁻ transport). Upon illumination the cells rapidly removed almost all the free CO₂ from the medium. Addition of carbonic anhydrase revealed that the CO₂ depletion resulted from a selective uptake of CO₂, rather than a total uptake of all inorganic carbon species. CO₂ transport stopped rapidly (<3 seconds) when the light was turned off. Iodoacetamide (3.3 millimolar) completely inhibited CO₂ fixation but had little effect on CO₂ transport. In iodoacetamide poisoned cells, transport of CO₂ occurred against a concentration gradient of about 18,000 to 1. Transport of CO₂ was completely inhibited by 10 micromolar diethylstilbestrol, a membrane-bound ATPase inhibitor. Studies with DCMU and PSI light indicated that CO₂ transport was driven by ATP produced by cyclic or pseudocyclic photophosphorylation. Low concentrations of Na⁺ (<100 microequivalents per liter), but not of K⁺, stimulated CO₂ transport as much as 2.4-fold. Unlike Na⁺-dependent HCO₃⁻ transport, the transport of CO₂ was not inhibited by high concentrations (30 milliequivalents per liter) of Li⁺. During illumination, the CO₂ concentration in the medium remained far below its equilibrium value for periods up to 15 minutes. This could only happen if CO₂ transport was continuously occurring at a rapid rate, since the continuing dehydration of HCO₃⁻ to CO₂ would rapidly raise the CO₂ concentration to its equilibrium value if transport ceased. Measurement of the rate of dissolved inorganic carbon accumulation under these conditions indicated that at least part of the continuing CO₂ transport was balanced by HCO₃⁻ efflux.     

High Affinity Transport of CO(2) in the Cyanobacterium Synechococcus UTEX 625

The active transport of CO₂ in Synechococcus UTEX 625 was measured by mass spectrometry under conditions that preclude HCO₃⁻ transport. The substrate concentration required to give one half the maximum rate for whole cell CO₂ transport was determined to be 0.4 ± 0.2 micromolar (mean ± standard deviation; n = 7) with a range between 0.2 and 0.66 micromolar. The maximum rates of CO₂ transport ranged between 400 and 735 micromoles per milligram of chlorophyll per hour with an average rate of 522 for seven experiments. This rate of transport was about three times greater than the dissolved inorganic carbon saturated rate of photosynthetic O₂ evolution observed under these conditions. The initial rate of chlorophyll a fluorescence quenching was highly correlated with the initial rate of CO₂ transport (correlation coefficient = 0.98) and could be used as an indirect method to detect CO₂ transport and calculate the substrate concentration required to give one half the maximum rate of transport. Little, if any, inhibition of CO₂ transport was caused by HCO₃⁻ or by Na⁺-dependent HCO₃⁻ transport. However, ¹²CO₂ readily interfered with ¹³CO₂ transport. CO₂ transport and Na⁺-dependent HCO₃⁻ transport are separate, independent processes and the high affinity CO₂ transporter is not only responsible for the initial transport of CO₂ into the cell but also for scavenging any CO₂ that may leak from the cell during ongoing photosynthesis.     

Energy Sources for HCO3? and CO2 Transport in Air-Grown Cells of Synechococcus UTEX 625

Light-dependent inorganic C (C_i) transport and accumulation in air-grown cells of Synechococcus UTEX 625 were examined with a mass spectrometer in the presence of inhibitors or artificial electron acceptors of photosynthesis in an attempt to drive CO₂ or HCO₃⁻ uptake separately by the cyclic or linear electron transport chains. In the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea, the cells were able to accumulate an intracellular C_i pool of 20 mm, even though CO₂ fixation was completely inhibited, indicating that cyclic electron flow was involved in the C_i-concentrating mechanism. When 200 μm N,N-dimethyl-p-nitrosoaniline was used to drain electrons from ferredoxin, a similar C_i accumulation was observed, suggesting that linear electron flow could support the transport of C_i. When carbonic anhydrase was not present, initial CO₂ uptake was greatly reduced and the extracellular [CO₂] eventually increased to a level higher than equilibrium, strongly suggesting that CO₂ transport was inhibited and that C_i accumulation was the result of active HCO₃⁻ transport. With 3-(3,4-dichlorophenyl)-1,1-dimethylurea-treated cells, C_i transport and accumulation were inhibited by inhibitors of CO₂ transport, such as COS and Na₂S, whereas Li⁺, an HCO₃⁻-transport inhibitor, had little effect. In the presence of N,N-dimethyl-p-nitrosoaniline, C_i transport and accumulation were not inhibited by COS and Na₂S but were inhibited by Li⁺. These results suggest that CO₂ transport is supported by cyclic electron transport and that HCO₃⁻ transport is supported by linear electron transport.     

Selective and Reversible Inhibition of Active CO(2) Transport by Hydrogen Sulfide in a Cyanobacterium

The active transport of CO₂ in the cyanobacterium Synechococcus UTEX 625 was inhibited by H₂S. Treatment of the cells with up to 150 micromolar H₂S + HS⁻ at pH 8.0 had little effect on Na⁺-dependent HCO₃⁻ transport or photosynthetic O₂ evolution, but CO₂ transport was inhibited by more than 90%. CO₂ transport was restored when H₂S was removed by flushing with N₂. At constant total H₂S + HS⁻ concentrations, inhibition of CO₂ transport increased as the ratio of H₂S to HS⁻ increased, suggesting a direct role for H₂S in the inhibitory process. Hydrogen sulfide does not appear to serve as a substrate for transport. In the presence of H₂S and Na⁺ -dependent HCO₃⁻ transport, the extracellular CO₂ concentration rose considerably above its equilibrium level, but was maintained far below its equilibrium level in the absence of H₂S. The inhibition of CO₂ transport, therefore, revealed an ongoing leakage from the cells of CO₂ which was derived from the intracellular dehydration of HCO₃⁻ which itself had been recently transported into the cells. Normally, leaked CO₂ is efficiently transported back into the cell by the CO₂ transport system, thus maintaining the extracellular CO₂ concentration near zero. It is suggested that CO₂ transport not only serves as a primary means of inorganic carbon acquisition for photosynthesis but also serves as a means of recovering CO₂ lost from the cell. A schematic model describing the relationship between the CO₂ and HCO₃⁻ transport systems is presented.     

The Role of External Carbonic Anhydrase in Inorganic Carbon Acquisition by Chlamydomonas reinhardii at Alkaline pH

The role of external carbonic anhydrase in inorganic carbon acquisition and photosynthesis by Chlamydomonas reinhardii at alkaline pH (8.0) was studied. Acetazolamide (50 micromolar) completely inhibited external carbonic anhydrase (CA) activity as determined from isotopic disequilibrium experiments. Under these conditions, photosynthetic rates at low dissolved inorganic carbon (DIC) were far greater than could be maintained by CO₂ supplied from the spontaneous dehydration of HCO₃⁻ thereby showing that C. reinhardii has the ability to utilize exogenous HCO₃⁻. Acetazolamide increased the concentration of DIC required to half-saturate photosynthesis from 38 to 80 micromolar, while it did not affect the maximum photosynthetic rate. External CA activity was also removed from the cell-wall-less mutant (CW-15) by washing. This had no effect on the photosynthetic kinetics of the algae while the addition of acetazolamide to washed cells (CW-15) increased the K_½^DIC from 38 to 80 micromolar. Acetazolamide also caused a buildup of the inorganic carbon pool upon NaHCO₃ addition, indicating that this compound partially inhibited internal CA activity. The effects of acetazolamide on the photosynthetic kinetics of C. reinhardii are likely due to the inhibition of internal rather than a consequence of the inhibition of external CA. Further analysis of the isotopic disequilibrium experiments at saturating concentration of DIC provided evidence consistent with active CO₂ transport by C. reinhardii. The observation that C. reinhardii has the ability to take up both CO₂ and bicarbonate throws into question the role of external CA in the accumulation of DIC in this alga.     

Use of Carbon Oxysulfide, a Structural Analog of CO(2), to Study Active CO(2) Transport in the Cyanobacterium Synechococcus UTEX 625

Carbon oxysulfide (carbonyl sulfide, COS) is a close structural analog of CO₂. Although hydrolysis of COS (to CO₂ and H₂S) does occur at alkaline pH (>9), at pH 8.0 the rate of hydrolysis is slow enough to allow investigation of COS as a possible substrate and inhibitor of the active CO₂ transport system of Synechococcus UTEX 625. A light-dependent uptake of COS was observed that was inhibited by CO₂ and the ATPase inhibitor diethylstilbestrol. The COS taken up by the cells could not be recovered when the lights were turned off or when acid was added. It was concluded that most of the COS taken up was hydrolyzed by intracellular carbonic anhydrase. The production of H₂S was observed and COS removal from the medium was inhibited by ethoxyzolamide. Bovine erythrocyte carbonic anhydrase catalysed the stoichiometric hydrolysis of COS to H₂S. The active transport of CO₂ was inhibited by COS in an apparently competitive manner. When Na⁺-dependent HCO₃⁻ transport was allowed in the presence of COS, the extracellular [CO₂] rose considerably above the equilibrium level. This CO₂ appearing in the medium was derived from the dehydration of transported HCO₃⁻ and was leaked from the cells. In the presence of COS the return to the cells of this leaked CO₂ was inhibited. These results showed that the Na⁺-dependent HCO₃⁻ transport was not inhibited by COS, whereas active CO₂ transport was inhibited. When COS was removed by gassing with N₂, a normal pattern of CO₂ uptake was observed. The silicone fluid centrifugation method showed that COS (100 micromolar) had little effect upon the initial rate of HCO₃⁻ transport or CO₂ fixation. The steady state rate of CO₂ fixation was, however, inhibited about 50% in the presence of COS. This inhibition can be at least partially explained by the significant leakage of CO₂ from the cells that occurred when CO₂ uptake was inhibited by COS. Neither CS₂ nor N₂O acted like COS. It is concluded that COS is an effective and selective inhibitor of active CO₂ transport.     

Photorespiration and Internal CO(2) Accumulation in Chara corallina as Inferred from the Influence of DIC and O(2) on Photosynthesis

An O₂ electrode system with a specially designed chamber for `whorl' cell complexes of Chara corallina was used to study the combined effects of inorganic carbon and O₂ concentrations on photosynthetic O₂ evolution. At pH = 5.5 and 20% O₂, cells grown in HCO₃⁻ medium (low CO₂, pH ≥ 9.0) exhibited a higher affinity for external CO₂ (K_½(CO₂) = 40 ± 6 micromolar) than the cells grown for at least 24 hours in high-CO₂ medium (pH = 6.5), (K_½(CO₂) = 94 ± 16 micromolar). With O₂ ≤ 2% in contrast, both types of cells showed a high apparent affinity (K_½(CO₂) = 50 − 52 micromolar). A Warburg effect was detectable only in the low affinity cells previously cultivated in high-CO₂ medium (pH = 6.5). The high-pH, HCO₃⁻-grown cells, when exposed to low pH (5.5) conditions, exhibited a response indicating an ability to fix CO₂ which exceeded the CO₂ externally supplied, and the reverse situation has been observed in high-CO₂-grown cells. At pH 8.2, the apparent photosynthetic affinity for external HCO₃⁻ (K_½[HCO₃⁻]) was 0.6 ± 0.2 millimolar, at 20% O₂. But under low O₂ concentrations (≤2%), surprisingly, an inhibition of net O₂ evolution was elicited, which was maximal at low HCO₃⁻ concentrations. These results indicate that: (a) photorespiration occurs in this alga and can be revealed by cultivation in high-CO₂ medium, (b) Chara cells are able to accumulate CO₂ internally by means of a process apparently independent of the plasmalemma HCO₃⁻ transport system, (c) molecular oxygen appears to be required for photosynthetic utilization of exogenous HCO₃⁻: pseudocyclic electron flow, sustained by O₂ photoreduction, may produce the additional ATP needed for the HCO₃⁻ transport.     

Ae4 (Slc4a9) Anion Exchanger Drives Cl? Uptake-dependent Fluid Secretion by Mouse Submandibular Gland Acinar Cells

Transcellular Cl⁻ movement across acinar cells is the rate-limiting step for salivary gland fluid secretion. Basolateral Nkcc1 Na⁺-K⁺-2Cl⁻ cotransporters play a critical role in fluid secretion by promoting the intracellular accumulation of Cl⁻ above its equilibrium potential. However, salivation is only partially abolished in the absence of Nkcc1 cotransporter activity, suggesting that another Cl⁻ uptake pathway concentrates Cl⁻ ions in acinar cells. To identify alternative molecular mechanisms, we studied mice lacking Ae2 and Ae4 Cl⁻/HCO₃⁻ exchangers. We found that salivation stimulated by muscarinic and β-adrenergic receptor agonists was normal in the submandibular glands of Ae2^−/− mice. In contrast, saliva secretion was reduced by 35% in Ae4^−/− mice. The decrease in salivation was not related to loss of Na⁺-K⁺-2Cl⁻ cotransporter or Na⁺/H⁺ exchanger activity in Ae4^−/− mice but correlated with reduced Cl⁻ uptake during β-adrenergic receptor activation of cAMP signaling. Direct measurements of Cl⁻/HCO₃⁻ exchanger activity revealed that HCO₃⁻-dependent Cl⁻ uptake was reduced in the acinar cells of Ae2^−/− and Ae4^−/− mice. Moreover, Cl⁻/HCO₃⁻ exchanger activity was nearly abolished in double Ae4/Ae2 knock-out mice, suggesting that most of the Cl⁻/HCO₃⁻ exchanger activity in submandibular acinar cells depends on Ae2 and Ae4 expression. In conclusion, both Ae2 and Ae4 anion exchangers are functionally expressed in submandibular acinar cells; however, only Ae4 expression appears to be important for cAMP-dependent regulation of fluid secretion.     

Inorganic Carbon Uptake during Photosynthesis : II. Uptake by Isolated Asparagus Mesophyll Cells during Isotopic Disequilibrium

The species of inorganic carbon (CO₂ or HCO₃⁻) taken up a source of substrate for photosynthetic fixation by isolated Asparagus sprengeri mesophyll cells is investigated. Discrimination between CO₂ or HCO₃⁻ transport, during steady state photosynthesis, is achieved by monitoring the changes (by ¹⁴C fixation) which occur in the specific activity of the intracellular pool of inorganic carbon when the inorganic carbon present in the suspending medium is in a state of isotopic disequilibrium. Quantitative comparisons between theoretical (CO₂ or HCO₃⁻ transport) and experimental time-courses of ¹⁴C incorporation, over the pH range of 5.2 to 7.5, indicate that the specific activity of extracellular CO₂, rather than HCO₃⁻, is the appropriate predictor of the intracellular specific activity. It is concluded, therefore, that CO₂ is the major source of exogenous inorganic carbon taken up by Asparagus cells. However, at high pH (8.5), a component of net DIC uptake may be attributable to HCO₃⁻ transport, as the incorporation of ¹⁴C during isotopic disequilibrium exceeds the maximum possible incorporation predicted on the basis of CO₂ uptake alone. The contribution of HCO₃⁻ to net inorganic carbon uptake (pH 8.5) is variable, ranging from 5 to 16%, but is independent of the extracellular HCO₃⁻ concentration. The evidence for direct HCO₃⁻ transport is subject to alternative explanations and must, therefore, be regarded as equivocal. Nonlinear regression analysis of the rate of ¹⁴C incorporation as a function of time indicates the presence of a small extracellular resistance to the diffusion of CO₂, which is partially alleviated by a high extracellular concentration of HCO₃⁻.     

Intracellular pH Regulation in Cultured Astrocytes from Rat Hippocampus : II. Electrogenic Na/HCO3 Cotransport

In the preceding paper (Bevensee, M.O., R.A. Weed, and W.F. Boron. 1997. J. Gen. Physiol. 110: 453–465.), we showed that a Na⁺-driven influx of HCO₃ ⁻ causes the increase in intracellular pH (pH_i) observed when astrocytes cultured from rat hippocampus are exposed to 5% CO₂/17 mM HCO₃ ⁻. In the present study, we used the pH-sensitive fluorescent indicator 2′,7′-biscarboxyethyl-5,6-carboxyfluorescein (BCECF) and the perforated patch-clamp technique to determine whether this transporter is a Na⁺-driven Cl-HCO₃ exchanger, an electrogenic Na/HCO₃ cotransporter, or an electroneutral Na/HCO₃ cotransporter. To determine if the transporter is a Na⁺-driven Cl-HCO₃ exchanger, we depleted the cells of intracellular Cl⁻ by incubating them in a Cl⁻-free solution for an average of ∼11 min. We verified the depletion with the Cl⁻-sensitive dye N-(6-methoxyquinolyl)acetoethyl ester (MQAE). In Cl⁻-depleted cells, the pH_i still increases after one or more exposures to CO₂/HCO₃ ⁻. Furthermore, the pH_i decrease elicited by external Na⁺ removal does not require external Cl⁻. Therefore, the transporter cannot be a Na⁺-driven Cl-HCO₃ exchanger. To determine if the transporter is an electrogenic Na/ HCO₃ cotransporter, we measured pH_i and plasma membrane voltage (V_m) while removing external Na⁺, in the presence/absence of CO₂/HCO₃ ⁻ and in the presence/absence of 400 μM 4,4′-diisothiocyanatostilbene-2,2′-disulphonic acid (DIDS). The CO₂/HCO₃ ⁻ solutions contained 20% CO₂ and 68 mM HCO₃ ⁻, pH 7.3, to maximize the HCO₃ ⁻ flux. In pH_i experiments, removing external Na⁺ in the presence of CO₂/HCO₃ ⁻ elicited an equivalent HCO₃ ⁻ efflux of 281 μM s⁻¹. The HCO₃ ⁻ influx elicited by returning external Na⁺ was inhibited 63% by DIDS, so that the predicted DIDS-sensitive V_m change was 3.3 mV. Indeed, we found that removing external Na⁺ elicited a DIDS-sensitive depolarization that was 2.6 mV larger in the presence than in the absence of CO₂/ HCO₃ ⁻. Thus, the Na/HCO₃ cotransporter is electrogenic. Because a cotransporter with a Na⁺:HCO₃ ⁻ stoichiometry of 1:3 or higher would predict a net HCO₃ ⁻ efflux, rather than the required influx, we conclude that rat hippocampal astrocytes have an electrogenic Na/HCO₃ cotransporter with a stoichiometry of 1:2.     

Na-H Exchanger Isoform-2 (NHE2) Mediates Butyrate-dependent Na+ Absorption in Dextran Sulfate Sodium (DSS)-induced Colitis

Diarrhea associated with ulcerative colitis (UC) occurs primarily as a result of reduced Na⁺ absorption. Although colonic Na⁺ absorption is mediated by both epithelial Na⁺ channels (ENaC) and Na-H exchangers (NHE), inhibition of NHE-mediated Na⁺ absorption is the primary cause of diarrhea in UC. As there are conflicting observations reported on NHE expression in human UC, the present study was initiated to identify whether NHE isoforms (NHE2 and NHE3) expression is altered and how Na⁺ absorption is regulated in DSS-induced inflammation in rat colon, a model that has been used to study UC. Western blot analyses indicate that neither NHE2 nor NHE3 expression is altered in apical membranes of inflamed colon. Na⁺ fluxes measured in vitro under voltage clamp conditions in controls demonstrate that both HCO₃⁻-dependent and butyrate-dependent Na⁺ absorption are inhibited by S3226 (NHE3-inhibitor), but not by HOE694 (NHE2-inhibitor) in normal animals. In contrast, in DSS-induced inflammation, butyrate-, but not HCO₃⁻-dependent Na⁺ absorption is present and is inhibited by HOE694, but not by S3226. These observations indicate that in normal colon NHE3 mediates both HCO₃⁻-dependent and butyrate-dependent Na⁺ absorption, whereas DSS-induced inflammation activates NHE2, which mediates butyrate-dependent (but not HCO₃⁻-dependent) Na⁺ absorption. In in vivo loop studies HCO₃⁻-Ringer and butyrate-Ringer exhibit similar rates of water absorption in normal rats, whereas in DSS-induced inflammation luminal butyrate-Ringer reversed water secretion observed with HCO₃⁻-Ringer to fluid absorption. Lumen butyrate-Ringer incubation activated NHE3-mediated Na⁺ absorption in DSS-induced colitis. These observations suggest that the butyrate activation of NHE2 would be a potential target to control UC-associated diarrhea.     

Is HCO3? Transport in Anabaena a Na+ Symport?

Na⁺ strongly promoted HCO₃⁻ transport in Anabaena variabilis. The effect was highly specific to this cation. Kinetic analysis indicated a progressive decrease in the K_m (HCO₃⁻) of the transport system with increasing Na⁺ concentration. V_max was also affected. We raise the possibility that the transport is a Na⁺-HCO₃⁻ symport; alternatively, that a Na⁺-H⁺ antiport (or Na⁺-OH⁺ symport) system mediates the efflux of the OH⁻ ions derived from the entering HCO₃⁻ ions, and that this antiport can rate-limit HCO₃⁻ influx.