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.     

Involvement of photorespiration and glycolate pathway in carbonic anhydrase induction and inorganic carbon concentration in Chlamydomonas reinhardtii

Interaction between induction of carbonic anhydrase (CA) activity, induction of inorganic carbon (C_i) concentrating mechanisms and the photorespiratory glycolate pathway has been studied in wild type 6145c and photorespiratory mutant 18–7F (low in phosphoglycolate phosphatase activity) cells of C. reinhardtii . Cell transfer from high CO₂ (5%, v/v) to low CO₂ (0.03%) provoked an increase of extracellular and total (extracellular plus intracellular) CA in both wild type and mutant cells. During adaptation to low CO₂ conditions, both strains excreted ammonium to the medium at a similar rate in the presence of l -methionine- d-l -sulfoximine (MSX), an inhibitor of glutamine synthetase (GS). MSX also provoked ammonium excretion by air adapted wild type and mutant cells, even though both strains had high levels of CA activity and of C_i concentrating activities.
GS increased in both strains after transfer from high to low CO₂ conditions. However, this increase was abolished by aminooxyacetate, an inhibitor of the glyoxylate-serine aminotransferase, and by glycolaldehyde, an inhibitor of triose phosphate to ribulose 1,5-bisphosphate conversion. CA synthesis did not occur in the presence of either aminooxyacetate or glycolaldehyde. Algae grown in high CO₂ in the presence of aminooxyacetate did not induce C_i concentrating mechanisms. Integration of these three processes, i.e., CA synthesis, C_i-concentration, and photorespiratory glycolate pathway is proposed in the framework of carbon metabolism of the alga.     

Carbonic anhydrase is induced prior to arylsulfatase under the simultaneous deprivation of inorganic carbon and sulfate in Chlamydomonas reinhardtii (Volvocales, Chlorophyta)

The activity of periplasmic arylsulfatase (Ars), which catalyzes the cleavage of sulfate from aromatic sulfur compounds, was detected in cells acclimated to the sulfate-deficient conditions in a unicellular green alga Chlamydomonas reinhardtii Dangeard, but not in Chlorella, Scenedesmus, Dunaliella and Porphyridium. Upon the transfer of cells to sulfate-deficient autotrophic media under high-CO₂ conditions, the induction of Ars was observed only in the light, but not in the light with dichlorophenyldimethylurea (DCMU) nor in the dark. However, Ars was induced in the light with DCMU or in the dark when acetate was present as an organic carbon source, but not citrate. Under similar high-CO₂ conditions, high-CO₂ requiring mutants of cia-3 and cia-5, whose photosynthetic activities are greatly limited under low CO₂, showed much lower level of Ars activities than wild type cells. Under Iow-CO₂ conditions the induction of Ars was greatly suppressed even in wild type and no induction was observed in both mutants. These results suggest that the stimulation of photosynthetic or respiratory carbon metabolism are necessary for the induction of Ars. In contrast, the induction of periplasmic carbonic anhydrase (CA) which was synthesized de novo specifically under CO₂-limited conditions was strongly suppressed by the addition of organic carbon sources, such as acetate and citrate. When cells are subjected to CO₂-limitation and sulfate-deficiency simultaneously, the induction of CA was initiated immediately, while that of Ars was initiated following the completion of CA induction with an about 4-h lag. When the concentration of CO₂ was suddenly lowered during the induction of Ars, the induction of Ars ceased quickly, and the induction of CA was initiated instead. From these results the induction of CA was suggested to have priority over that of Ars under the dual stress of CO₂, and sulfate-deprivation.     

The induction of the CO2 concentrating mechanism in a starch-less mutant of Chlamydomonas reinhardtii

In Chlamydomonas reinhardtii the formation of a starch sheath surrounding the pyrenoid is observed when cells grown under high CO₂ (5% CO₂ in air) are transferred to low CO₂ (0.03%) conditions. Formation of the starch sheath occurs coincidentally with induction of the CO₂ concentrating mechanism and with de novo synthesis of 5 polypeptides with molecular masses of 21, 36, 37, 42–44 kDa. We studied the effect of CO₂ concentrations on photosynthesis, ultrastructure and protein synthesis in Chlamydomonas reinhardtii cw-15 (wild phenotype for photosynthesis) and in the starch-less mutant BAFJ -6, with the aim to clarify the role of the pyrenoid starch sheath in the operation of the CO₂ concentrating mechanism and whether these low CO₂-inducible polypeptides are involved in the formation of starch sheath. When wild type and starch-less mutant cells were transferred from high to low CO₂, the CO₂ requirement for half-maximal rates of photosynthesis decreased from 40 μM to 2 μM CO₂. ³⁵SO₄^2- labeling analyses showed that the starch-less mutant induced the 5 low CO₂-inducible polypeptides. These observations suggest that the starch-less mutant was able to induce a fully active CO₂ concentrating mechanism. Since the starch-less mutant did not form a pyrenoid starch sheath, we suggest that the starch sheath is not involved in the operation of the CO₂ concentrating mechanism and that none of these 5 low CO₂-inducible proteins is involved in the formation of the starch sheath in Chlamydomonas .     

Effects of doubled atmospheric CO2 concentration on the growth and photosynthesis of Chlamydomonas reinhardtii (Volvocales, Chlorophyceae)

The freshwater microalga, Chlamydomonas reinhardtii Dangeard, was cultured under 350 and 700 ppmv CO₂ to determine the impact of doubled atmospheric CO₂ concentration on its growth and photosynthesis. No significant difference was observed in the specific growth rate, photosynthetic efficiency, maximal net photo‐synthetic rate and light‐saturating point between the low and high CO₂ cultures. Both the low‐ and high‐CO₂‐grown cells showed reduced light‐dependent O₂ evolution rate and photochemical efficiency (F_v/F_m) owing to photoinhibition when exposed to high photon flux density. However, high‐CO₂‐grown cells were less photoinhibited, and showed better recovery in dim light or darkness during the initial period of the recovery process.     

The CO2-concentrating mechanism is absent in the green alga Coccomyxa: a comparative study of photosynthetic CO2 and light responses of Coccomyxa, Chlamydomonas reinhardtii and barley protoplasts

Photosynthesis was characterized for the unicellular green alga Coccomyxa sp., grown at low inorganic carbon (C_i) concentrations, and compared with Chlamydomonas reinhardtii, which had been grown so that the CO₂ concentrating mechanism (CCM) was expressed, and with protoplasts isolated from the C₃ plant barley (Hordeum vulgare). Chlamydomonas had a significantly higher C_i-use efficiency of photosynthesis, with an initial slope of the C_i-response curve of 0.7 mol(gChl)⁻¹ h⁻¹ mmol C_im⁻³)⁻¹, as compared to 0.3 and 0.23 mol(gChl)⁻¹ h⁻¹ (mmol C_im⁻³)⁻¹ for Coccomyxa and barley, respectively. The affinity for C_i was also higher in Chlamydomonas, as the half maximum rate of photosynthesis [K_0.5 (C_i)] was reached at 0.18 mol m⁻³, as compared to 0.30 and 0.45 mol m⁻³ for Coccomyxa and barley, respectively. Ethoxyzolamide (EZ), an inhibitor of the enzyme carbonic anhydrase (CA) and the CCM, caused a 17-fold decrease in the initial slope of the photosynthetic Cj-response curve in Chlamydomonas, but only a 1.5- to two-fold decrease in Coccomyxa and barley. The photosynthetic light-response curve showed further similarities between barley and Coccomyxa. The rate of bending of the curve, described by the convexity parameter, was 0.99 (sharp bending) and 0.81–0.83 (gradual bending) for cells grown under low and high light, respectively. In contrast, the maximum convexity of Chlamydomonas was 0.85. The intrinsically lower convexity of Chlamydomonas is suggested to result from the diversion of electron transport from carbon fixation to the CCM. Taken together, these results suggest that Coccomyxa does not possess a CCM and due to this apparent lack of a CCM, we propose that Coccomyxa is a better cell model system for studying C₃ plant photosynthesis than many algae currently used.     

Impacts of Elevated CO2 Concentration on Biochemical Composition, Carbonic Anhydrase, and Nitrate Reductase Activity of Freshwater Green Algae

To investigate the biochemical response of freshwater green algae to elevated CO2 concentrations, Chlorella pyrenoidosa Chick and Chlamydomonas reinhardtii Dang cells were cultured at different CO2 concentrations within the range 3-186μmol/L and the biochemical composition, carbonic anhydrase (CA),and nitrate reductase activities of the cells were investigated. Chlorophylls (Chl), carotenoids, carbonhydrate,and protein contents were enhanced to varying extents with increasing CO2 concentration from 3-186μmol/L. The CO2 enrichment significantly increased the Chl a/Chl b ratio in ChloreUa pyrenoidosa, but not in Chlamydomonas reinhardtii. The CO2 concentration had significant effects on CA and nitrate reductase activity. Elevating CO2 concentration to 186μmol/L caused a decline in intracellular and extracellullar CA activity. Nitrate reductase activity, under either light or dark conditions, in C. reinhardtii and C. pyrenoidosa was also significantly decreased with CO2 enrichment. From this study, it can be concluded that CO2 enrichment can affect biochemical composition, CA, and nitrate reductase activity, and that the biochemical response was species dependent.     

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.     

Active transport of CO2 by three species of marine microalgae

The occurrence of an active CO₂ transport system and of carbonic anhydrase (CA) has been investigated by mass spectrometry in the marine, unicellular rhodophyte Porphyridium cruentum (S.F. Gray) Naegeli and two marine chlorophytes Nannochloris atomus Butcher and Nannochloris maculata Butcher. Illumination of darkened cells incubated with 100 μM H¹³CO₃^? caused a rapid initial drop, followed by a slower decline in the extracellular CO₂ concentration. Addition of bovine CA to the medium raised the CO₂ concentration by restoring the HCO₃^?–CO₂ equilibrium, indicating that cells were taking up CO₂ and were maintaining the CO₂ concentration in the medium below its equilibrium value during photosynthesis. Darkening the cell suspensions caused a rapid increase in the extracellular CO₂ concentration in all three species, indicating that the cells had accumulated an internal pool of unfixed inorganic carbon. CA activity was detected by monitoring the rate of exchange of ¹⁸O from ¹³C¹⁸O₂ into water. Exchange of ¹⁸O was rapid in darkened cell suspensions, but was not inhibited by 500 μM acetazolamide, a membrane‐impermeable inhibitor of CA, indicating that external CA activity was not present in any of these species. In all three species, the rate of exchange was completely inhibited by 500 μM ethoxyzolamide, a membrane‐permeable CA‐inhibitor, showing that an intracellular CA was present. These results demonstrate that the three species are capable of CO₂ uptake by active transport for use as a carbon source for photosynthesis.     

A Comparison of CO2 Uptake by the Green Algae Tetraedron minimum and Chlamydomonas monoica

Abstract: The ability of the green alga Tetraedron minimum to acquire inorganic carbon from its environment was investigated and compared with that of Chlamydomonas monoica. T. minimum showed a higher affinity for bicarbonate ions than C. monoica, regardless of whether it was grown at high or low CO₂ concentrations. Furthermore, T. minimum was distinguished by the fact that it maintained a large intracellular pool of inorganic carbon. These features may explain why this alga is able to proliferate in alkaline conditions.     

The requirement for external carbonic anhydrase in diatoms is influenced by the supply and demand for dissolved inorganic carbon

Photosynthesis by marine diatoms contributes significantly to the global carbon cycle. Due to the low concentration of CO₂ in seawater, many diatoms use extracellular carbonic anhydrase (eCA) to enhance the supply of CO₂ to the cell surface. While much research has investigated how the requirement for eCA is influenced by changes in CO₂ availability, little is known about how eCA contributes to CO₂ supply following changes in the demand for carbon. We therefore examined how changes in photosynthetic rate influence the requirement for eCA in three centric diatoms. Modeling of cell surface carbonate chemistry indicated that diffusive CO₂ supply to the cell surface was greatly reduced in large diatoms at higher photosynthetic rates. Laboratory experiments demonstrated a trend of an increasing requirement for eCA with increasing photosynthetic rate that was most pronounced in the larger species, supporting the findings of the cellular modeling. Microelectrode measurements of cell surface pH and O₂ demonstrated that individual cells exhibited an increased contribution of eCA to photosynthesis at higher irradiances. Our data demonstrate that changes in carbon demand strongly influence the requirement for eCA in diatoms. Cell size and photosynthetic rate will therefore be key determinants of the mode of dissolved inorganic carbon 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.     

Effect of CO2, CO2 and Diamox on photosynthesis and photorespiration in Chlamydomonas reinhardtii (green alga) and Anacystis nidulans (Cyanobacterium, blue-green alga)

Photorespiration by Chlamydomonas reinhardtii and Anacystis nidulans was measured as the oxygen inhibition of CO₂ uptake and the CO₂ compensation points. Net photosynthesis was oxygen dependent in Chlamydomonas grown in 5% CO₂, but CO₂ insensitive in cultures bubbled with air. Anacystis, even when cultured in 5% CO₂, exhibited an CO₂ insensitive net photosynthesis. The CO₂ compensation point of Chlamydomonas grown in cultures bubbled with air and Anacystis grown in 5% CO₂ enriched air, were reached shortly after the measurement was begun and the values were very low, less than 10 μl CO₂ 1^?1; while Chlamydomonas grown in 5% CO₂ enriched air for 4 days showed a high, but temporary CO₂ compensation point (60 μl CO₂ 1^?1). After a two hour adaptation in low CO₂, a stable, low CO₂ compensation point was reached. It seems that photorespiration can only be detected by the methods used in this study when the algae are cultured in high CO₂, but a mechanism exists which blocks photorespiration when the green algae are adapted to low CO₂ concentrations. When Chlamydomonas was treated with Diamox, an inhibitor of carbonic anhydrase, after cultivation in low CO₂ (air), the cells behaved as if they had been grown in high CO₂. They showed an oxygen sensitive net photosynthesis and a high CO₂ compensation point. This indicates that carbonic anhydrase plays an important role in the regulation of a measurable photorespiration in Chlamydomonas. The results are discussed in relation to previous observations of photorespiration measured by enzyme assay, metabolic products and gas exchange properties.     

CO2 is the main inorganic C species entering photosynthetically active leaf protoplasts of the freshwater macrophyte Ranunculus penicillatus ssp. pseudofluitans

Submerged aquatic macrophytes growing in water where free CO₂ is unavailable (above pH 8·2) must use mechanisms to supply external dissolved inorganic carbon in a form available to chloroplasts (CO₂). Active transport of HCO₃^– across the plasmalemma has not been proven to be widespread in aquatic macrophytes and catalytic conversion of HCO₃^– to CO₂ is the usual supply mechanism in submerged macrophytes. The interaction of leaf form and function in this respect was investigated in the linear, submerged leaves of Ranunculus penicillatus (Dumort.) Bab ssp. pseudofluitans (Syme) S.Webster. Viable protoplasts were isolated using a mixture of cell wall degrading enzymes optimized for this species. Protoplast viabilities greater than 80% after 5 h of isolation were achieved. Photosynthetic rates of isolated protoplasts were comparable with that of intact plant tissue. Results of carbon isotopic disequilibrium experiments showed that CO₂ was the preferred species of dissolved inorganic carbon for photosynthesis by protoplasts and that HCO₃^– which predominates in the plant’s natural environment mainly contributes by supplying CO₂ outside the cells.     

Quantification of the rate of CO2 formation in the periplasmic space of microalgae during photosynthesis. A comparison of whole-cell rate constants for CO2 and HCO3– uptake among three species of the green alga Chlorella

As previously described, the absolute rate of photosynthesis due to a limited concentration of dissolved inorganic carbon at alkaline pH, where the rate of CO₂ formation is strictly limited, plotted as a function of chlorophyll (Chl) concentration, will take the form of a rectangular hyperbola combined with a linear rate directly proportional to [Chl], which are, respectively, due to the contribution of CO₂ and HCO₃^– to photosynthesis. This model represents that the mathematical asymptote of absolute rate of photosynthesis versus cell density is described by the whole-cell rate constant for HCO₃^– uptake and the maximum rate of CO₂ formation in the extracellular space. This means that any trace modification of the CO₂ formation rate outside the cell will alter the photosynthetic rate and should be detectable experimentally. In air-grown Chlorella ellipsoidea and C. kessleri and in high CO₂-grown C. saccharophila, the graph of the absolute rate of photosynthesis against [Chl] clearly followed the mathematical model described above and the actual CO₂ formation rates outside the cells were not significantly different from the calculated rates. It also indicated that the whole-cell rate constants for CO₂ and HCO₃^– uptake in air-grown C. ellipsoidea and C. saccharophila were similar at ≈ 300 and 2·0 mm³μg^–1 Chl min^–1, respectively, whereas those in air-grown C. kessleri were ≈ 550 and 15 mm³μg^–1 Chl min^–1. These results indicate that no acidification of the periplasmic space occurs, and there is no trace activity of external carbonic anhydrase in these microalgae.     

The regulation of photosynthetic rate and activation of extracellular carbonic anhydrase under CO2-limiting conditions in the marine diatom Skeletonema costatum

In the marine diatom Skeletonema costatum , carbonic anhydrase activity exterior to the plasma membrane (CA_ext) was detected only when the available CO₂ concentration was less than 5·0 mmol m^–3, this activity being unaffected by the total dissolved inorganic carbon concentration. The inhibition of CA_ext by dextran bound sulphonamide (DBS) demonstrated the key role of this enzyme in maintaining photosynthetic rate under CO₂-limited conditions. Treatment with trypsin followed by affinity chromatography on p-aminomethylbenzene-sulphamide agarose and subsequent SDS-PAGE analysis revealed a polypeptide from carbon-replete cells of identical molecular mass to the CA_ext released by trypsin from CO₂-limited cells. Redox activity in the plasma membrane of intact cells was measured by following the light-dependent reduction of ferricyanide or NADP, the greatest activity being shown by CO₂-limited cells. Overall the results suggest that high rates of redox activity under conditions of CO₂-limitation were required for the activation of CA_ext.     

Evaporation and carbonic anhydrase activity recorded in oxygen isotope signatures of net CO2 fluxes from a Mediterranean soil

The oxygen stable isotope composition (δ¹⁸O) of CO₂ is a valuable tool for studying the gas exchange between terrestrial ecosystems and the atmosphere. In the soil, it records the isotopic signal of water pools subjected to precipitation and evaporation events. The δ¹⁸O of the surface soil net CO₂ flux is dominated by the physical processes of diffusion of CO₂ into and out of the soil and the chemical reactions during CO₂–H₂O equilibration. Catalytic reactions by the enzyme carbonic anhydrase, reducing CO₂ hydration times, have been proposed recently to explain field observations of the δ¹⁸O signatures of net soil CO₂ fluxes. How important these catalytic reactions are for accurately predicting large‐scale biosphere fluxes and partitioning net ecosystem fluxes is currently uncertain because of the lack of field data. In this study, we determined the δ¹⁸O signatures of net soil CO₂ fluxes from soil chamber measurements in a Mediterranean forest. Over the 3 days of measurements, the observed δ¹⁸O signatures of net soil CO₂ fluxes became progressively enriched with a well‐characterized diurnal cycle. Model simulations indicated that the δ¹⁸O signatures recorded the interplay of two effects: (1) progressive enrichment of water in the upper soil by evaporation, and (2) catalytic acceleration of the isotopic exchange between CO₂ and soil water, amplifying the contributions of ‘atmospheric invasion’ to net signatures. We conclude that there is a need for better understanding of the role of enzymatic reactions, and hence soil biology, in determining the contributions of soil fluxes to oxygen isotope signals in atmospheric CO₂.     

The molecular and biochemical analyses of CO2-concentrating mechanisms in cyanobacteria and microalgae

Abstract. The supply of dissolved inorganic carbon for photosynthesis in the aquatic environment is much more variable than that experienced by terrestrial plants. In response to this variability, cyanobacteria and many species of microalgae acclimate to rapid changes in the availability of dissolved inorganic carbon by the induction of high affinity/high capacity CO₂-concentrating systems (CCMs). Biochemical and molecular analyses of the acclimation response have recently identified several components that are required for efficient operation of the CCMs and CO₂ assimilation. This has been accomplished using in vivo labelling studies, and characterization of high inorganic carbon (C_i) requiring cyanobacterial and algal mutants. The identification and regulation of expression of polypeptides synthesized in response to limiting C_i concentrations, and the proposed role of the carboxysome and the pyrenoid in the functioning of the CCMs are examined.     

Regulation of the induction of bicarbonate uptake by dissolved CO2 in the marine diatom, Phaeodactylum tricornutum

Physiological properties of photosynthesis were determined in the marine diatom, Phaeodactylum tricornutum UTEX640, during acclimation from 5% CO₂ to air and related to H₂CO₃ dissociation kinetics and equilibria in artificial seawater. The concentration of dissolved inorganic carbon at half maximum rate of photosynthesis (K_0·5[DIC]) value in high CO₂‐grown cells was 1009 mmol m ^{? 3} but was reduced three‐fold by the addition of bovine carbonic anhydrase (CA), whereas in air‐grown cells K_0·5[DIC] was 71 mmol m ^{? 3}, irrespective of the presence of CA. The maximum rate of photosynthesis (P_max) values varied between 300 and 500 μ mol O₂ mg Chl ^{? 1} h ^{? 1} regardless of growth pCO₂. Bicarbonate dehydration kinetics in artificial seawater were re‐examined to evaluate the direct HCO₃ ^? uptake as a substrate for photosynthesis. The uncatalysed CO₂ formation rate in artificial seawater of 31·65°/_oo of salinity at pH 8·2 and 25 °C was found to be 0·6 mmol m ^{? 3} min ^{? 1} at 100 mmol m ^{? 3} DIC, which is 53·5 and 7·3 times slower than the rates of photosynthesis exhibited in air‐ and high CO₂‐grown cells, respectively. These data indicate that even high CO₂‐grown cells of P. tricornutum can take up both CO₂ and HCO₃ ^? as substrates for photosynthesis and HCO₃ ^? use improves dramatically when the cells are grown in air. Detailed time courses were obtained of changes in affinity for DIC during the acclimation of high CO₂‐grown cells to air. The development of high‐affinity photosynthesis started after a 2–5 h lag period, followed by a steady increase over the next 15 h. This acclimation time course is the slowest to be described so far. High CO₂‐grown cells were transferred to controlled DIC conditions, at which the concentrations of each DIC species could be defined, and were allowed to acclimate for more than 36 h. The K_0·5[DIC] values in acclimated cells appeared to be correlated only with [CO_2(aq)] in the medium but not to HCO₃ ^? , CO₃^{2 ?} , total [DIC] or the pH of the medium and indicate that the critical signal regulating the affinity of cells for DIC in the marine diatom, P. tricornutum, is [CO_2(aq)] in the medium.