Carbonic anhydrase inhibitors that directly inhibit anion transport by the human Cl−/HCO3− exchanger,AE1

Carbonic anhydrases (CA, EC 4.2.1.1.) catalyze reversible hydration of CO₂ to HCO₃^?+H⁺. Bicarbonate transport proteins, which catalyze the transmembrane movement of membrane-impermeant bicarbonate, function in cooperation with CA. Since CA and bicarbonate transporters share the substrate, bicarbonate, we examined whether novel competitive inhibitors of CA also have direct inhibitory effects on bicarbonate transporters. We expressed the human erythrocyte membrane Cl^?/HCO₃^? exchanger, AE1, in transfected HEK293 cells as a model bicarbonate transporter. AE1 activity was assessed in both Cl^?/NO₃^? exchange assays, which were independent of CA activity, and in Cl^?/HCO₃^? exchange assays. Transport was measured by following changes of intracellular [Cl^?] and pH, using the intracellular fluorescent reporter dyes 6-methoxy-N-(3-sulfopropyl)quinolinium and 2′,7′-bis-(2-carboxyethyl)-5-(and-6)carboxyfluorescein, respectively. We examined the effect of 16 different carbonic anhydrase inhibitors on AE1 transport activity. Among these 12 were newly-reported compounds; two were clinically used non-steroidal anti-inflammatory drugs (celecoxib and valdecoxib) and two were anti-convulsant drugs (topiramate and zonisamide). Celecoxib and four of the novel compounds significantly inhibited AE1 Cl^?/NO₃^? exchange activity with EC₅₀ values in the range 0.22–2.8 μM. It was evident that bulkier compounds had greater AE1 inhibitory potency. Maximum inhibition using 40 μM of each compound was only 22–53% of AE1 transport activity, possibly because assays were performed in the presence of competing substrate. In Cl^?/HCO₃^? exchange assays, which depend on functional CA to produce transport substrate, 40 μM celecoxib inhibited AE1 by 62±4%. We conclude that some carbonic anhydrase inhibitors, including clinically-used celecoxib, will inhibit bicarbonate transport at clinically-significant concentrations.     

Two modes of bicarbonate utilization in the marine green macroalga Ulva lactuca

The green marine macroalga Ulva lactuca L. was found to be able to utilize HCO₃^? from sea water in two ways. When grown in flowing natural sea water at 16°C under constant dim irradiance, photosynthesis at pH8.4 was suppressed by acetazolamide but unaffected by 4,4′-diisothiocyanostilbene-2,2′-disulphonate. These responses indicate that photosynthetic HCO₃^? utilization was via extracellular carbonic anhydrase (CA) -mediated dehydration followed by CO₂ uptake. The algae were therefore described as being in a ‘CA state’. If treated for more than 10 h in a sea water flow-through system at pH9.8, these thalli became insensitive to acetazolamide but sensitive to 4,4′-diisothiocyanostilbene-2,2′-disulphonate. This suggests the involvement of an anion exchanger (AE) in the direct uptake of HCO₃^?, and these plants were accordingly described as being in an ‘AE state’. Such thalli showed an approximately 10-fold higher apparent affinity for HCO₃^? (at pH9.4) than those in the ‘CA state’, while thalli of both states showed a very high apparent affinity for CO₂. These results suggest that the two modes of HCO₃^? utilization constitute two ways in which inorganic carbon may enter the Ulva lactuca cells, with the direct entry of HCO₃^?, characterizing the ‘AE state’, being inducible and possibly functioning as a complementary uptake system at high external pH values (e.g. under conditions conducive to high photosynthetic rates). Both mechanisms of entry appear to be connected to concentrating CO₂ inside the cell, probably via a separate mechanism operating intracellularly.     

Governing effect of regulatory proteins for Cl−/HCO3− exchanger 2 activity

Anion exchanger 2 (AE2) has a critical role in epithelial cells and is involved in the ionic homeostasis such as Cl^? uptake and HCO₃^? secretion. However, little is known about the regulatory mechanism of AE2. The main goal of the present study was to investigate potential regulators, such as spinophilin (SPL), inositol-1,4,5-trisphosphate [IP₃] receptors binding protein released with IP₃ (IRBIT), STE20/SPS1-related proline/alanine-rich kinase (SPAK) kinase, and carbonic anhydrase XII (CA XII). We found that SPL binds to AE2 and markedly increased the Cl^?/HCO₃^? exchange activity of AE2. Especially SPL 1–480 domain is required for enhancing AE2 activity. For other regulatory components that affect the fidelity of fluid and HCO₃^? secretion, IRBIT and SPAK had no effect on the activity of AE2 and no protein-protein interaction with AE2. It has been proposed that CA activity is closely associated with AE activity. In this study, we provide evidence that the basolateral membrane-associated CA isoform CA XII significantly increased the activity of AE2 and co-localized with AE2 to the plasma membrane. Collectively, SPL and CA XII enhanced the Cl^?/HCO₃^? exchange activity of AE2. The modulating action of these regulatory proteins could serve as potential therapeutic targets for secretory diseases mediated by AE2.     

Evidence for a membrane carbonic anhydrase IV anchored by its C-terminal peptide in normal human pancreatic ductal cells

The high concentration of HCO₃ ^– ions (150 mM) in the human pancreatic ducts raises the question of the membrane proteins responsible for their secretion in addition to the Cl^–/HCO₃ ^– exchanger. In this study, we investigated the expression of carbonic anhydrase IV (CA IV), a possible candidate. Experiments were carried out on specimens of normal human pancreas obtained from brain-dead donors (n=9) as well as on isolated human ductal cells. Two antibodies were generated: CA IV NH₂ antibody directed against the NH₂ terminal of human glycosyl phosphatidylinositol (GPI)-anchored CA IV and CA IV COOH antibody directed against the COOH terminal of the same protein before its association with a GPI in the rough endoplasmic reticulum. A 35-kDa CA IV was detected in the homogenates of human pancreas. Immunocytochemistry demonstrated the expression of CA IV in centroacinar cells and in intercalated, intralobular, and interlobular ductal cells. The immunoreactivity observed with the CA IV COOH antibody was mainly localized on luminal membranes of ductal cells. Treatment of purified plasma membranes with phosphatidylinositol-phospholipase C indicated that the CA IV expressed in pancreatic ducts was not GPI-anchored. Its detection in the same extracts by the CA IV COOH antibody indicated that it was anchored by a hydrophobic segment at the carboxy terminal. Taken together, these results suggest that normal human pancreatic ductal cells express a 35-kDa CA IV anchored in their luminal plasma membrane by a hydrophobic segment of the COOH terminus. In view of its localization and its mode of anchorage in luminal plasma membranes, this CA IV may participate in the maintenance of luminal pH.The first two authors have contributed equally to this work     

The active uptake of carbon dioxide by the marine diatoms Phaeodactylum ticornutum and Cyclotella sp.

Mass spectromelry has been used to investigate the uptake of CO₂ by two marine diatoms, Phaeodactylum tricornutum and Cyclotella sp. The time course of CO₂ formation in the dark after addition of 100 mmol m^?3 dissolved inorganic carbon (DIC) to cell suspensions showed that external carbonic anhydrase (CA) was not present in cells of P. tricornutum but was present in Cyclotella sp. In the absence of external CA, or when it was inhibited by 5 mmol m^?3 acetazolamide, cells of both species preincubated with 100 mmol m^?3 DIG rapidly depleted almost all of the free CO₂ (3·2mmol m^?31 at pH7·5) from the suspending medium within seconds of illumination and prior to the onset of steady-state photosynthesis. Addition of bovine CA quickly restored the HCO₃^?–CO₂ equilibrium in the medium, indicating that the initial depletion of CO₂ resulted from the selective uptake of CO₂ rather than uptake of all DIG species. Transfer of cells to the dark caused a rapid increase in the CO₂ concentration in the medium, largely as a result of the efflux of unfixed inorganic carbon from the cells. The measured CO₂ uptake rates for both species accounted for 50% of the total DIG uptake at HCO₃^?–CO₂ equilibrium, indicating that HCOHCO₃^? was also being taken up. These results indicate that both Phaeodactylum tricornutum and Cyclotella sp. have the capacity to transport CO₂ actively against concentration and pH gradients.     

ACQUISITION OF INORGANIC CARBON BY THE MARINE HAPTOPHYTE ISOCHRYSIS GALBANA (PRYMNESIOPHYCEAE)1

Inorganic carbon acquisition has been investigated in the marine haptophyte Isochrysis galbana. External carbonic anhydrase (CA) was present in air‐grown (0.034% CO₂) cells but completely repressed in high (3%) CO₂‐grown cells. External CA was not inhibited by 1.0 mM acetazolamide. The capacity of cells to take up bicarbonate was examined by comparing the rate of photosynthetic O₂ evolution with the calculated rate of spontaneous CO₂ supply; at pH 8.2 the rates of O₂ evolution exceeded the CO₂ supply rate 14‐fold, indicating that this alga was able to take up HCO₃ ^? . Monitoring CO₂ concentrations by mass spectrometry showed that suspensions of high CO₂‐grown cells caused a rapid drop in the extracellular CO₂ in the light and addition of bovine CA raised the CO₂ concentration by restoring the HCO₃ ^? ‐CO₂ equilibrium, indicating that cells were maintaining the CO₂ in the medium below its equilibrium value during photosynthesis. A rapid increase in extracellular CO₂ concentration occurred on darkening the cells, indicating that the cells had accumulated an internal pool of unfixed inorganic carbon. Active CO₂ uptake was blocked by the photosynthetic electron transport inhibitor 3‐(3′,4′‐dichlorphenyl)‐1,1‐dimethylurea, indicating that CO₂ transport was supported by photosynthetic reactions. These results demonstrate that this species has the capacity to take up HCO₃ ^? and CO₂ actively as sources of substrate for photosynthesis and that inorganic carbon transport is not repressed by growth on high CO₂, although external CA expression is regulated by CO₂ concentration.     

CO2-concentrating mechanisms: a direct role for thylakoid lumen acidification?

A testable mechanism of CO₂ accumulation in photolithotrophs, originally suggested by Pronina & Semenenko, is quantitatively analysed. The mechanism involves (as does the most widely accepted hypothesis) the delivery of HCO₃^? to the compartment containing Rubisco. It differs in proposing subsequent HCO₃^? entry (by passive uniport) to the thylakoid lumen, followed by carbonic anhydrase activity in the lumen; uncatalysed conversion of HCO₃^? to CO₂, even at the low pH of the lumen, is at least 300 times too slow to account for the rate of inorganic C acquisition. Carbonic anhydrase converts the HCO₃^? to CO₂ at the lower pH maintained in the illuminated thylakoid lumen by the light-driven H⁺ pump, generating CO₂ at 10 times or more the thylakoid HCO₃^? concentration. Efflux of this CO₂ can suppress Rubisco oxygenase activity and stimulate carboxylase activity in the stroma. This mechanism differs from the widely accepted hypotheses in the required location of carbonic anhydrase, i.e. in the thylakoid lumen rather than the stroma or pyrenoid, and in the need for HCO₃^? influx to thylakoids. The capacity for anion (assayed as Cl^?) entry by passive uniport reported for thylakoid membranes is adequate for the proposed mechanism; if the Cl^? channel does not transport HCO₃^?, HCO₃^? entry could be by combination of the Cl^? channel with a Cl^? HCO₃^? antiporter. This mechanism is particularly appropriate for organisms which lack overt accumulation of total inorganic C in cells, but which nevertheless have the gas exchange characteristics of an organism with a CO₂-concentrating mechanism.     

INORGANIC CARBON UTILIZATION BY ROSS SEA PHYTOPLANKTON ACROSS NATURAL AND EXPERIMENTAL CO2 GRADIENTS1

We present results from a field study of inorganic carbon (C) acquisition by Ross Sea phytoplankton during Phaeocystis‐dominated early season blooms. Isotope disequilibrium experiments revealed that HCO₃^? was the primary inorganic C source for photosynthesis in all phytoplankton assemblages. From these experiments, we also derived relative enhancement factors for HCO₃^?/CO₂ interconversion as a measure of extracellular carbonic anhydrase activity (eCA). The enhancement factors ranged from 1.0 (no apparent eCA activity) to 6.4, with an overall mean of 2.9. Additional eCA measurements, made using membrane inlet mass spectrometry (MIMS), yielded activities ranging from 2.4 to 6.9 U · [μg chl a]^?1 (mean 4.1). Measurements of short‐term C‐fixation parameters revealed saturation kinetics with respect to external inorganic carbon, with a mean half‐saturation constant for inorganic carbon uptake (K_1/2) of ～380 μM. Comparison of our early springtime results with published data from late‐season Ross Sea assemblages showed that neither HCO₃^? utilization nor eCA activity was significantly correlated to ambient CO₂ levels or phytoplankton taxonomic composition. We did, however, observe a strong negative relationship between surface water pCO₂ and short‐term ¹⁴C‐fixation rates for the early season survey. Direct incubation experiments showed no statistically significant effects of pCO₂ (10 to 80 Pa) on relative HCO₃^? utilization or eCA activity. Our results provide insight into the seasonal regulation of C uptake by Ross Sea phytoplankton across a range of pCO₂ and phytoplankton taxonomic composition.     

A NEW METHOD FOR ESTIMATING EXTERNAL,CARBONIC ANHYDRASE ACTMTY IN MACROALGAE1,2

The effects of external carbonic anhydrase (CA, E.C. 4.2.1.1) on HCO^?₃and CO₂use under disequilibnum conditions were examined in 14 species of macroalgae. CO₂ was added to the algae in synthetic seawater free from inorganic carbon and buffered to pH 8.7. This resulted in a transient O₂ evolution, which was similar for most of the species tested: an initial rapid increase in the rate was followed by a gradual decrease, approaching a steady state within 10 min. The initial high rate of O₂evolution was attributed to diffusive entry of CO₂into the cells and the steady state to use of HCO^?₃. An enhancement of CO₂diffusive entry was obtained with acetazolamide, an inhibitor of external CA activity. Using this enhancement, a variable was developed to quantify the degree to which CO₂entry into the cell was prevented by the external CA. This variable, CA (%), was used as a measure of the external CA activity of the alga. Comparative measurements of the external CA activity using a potentiomtric method revealed that the new method was able to detect low levels of external CA activity, where the potentiometric method failed. These two different methods could be used together to increase the reliability of the measurements. The new method was useful for red and brown macroalgae and for those green macroalgae that lacked direct HCO₃uptake. Thus prominent external CA activity was found for Valonia utricularis (green), Halopteris scoparia (brown), and Osmunda pinnatifida (red), where the potentiometric method failed, or nearly failed, to indicate any external CA activity. Direct uptake of HCO^?₃interfered with the new method and the degree of this interference was dependent on the magnitude of the uptake.     

The effects of pH and dissolved inorganic carbon on external carbonic anhydrase activity in Chlorella saccharophila

External carbonic anhydrase (CA) activity in Chlorella saccharophila is suppressed by growth at high dissolved inorganic carbon and at acid pH. External CA activity was shown to be suppressed by growth at pHs below 7.0, with total repression at pH5.0. Growth in the presence of the buffer 3-[N-Morpholino]propane-sulphonic acid (MOPS) between pH 7 and 8 suppressed CA activity. Cells grown at pH8.0 aerated at 6 dm³ h^?1 exhibited external CA activity of 5 units mg^?1 Chl once the dissolved inorganic carbon (DIC) was reduced to 300 mmol m^?3, and this increased to 30 units mg^?1 Chl over a period of 3d while the DIC dropped to 30mmol m^?3. Cells aerated at 180 dm³ h^?1 showed a similar trend in CA activity, although the onset was delayed by 1 d and the DIC did not drop below 300 mmol m^?3. Cells grown at pH 7.8 near an air equilibrium DIC of 300 mmol m^?3had no detectable external CA activity. It is probable that it is the CO² supply to the cell, and not total DIC or HCO^?₃ which controls external CA activity. Cells grown at pH 5.0 had no detectable activity, although they reduced the CO² concentration to 0.6 mmol m^?3. The loss of CA upon transfer of air-grown cells to 10 mmol mol^?1 CO² took place over 48 h and was light dependent, while the loss upon transfer from alkaline pH to acid pH look place over 12 h and was independent of light. The effects of pH are independent of the response to CO₂.     

Carbonic anhydrase in Ranunculus penicillatus spp. pseudofluitans: activity, location and implications for carbon assimilation

Levels of carbonic anhydrase activity were determined on a total (60 E_Umg^?1 protein), external (7.36 E_U), internal (50.14 E_U) and protoplast (15.63 E_U) basis for Ranunculus penicillatus (Dumort.) Bab ssp. pseudofluitans (Syme) S. Webster, a freshwater aquatic macrophyte, by conventional electrometric methods. The site of activity of ‘external’ carbonic anhydrase (CA) has been visualized using 5-Dimethylaminonapthalene-1- sulphonamide (DNSA)-CA fluorescent complex formation, and is postulated to be closely associated with the epidermal cell wall. The photosynthetic rate of R. penicillatus ssp. pseudofluitans at pH 9.0 is in excess of the uncatalysed rate of production of CO₂ from HCO^?₃, and this plant is therefore using HCO^?₃ for photosynthesis. The possible contribution of CA activity to inorganic carbon assimilation, and specifically to transport of HCO^?₃, in submerged aquatic plants is discussed.     

PHOTOSYNTHETIC UTILIZATION OF INORGANIC CARBON IN THE ECONOMIC BROWN ALGA,HIZIKIA FUSIFORME (SARGASSACEAE) FROM THE SOUTH CHINA SEA1

The mechanism of inorganic carbon (C_i) acquisition by the economic brown macroalga, Hizikia fusiforme (Harv.) Okamura (Sargassaceae), was investigated to characterize its photosynthetic physiology. Both intracellular and extracellular carbonic anhydrase (CA) were detected, with the external CA activity accounting for about 5% of the total. Hizikia fusiforme showed higher rates of photosynthetic oxygen evolution at alkaline pH than those theoretically derived from the rates of uncatalyzed CO₂ production from bicarbonate and exhibited a high pH compensation point (pH 9.66). The external CA inhibitor, acetazolamide, significantly depressed the photosynthetic oxygen evolution, whereas the anion‐exchanger inhibitor 4,4′‐diisothiocyano‐stilbene‐2,2′‐disulfonate had no inhibitory effect on it, implying the alga was capable of using HCO₃^? as a source of C_i for its photosynthesis via the mediation of the external CA. CO₂ concentrations in the culture media affected its photosynthetic properties. A high level of CO₂ (10,000 ppmv) resulted in a decrease in the external CA activity; however, a low CO₂ level (20 ppmv) led to no changes in the external CA activity but raised the intracellular CA activity. Parallel to the reduction in the external CA activity at the high CO₂ was a reduction in the photosynthetic CO₂ affinity. Decreased activity of the external CA in the high CO₂ grown samples led to reduced sensitiveness of photosynthesis to the addition of acetazolamide at alkaline pH. It was clearly indicated that H. fusiforme, which showed CO₂‐limited photosynthesis with the half‐saturating concentration of C_i exceeding that of seawater, did not operate active HCO₃^? uptake but used it via the extracellular CA for its photosynthetic carbon fixation.     

Gas transfer in dogfish: A unique model of CO2 excretion

Carbonic anhydrase (CA) is a zinc metalloenzyme that catalyzes the reversible hydration–dehydration reactions of CO₂. It is present in high abundance in the cytoplasm of vertebrate red blood cells, where it contributes to CO₂ excretion. A membrane-bound CA isoform (CA IV) is also present in the lungs of mammals and reptiles, but plays little role in CO₂ excretion. The gills of teleost fish appear to lack plasma-accessible CA activity. In elasmobranchs, however, evidence gathered using a variety of physiological, biochemical and molecular approaches suggests that CA IV is present in the gills, and that at least in dogfish, this CA IV makes a significant contribution to CO₂ excretion by catalyzing the dehydration of plasma HCO₃^?. The contribution of CA IV to CO₂ excretion is favoured by unusually high relative plasma buffering that aids in the provision of protons for HCO₃^? dehydration. Moreover, reduced emphasis on HCO₃^? flux through the red blood cell may reflect the occurrence of a slower turnover cytosolic CA in dogfish. This model of CO₂ excretion, in which HCO₃^? dehydration in the red blood cell catalyzed by cytosolic CA and HCO₃^? dehydration in the plasma catalyzed by membrane-bound CA IV are of comparable importance, has been described for the dogfish. Further work is required to determine whether it applies to elasmobranch fish as a group.     

CO2‐CONCENTRATING MECHANISMS OF THE POTENTIALLY TOXIC DINOFLAGELLATE PROTOCERATIUM RETICULATUM (DINOPHYCEAE,GONYAULACALES)1

The low CO₂ concentration in seawater poses severe restrictions on photosynthesis, especially on those species with form II RUBISCO. We found that the potentially toxic dinoflagellate Protoceratium reticulatum Clap. et J. Lachm. possesses a form II RUBISCO. To cast some light on the mechanisms this organism undergoes to cope with low CO₂ availability, we compared cells grown at atmospheric (370 ppm) and high (5000 ppm) CO₂ concentrations, with respect to a number of physiological parameters related to dissolved inorganic carbon (DIC) acquisition and assimilation. The photosynthetic affinity for DIC was about one order of magnitude lower in cells cultivated at high [CO₂]. End‐point pH‐drift experiments suggest that P. reticulatum was not able to efficiently use HCO₃^? under our growth conditions. Only internal carbonic anhydrase (CA) activity was detected, and its activity decreased by about 60% in cells cultured at high [CO₂]. Antibodies raised against a variety of algal CAs were used for Western blot analysis: P. reticulatum extracts only cross‐reacted with anti‐ß‐CA sera, and the amount of immunoreactive protein decreased in cells grown at high [CO₂]. No pyrenoids were observed under all growth conditions. Our data indicate that P. reticulatum has an inducible carbon‐concentrating mechanism (CCM) that operates in the absence of pyrenoids and with little intracellular CO₂ accumulation. Calculations on the impact of the CA activity to photosynthetic growth [CO₂] suggest that it is an essential component of the CCM of P. reticulatum and is necessary to sustain the photosynthetic rates observed at ambient CO₂.     

PHOTOSYNTHETIC PROPERTIES OF PROTOPLASTS,AS COMPARED WITH THALLI,OF ULVA FASCIATA (CHLOROPHYTA)1

Protoplasts were prepared from Ulva fasciata Delile, and their photosynthetic performance was measured and compared with that of thalli discs. These protoplasts maintained maximal rates of photosynthesis as high as those of thalli (up to 300 μmol O₂·mg chlorophyll^?1·h^?1) for several hours after preparation and were therefore considered suitable for kinetic studies of inorganic carbon utilization. The photosynthetic K_1/2(inorganic carbon) at pH 6.1 was 3.8 μM and increased to 67, 158, and 1410 μM at the pH values 7.0, 7.9, and 8.9, respectively. Compared with these protoplasts, thalli had a much lower affinity for CO₂ but approximately the same affinity for HCO₃^?. Comparisons between rates of photosynthesis and the spontaneous dehydration of HCO₃^? (at 50 μM inorganic carbon) revealed that photosynthesis of both protoplasts (which lacked apparent activity of extracellular/surface-bound carbonic anhydrase) and thalli (which were only 25% inhibited by the external carbonic anhydrase inhibitor acetazolamide) could not be supported by CO₂ formation in the medium at the higher pH values, indicating HCO₃^? uptake. Since both protoplasts and thalli were sensitive to 4,4′-diisothiocyanostilbene-2,2′-disulfonate, we suggest that HCO₃^? transport was facilitated by the membrane-located anion exchange protein recently reported to function in certain Ulva thalli. These findings suggest that the presence of a cell wall may constitute a diffusion barrier for CO₂, but not for HCO₃^?, utilization under natural seawater conditions.     

Photosynthetic inorganic carbon uptake and accumulation in two marine diatoms

Some physiological characteristics of photosynthetic inorganic carbon uptake have been examined in the marine diatoms Phaeodactylum tricornutum and Cyclotella sp. Both species demonstrated a high affinity for inorganic carbon in photosynthesis at pH7.5, having K_1/2(CO₂) in the range 1.0 to 4.0mmol m^?3 and O_2? and temperature-insensitive CO₂ compensation concentrations in the range 10.8 to 17.6 cm³ m^?3. Intracellular accumulation of inorganic carbon was found to occur in the light; at an external pH of 7.5 the concentration in P. tricornutum was twice, and that in Cyclotella 3.5 times, the concentration in the suspending medium. Carbonic anhydrase (CA) was detected in intact Cyclotella cells but not in P. tricornutum, although internal CA was detected in both species. The rates of photosynthesis at pH 8.0 of P. tricornutum cells and Cyclotella cells treated with 0.1 mol m^?3 acetazolamide, a CA inhibitor, were 1.5- to 5-fold the rate of CO₂ supply, indicating that both species have the capacity to take up HCO₃^? as a source of substrate for photosynthesis. No Na⁺ dependence for HCO₃^? could be detected in either species. These results indicate that these two marine diatoms have the capacity to accumulate inorganic carbon in the light as a consequence, in part, of the active uptake of bicarbonate.     

Production,purification, and characterization of a fusion protein of carbonic anhydrase from Neisseria gonorrhoeae and cellulose binding domain from Clostridium thermocellum

Carbon dioxide capture technologies have the potential to become an important climate change mitigation option through sequestration of gaseous CO₂. A new concept for CO₂ capture involves use of immobilized carbonic anhydrase (CA) that catalyzes the reversible hydration of CO₂ to HCO₃^? and H⁺. Cost‐efficient production of the enzyme and an inexpensive immobilization system are critical for development of economically feasible CA‐based CO₂ capture processes. An artificial, bifunctional enzyme containing CA from Neisseria gonorrhoeae and a cellulose binding domain (CBD) from Clostridium thermocellum was constructed with a His₆ tag. The chimeric enzyme exhibited both CA activity and CBD binding affinity. This fusion enzyme is of particular interest due to its binding affinity for cellulose and retained CA activity, which could serve as the basis for improved technology to capture CO₂ from flue gasses. © 2009 American Institute of Chemical Engineers Biotechnol. Prog., 2009     

The role of extracellular carbonic anhydrase for accumulation of inorganic carbon in the green alga Chlamydomonas reinhardtii. A comparison between wild-type and cell-wall-less mutant cells

The role of extracellular carbonic anhydrase (CA_ex) for dissolved inorganic carbon (DIC) accumulation in the green alga Chlamydomonas reinhardtii was investigated. It was found that when algal cells were bubbled with ambient air, cell-wall-less mutant cells exhibited the same high photosynthetic affinity for CO₂ as wild-type cells despite a 10 times lower activity of CA^ex. It was also found that the affinity for CO₂ was further increased when the total DIC concentration of the algal medium was reduced from that in equilibrium with ambient air to even lower levels. This increased affinity was not correlated with any further increase in the CA_ex activity. Dextran-bound sulfonamide (DBS. 100 μM bound ligand) completely inhibited the activity of CA_ex in intact, low-DIC grown, wild-type cells, while photosynthesis at <2 μM CO₂(aq) proceeded at a far greater rate than could be maintained by CO₂ supplied from the spontaneous dehydration of HCO^?₃. DBS-inhibition of CA_ex, during the induction of the DIC-accumulating mechanism in previously high-DIC grown cells, only caused a 50% inhibition of photosynthesis at 10 μM CO₂(aq) after 1 h of low-DIC acclimation. It was also shown that 50 μM acetazolamide (AZ) inhibited photosynthesis at low DIC concentrations to a relatively higher degree than DBS, suggesting that AZ inhibited intracellular CA as well. Taken together, these results suggest that low-DIC grown cells of C. reinhardtii have the ability to transport HCO^?₃ across the plasma membrane in addition to the CA_ex-mediated, facilitated diffusion and/or transport of CO₂. It is also suggested that the relative importance of these two fluxes (CO₂ or HCO^?₃) is dependent on the growth and experimental conditions. Facilitated CO₂ uptake seems to be most prevalent, supported by HCO^?₃-transport under more or less extreme situations, such as a reduction of CO₂ to extremely low concentrations, leakage of CA_ex to the medium as in cultures of cell-wall-less mutant cells or when the activity of CA_ex has been artificially inhibited.     

CLONING AND QUANTITATIVE ANALYSIS OF THE CARBONIC ANHYDRASE GENE FROM PORPHYRA YEZOENSIS1

Carbonic anhydrase (CA), an enzyme that catalyzes the interconversion of CO₂ and HCO₃^?, has a critical role in inorganic carbon acquisition in many kingdoms, including animals, plants, and bacteria. In this study, the full‐length cDNA of the CA gene from Porphyra yezoensis Ueda (denoted as PyCA) was cloned by using an expressed sequence tag (EST) and rapid amplification of cDNA ends (RACE). The nucleotide sequence of PyCA consists of 1,153 bp, including a 5′ untranslated region (UTR) of 177 bp, a 3′ UTR of 151 bp, and an open reading frame (ORF) of 825 bp that can be translated into a 274‐amino‐acid putative peptide with a molecular mass (M) of 29.8 kDa and putative isoelectric point (pI) of 8.51. The predicted polypeptide has significant homology to the β‐CA from bacteria and unicellular algae, such as Porphyridium purpureum. The mRNA in filamentous thalli, leafy thalli, and conchospores was examined, respectively, by real‐time fluorescent quantitative PCR (qPCR), and the levels of PyCA are different at different stages of the life cycle. The lowest level of mRNA was observed in leafy thalli, and the level in filamentous thalli and in the conchospores was 4‐fold higher and 10‐fold higher, respectively.     

Normal Fertility Requires the Expression of Carbonic Anhydrases II and IV in Sperm

HCO₃⁻ is a key factor in the regulation of sperm motility. High concentrations of HCO₃⁻ in the female genital tract induce an increase in sperm beat frequency, which speeds progress of the sperm through the female reproductive tract. Carbonic anhydrases (CA), which catalyze the reversible hydration of CO₂ to HCO₃⁻, represent potential candidates in the regulation of the HCO₃⁻ homeostasis in sperm and the composition of the male and female genital tract fluids. We show that two CA isoforms, CAII and CAIV, are distributed along the epididymal epithelium and appear with the onset of puberty. Expression analyses reveal an up-regulation of CAII and CAIV in the different epididymal sections of the knockout lines. In sperm, we find that CAII is located in the principal piece, whereas CAIV is present in the plasma membrane of the entire sperm tail. CAII and CAIV single knockout animals display an imbalanced HCO₃⁻ homeostasis, resulting in substantially reduced sperm motility, swimming speed, and HCO₃⁻-enhanced beat frequency. The CA activity remaining in the sperm of CAII- and CAIV-null mutants is 35% and 68% of that found in WT mice. Sperm of the double knockout mutant mice show responses to stimulus by HCO₃⁻ or CO₂ that were delayed in onset and reduced in magnitude. In comparison with sperm from CAII and CAIV double knockout animals, pharmacological loss of CAIV in sperm from CAII knockout animals, show an even lower response to HCO₃⁻. These results suggest that CAII and CAIV are required for optimal fertilization.