Inhibition by cupric ions of the hydration of CO2 catalyzed by carbonic anhydrase II

The inhibition by cupric ions of the hydration of CO₂ catalyzed by carbonic anhydrase II is interesting because of the results of Tuet al. obtained at chemical equilibrium, indicating that Cu²⁺ inhibits specifically a proton transfer in the catalytic pathway. We have measured this inhibition at steady state, using stopped-flow methods. The inhibition by Cu²⁺ of the hydration of CO₂ catalyzed by carbonic anhydrase II had aK _I near 1×10^?6 M atpH 7.0 and gave inhibition that is noncompetitive atpH 6.0 and mixed, but close to uncompetitive, atpH 6.8. ThepH dependence of this binding is consistent with a binding site for Cu²⁺ on the enzyme with apK _a near 7. The binding interaction between Cu²⁺ and the fluorescent inhibitor 5-dimethylaminonaphthalene-l-sulfonamide on carbonic anhydrase II was noncompetitive, indicating that the binding site for Cu²⁺ is distinct from the coordination sphere of zinc in which the actual interconversion of CO₂ and HCO ₃ ^? and the binding of sulfonamides takes place.     

Inhibition by cupric ions of the hydration of CO2 catalyzed by carbonic anhydrase II

The inhibition by cupric ions of the hydration of CO₂ catalyzed by carbonic anhydrase II is interesting because of the results of Tuet al. obtained at chemical equilibrium, indicating that Cu²⁺ inhibits specifically a proton transfer in the catalytic pathway. We have measured this inhibition at steady state, using stopped-flow methods. The inhibition by Cu²⁺ of the hydration of CO₂ catalyzed by carbonic anhydrase II had aK _I near 1×10^–6 M atpH 7.0 and gave inhibition that is noncompetitive atpH 6.0 and mixed, but close to uncompetitive, atpH 6.8. ThepH dependence of this binding is consistent with a binding site for Cu²⁺ on the enzyme with apK _a near 7. The binding interaction between Cu²⁺ and the fluorescent inhibitor 5-dimethylaminonaphthalene-l-sulfonamide on carbonic anhydrase II was noncompetitive, indicating that the binding site for Cu²⁺ is distinct from the coordination sphere of zinc in which the actual interconversion of CO₂ and HCO ₃ ^– and the binding of sulfonamides takes place.     

Dioxygen,an unexpected carbonic anhydrase ligand

Carbonic anhydrases (CAs, EC 4.2.1.1) are ubiquitous metalloenzymes, grouped into seven different classes, which catalyze the reaction of CO₂ hydration to bicarbonate and protons. All of the fifteen human isoforms reported to date belong to the α-class and contain zinc as a cofactor. The structure of human Zn,Cu-CA II has been solved which contains a copper ion bound at its N-terminal, coordinated to His4 and His64. In the active site a dioxygen molecule is coordinated to the zinc ion. Since dioxygen is a rather unexpected CA ligand, molecular dynamics (MD) simulations were performed which suggested a superoxide character of the zinc bound O₂.     

Bolide impacts and the oxidation state of carbon in the Earth's early atmosphere

A one-dimensional photochemical model was used to examine the effect of bolide impacts on the oxidation state of Earth's primitive atmosphere. The impact rate should have been high prior to 3.8 Ga before present, based on evidence derived from the Moon. Impacts of comets or carbonaceous asteroids should have enhanced the atmospheric CO/CO₂ ratio by bringing in CO ice and/or organic carbon that can be oxidized to CO in the impact plume. Ordinary chondritic impactors would contain elemental iron that could have reacted with ambient CO₂ to give CO. Nitric oxide (NO) should also have been produced by reaction between ambient CO₂ and N₂ in the hot impact plumes. High NO concentrations increase the atmospheric CO/CO₂ ratio by increasing the rainout rate of oxidized gases. According to the model, atmospheric CO/CO₂ ratios of unity or greater are possible during the first several hundred million years of Earth's history, provided that dissolved CO was not rapidly oxidized to bicarbonate in the ocean. Specifically, high atmospheric CO/CO₂ ratios are possible if either: (1) the climate was cool (like today's climate), so that hydration of dissolved CO to formate was slow, or (2) the formate formed from CO was efficiently converted into volatile, reduced carbon compounds, such as methane. A high atmospheric CO/CO₂ ratio may have helped to facilitate prebiotic synthesis by enhancing the production rates of hydrogen cyanide and formaldehyde. Formaldehyde may have been produced even more efficiently by photochemical reduction of bicarbonate and formate in Fe⁺⁺-rich surface waters.     

Theoretical Study of the Water Exchange Reaction on Divalent Zinc Ion using Density Functional Theory

Recent ab initio studies reported in the literature have challenged the mechanistic assignments made on the basis of volume of activation data [1,2]. In addition to that ab initio molecular orbital calculations on hydrated zinc(II)-ions were used to elucidate the general role of this ion in metalloproteins [3]. Due to our interest in both inorganic reaction mechanisms and enzymatic catalysis we started a systematic investigation of solvent exchange processes on divalent zinc-ion using density functional calculations. Our investigations cover aqua complexes of the general form [Zn(H₂O)_n]²⁺·mH₂0 with n=3-6 and m=0-2, where n and m represent the number of water molecules in the coordination and solvation sphere, respectively.The complexes [Zn(H₂O)₅]²⁺·2H₂O and [Zn(H₂O)₄]²⁺·2H₂O turnend out to be the most stable zinc complexes with seven and six water molecules, respectively. This implies that a heptacoordinated zinc(II) complex, where all water molecules are located in the co-ordination sphere, should be energetically highly unfavorable and that [Zn(H₂O)₆]²⁺ can quite readily push two coordinated water molecules into the solvation sphere. For the pentaqua complex [Zn(H₂O)₅]²⁺ only one water molecule is easily lost to the solvation sphere, which makes the [Zn(H2O)₄]²⁺·H₂O complex the most favorable in order to consider the limiting dissociative and associative water exchange process of hexacoordinated zinc(II). The dehydration and hydration energies using the most stable zinc(II) complexes [Zn(H₂O)₄]²⁺·2H₂O, [Zn(H₂O)₅]²⁺·2H₂O and [Zn(H₂O)₄]²⁺·H₂O were calculated to be 24.1 and -21.0 kcal/mol, respectively.     

Structural analysis of the zinc hydroxide–Thr-199–Glu-106 hydrogen-bond network in human carbonic anhydrase II

The singnificance of the zinc hydroxide–Thr-199–Glu-106 hydrogen-bond network in the active site of human carbonic anhydrase II has been examined by X-ray crystallographic analyses of site-specific mutants. Mutants with Ala-199 and Ala-106 or Gln-106 have low catalytic activities, while a mutant with Asp-106 has almost full CO₂ hydration activity. The structures of these four mutants, as well as that of the bicarbonate complex of the mutant with Ala-199, have been determined at 1.7 to 2.2 Å resolution. Removal of the γ atoms of residue 199 leads to distorted tetrahedral geometry at the zine ion, and a catalytically important zinc-bound water molecule has moved towards Glu-106. In the bicarbonate complex of the mutant with Ala-199 one oxygen atom from bicarbonate binds to zinc without displacing this water molecule. Tetrahedral coordination geometries are retained in the mutants at position 106. The mutants with Ala-106 and Gln-106 have a zinc-bound sulfate ion, whereas this sulfate site is only partially occupied in the mutant with Asp-106. The hydrogen-bond network seems to be “reversed” in the mutants with Ala-106 and Gln-106. The network is preserved as in native enzyme in the mutant with Asp-106 but the side chain of Asp-106 is more extended than that of Glu-106 in the native enzyme. These results illustrate the importance of Glu-106 and Thr-199 for controlling the precise coordination geometry of the zinc ion and its ligand preferences with results in an optimal orientation of a zine-bound hydroxide ion for an attack on the CO₂ substrate. © 1993 Wiley-Liss, Inc.     

A proposal for the mechanism of carbonic anhydrase action

A new catalytic mechanism is proposed for the hydration of CO₂ by the zinc metalloenzyme carbonic anhydrase. This mechanism identifies the group controlling catalytic activity as an active site histidine, in which the protonated imidazole ring coordinates to zinc, losing a proton. Geometric constraints on the histidine unit make the metal-ligand bond a strained and, therefore, labile one. In the hydration reaction, the metal-bound neutral histidine moiety serves as a proton acceptor for the transient ionization of metal-bound water. Zinc-bound hydroxide attacks the carbon of the substrate to generate metal-bound bicarbonate, and the system regenerates itself by losing the elements of carbonic acid.     

In vitro and in vivo analyses of the role of the carboxysomal β-type carbonic anhydrase of the cyanobacterium Synechococcus elongatus in carboxylation of ribulose-1,5-bisphosphate

The carboxylase activities of crude carboxysome preparations obtained from the wild-type Synechococcus elongatus strain PCC 7942 strain and the mutant defective in the carboxysomal carbonic anhydrase (CA) were compared. The carboxylation reaction required high concentrations of bicarbonate and was not even saturated at 50 mM bicarbonate. With the initial concentrations of 50 mM and 25 mM for bicarbonate and ribulose-1,5-bisphosphate (RuBP), respectively, the initial rate of RuBP carboxylation by the mutant carboxysome (0.22 μmol mg^?1 protein min^?1) was only 30 % of that observed for the wild-type carboxysomes (0.71 μmol mg^?1 protein min^?1), indicating the importance of the presence of CA in efficient catalysis by ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco). While the mutant defective in the ccmLMNO genes, which lacks the carboxysome structure, could grow under aeration with 2 % (v/v) CO₂ in air, the mutant defective in ccaA as well as ccmLMNO required 5 % (v/v) CO₂ for growth, indicating that the cytoplasmically localized CcaA helped utilization of CO₂ by the cytoplasmically localized Rubisco by counteracting the action of the CO₂ hydration mechanism. The results predict that overexpression of Rubisco would hardly enhance CO₂ fixation by the cyanobacterium at CO₂ levels lower than 5 %, unless Rubisco is properly organized into carboxysomes.     

Modeling and mutagenesis of amino acid residues critical for CO2 hydration by specialized NDH-1 complexes in cyanobacteria

The uptake of inorganic carbon in cyanobacteria is facilitated by an energetically intensive CO₂-concentrating mechanism (CCM). This includes specialized Type-1 NDH complexes that function to couple photosynthetic redox energy to CO₂ hydration forming the bicarbonate that accumulates to high cytoplasmic concentrations during the operation of the CCM, required for effective carbon fixation. Here we used a Synechococcus PCC7942 expression system to investigate the role of conserved histidine and cysteine residues in the CupB (also designated, ChpX) protein, which has been hypothesized to participate in a vectoral CO₂ hydration reaction near the interface between CupB protein and the proton-pumping subunits of the NDH-1 complex. A homology model has been constructed and most of the targeted conserved residues are in the vicinity of a Zn ion modeled to form the catalytic site of deprotonation and CO₂ hydration. Growth and CO₂ uptake assays show that the most severe defects in activity among the targeted residues are due to a substitution of the predicted Zn ligand, CupB-His86. Mutations at other sites produced intermediate effects. Proteomic analysis revealed that some amino acid substitution mutations of CupB caused the induction of bicarbonate uptake proteins to a greater extent than complete deletion of CupB, despite growth under CO₂-enriched conditions. The results are discussed in terms of hypotheses on the catalytic function of this unusual enzyme.     

Coordination abilities of substituted β-aminophosphonates towards Cu and Zn ions

The formation constants of equimolar and bis-chelate copper(II) and zinc(II) complexes with three aliphatic and four aromatic-substituted β-aminophosphonates have been determined in water solution by potentiometric studies. Spectroscopic parameters clearly indicate involvement of {NH₃, PO₃ ²⁻} in both metal ions coordination. The comparison of the stability constants reveals slightly higher coordination power of the aliphatic-substituted β-aminophosphonic acids, which may be due to the higher basicity of their amino groups. All studied ligands are more effective in Cu²⁺ and Zn²⁺ coordination than phosphonic analogue of simple β-amino acid.     

Acidosis and Ca2+ distribution in myocardial tissue of flounder and rat

Summary The effect of acidosis on the myocardial Ca²⁺ distribution was examined at 15°C in ventricular strips of the flounder (Platichthys flesus) and at 30°C in atrial strips of the rat (Rattus norvegicus).Lowering the Ringer pH from 7.6 to 6.9 by increasing its CO₂ (flounder 2% to 12%, rat 4% to 14%), resulted in an elevated Ca²⁺ efflux in resting strips as well as in strips stimulated (12/min) to contraction. A decrease in pH of the Ringer used for the flounder myocardium by a lowering of bicarbonate (30 mM to 5 mM) also resulted in an elevation of the Ca²⁺ efflux, but the effect was smaller than that produced by an increased CO₂.With 11 mM Ca²⁺ and 10 mM EGTA added to the Ringer to reduce the amount of⁴⁵Ca²⁺ bound to extracellular sites, an increased CO₂ with a concomitant drop in Ringer pH resulted in an increased Ca²⁺ efflux in both myocardia. The Ca²⁺ efflux was only marginally elevated in the flounder myocardium and unchanged in that of rat when the same drop in Ringer pH was produced with a lowering in bicarbonate.In a nominally Ca²⁺-free Ringer with 0.1 mM EGTA the⁴⁵Ca²⁺ efflux was stimulated for both myocardia by an increase in CO₂.The flounder myocardium was exposed to high CO₂ in a nominally Na⁺, Ca²⁺-free Ringer and again the⁴⁵Ca²⁺ efflux increased. After a return to Na, Ca and low CO₂ in the Ringer, a higher efflux persisted in the strips being subjected to a high CO₂ than in the controls.The Ca²⁺ uptake rate was about the same at high and low CO₂ for both myocardia.Based on these results the measured increase in Ca efflux following an increase in CO₂ or a decrease in bicarbonate probably results from an elevated cytoplasmatic Ca²⁺ activity. It seems unlikely that an increased uptake rate of Ca²⁺ or a direct stimulation of Ca²⁺ transporting mechanisms in the cell membrane are responsible for the change.     

Factors affecting interconversion between kinetic forms of ribulose diphosphate carboxylase-oxygenase from spinach

Ribulose diphosphate carboxylase was found to exist in two distinct kinetic forms in spinach leaf extracts. One form displayed an apparent K_m for CO₂ in excess of 200 μm and is likely to be the form purified and studied by many previous workers. However, if leaf extracts were prepared in the presence of Mg²⁺ and atmospheric levels of CO₂, the recently described high-affinity form was obtained. It had a K_m for CO₂ of about 20 μm, was quite stable even at 25 °C, and its properties were consistent with it being the form which operates in photosynthesis in vivo. Mg²⁺ was also able to convert the high-K_m (CO₂) form to the low-K_m (CO₂) form when it was added to an extract which had been prepared in its absence. Mg²⁺ was more effective in causing this conversion if bicarbonate was added as well. This activating effect of bicarbonate is a probable cause of previously reported apparent homotropic effects of bicarbonate on ribulose diphosphate carboxylase activity. It is possible that the apparently high-K_m (CO₂) form is not intrinsically active and appears to have activity only by virtue of the low-K_m (CO₂) form produced by contact with Mg²⁺ and bicarbonate (or CO₂) during the course of the assay. Extracts prepared with ribose 5-phosphate in the absence of Mg₂₊ also showed low-K_m (CO₂) carboxylase activity initially, but the presence of this sugar phosphate was deleterious during storage at 25 °C, where it promoted conversion to the apparently high-K_m (CO₂) form.Effects on the affinity of ribulose diphosphate carboxylase for CO₂ were paralleled by effects on the activity of the associated ribulose diphosphate oxygenase. Treatments which produced the low-K_m (CO₂) form of the carboxylase also resulted in high oxygenase activity, and it is possible that the apparently high-K_m (CO₂) form of the carboxylase has little, if any, oxygenase activity associated with it.The carboxylase and oxygenase activities of the low-K_m (CO₂) form showed broad and quite similar responses to pH variation, and the oxygenase had a K_m for O₂ of 0.22 mm.The stability of the low-K_m (CO₂) form in the presence of Mg²⁺ and bicarbonate was quite sufficient for it to be partially purified by Sepharose chromatography. The significance of the low-K_m (CO₂) form is discussed with respect to activation of photosynthesis by Mg²⁺.     

The Important Role of Active Site Water in the Catalytic Mechanism of Human Carbonic Anhydrase II – A Semiempirical MO Approach to the Hydration of CO2 †

The approach of CO₂ to a series of active site model complexes of human carbonic anhydrase II (HCAII) and its catalytic hydration to bicarbonate anion have been investigated using semiempirical MO theory (AM1). The results show that direct nucleophilic attack of zinc-bound hydroxide to the substrate carbon occurs in each model system. Further rearrangement of the bicarbonate complex thus formed via a rotation-like movement of the bicarbonate ligand can only be found in active site model systems that include at least one additional water molecule. Further refinement of the model complex by adding a methanol molecule to mimic Thr-199 makes this process almost activationless. The formation of the final bicarbonate complex by an internal (intramolecular) proton transfer is only possible in the simplest of all model systems, namely {[Im₃Zn(OH)]⁺·CO₂}. The energy of activation for this process, however, is 36.8 kcal·mol^–1 and thus too high for enzymatic catalysis. Therefore, we conclude that within the limitations of the model systems presented and the level of theory employed, the overall mechanism for the formation of the bicarbonate complex comprises an initial direct nucleophilic attack of zinc-bound hydroxide to carbon dioxide followed by a rotation-like rearrangement of the bicarbonate ligand via a penta-coordinate Zn²⁺ transition state structure, including the participation of an extra active site water molecule.Electronic Supplementary Material available.     

Invasive submerged freshwater macrophytes are more plastic in their response to light intensity than to the availability of free CO2 in air‐equilibrated water

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Carbon dioxide and the reduction of indophenol and ferricyanide by chloroplasts

Pea chloroplasts isolated in salt media show decreased rates of 2:6 dichlorophenolindophenol (DCPIP) and ferricyanide reduction when depleted of CO₂ at pH values below 7.5. The greatest effect of CO₂ was on uncoupled systems. The incorporation of 10⁻², 2 × 10⁻² and 4 × 10⁻² m sodium acetate into the reaction mixtures progressively increased the bicarbonate concentration required for half maximal rates of reduction of DCPIP. The reaction was saturated by bicarbonate concentrations of 1 to 4 × 10⁻² m. With both DCPIP and ferricyanide, the addition of bicarbonate to illuminated chloroplast systems depleted of CO₂ gave very rapid increases in the rates of reduction. Bicarbonate also stimulated oxygen uptake by the illuminated chloroplasts when added hydrogen acceptors had been reduced. There was no effect of bicarbonate on ferricyanide reduction at low light intensities, but with DCPIP reduction, the apparent magnitude of the effect was independent of light intensity. This suggests that DCPIP reacts with the chloroplast electron transport chain at a site nearer to a photochemical stage than does ferricyanide. It also suggests that CO₂ has at least 2 sites of action.     

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.     

Forms of Dissolved Carbon Dioxide Required for Photosystem II Activity in Chloroplast Membranes

High concentrations of both bicarbonate and formate inhibit photosynthetic O₂ evolution at pH 8.0. At this pH, only 2.4% of the total dissolved carbon dioxide exists as CO₂. At pH 7.3, where 11% of the total dissolved carbon dioxide exists as CO₂, HCO₃⁻ no longer inhibits. While formate still inhibits O₂ evolution at pH 7.3, its effect can be partially overcome if CO₂ is also present. The rate of binding of added ¹⁴C-labeled inorganic carbon is nearly 10-fold more rapid when the internal pH of thylakoid membranes is at 6.0 than when it is at 7.8. These observations suggest that CO₂, not HCO₃⁻, is initially bound to the photosystem II reaction center and that the location of the binding site is on the inside thylakoid surface. However, additional data presented here suggest that, after binding, CO₂ is hydrated to HCO₃⁻ + H⁺ in a pH-dependent reaction. Two possible explanations of the “bicarbonate effect” are presented.     

Bicarbonate assimilation by fresh-water charophytes and higher plants: I. Membrane transport of bicarbonate ions is not proven

Summary Although it is generally believed thatChara and some fresh-water angiosperms transport bicarbonate ions inwards across their plasma membranes, there has been no direct demonstration of such transport in these plants. The (indirect) arguments for their transporting HCO ₃ ^– are arguments against the inward diffusion of CO₂ at the observed rates. They rest on calculations of the equilibrium concentration of CO₂ or of the maximum rate at which CO₂ might be produced from HCO ₃ ^– at the pH of the medium outside the cells. SinceChara acidifies the medium over about half the cell surface during C assimilation, these calculations have been based on questionable premises.We propose a model forChara in which the acidification is attributed to active efflux of H⁺, and we calculate that both the equilibrium concentration of CO₂ and its rate of production outside the cell can be high enough to support the observed rates of C assimilation, without postulating transport of the species HCO ₃ ^– or H₂CO₃.Calculations are presented also for alternative models in which there is membrane transport of HCO ₃ ^– . The first includes symport of H⁺ with HCO ₃ ^– , again dependent on active H⁺ efflux. In the second, there is active electrogenic transport of HCO ₃ ^– . In this case the low pH in the medium outside the cell is caused by the dissociation of H₂CO₃ produced by hydration of CO₂ which leaks from the cell cytoplasm.All three models are consistent with the observations to date, but the first is more economical of postulates. It can also explain the apparent transport of HCO ₃ ^– by fresh-water angiosperms such asEgeria.     

Acetate and Bicarbonate Assimilation and Metabolite Formation in Chlamydomonas reinhardtii: A 13C-NMR Study

Cellular metabolite analyses by ¹³C-NMR showed that C. reinhardtii cells assimilate acetate at a faster rate in heterotrophy than in mixotrophy. While heterotrophic cells produced bicarbonate and CO₂ ^aq, mixotrophy cells produced bicarbonate alone as predominant metabolite. Experiments with singly ¹³C-labelled acetate (¹³CH₃-COOH or CH₃-¹³COOH) supported that both the ¹³C nuclei give rise to bicarbonate and CO₂ ^aq. The observed metabolite(s) upon further incubation led to the production of starch and triacylglycerol (TAG) in mixotrophy, whereas in heterotrophy the TAG production was minimal with substantial accumulation of glycerol and starch. Prolonged incubation up to eight days, without the addition of fresh acetate, led to an increased TAG production at the expense of bicarbonate, akin to that of nitrogen-starvation. However, such TAG production was substantially high in mixotrophy as compared to that in heterotrophy. Addition of mitochondrial un-coupler blocked the formation of bicarbonate and CO₂ ^aq in heterotrophic cells, even though acetate uptake ensued. Addition of PSII-inhibitor to mixotrophic cells resulted in partial conversion of bicarbonate into CO₂ ^aq, which were found to be in equilibrium. In an independent experiment, we have monitored assimilation of bicarbonate via photoautotrophy and found that the cells indeed produce starch and TAG at a much faster rate as compared to that in mixotrophy and heterotrophy. Further, we noticed that the accumulation of starch is relatively more as compared to TAG. Based on these observations, we suggest that acetate assimilation in C. reinhardtii does not directly lead to TAG formation but via bicarbonate/CO₂ ^aq pathways. Photoautotrophic mode is found to be the best growth condition for the production of starch and TAG and starch in C. reinhardtii.     

The effect of carbonic anhydrase inhibitors on secretion by the parotid and mandibular glands of red kangaroos Macropus rufus

Summary The effects of carbonic anhydrase inhibitors on secretion by macropodine parotid and mandibular glands were investigated using anaesthetized red kangaroos. In the parotid gland, acetazolamide (500 mol·l^-1) reduced a stable acetylcholine-evoked, half-maximal flow rate of 2.02±0.034 to 0.27±0.023 ml·min^-1 (87% reduction). Concurrently, salivary bicarbonate concentration and secretion fell (129.4±1.46 to 80.9±1.63 mmol·l^-1 and 264.8±7.96 to 22.3±2.30 mol·min^-1, respectively), phosphate and chloride concentrations rose (14.0±0.79 to 27.6±0.85 mmol·l^-1 and 5.6±0.25 to 27.5±1.32 mmol·l^-1, respectively), sodium concentration and osmolality were unaltered, and potassium concentration fell (8.8±0.33 to 6.4±0.29 mmol·l^-1). High-rate cholinergic stimulation during acetazolamide blockade was unable to increase salivary flow beyond 11±0.9% of that for equivalent unblocked control stimulation. However, superimposition of isoprenaline infusion on the acetylcholine stimulation caused a three-fold increase in the blocked flow rate. These treatments were accompanied by small increases in salivary phosphate and chloride concentrations but not bicarbonate concentration. Methazolamide infusion caused similar changes in parotid secretion. In the mandibular gland, acetazolamide infusion had no effect on salivary flow rate during either low- or high-level acetylcholine stimulation. Acetazolamide caused no alterrations in salivary electrolyte secretion at low flow rates, but curtailed the rise in bicarbonate concentration associated with high-level acetylcholine stimulation. Acetazolamide administration did not affect the increase in salivary flow rate associated with isoprenaline infusion, but did block the concomitant increase in bicarbonate concentration and secretion substantially. It was concluded that neither cholinergic nor adrenergic stimulation of mandibular fluid secretion depends on secretion of bicarbonate derived from catalysed hydration of CO₂, but a substantial proportion of the increase in bicarbonate secretion during isoprenaline administration, which is probably ductal in origin, is so dependent. In contrast to other salivary glands, including the ovine parotid, fluid secretion by the kangaroo parotid gland during cholinergic stimulation is largely dependent (about 90%) on secretion of bicarbonate derived from hydration of CO₂ catalysed by glandular carbonic anhydrase. Fluid secretion during adrenergic stimulation is not bicarbonate dependent.Abbreviations b.w. body weight - PAH p-aminohippurate - PCO₂ partial pressure carbon dioxide - PCO₂ partial pressure of oxygen