Carbonic Anhydrase-Deficient Mutant of Chlamydomonas reinhardii Requires Elevated Carbon Dioxide Concentration for Photoautotrophic Growth

A mendelian mutant of the unicellular green alga Chlamydomonas reinhardii has been isolated which is deficient in carbonic anhydrase (EC 4.2.1.1) activity. This mutant strain, designated ca-1-12-1C (gene locus ca-1), was selected on the basis of a high CO₂ requirement for photoautotrophic growth. Photosynthesis by the mutant at atmospheric CO₂ concentration was very much reduced compared to wild type and, unlike wild type, was strongly inhibited by O₂. In contrast to a CO₂ compensation concentration of near zero in wild type at all O₂ concentrations examined, the mutant exhibited a high, O₂-stimulated CO₂ compensation concentration. Evidence of photorespiratory activity in the mutant but not in wild type was obtained from the analysis of photosynthetic products in the presence of ¹⁴CO₂. At air levels of CO₂ and O₂, the mutant synthesized large amounts of glycolate, while little glycolate was synthesized by wild type under identical conditions. Both mutant and wild type strains formed only small amounts of glycolate at saturating CO₂ concentration. At ambient CO₂, wild type accumulated inorganic carbon to a concentration several-fold higher than that in the suspension medium. The mutant cells accumulated inorganic carbon internally to a concentration 6-fold greater than found in wild type, yet photosynthesis was CO₂ limited. The mutant phenotype was mimicked by wild type cells treated with ethoxyzolamide, an inhibitor of carbonic anhydrase activity. These observations indicate a requirement for carbonic anhydrase-catalyzed dehydration of bicarbonate in maintaining high internal CO₂ concentrations and high photosynthesis rates. Thus, in wild type cells, carbonic anhydrase rapidly converts the bicarbonate taken up to CO₂, creating a high internal CO₂ concentration which stimulates photosynthesis and suppresses photorespiration. In mutant cells, bicarbonate is taken up rapidly but, because of a carbonic anhydrase deficiency, is not dehydrated at a rate sufficiently rapid to maintain a high internal CO₂ concentration.     

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.     

Evidence That an Internal Carbonic Anhydrase Is Present in 5% CO(2)-Grown and Air-Grown Chlamydomonas

Inorganic carbon (C_i) uptake was measured in wild-type cells of Chlamydomonas reinhardtii, and in cia-3, a mutant strain of C. reinhardtii that cannot grow with air levels of CO₂. Both air-grown cells, that have a CO₂ concentrating system, and 5% CO₂-grown cells that do not have this system, were used. When the external pH was 5.1 or 7.3, air-grown, wild-type cells accumulated inorganic carbon (C_i) and this accumulation was enhanced when the permeant carbonic anhydrase inhibitor, ethoxyzolamide, was added. When the external pH was 5.1, 5% CO₂-grown cells also accumulated some C_i, although not as much as air-grown cells and this accumulation was stimulated by the addition of ethoxyzolamide. At the same time, ethoxyzolamide inhibited CO₂ fixation by high CO₂-grown, wild-type cells at both pH 5.1 and 7.3. These observations imply that 5% CO₂-grown, wild-type cells, have a physiologically important internal carbonic anhydrase, although the major carbonic anhydrase located in the periplasmic space is only present in air-grown cells. Inorganic carbon uptake by cia-3 cells supported this conclusion. This mutant strain, which is thought to lack an internal carbonic anhydrase, was unaffected by ethoxyzolamide at pH 5.1. Other physiological characteristics of cia-3 resemble those of wild-type cells that have been treated with ethoxyzolamide. It is concluded that an internal carbonic anhydrase is under different regulatory control than the periplasmic carbonic anhydrase.     

Identification of Extracellular Carbonic Anhydrase of Chlamydomonas reinhardtii

We have examined the induction of carbonic anhydrase activity in Chlamydomonas reinhardtii and have identified the polypeptide responsible for this activity. This polypeptide was not synthesized when the alga was grown photoautotrophically on 5% CO₂, but its synthesis was induced under low concentrations of CO₂ (air levels of CO₂). In CW-15, a mutant of C. reinhardtii which lacks a cell wall, between 80 and 90% of the carbonic anhydrase activity of air-adapted cells was present in the growth medium. Furthermore, between 80 and 90% of the carbonic anhydrase is released if wild type cells are treated with autolysin, a hydrolytic enzyme responsible for cell wall degradation during mating of C. reinhardtii. These data extend the work of Kimpel, Togasaki, Miyachi (1983 Plant Cell Physiol 24: 255-259) and indicate that the bulk of the carbonic anhydrase is located either in the periplasmic space or is loosely bound to the algal cell wall. The polypeptide associated with carbonic anhydrase activity has a molecular weight of approximately 37,000. Several lines of evidence indicate that this polypeptide is responsible for carbonic anhydrase activity: (a) it appears following the transfer of C. reinhardtii from growth on 5% CO₂ to growth on air levels of CO₂, (b) it is located in the periplasmic space or associated with the cell wall, like the bulk of the carbonic anhydrase activity, (c) it binds dansylamide, an inhibitor of the enzyme which fluoresces upon illumination with ultraviolet light, (d) antibodies which inhibit carbonic anhydrase activity only cross-react with this 37,000 dalton species.     

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.

     

Nutrient availability affects the response of the calcifying chlorophyte Halimeda opuntia (L.) J.V. Lamouroux to low pH

Atmospheric carbon dioxide emissions cause a decrease in the pH and aragonite saturation state of surface ocean water. As a result, calcifying organisms are expected to suffer under future ocean conditions, but their physiological responses may depend on their nutrient status. Because many coral reefs experience high inorganic nutrient loads or seasonal changes in nutrient availability, reef organisms in localized areas will have to cope with elevated carbon dioxide and changes in inorganic nutrients. Halimeda opuntia is a dominant calcifying primary producer on coral reefs that contributes to coral reef accretion. Therefore, we investigated the carbon and nutrient balance of H. opuntia exposed to elevated carbon dioxide and inorganic nutrients. We measured tissue nitrogen, phosphorus and carbon content as well as the activity of enzymes involved in inorganic carbon uptake and nitrogen assimilation (external carbonic anhydrase and nitrate reductase, respectively). Inorganic carbon content was lower in algae exposed to high CO₂, but calcification rates were not significantly affected by CO₂ or inorganic nutrients. Organic carbon was positively correlated to external carbonic anhydrase activity, while inorganic carbon showed the opposite correlation. Carbon dioxide had a significant effect on tissue nitrogen and organic carbon content, while inorganic nutrients affected tissue phosphorus and N:P ratios. Nitrate reductase activity was highest in algae grown under elevated CO₂ and inorganic nutrient conditions and lowest when phosphate was limiting. In general, we found that enzymatic responses were strongly influenced by nutrient availability, indicating its important role in dictating the local responses of the calcifying primary producer H. opuntia to ocean acidification.     

Genetic and physiological analysis of the CO2-concentrating system of Chlamydomonas reinhardii

When grown photoautotrophically at air levels of CO₂, Chlamydomonas reinhardii possesses a system involving active transport of inorganic carbon which increases the intracellular CO₂ concentration considerably above ambient, thereby stimulating photosynthetic CO₂ assimilation. In previous investigations, two mutant strains of this unicellular green alga deficient in some component of this CO₂-concentrating system were recovered as strains requiring high levels of CO₂ to support photoautotrophic growth. One of the mutants, ca-1-12-1C, is a leaky (nonstringent) CO₂-requiring strain deficient in carbonic anhydrase (EC 4.2.1.1) activity, while the other, pmp-1-16-5K, is a stringent CO₂-requiring strain deficient in inorganic carbon transport. In the present study a double mutant (ca pmp) was constructed to investigate the physiological and biochemical interaction of the two mutations. The two mutations are unlinked and inherited in a Mendelian fashion. The double mutant was found to have a leaky CO₂-requiring phenotype, indicating that the mutation ca-1 overcomes the stringent CO₂-requirement conferred by the mutation pmp-1. Several physiological characteristics of the double mutant were very similar to the carbonic-anhydrase-deficient mutant, including high CO₂ compensation concentration, photosynthetic CO₂ response curve, and deficiency of carbonic-anhydrase activity. However, the labeling pattern of metabolites during photosynthesis in ¹⁴CO₂ was more like that of the bicarbonatetransport-deficient mutant, and accumulation of internal inorganic carbon was intermediate between that of the two original mutants. These data indicate a previously unsuspected complexity in the Chlamydomonas CO₂-concentrating system.     

Carboxysomal carbonic anhydrases: Structure and role in microbial CO2 fixation

Cyanobacteria and some chemoautotrophic bacteria are able to grow in environments with limiting CO₂ concentrations by employing a CO₂-concentrating mechanism (CCM) that allows them to accumulate inorganic carbon in their cytoplasm to concentrations several orders of magnitude higher than that on the outside. The final step of this process takes place in polyhedral protein microcompartments known as carboxysomes, which contain the majority of the CO₂-fixing enzyme, RubisCO. The efficiency of CO₂ fixation by the sequestered RubisCO is enhanced by co-localization with a specialized carbonic anhydrase that catalyzes dehydration of the cytoplasmic bicarbonate and ensures saturation of RubisCO with its substrate, CO₂. There are two genetically distinct carboxysome types that differ in their protein composition and in the carbonic anhydrase(s) they employ. Here we review the existing information concerning the genomics, structure and enzymology of these uniquely adapted carbonic anhydrases, which are of fundamental importance in the global carbon cycle.     

Mass Spectrometric Measurement of Intracellular Carbonic Anhydrase Activity in High and Low C(i) Cells of Chlamydomonas: Studies Using O Exchange with C/O Labeled Bicarbonate

By measuring ¹⁸O exchange from doubly labeled CO₂ (¹³C¹⁸O¹⁸O), intracellular carbonic anhydrase activity was studied with protoplasts and chloroplasts isolated from Chlamydomonas reinhardtii grown either on air (low inorganic carbon [C_i]) or air enriched with 5% CO₂ (high C_i). Intact low C_i protoplasts had a 10-fold higher carbonic anhydrase activity than did high C_i protoplasts. Application of dextran-bound inhibitor and quaternary ammonium sulfanilamide, both known as membrane impermeable inhibitors of carbonic anhydrase, had no influence on the catalysis of ¹⁸O exchange, indicating that cross-contamination with extracellular carbonic anhydrase was not responsible for the observed activity. This intracellular in vivo activity from protoplasts was inhibited by acetazolamide and ethoxyzolamide. Intracellular carbonic anhydrase activity was partly associated with intact chloroplasts isolated from high and low C_i cells, and the latter had a sixfold greater rate of catalysis. The presence of dextran-bound inhibitor had no effect on chloroplast-associated carbonic anhydrase, whereas 150 micromolar ethoxyzolamide caused a 61 to 67% inhibition of activity. These results indicate that chloroplastic carbonic anhydrase was located within the plastid and that it was relatively insensitive to ethoxyzolamide. Carbonic anhydrase activity in crude homogenates of protoplasts and chloroplasts was about six times higher in the low C_i than in high C_i preparations. Further separation into soluble and insoluble fractions together with inhibitor studies revealed that there are at least two different forms of intracellular carbonic anhydrase. One enzyme, which was rather insoluble and relatively insensitive to ethoxyzolamide, is likely an intrachloroplastic carbonic anhydrase. The second carbonic anhydrase, which was soluble and sensitive to ethoxyzolamide, is most probably located in an extrachloroplastic compartment.     

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⁻.     

Endopolyploidy in Chlorella

A mutant of Dunaliella tertiolecta produced by treatment with methyl nitrosoguanidine and designated HL25/8, grew more slowly than the parent strain under all experimental conditions and was conspicuously less tolerant of NaCl. Total photosynthetic activity (C-fixation and O₂ evolution) was less in HL25/8 than in the parent strain and was affected differently by [NaCl] in the two strains. Various growth characteristics indicated that the mutant had a greater need than the parent strain for CO₂ as distinct from HCO ₃ ^– as a source of carbon. Gaseous CO₂ extended the range of salt tolerance of the mutant. For example, HL25/8 could not sustain growth at 1.02 M NaCl in a conventional buffered medium containing bicarbonate as the sole carbon source but could do so if the medium were sparged with a CO₂/air mixture. The mutant strain has a lower activity of carbonic anhydrase on the cell surface than the parent D. tertiolecta. Moreover, the two strains differ sharply in the responses of their surface carbonic anhydrase activity to salinity of the growth medium. Increasing sodium chloride concentration above 0.17 M raised activity of the enzyme in the parent strain but decreased it in HL25/8. We conclude that the low activity of carbonic anhydrase and its response to salinity can largely, but perhaps not fully, explain the diminished salt tolerance of the mutant. A plate counting method applicable to Dunaliella is described.     

CO2 exchange characteristics during dark-light transitions in wild-type and mutant Chlamydomonas reinhardii cells

A burst of net CO₂ uptake was observed during the first 3–4 min after the onset of illumination in both wild-type Chlamydomonas reinhardii in which carbonic anhydrase was chemically inhibited with ethoxyzolamide and in a mutant of C. reinhardii (ca-1-12-1C) deficient in carbonic anhydrase activity. The burst was followed by a rapid decrease in the CO₂ uptake rate so that net evolution often occurred. After a 2–3 min period of CO₂ evolution, net CO₂ uptake again increased and ultimately reached a steady-state, positive rate. From [¹⁴CO₂]-tracer studies it was determined that CO₂ fixation proceeded at a nearly linear rate throughout the period of illumination. Thus, prior to reaching a steady state, there was a rapid accumulation of inorganic carbon inside the cells which apparently reached a supercritical concentration and the excess was excreted, causing a subsequent efflux of CO₂. A post illumination burst of net CO₂ efflux was also observed in ethoxyzolamide-inhibited wild type and ca-1 mutant cells, but not in the unihibited wild type. [¹⁴CO₂]-tracer experiments revealed that this burst was the result of a collapse of a large internal inorganic carbon pool at the onset of darkness rather than a photorespiratory post-illumination burst. These results indicate that upon illumination, chemical or genetic inhibition of carbonic anhydrase initially causes an accumulation of excess inroganic carbon in C. reinhardii cells, and that unknown regulatory mechanisms correct for this imbalance by first excreting the excess inorganic carbon and then, after several dampened oscillations, achieving an equilibrium between bicarbonate uptake, bicarbonate dehydration, and CO₂ fixation.     

A role for mitochondrial carbonic anhydrase in limiting CO2 leakage from low CO2-grown cells of Chlamydomonas reinhardtii

A model is presented which quantifies a possible role for the carbonic anhydrase in the mitochondrial matrix of Chlamydomonas reinhardtii which incorporates the observation that the expression of this enzyme is increased under growth conditions in which the expression of the carbon dioxide-concentrating mechanism is increased. It is assumed that the inorganic carbon enters the cytosol from the medium, and leaves the cytosol to the plastids, as HCO₃⁻ and that there is negligible carbonic anhydrase activity in the cytosol. The role of the mitochondrial carbonic anhydrase is suggested to be the conversion to HCO₃^– of the CO₂ produced in the mitochondria in the light from tricarboxylic acid cycle activity and from decarboxylation of glycine in any photorespiratory carbon oxidation cycle activity which is not suppressed by the carbon concentrating mechanism. If there is a HCO₃⁻ channel in the inner mitochondrial membrane then almost all of the inorganic carbon leaves the mitochondria as HCO₃⁻, thus limiting the potential for CO₂ leakage through the plasmalemma. This mechanism could increase inorganic C supply to ribulose bisphosphate carboxylase-oxygenase by some 10% at the energetic expense of less than 1% of the total ATP generation by plastids plus mitochondria.     

Dissolved inorganic carbon concentration mechanism in Chlamydomonas moewusii

The dissolved inorganic carbon concentrating mechanism(s) of Chlamydomonas moewusii CC 55 was compared with C. reinhardtii strain 137. C. moewusii is similar to C. reinhardtii with respect to maximal rates of photosynthetic oxygen evolution, CO₂ fixation, respiration, and the ability to efficiently concentrate inorganic carbon. C. moewusii has a low, but measurable amount of external carbonic anhydrase (CA) that was not inhibited by acetazolamide (AZ), an inhibitor of periplasmic carbonic anhydrase (pCA) in C. reinhardtii. The K_0.5(CO₂) for air-grown C. moewusii is about 1 μM and the algal cells accumulated dissolved inorganic carbon (DIC) to a level of about 1 mM in 60 s. AZ did not inhibit CO₂ fixation and the DIC accumulation by air-grown cells of C. moewusii. The K_0.5(CO₂) for both species remains constant from pH 6.5 to 9.5 while K_0.5(HCO₃^-) increased logarithmically, which indicates that CO₂ is the apparent inorganic carbon species that enters the cells in both algae. Antiserum prepared against the 37 kDa peptide of pCA from C. reinhardtii was immunoreactive with polypeptides of 26, 28, and 32 kDa in C. moewusii. The periplasmic carbonic anhydrase (pCA) activity is a part of the dissolved inorganic carbon concentrating mechanism in C. reinhardtii, but C  moewusii accomplished inorganic carbon accumulation without an AZ-sensitive pCA.     

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.     

Correlation between Carbonic Anhydrase Activity and Inorganic Carbon Internal Pool in Strain Synechocystis PCC 6174

Existence of an internal carbonic anhydrase was demonstrated in the cyanobacterium Synechocystis PCC 6714. The enzyme, present at a low specific activity, was inducible by limitation in inorganic carbon and inhibited both in vivo and in vitro by acetazolamide. The internal inorganic carbon pool as determined by mass spectrometry, was similarly modulated by the actual inorganic carbon growth regime; its building up was also sensitive to acetazolamide. A possible role of carbonic anhydrase in inorganic carbon metabolism regulation through the control of the dimension and nature of the inorganic carbon pool is discussed.     

Role of Photosynthetic Reactions in the Activity of Carbonic Anhydrase in Synechococcus sp. (UTEX 2380) in the Light : Inhibitor Studies Using the O-Exchange in C/O-Labeled Bicarbonate

The role of the photosystems in the exchange of ¹⁸O between species of inorganic carbon and water was studied in suspensions of the cyanobacterium Synechococcus sp. (UTEX 2380) using membrane-inlet mass spectrometry. This ¹⁸O exchange is caused by the hydration-dehydration cycle of CO₂ and is catalyzed by carbonic anhydrase. We observed the complex ¹⁸O exchange kinetics including dark-light-dark transients in suspensions of whole cells and found these to be identical to the ¹⁸O exchange kinetics of physiologically fully active spheroplast preparations. There was no enhancement effect of inorganic nitrogen on inorganic carbon accumulation. Membrane preparations exhibited no uptake of inorganic carbon and very little carbonic anhydrase activity, although these membranes were photosynthetically fully competent. DCMU, the inhibitor of photosystem II, eliminated almost entirely the ¹⁸O exchange activity of whole cells in the light. But this effect of DCMU could be reversed by addition of the electron donor couple 3,6-diaminodurene/ascorbate, suggesting the involvement of photosystem I in the events leading to ¹⁸O exchange. Iodoacetamide, an inhibitor of CO₂ fixation, enhanced the ¹⁸O exchange in whole cell suspensions and inhibited neither the uptake of inorganic carbon nor the dehydration of bicarbonate in the light. The proton carrier carbonylcyanide m-chlorophenylhydrazone and the inhibitors diethylstilbestrol and N,N′ -dicyclohexyl carbodiimide affecting the membrane potential, totally abolished ¹⁸O exchange in the light. From ¹⁸ O-labeled inorganic carbon experiments we conclude that one of the roles of photosystem I is to provide the active uptake of inorganic carbon into the cells, where carbonic anhydrase catalyzes the interconversion between CO₂ and HCO₃⁻ resulting in the ¹⁸O exchange from inorganic carbon to water.     

Identification of Intracellular Carbonic Anhydrase in Chlamydomonas reinhardtii which Is Distinct from the Periplasmic Form of the Enzyme

A physiologically significant level of intracellular carbonic anhydrase has been identified in Chlamydomonas reinhardtii after lysis of the cell wall-less mutant, cw15, and two intracellular polypeptides have been identified which bind to anti-carbonic anhydrase antisera. The susceptibility of the intracellular activity to sulfonamide carbonic anhydrase inhibitors is more than three orders-of-magnitude less than that of the periplasmic enzyme, indicating that the intracellular activity was distinct from the periplasmic from of the enzyme. When electrophoretically separated cell extracts or chloroplast stromal fractions were probed with either anti-C. reinhardtii periplasmic carbonic anhydrase antiserum or anti-spinach carbonic anhydrase antiserum, immunoreactive polypeptides of 45 kilodaltons and 110 kilodaltons were observed with both antisera. The strongly immunoreactive 37 kilodalton polypeptide due to the periplasmic carbonic anhydrase was also observed in lysed cells, but neither the 37 kilodalton nor the 110 kilodalton polypeptides were present in the chloroplast stromal fraction. These studies have identified intracellular carbonic anhydrase activity, and putative intracellular carbonic anhydrase polypeptides in Chlamydomonas reinhardtii represented by a 45 kilodalton polypeptide in the chloroplast and a 110 kilodalton form probably in the cytoplasm, which may be associated with an intracellular inorganic carbon concentrating system.     

Acclimation to High CO(2) in Bean : Carbonic Anhydrase and Ribulose Bisphosphate Carboxylase

Young bean plants (Phaseolus vulgaris L. cv Seafarer) grew faster in air enriched with CO₂ (1200 microliters per liter) than in ambient CO₂ (330 microliters per liter). However, by 7 days when increases in overall growth (dry weight, leaf area) were visible, there was a significant decline (about 25%) in the leaf mineral content (N, P, K, Ca, Mg) and a drop in the activity of two enzymes of carbon fixation, carbonic anhydrase and ribulose 1,5-bisphosphate (RuBP) carboxylase under high CO₂. Although the activity of neither enzyme was altered in young, expanding leaves during the acclimation period, in mature leaves the activity of carbonic anhydrase was reduced 95% compared with a decline of 50% in ambient CO₂. The drop in RuBP carboxylase was less extreme with 40% of the initial activity retained in the high CO₂ compared with 50% in the ambient atmosphere. While CO₂ enrichment might alter the flow of carbon into the glycolate pathway by modifying the activities of carbonic anhydrase or RuBP carboxylase, there is no early change in the ability of photosynthetic tissue to oxidize glycolate to CO₂.     

Regulation of carbonic-anhydrase activity,inorganic-carbon uptake and photosynthetic biomass yield inChlamydomonas reinhardtii

The regulation of carbonic anhydrase by environmental conditions was determined forChlamydomonas reinhardtii. The depression of carbonic anhydrase in air-grown cells was pH-dependent. Growth of cells on air at acid pH, corresponding to 10 m CO₂ in solution, resulted in complete repression of carbonic-anhydrase activity. At pH 6.9, increasing the CO₂ concentration to 0.15% (v/v) in the gas phase, corresponding to 11 M in solution, was sufficient to completely repress carbonic-anhydrase activity. Photosynthesis and intracellular inorganic carbon were measured in air-grown and high-CO₂-grown cells using a silicone-oil centrifugation technique. With carbonic anhydrase repressed cells limited inorganic-carbon accumulation resulted from non-specific binding of CO₂. With air-grown cells, inorganic-carbon uptake at acid pH, i.e. 5.5, was linear up to 0.5 mM external inorganic-carbon concentration whereas at alkaline pH, i.e. 7.5, the accumulation ratio decreased with increase in external inorganic-carbon concentration. It is suggested that in air-grown cells at acid pH, CO₂ is the inorganic carbon species that crosses the plasmalemma. The conversion of CO₂ to HCO ₃ ^- by carbonic anhydrase in the cytosol results in inorganic-carbon accumulation and maintains the diffusion gradient for carbon dioxide across the cell boundary. However, this mechanism will not account for energy-dependent accumulation of inorganic carbon when there is little difference in pH between the exterior and cytosol.