Two Systems for Concentrating CO(2) and Bicarbonate during Photosynthesis by Scenedesmus

Scenedesmus cells grown on high CO₂, when adapted to air levels of CO₂ for 4 to 6 hours in the light, formed two concentrating processes for dissolved inorganic carbon: one for utilizing CO₂ from medium of pH 5 to 8 and one for bicarbonate accumulation from medium of pH 7 to 11. Similar results were obtained with assays by photosynthetic O₂ evolution or by accumulation of dissolved inorganic carbon inside the cells. The CO₂ pump with K_0.5 for O₂ evolution of less than 5 micromolar CO₂ was similar to that previously studied with other green algae such as Chlamydomonas and was accompanied by plasmalemma carbonic anhydrase formation. The HCO₃⁻ concentrating process between pH 8 to 10 lowered the K_0.5 (DIC) from 7300 micromolar HCO₃⁻ in high CO₂ grown Scenedesmus to 10 micromolar in air-adapted cells. The HCO₃⁻ pump was inhibited by vanadate (K_i of 150 micromolar), as if it involved an ATPase linked HCO₃⁻ transporter. The CO₂ pump was formed on low CO₂ by high-CO₂ grown cells in growth medium within 4 to 6 hours in the light. The alkaline HCO₃⁻ pump was partially activated on low CO₂ within 2 hours in the light or after 8 hours in the dark. Full activation of the HCO₃⁻ pump at pH 9 had requirements similar to the activation of the CO₂ pump. Air-grown or air-adapted cells at pH 7.2 or 9 accumulated in one minute 1 to 2 millimolar inorganic carbon in the light or 0.44 millimolar in the dark from 150 micromolar in the media, whereas CO₂-grown cells did not accumulate inorganic carbon. A general scheme for concentrating dissolved inorganic carbon by unicellular green algae utilizes a vanadate-sensitive transporter at the chloroplast envelope for the CO₂ pump and in some algae an additional vanadate-sensitive plasmalemma HCO₃⁻ transporter for a HCO₃⁻ pump.     

Photosynthetic Response to Alkaline pH in Anabaena variabilis

The rate of O₂ evolution and alkalization of the medium in low CO_2⁻ grown Anabaena variabilis was observed as affected by the pH in the medium. Both rates are severely inhibited by pH values higher than 9.5, but the latter is more sensitive to this treatment. This finding, as well as the lag observed in alkalization of the medium, but not in O₂ evolution, following the addition of HCO₃⁻ indicates that the transport of HCO₃ and OH⁻ (or H⁺) are not compulsorily coupled. The inhibition of photosynthesis by strongly alkaline pH is attributed to an alteration of the internal pH and, hence, the rate of carboxylation. This conclusion is supported by data showing that the rate of O₂ evolution is affected by pH more strongly at saturating [HCO₃⁻] than at limiting [HCO₃⁻]. Also, the rate of O₂ evolution at saturating light intensity is affected by pH more strongly than is the initial slope of the curve against light intensity or the rate of dark respiration.     

Effect of Carbonic Anhydrase Inhibitors on Inorganic Carbon Accumulation by Chlamydomonas reinhardtii

Membrane-permeable and impermeable inhibitors of carbonic anhydrase have been used to assess the roles of extracellular and intracellular carbonic anhydrase on the inorganic carbon concentrating system in Chlamydomonas reinhardtii. Acetazolamide, ethoxzolamide, and a membrane-impermeable, dextran-bound sulfonamide were potent inhibitors of extracellular carbonic anhydrase measured with intact cells. At pH 5.1, where CO₂ is the predominant species of inorganic carbon, both acetazolamide and the dextran-bound sulfonamide had no effect on the concentration of CO₂ required for the half-maximal rate of photosynthetic O₂ evolution (K_0.5[CO₂]) or inorganic carbon accumulation. However, a more permeable inhibitor, ethoxzolamide, inhibited CO₂ fixation but increased the accumulation of inorganic carbon as compared with untreated cells. At pH 8, the K_0.5(CO₂) was increased from 0.6 micromolar to about 2 to 3 micromolar with both acetazolamide and the dextran-bound sulfonamide, but to a higher value of 60 micromolar with ethoxzolamide. These results are consistent with the hypothesis that CO₂ is the species of inorganic carbon which crosses the plasmalemma and that extracellular carbonic anhydrase is required to replenish CO₂ from HCO₃⁻ at high pH. These data also implicate a role for intracellular carbonic anhydrase in the inorganic carbon accumulating system, and indicate that both acetazolamide and the dextran-bound sulfonamide inhibit only the extracellular enzyme. It is suggested that HCO₃⁻ transport for internal accumulation might occur at the level of the chloroplast envelope.     

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.     

Evidence for HCO(3) Transport by the Blue-Green Alga (Cyanobacterium) Coccochloris peniocystis

The possibility of HCO₃⁻ transport in the blue-green alga (cyanobacterium) Coccochloris peniocystis has been investigated. Coccochloris photosynthesized most rapidly in the pH range 8 to 10, where most of the inorganic C exists as HCO₃⁻. If photosynthesis used only CO₂ from the external solution the rate of photosynthesis would be limited by the rate of HCO₃⁻ dehydration to CO₂. Observed rates of photosynthesis at alkaline pH were as much as 48-fold higher than could be supported by spontaneous dehydration of HCO₃⁻ in the external solution. Assays for extracellular carbonic anhydrase were negative. The evidence strongly suggests that HCO₃⁻ was a direct C source for photosynthesis.     

Utilization of Inorganic Carbon by Ulva lactuca

Thalli discs of the marine macroalga Ulva lactuca were given inorganic carbon in the form of HCO₃⁻, and the progression of photosynthetic O₂ evolution was followed and compared with predicted O₂ evolution as based on calculated external formation of CO₂ (extracellular carbonic anhydrase was not present in this species) and its carboxylation (according to the K_m(CO₂) of ribulose-1,5-bisphosphate carboxylase/oxygenase), at two different pHs, assuming a photosynthetic quotient of 1. The K_m(inorganic carbon) was some 2.5 times lower at pH 5.6 than at the natural seawater pH of 8.2, whereas V_max was similar under the two conditions, indicating that the unnaturally low pH per se had no adverse effect on U. lactuca's photosynthetic performance. These results, therefore, could be evaluated with regard to differential CO₂ and HCO₃⁻ utilization. The photosynthetic performance observed at the lower pH largely followed that predicted, with a slight discrepancy probably reflecting a minor diffusion barrier to CO₂ uptake. At pH 8.2, however, dehydration rates were too slow to supply CO₂ for the measured photosynthetic response. Given the absence of external carbonic anhydrase activity, this finding supports the view that HCO₃⁻ transport provides higher than external concentrations of CO₂ at the ribulose-1,5-bisphosphate carboxylase/oxygenase site. Uptake of HCO₃⁻ by U. lactuca was further indicated by the effects of potential inhibitors at pH 8.2. The alleged band 3 membrane anion exchange protein inhibitor 4,4′-diisothiocyanostilbene-2,2′disulphonate reduced photosynthetic rates only when HCO₃⁻ (but not CO₂) could be the extracellular inorganic carbon form taken up. A similar, but less drastic, HCO₃⁻-competitive inhibition of photosynthesis was obtained with Kl and KNO₃. It is suggested that, under ambient conditions, HCO₃⁻ is transported into cells at defined sites either via facilitated diffusion or active uptake, and that such transport is the basis for elevated internal [CO₂] at the site of ribulose-1,5-bisphosphate carboxylase/oxygenase carboxylation.     

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.     

Carbon Oxysulfide Is an Inhibitor of Both CO(2) and HCO(3) Uptake in the Cyanobacterium Synechococcus PCC7942

Carbon oxysulfide (COS) was reinvestigated as an inhibitor of active inorganic carbon transport in cells of Synechococcus PCC7942 adapted to growth at low inorganic carbon. COS inhibited both CO₂ and HCO₃⁻ transport processes in a reversible (in the short term) and mixed competitive manner. The inhibition of COS was established using both silicone oil centrifugation experiments and O₂-evolution studies. The K_i for COS inhibition was 29 micromolar for CO₂ transport and 110 micromolar for HCO₃⁻ transport. These results support a model of inorganic carbon transport with a central CO₂ pump and an inducible HCO₃⁻ utilizing accessory protein which supplies CO₂ to the primary pump.     

Salicylhydroxamic Acid (SHAM) Inhibition of the Dissolved Inorganic Carbon Concentrating Process in Unicellular Green Algae

Rates of photosynthetic O₂ evolution, for measuring K_0.5(CO₂ + HCO₃⁻) at pH 7, upon addition of 50 micromolar HCO₃⁻ to air-adapted Chlamydomonas, Dunaliella, or Scenedesmus cells, were inhibited up to 90% by the addition of 1.5 to 4.0 millimolar salicylhydroxamic acid (SHAM) to the aqueous medium. The apparent K₁(SHAM) for Chlamydomonas cells was about 2.5 millimolar, but due to low solubility in water effective concentrations would be lower. Salicylhydroxamic acid did not inhibit oxygen evolution or accumulation of bicarbonate by Scenedesmus cells between pH 8 to 11 or by isolated intact chloroplasts from Dunaliella. Thus, salicylhydroxamic acid appears to inhibit CO₂ uptake, whereas previous results indicate that vanadate inhibits bicarbonate uptake. These conclusions were confirmed by three test procedures with three air-adapted algae at pH 7. Salicylhydroxamic acid inhibited the cellular accumulation of dissolved inorganic carbon, the rate of photosynthetic O₂ evolution dependent on low levels of dissolved inorganic carbon (50 micromolar Na-HCO₃), and the rate of ¹⁴CO₂ fixation with 100 micromolar [¹⁴C] HCO₃⁻. Salicylhydroxamic acid inhibition of O₂ evolution and ¹⁴CO₂-fixation was reversed by higher levels of NaHCO₃. Thus, salicylhydroxamic acid inhibition was apparently not affecting steps of photosynthesis other than CO₂ accumulation. Although salicylhydroxamic acid is an inhibitor of alternative respiration in algae, it is not known whether the two processes are related.     

Extracellular Carbonic Anhydrase Facilitates Carbon Dioxide Availability for Photosynthesis in the Marine Dinoflagellate Prorocentrum micans

This study investigated inorganic carbon accumulation in relation to photosynthesis in the marine dinoflagellate Prorocentrum micans. Measurement of the internal inorganic carbon pool showed a 10-fold accumulation in relation to external dissolved inorganic carbon (DIC). Dextran-bound sulfonamide (DBS), which inhibited extracellular carbonic anhydrase, caused more than 95% inhibition of DIC accumulation and photosynthesis. We used real-time imaging of living cells with confocal laser scanning microscopy and a fluorescent pH indicator dye to measure transient pH changes in relation to inorganic carbon availability. When steady-state photosynthesizing cells were DIC limited, the chloroplast pH decreased from 8.3 to 6.9 and cytosolic pH decreased from 7.7 to 7.1. Re-addition of HCO₃⁻ led to a rapid re-establishment of the steady-state pH values abolished by DBS. The addition of DBS to photosynthesizing cells under steady-state conditions resulted in a transient increase in intracellular pH, with photosynthesis maintained for 6 s, the amount of time needed for depletion of the intracellular inorganic carbon pool. These results demonstrate the key role of extracellular carbonic anhydrase in facilitating the availability of CO₂ at the exofacial surface of the plasma membrane necessary to maintain the photosynthetic rate. The need for a CO₂-concentrating mechanism at ambient CO₂ concentrations may reflect the difference in the specificity factor of ribulose-1,5 bisphosphate carboxylase/oxygenase in dinoflagellates compared with other algal phyla.     

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.     

A Model for HCO(3) Accumulation and Photosynthesis in the Cyanobacterium Synechococcus sp: Theoretical Predictions and Experimental Observations

A simple model based on HCO₃⁻ transport has been developed to relate photosynthesis and inorganic carbon fluxes for the marine cyanobacterium, Synechococcus sp. Nägeli (strain RRIMP N1). Predicted relationships between inorganic carbon transport, CO₂ fixation, internal carbonic anhydrase activity, and leakage of CO₂ out of the cell, allow comparisons to be made with experimentally obtained data. Measurements of inorganic carbon fluxes and internal inorganic carbon pool sizes in these cells were made by monitoring time-courses of CO₂ changes (using a mass spectrometer) during light/dark transients. At just saturating CO₂ conditions, total inorganic carbon transport did not exceed net CO₂ fixation by more than 30%. This indicates CO₂ leakage similar to that estimated for C₄ plants.

For this leakage rate, the model predicts the cell would need a conductance to CO₂ of around 10⁻⁵ centimeters per second. This is similar to estimates made for the same cells using inorganic carbon pool sizes and CO₂ efflux measurements. The model predicts that carbonic anhydrase is necessary internally to allow a sufficiently fast rate of CO₂ production to prevent a large accumulation of HCO₃⁻. Intact cells show light stimulated carbonic anhydrase activity when assayed using ¹⁸O-labeled CO₂ techniques. This is also supported by low but detectable levels of carbonic anhydrase activity in cell extracts, sufficient to meet the requirements of the model.

     

Uptake of Inorganic Carbon by Isolated Chloroplasts of the Unicellular Green Alga Chlorella ellipsoidea

Chloroplasts, isolated from protoplasts of the green alga, Chlorella ellipsoidea, were estimated to be 99% intact by the ferricyanide-reduction assay, and gave CO₂ and PGA-dependent rates of O₂ evolution of 64.5 to 150 micromoles per milligram of chlorophyll per hour, that is 30 to 70% of the photosynthetic activity of the parent cells. Intact chloroplasts showed no carbonic anhydrase activity, but it was detected in preparations of ruptured organelles. Rates of photosynthesis, measured in a closed system at pH 7.5, were twice the calculated rate of CO₂ supply from the uncatalyzed dehydration of HCO₃⁻ indicating a direct uptake of bicarbonate by the intact chloroplasts. Mass spectrometric measurements of CO₂ depletion from the medium on the illumination of chloroplasts indicate the lack of an active CO₂ transport across the chloroplast envelope.     

Oxygen-18 Exchange as a Measure of Accessibility of CO(2) and HCO(3) to Carbonic Anhydrase in Chlorella vulgaris (UTEX 263)

We have measured the exchange of ¹⁸O between CO₂ and H₂O in stirred suspensions of Chlorella vulgaris (UTEX 263) using a membrane inlet to a mass spectrometer. The depletion of ¹⁸O from CO₂ in the fluid outside the cells provides a method to study CO₂ and HCO₃⁻ kinetics in suspensions of algae that contain carbonic anhydrase since ¹⁸O loss to H₂O is catalyzed inside the cells but not in the external fluid. Low-CO₂ cells of Chlorella vulgaris (grown with air) were added to a solution containing ¹⁸O enriched CO₂ and HCO₃⁻ with 2 to 15 millimolar total inorganic carbon. The observed depletion of ¹⁸O from CO₂ was biphasic and the resulting ¹⁸C content of CO₂ was much less than the ¹⁸O content of HCO₃⁻ in the external solution. Analysis of the slopes showed that the Fick's law rate constant for entry of HCO₃⁻ into the cell was experimentally indistinguishable from zero (bicarbonate impermeable) with an upper limit of 3 × 10⁻⁴ s⁻¹ due to our experimental errors. The Fick's law rate constant for entry of CO₂ to the sites of intracellular carbonic anhydrase was large, 0.013 per second, but not as great as calculated for no membrane barrier to CO₂ flux (6 per second). The experimental value may be explained by a nonhomogeneous distribution of carbonic anhydrase in the cell (such as membrane-bound enzyme) or by a membrane barrier to CO₂ entry into the cell or both. The CO₂ hydration activity inside the cells was 160 times the uncatalyzed CO₂ hydration rate.     

Inorganic carbon transport across cell compartments of the halotolerant alga Dunaliella salina

The inorganic carbon (C_i) accumulation and the intracellular location of carbonic anhydrase (CA, EC 4.2.1.1) in the halotolerant unicellular alga Dunaliella salina have been investigated. The rate of HCO₃ -dependent O₂ evolution was determined by growth conditions. Algae grown under high CO₂ conditions (5% CO₂ in air, v/v; high C_i cells) had a very low affinity for HCO₃^? at pH 7.0 and 8.2, whereas algae grown under low CO₂ conditions (0.03% CO₂ in air; low C_i cells) showed a high affinity for HCO₃^? at both pH values and were sensitive to Dextran-bound sulfonamide (DBS), an inhibitor of extracellular CA. The photosynthetic rate or HCO₄^? dependent O₂ evolution was always higher at pH 7.0 than at pH 8.2. Ethoxyzolamide (EZ), an inhibitor of total (extacellular plus intracellular) CA activity, strongly inhibited photosynthesis at both pH values. During adaptation from high to low CO₂ conditions CA activity increased in chloroplasts in a process dependent on the novo protein synthesis. Carbonic anhydrase activity was found in the supernatant and pellet fractions of chloroplast homogenates. The rate of photosynthesis of chloroplasts from low C_i cells was higher at pH 7.0 than at pH 8.2. The alkalinization of the growth medium, which took place only in the presence of C_i, was partially inhibited by DBS and completely by EZ. We suggest that in D. salina CO₂ is the general form of C_i transported across the plasma membrane and the chloroplast envelope and that bicarbonate enters the cell mainly, although not entirely, by an ‘indirect’ mechanism after dehydration to CO₂.     

Role of external carbonic anhydrase in light-dependent alkalization byFucus serratus L. andLaminaria saccharina (L.) Lamour. (Phaeophyta)

It has been proposed that many marine macroalgae are able to utilize HCO ₃ ^– for photosynthesis and growth, and that energy-dependent ion pumping is involved in this process. We have therefore studied the light-dependent alkalization of the surrounding medium by two species of marine macroscopic brown algae,Fucus serratus L. andLaminaria saccharina (L.) Lamour. with the aim of investigating the role of extracellular carbonic anhydrase (EC 4.2.1.1.) in the assimilation of inorganic carbon from the seawater medium. In particular, the influence of membrane-impermeable or slowly permeable carbonic-anhydrase inhibitors on the rate of alkalization of the seawater has been investigated. Inhibition of the alkalization rate occurred in both species at an alkaline pH (pH 8.0) but no inhibition was observed at an acidic pH (pH 6.0). The alkalization was found to be light-dependent and inhibited by 3-(3,4-dichlorophenyl)-1, 1-dimethylurea and, thus, correlated with photosynthesis. Alkalization by macroalgae has previously been shown to be proportional to inorganiccarbon uptake. We suggest that alkalization of the medium at alkaline pH in both of the species examined is mainly the consequence of an extracellular reaction. The reaction is catalyzed by extracellular carbonic anhydrase which converts HCO ₃ ^– to OH^– and CO₂; CO₂ is then taken up through the plasmalemma. However, we do not exclude the involvement of other mechanisms of inorganic-carbon uptake.Abbreviations AZ acetazolamide - CA carbonic anhydrase - CAext extracellular carbonic anhydrase - C_i inorganic carbon - DBS dextran-bound sulfonamide - DCMU 3-(3,4-dichloro-phenyl)-1,1-dimethylurea - PPFD photosynthetic photon flux density This study was carried out with financial support by SAREC (Swedish Agency for Research Cooperation with Developing Countries), Carl Trygger's Fund for Scientific Research (Sweden), SJFR (Swedish Council for Forestry and Agricultural Research) and CICYT (Spain). Z. Ramazanov is an invited professor of Ministerio de Educación y Ciencia, Spain.     

Carbonic anhydrase activity in leaves and its role in the first step of c(4) photosynthesis

In C₄ plants carbonic anhydrase catalyzes the critical first step of C₄ photosynthesis, the hydration of CO₂ to bicarbonate. The maximum activity of this enzyme in C₄ leaf extracts, measured by H⁺ production with saturating CO₂ and extrapolated to 25°C, was found to be 3,000 to 10,000 times the maximum photosynthesis rate for these leaves. Similar activities were found in C₃ leaf extracts. However, the calculated effective activity of this enzyme at in vivo CO₂ concentrations was apparently just sufficient to prevent the rate of conversion of CO₂ to HCO₃⁻ from limiting C₄ photosynthesis. This conclusion was supported by the mass spectrometric determination of leaf carbonic anhydrase activities.     

Active CO(2) Transport by the Green Alga Chlamydomonas reinhardtii

Mass spectrometric measurements of dissolved free ¹³CO₂ were used to monitor CO₂ uptake by air grown (low CO₂) cells and protoplasts from the green alga Chlamydomonas reinhardtii. In the presence of 50 micromolar dissolved inorganic carbon and light, protoplasts which had been washed free of external carbonic anhydrase reduced the ¹³CO₂ concentration in the medium to close to zero. Similar results were obtained with low CO₂ cells treated with 50 micromolar acetazolamide. Addition of carbonic anhydrase to protoplasts after the period of rapid CO₂ uptake revealed that the removal of CO₂ from the medium in the light was due to selective and active CO₂ transport rather than uptake of total dissolved inorganic carbon. In the light, low CO₂ cells and protoplasts incubated with carbonic anhydrase took up CO₂ at an apparently low rate which reflected the uptake of total dissolved inorganic carbon. No net CO₂ uptake occurred in the dark. Measurement of chlorophyll a fluorescence yield with low CO₂ cells and washed protoplasts showed that variable fluorescence was mainly influenced by energy quenching which was reciprocally related to photosynthetic activity with its highest value at the CO₂ compensation point. During the linear uptake of CO₂, low CO₂ cells and protoplasts incubated with carbonic anhydrase showed similar rates of net O₂ evolution (102 and 108 micromoles per milligram of chlorophyll per hour, respectively). The rate of net O₂ evolution (83 micromoles per milligram of chlorophyll per hour) with washed protoplasts was 20 to 30% lower during the period of rapid CO₂ uptake and decreased to a still lower value of 46 micromoles per milligram of chlorophyll per hour when most of the free CO₂ had been removed from the medium. The addition of carbonic anhydrase at this point resulted in more than a doubling of the rate of O₂ evolution. These results show low CO₂ cells of Chlamydomonas are able to transport both CO₂ and HCO₃⁻ but CO₂ is preferentially removed from the medium. The external carbonic anhydrase is important in the supply to the cells of free CO₂ from the dehydration of HCO₃⁻.     

Continuous Measurements of the Free Dissolved CO(2) Concentration during Photosynthesis of Marine Plants: Evidence for HCO(3) Use in Chondrus crispus

An experimental system consisting of a gas exchange column linked to an assimilation chamber has been developed to record continuously the free dissolved CO₂ concentration in seawater containing marine plants. From experiments performed on the red macroalga Chondrus crispus (Rhodophyta, Gigartinales), this measurement is in agreement with the free CO₂ concentration calculated from the resistance to CO₂ exchanges in a biphasic system (gas and liquid) as earlier reported. The response time of this apparatus is short enough to detect, in conditions of constant pH, a photosynthesis-caused gradient between free CO₂ and HCO₃⁻ pools which half-equilibrates in 25 seconds. Abolished by carbonic anhydrase, the magnitude of this gradient increases with decreasing time of seawater transit from the chamber to the column apparatus. But its maximum magnitude (0.35 micromolar CO₂) is negligible compared to the difference between air and free CO₂ (11.4 micromolar CO₂). This illustrates the extent of the physical limiting-step occurring at the air-water interface when inorganic carbon consumption in seawater is balanced by dissolving gaseous CO₂. The direction of this small free CO₂/HCO₃⁻ gradient indicates that HCO₃⁻ is consumed during photosynthesis.     

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.