SOLVENT HYDROGEN ISOTOPE EFFECTS AND ANION INHIBITION OF CO2 HYDRATION CATALYZED BY CARBONIC-ANHYDRASE FROM PISUM-SATIVUM

Chloroplast carbonic anhydrase from Pisum sativum has been studied to elucidate the catalytic mechanism and to test if the mechanism proposed for human carbonic anhydrase II is also valid for pea carbonic anhydrase. The catalytic activity was found to depend on the chemical nature of the buffer. Barbital buffer gives the highest turnover number at infinite buffer concentration and the lowest K-m value with respect to the buffer, while the kinetic parameters obtained in the imidazole-type buffer, 1-methylimidazole, do not differ from those obtained using the biological-type buffer Mops. The anion inhibition of CO2 hydration was investigated using SCN- at pH 6-9. The binding of the anion was found to be pH dependent with the strongest interaction at low pH. We obtained an uncompetitive inhibition pattern at high pH and noncompetitive inhibition patterns at pH 7 and low pH. The catalytic mechanism was further tested by measurements of the solvent hydrogen isotope effects on the kinetic parameters for CO2 hydration. The observed effects were comparatively small with a k(cat) value of approximately 2 irrespective of the pH. The effect on k(cat)/K-m and on K-m changes when going from high pH to p(H) 7 and low pH. At high pH, the solvent isotope effect in K-m is at least 3, giving a value below 1 for k(cat)/K-m, while at pH 7 and low pH the major effect is found in k(cat)/K-m with values of 2.6 and 2.9. The dependence of the CO2-hydration activity on the buffer concentration is in agreement with a ping-pong mechanism with buffer acting as a second substrate. This is analogous to the behaviour of human carbonic anhydrase II. The inhibition patterns and the observed isotope effects at high pH can also be explained within the framework of the catalytic mechanism for human carbonic anhydrase II, with a rate-determining and buffer-dependent part. The results are consistent with a mechanism involving a proton transfer that contributes to rate limitation. However, the isotope effects found at pH 7 and low pH indicate that some part of the mechanism has changed. Moreover, we cannot decide whether the mechanism for pea carbonic anhydrase involves an internal proton-shuttle group, or if the buffer molecule acts in a direct proton transfer from the zinc-coordinated water.