Catalysis by cobalt(II)-substituted carbonic anhydrase II of the exchange of oxygen-18 between CO2 and H2O

We have measured the catalysis by Co(II)-substituted bovine carbonic anhydrase II from red cells of the exchange of 18O between CO2 and H2O using membrane-inlet mass spectrometry. We chose Co(II)-substituted carbonic anhydrase II because the apparent equilibrium dissociation constant of HCO3- and enzyme at pH 7.4, KHCO3-eff approximately equal to 55 mM, was within a practicable range of substrate concentrations for the 18O method. For the native, zinc-containing enzyme KHCO3-eff is close to 500 mM at this pH. The rate constant for the release from the active site of water bearing substrate oxygen kH2O was dependent on the fraction of enzyme that was free, not bound by substrate HCO3- or anions. The pH dependence of kH2O in the pH range 6.0-9.0 can be explained entirely by a rate-limiting, intramolecular proton transfer between cobalt-bound hydroxide and a nearby group, probably His-64. The rate constant for this proton transfer was found to be 7 X 10(5) S-1 for the Co(II)-substituted enzyme and 2 X 10(6) S-1 for the native enzyme. These results are applied to models derived from proton-relaxation enhancement of water exchanging from the inner coordination shell of the cobalt in carbonic anhydrase. The anions iodide, cyanate, and thiocyanate inhibited catalysis of 18O exchange by Co(II)-substituted carbonic anhydrase II in a manner competitive with total substrate (CO2 and HCO3-) at chemical equilibrium and pH 7.4. These results are discussed in terms of observed steady-state inhibition patterns and suggest that there is no significant contribution of a ternary complex between substrate, inhibitor, and enzyme.     

A 13C nuclear magnetic resonance study of CO2/HCO-3 exchange catalyzed by human carbonic anhydrase I

Rates of CO2/HCO-3 exchange, catalyzed by human carbonic anhydrase I (or B) at chemical equilibrium, were estimated from the nuclear magnetic resonance linewidths of 13C-labeled substrates. The results show that the maximal exchange rate constant is independent of pH in the range 5.7-8.0, whereas the apparent substrate dissociation constant depends on pH. Exchange proceeds rapidly in the absence of added buffers, and the addition of buffers has negligible effects on exchange rates. Exchange is equally rapid with 1H2O or 2H2O as solvents. Chloride ions inhibit CO2/HCO-3 exchange competitively. The maximal exchange rates obtained with human carbonic anhydrase I are 50 times slower than those obtained with human isoenzyme II (or C). From a comparison of the exchange kinetics with the steady-state kinetics of CO2 hydration and HCO-3 dehydration it is tentatively concluded that the transfer of H+ between active site and medium proceeds with rates of similar magnitudes in the two isoenzymes, whereas the central catalytic step, the interconversion of enzyme-bound CO2 and HCO-3, is much slower in isoenzyme I than in isoenzyme II.     

Molecular basis of the oxygen exchange from CO2 catalyzed by carbonic anhydrase III from bovine skeletal muscle

The exchange of 18O from CO2 to H2O in aqueous solution is caused by the hydration-dehydration cycle and is catalyzed by the carbonic anhydrases. In our previous studies of 18O exchange at chemical equilibrium catalyzed by isozymes I and II of carbonic anhydrase, we observed simple first-order depletion of 18O from CO2 with the 18O distribution among the species C18O18O, C16O18O, and C16O16O described by the binomial expansion (i.e., a random distribution of 18O). Using membrane-inlet mass spectrometry, we have measured 18O exchange between CO2 and H2O catalyzed by native zinc-containing and cobalt(II)-substituted carbonic anhydrase III from bovine skeletal muscle near pH 7.5. The distributions of 18O in CO2 deviate from the binomial expansion and are accompanied by biphasic 18O-exchange patterns; moreover, we observed regions in which 18O loss from CO2 was faster than 18O loss from HCO3-. These data are interpreted in terms of a model that includes 18O loss from an enzyme-substrate or intermediate complex. We conclude that more than one 18O can be lost from CO2 per encounter with the active site of isozyme III, a process that requires scrambling of oxygens in a bicarbonate-enzyme complex and cycling between intermediate complexes. This suggests that the rate of dissociation of H2(18)O (or 18OH-) from isozyme III is comparable to or faster than substrate and product dissociation.     

Buffer enhancement of proton transfer in catalysis by human carbonic anhydrase III

Among the isozymes of carbonic anhydrase, isozyme III is the least efficient in the catalysis of the hydration of CO2 and was previously thought to be unaffected by proton transfer from buffers to the active site. We report that buffers of small size, especially imidazole, increase the rate of catalysis by human carbonic anhydrase III (HCA III) of (1) 18O exchange between HCO3- and water measured by membrane-inlet mass spectrometry and (2) the dehydration of HCO3- measured by stopped-flow spectrophotometry. Imidazole enhanced the rate of release of 18O-labeled water from the active site of wild-type carbonic anhydrase III and caused a much greater enhancement, up to 20-fold, for the K64H, R67H, and R67N mutants of this isozyme. Imidazole had no effect on the rate of interconversion of CO2 and HCO3- at chemical equilibrium. Steady-state measurements showed that the addition of imidazole resulted in increases in the turnover number (kcat) for the hydration of CO2 catalyzed by HCA III and for the dehydration of HCO3- catalyzed by R67N HCA III. These results are consistent with the transfer of a proton from the imidazolium cation to the zinc-bound hydroxide at the active site, a step required to regenerate the active form of enzyme in the catalytic cycle. Like isozyme II of carbonic anhydrase, isozyme III can be enhanced in catalytic rate by the presence of small molecule buffers in solution.     

Comparison of 18O exchange and pH stop-flow assays for carbonic anhydrase

The hydration velocity of CO2 (0.002 M) catalyzed by bovine carbonic anhydrase (BCA) was measured at 25 degrees C and pH 7.4 by three different techniques: two initial-rate (steady-state) stop-flow methods, one using a glass pH electrode (in Hannover, method 1) and one using spectrophotometric measurements of a pH indicator (in Philadelphia, method 2), and an exchange method in which the disappearance of C18O16O from a bicarbonate solution was determined at equilibrium (in Philadelphia, method 3). The Michaelis-Menten constant (Km) and the inhibition constants for chloride (Ki,Cl) and ethoxzolamide (Ki,ez) were the same for methods 1, 2, and 3. The turnover numbers were 270,000, 400,000, and 555,000 s-1 by methods 1, 2, and 3, respectively. Values for CO2 hydration velocity measured by methods 2 and 3 on the same solution of BCA at the same time were the same. Km, maximal reaction velocity (Vmax), Ki,ez, and Ki,Cl obtained from normal human hemolysate at 37 degrees C and pH 7.2 by methods 2 and 3 were the same. Km and Vmax of the carbonic anhydrase isozyme CA III of homogenate from rabbit soleus were also identical by methods 1 and 3. According to Michaelis-Menten theory, the values of Km and Vmax obtained by method 3 should have been significantly smaller than those obtained by methods 1 and 2. We conclude that the catalytic step itself is apparently not rate limiting under physiological conditions and that method 3 can be used to obtain Michaelis-Menten characteristics of carbonic anhydrase.     

Purification and characterization of carbonic anhydrase from the saliva of the rat

Carbonic anhydrase purified from the saliva of the rat had kinetic properties identical with those of carbonic anhydrase II from rat red cells, but its molecular properties were distinctly different from the type II isozyme. Kinetic parameters were measured under steady state conditions by stopped-flow spectrophotometry and under equilibrium conditions by an 18O exchange method. The turnover number kcat for hydration of CO2 was 6.5 X 10(4) s-1 and the Michaelis constant was 4.2 mM at pH 7.5 and 25 degrees C, values which are equal to the steady state constants for red cell carbonic anhydrase II from the rat. Inhibition of the salivary isozyme by sulfanilamide (Ki = 3.7 microM) was nearly as efficient as inhibition of the erythrocyte isozyme II (Ki = 1.1 microM). The molecular weight for the salivary isozyme was 46,000 and the isoelectric point was 5.5. Salivary carbonic anhydrase had high mannose oligosaccharide components as measured by concanavalin A binding. The amino acid composition for the salivary isozyme was not similar to rat type II, but it was similar to that reported for membrane-bound carbonic anhydrase from bovine lung (Whitney, P.L., and Briggle, T.V. (1982) J. Biol. Chem. 257, 12056-12059). These observations suggest to us that salivary carbonic anhydrase is a secretory product.     

Carbonic anhydrase catalyzed oxygen-18 exchange between bicarbonate and water

Oxygen-18 exchange techniques were applied to the dehydration of bicarbonate catalyzed by human carbonic anhydrase C. The rates of depletion of oxygen-18 from labeled bicarbonate were measured for both the catalyzed and uncatalyzed reactions at pH 9.4 and 25 °C. The equilibrium dissociation constant of the enzyme-substrate complex K is 0.321 ± 0.040 m and $\text{k}{}_{\mathrm{<mtext>enz</mtext>}}\text{=}\text{k}{}_2\text{K}{}_{\mathrm{m}}$ is (8.3 ± 1.9) × 10⁵m^?1 sec^?1 under these conditions. On the basis of these results it is demonstrated that the oxygen-18 exchange technique is capable of measuring K and k_enz for the carbonic anhydrase catalyzed dehydration of bicarbonate at a high pH range in which other kinetic techniques are not effective.It was also shown that the oxygen-18 exchange technique is an effective micromethod for the determination of carbonic anhydrase. Rates of isotopic depletion of labeled bicarbonate (in solutions of the enzyme) which fall outside the limits of error for the uncatalyzed rate of depletion demonstrate that this technique can detect concentrations of human carbonic anhydrase C as low as 5 × 10^?11m.     

The pH dependence of the hydration of CO2 catalyzed by carbonic anhydrase III from skeletal muscle of the cat. Steady state and equilibrium studies

We have measured the pH dependence of the kinetics of CO2 hydration catalyzed by carbonic anhydrase III from the skeletal muscle of the cat. Two methods were used: an initial velocity study in which the change in absorbance of a pH indicator was measured in a stopped flow spectrophotometer, and an equilibrium study in which the rate of exchange of 18O between CO2 and H2O was measured with a mass spectrometer. We have found that the steady state constants kCO2 cat and KCO2 m are independent of pH within experimental error in the range of pH 5.0 to 8.5; the rate of release from the enzyme of the oxygen abstracted from substrate HCO-3 in the dehydration is also independent of pH in this range. This behavior is very different from that observed for carbonic anhydrase II for which kCO2 cat and the rate of release of substrate oxygen are very pH-dependent. The rate of interconversion of CO2 and HCO-3 at equilibrium catalyzed by carbonic anhydrase III is not altered when the solvent is changed from H2O to 98% D2O and 2% H2O. Thus, the interconversion probably proceeds without proton transfer in its rate-limiting steps, similar to isozymes I and II.     

Kinetic characterization of wild-type and proton transfer-impaired variants of beta-carbonic anhydrase from Arabidopsis thaliana

We have cloned and overexpressed a truncated, recombinant form of beta-carbonic anhydrase from Arabidopsis thaliana. The wild-type enzyme and two site-directed variants, H216N and Y212F, have been kinetically characterized both at steady state by stopped-flow spectrophotometry and at chemical equilibrium by (18)O isotope exchange methods. The wild-type enzyme has a maximal k(cat) for CO2 hydration of 320 ms(-1) and is rate limited by proton transfer involving two residues with apparent pK(a) values of 6.0 and 8.7. The mutant enzyme H216N has a maximal k(cat) at high pH that is 43% that of wild type, but is only 5% that of wild type at pH 7.0. (18)O exchange studies reveal that the effect of the mutations H216N or Y212F is primarily on proton transfer steps in the catalytic mechanism and not in the rate of CO2-HCO3- exchange. These results suggest that residues His-216 and Tyr-212 are both important for efficient proton transfer in A. thaliana carbonic anhydrase.     

The carbon dioxide hydration activity of brush-border carbonic anhydrase from the dog kidney

The steady-state kinetic parameters for the hydration of CO₂ catalyzed by membrane-bound carbonic anhydrase from the renal brush-border of the dog are compared with the same parameters for water-soluble bovine erythrocyte carbonic anhydrase. For the membrane-bound enzyme, the turnover number k_cat is 6.5 × 10⁵ s^?1 and the Michaelis constant is 7.5 mm for CO₂ hydration at pH 7.4 and 25 °C. The corresponding constants for bovine carbonic anhydrase under these conditions are 6.3 × 10⁵ s^?1 and 15 mm (Y. Pocker and D.W. Bjorkquist (1977)Biochemistry16, 5698–5707). The rate constant for the transfer of a proton between carbonic anhydrase and buffer was determined from the dependence of the catalytic rate on the concentration of the buffers imidazole and N-2-hydroxyethylpiperazine-N′-2-ethanesulfonic acid (Hepes); the value of 2 × 10⁸m^?1s^?1 describes this constant for both forms of carbonic anhydrase at pH 7.4. Furthermore, the pH dependence of the initial velocity of hydration of CO₂ in the range of pH 6.5 to 8.0 is identical for the membrane-bound and soluble enzyme at low buffer concentration (1–2 mm imidazole). We conclude that the membrane plays no detectable role in affecting the CO₂ hydration activity and that the active site of the renal, membrane-bound carbonic anhydrase is exposed to the aqueous phase.     

Enhancement of the catalytic activity of carbonic anhydrase III by phosphates

Phosphate and phosphate-containing buffers of physiological interest such as ATP and 3-phosphoglycerate were found to enhance catalysis by human carbonic anhydrase III (HCA III). Addition of phosphate caused an increase in both the catalyzed rate of hydration of CO2 at steady state measured by stopped-flow spectrophotometry and the exchange of 18O between CO2 and water at chemical equilibrium measured by mass spectrometry. The results are consistent with a mechanism in which phosphate enhances the transfer of protons between zinc-bound water at the active site and solution. Site-directed mutations to replace lysine 64 and arginine 67 in the active-site cavity resulted in greater enhancement by phosphate when compared with wild-type HCA III and showed that these basic residues are not essential as a binding site for phosphate. Phosphate did not enhance catalysis by HCA II.     

Chemical modification of carbonic anhydrase II with acrolein

We have reacted acrolein with human carbonic anhydrase II using conditions reported to result in maximal formylethylation of exposed histidine and lysine residues (Pocker, Y., and Janji?, N. (1988) J. Biol. Chem. 263, 6169-6176). Pocker and Janji? proposed that the decrease by 95-98% in the steady-state turnover number for the hydration of CO2 caused by this chemical modification is due predominantly to the alkylation of one residue, the imidazole side chain of histidine 64. We measured the rate of 18O exchange between CO2 and water catalyzed by these enzymes at chemical equilibrium using membrane inlet mass spectrometry. The catalyzed rate of interconversion of CO2 and HCO3- at chemical equilibrium was the same for the acrolein-modified and the unmodified carbonic anhydrases, but the rate of release of 18O-labeled water from the active site had decreased by as much as 85% for the acrolein-modified enzyme. The 18O-exchange kinetics catalyzed by the acrolein-modified carbonic anhydrase II was similar to that catalyzed by a mutant human carbonic anhydrase II in which histidine at residue 64 was replaced with alanine. Moreover, modification of this mutant carbonic anhydrase II with acrolein did not alter to a significant extent its 18O-exchange pattern. These results support the proposal of Pocker and Janji? and the suggested role of histidine 64 in carbonic anhydrase II as a proton shuttle residue that transfers a proton from zinc-bound water to buffer in solution.     

Inhibition of the hydration of CO2 catalyzed by carbonic anhydrase III from cat muscle

Using stopped flow methods, we have measured the steady state rate constants and the inhibition by N3- and I- of the hydration of CO2 catalyzed by carbonic anhydrase III from cat muscle. Also, using fluorescence quenching of the enzyme at 330 nm, we have measured the binding of the sulfonamide chlorzolamide to cat carbonic anhydrase III. Inhibition by the anions was uncompetitive at pH 6.0 and was mixed at higher values of pH. The inhibition constant of azide was independent of pH between 6.0 and 7.5 with a value of KIintercept = 2 X 10(-5) M; the binding constant of chlorzolamide to cat carbonic anhydrase III was also independent of pH in the range of 6.0 to 7.5 with a value Kdiss = 2 X 10(-6) M. Both of these values increased as pH increased above 8. There was a competition between chlorzolamide and the anions N-3 and OCN- for binding sites on cat carbonic anhydrase III. The pH profiles for the kinetic constants and the uncompetitive inhibition at pH 6.0 can be explained by an activity-controlling group in cat carbonic anhydrase III with a pKa less than 6. Moreover, the data suggest that like isozyme II, cat isozyme III is limited in rate by a step occurring outside the actual interconversion of CO2 and HCO3- and involving a change in bonding to hydrogen exchangeable with solvent water.     

Kinetic and crystallographic studies of the role of tyrosine 7 in the active site of human carbonic anhydrase II

The rate limiting step in catalysis of bicarbonate dehydration by human carbonic anhydrase II (HCA II) is an intramolecular proton transfer from His64 to the zinc-bound hydroxide. We have examined the role of Tyr7 using site-specific mutagenesis and measuring catalysis by the ¹⁸O exchange method using membrane inlet mass spectrometry. The side chain of Tyr7 in HCA II extends into the active-site cavity about 7 Å from the catalytic zinc atom. Replacement of Tyr7 with eight other amino acids had no effect on the interconversion of bicarbonate and CO₂, but in some cases caused enhancements in the rate constant of proton transfer by nearly 10-fold. The variant Y7I HCA II enhanced intramolecular proton transfer approximately twofold; its structure was determined by X-ray crystallography at 1.5 Å resolution. No changes were observed in the ordered solvent structure in the active-site cavity or in the conformation of the side chain of the proton shuttle His64. However, the first 11 residues of the amino-terminal chain in Y7I HCA II assumed an alternate conformation compared with the wild type. Differential scanning calorimetry showed variants at position 7 had a melting temperature approximately 8 °C lower than that of the wild type.     

Carbon isotope effect on dehydration of bicarbonate ion catalyzed by carbonic anhydrase

The carbon-13 kinetic isotope effect on the dehydration of HCO3- by bovine carbonic anhydrase has been measured. To accomplish this, bicarbonate was added to a buffer solution at pH 8 containing carbonic anhydrase under conditions where purging of the product CO2 from the solution is rapid. Measurement of the isotopic composition of the purged CO2 as a function of the concentration of carbonic anhydrase permits calculation of the isotope effect on the enzymic reaction. The isotope effect on the dehydration is k12/k13 = 1.0101 +/- 0.0004. This effect is most consistent with a ping-pong mechanism for carbonic anhydrase action, in which proton transfer to or from the enzyme occurs in a step separate from the dehydration step. Substrate and product dissociation steps are at least 2-3-fold faster than the hydration/dehydration step.     

A comparison of the kinetic properties of native bovine muscle carbonic anhydrase and an activated derivative with modified thiol groups

Steady-state and equilibrium kinetic properties of native bovine carbonic anhydrase III (carbonate hydrolyase, EC 4.2.1.1) and a derivative modified with methyl methanethiosulfonate were investigated. The modified enzyme has a markedly increased CO2 hydration activity compared to the native form with a 3-times higher value of kcat and a 6-10-times higher value of kcat/Km. Qualitatively, the activated enzyme shows the same kinetic behavior as native isoenzyme III. This is reflected in similar pH dependences of the kinetic parameters for CO2 hydration, similar solvent hydrogen isotope effects on these parameters, similar deviations from Michaelis-Menten kinetics for the HCO3- dehydration reaction, and similar behavior of the kinetics of CO2/HCO3- exchange at chemical equilibrium as measured by a 13C-NMR magnetization transfer technique. It is concluded that the conversion of -SH groups to -S-S-CH3 moieties does not change the catalytic mechanism, but leads to an increased rate of CO2/HCO3- interconversion as well as to an increased rate of proton transfer between the active site and the reaction medium.     

Chemical rescue of proton transfer in catalysis by carbonic anhydrases in the beta- and gamma-class

Catalysis of the dehydration of HCO(3)(-) by carbonic anhydrase requires proton transfer from solution to the zinc-bound hydroxide. Carbonic anhydrases in each of the alpha, beta, and gamma classes, examples of convergent evolution, appear to have a side chain extending into the active site cavity that acts as a proton shuttle to facilitate this proton transfer, with His 64 being the most prominent example in the alpha class. We have investigated chemical rescue of mutants in two of these classes in which a proton shuttle has been replaced with a residue that does not transfer protons: H216N carbonic anhydrase from Arabidopsis thaliana (beta class) and E84A carbonic anhydrase from the archeon Methanosarcina thermophila (gamma class). A series of structurally homologous imidazole and pyridine buffers were used as proton acceptors in the activation of CO(2) hydration at steady state and as proton donors of the exchange of (18)O between CO(2) and water at chemical equilibrium. Free energy plots of the rate constants for this intermolecular proton transfer as a function of the difference in pK(a) of donor and acceptor showed extensive curvature, indicating a small intrinsic kinetic barrier for the proton transfers. Application of Marcus rate theory allowed quantitative estimates of the intrinsic kinetic barrier which were near 0.3 kcal/mol with work functions in the range of 7-11 kcal/mol for mutants in the beta and gamma class, similar to results obtained for mutants of carbonic anhydrase in the alpha class. The low values of the intrinsic kinetic barrier for all three classes of carbonic anhydrase reflect proton transfer processes that are consistent with a model of very rapid proton transfer through a flexible matrix of hydrogen-bonded solvent structures sequestered within the active sites of the carbonic anhydrases.     

Proton transfer within the active-site cavity of carbonic anhydrase III

The maximal turnover rate of CO2 hydration catalyzed by the carbonic anhydrases is limited by proton transfer steps from the zinc-bound water to solution, steps that regenerate the catalytically active zinc-bound hydroxide. Catalysis of CO2 hydration by wild-type human carbonic anhydrase III (HCA III) (k(cat) = 2 ms (-1)) is the least efficient among the carbonic anhydrases in its class, in part because it lacks an efficient proton shuttle residue. We have used site-directed mutagenesis to test positions within the active-site cavity of HCA III for their ability to carry out proton transfer by replacing various residues with histidine. Catalysis by wild-type HCA III and these six variants was determined from the initial velocity of hydration of CO2 measured by stopped-flow spectrophotometry and from the exchange of 18O between CO2 and H2O at chemical equilibrium by mass spectrometry. The results show that histidine at three positions (Lys64His, Arg67His and Phe131His) have the capacity to transfer protons during catalysis, enhancing maximal velocity of CO2 hydration and 18O exchange from 4- to 15-fold compared with wild-type HCA III. Histidine residues at the other three positions (Trp5His, Tyr7His, Phe20His) showed no firm evidence for proton transfer. These results are discussed in terms of the stereochemistry of the active-site cavity and possible proton transfer pathways.     

Exchange of labeled bicarbonate and carbon dioxide with erythrocytes suspended in an elutriator

An elutriator was used to study exchange of labeled CO2 and bicarbonate with erythrocytes. Rabbit erythrocytes were suspended by centrifugation in a stream of fluid and exposed to transient injections of an extracellular indicator (125I-albumin or 22Na+), a water indicator (3H2O), and H14CO3- and/or 14CO2. Diffusion of indicators into erythrocytes was judged by comparison of initial concentrations of diffusible and extracellular indicators in the elutriator outflow. It was possible to conduct these experiments at normal hematocrits because any carbonic anhydrase released from erythrocytes by hemolysis was washed away in the elutriator flow, and ambient pH, PO2, and PCO2 were kept constant by the inflow of fresh fluid. Equilibration of HCO3- with erythrocytes was complete during the 7- to 10-s transit time through the chamber. After this exchange was irreversibly inhibited by the anion exchange inhibitor, DIDS (4,4'-diisothiocyanostilbene-2,2'-disulfonic acid), addition of carbonic anhydrase (100 mg/dl) accelerated exchange, but acetazolamide (20 mg/dl) was without effect. These observations were consistent with the absence of carbonic anhydrase on the surface of the erythrocytes.     

A 13C nuclear-magnetic-resonance study of CO2-HCO3-exchange catalyzed by human carbonic anhydrase C at chemical equilibrium.

The effects of human carbonic anhydrase C on the 13C nuclear magnetic resonance spectra of equilibrium mixtures of 13CO2 and NaH13CO3 were measured at 67.89 MHz. Enzyme-catalyzed CO2-HCO-3 exchange rates were estimated from the linewidths of the resonances. The results show that: (a) the maximal exchange rates are larger than the maximal turnover rates; (b) the exchange is equally rapid with 1H2O or with 2H2O as solvents; (c) the exchange is equally rapid in the presence or in the absence of added buffers; (d) the apparent substrate binding is weaker than predicted if steady-state Km values are assumed to represent substrate dissociation constants. The main conclusion concerning the catalytic mechanism of the enzyme is that the proton-transfer processes which limit turnover rates in the steady state are not directly involved in CO2-HCO-3 exchange. In addition, the results suggest that CO2-HCO-3 interconversion takes place by a nucleophilic mechanism, such as a reversible reaction of zinc-coordinated OH- with CO2.