Are mutated enzymes good models for interpretation of intrinsic isotope effects?

Viewpoint: Carbon isotope effect predictions for enzymes involved in the primary carbon metabolism of plant leaves

Carbon isotope effects of enzymes involved in primary carbon metabolism are key parameters in our understanding of plant metabolism. Nevertheless, some of them are poorly known because of the lack of in vitro experimental data on purified enzymes. Some studies have focused on theoretical predictions of isotope effects. Here we show how quantum chemical calculations can be adapted for calculation of isotope effects for the Rubisco-catalysed carboxylation and oxygenation reactions and the citrate synthase reaction. The intrinsic isotope effect of the carboxylation by Rubisco appears to be much smaller than previously thought, being close to the overall isotope effect of the reaction that is, between 25 and 30 per mil. The same applies to the enzyme citrate synthase, that catalyses the first step of the Krebs cycle, with an isotope effect of around 23 per mil. Combined with the isotope effects of equilibrium reactions calculated with β-factors, the Krebs cycle then has an overall isotope effect that depletes organic acids in ¹³C.

Dependence of Transition State Structure on Substrate: The Intrinsic C-13 Kinetic Isotope Effect Is Different for Physiological and Slow Substrates of the Ornithine Decarboxylase Reaction Because of Different Hydrogen Bonding Structures

Ornithine decarboxylase is the first and the rate-controlling enzyme in polyamine biosynthesis; it decarboxylates l-ornithine to form the diamine putrescine. We present calculations performed using a combined quantum mechanical and molecular mechanical (QM/MM) method with the AM1 semiempirical Hamiltonian for the wild-type ornithine decarboxylase reaction with ornithine (the physiological substrate) and lysine (a "slow" substrate) and for mutant E274A with ornithine substrate. The dynamical method is variational transition state theory with quantized vibrations. We employ a single reaction coordinate equal to the carbon-carbon distance of the dissociating bond, and we find a large difference between the intrinsic kinetic isotope effect for the physiological substrate, which equals 1.04, and that for the slow substrate, which equals 1.06. This shows that, contrary to a commonly accepted assumption, kinetic isotope effects on slow substrates are not always good models of intrinsic kinetic isotope effects on physiological substrates. Furthermore, analysis of free-energy-based samples of transition state structures shows that the differences in kinetic isotope effects may be traced to different numbers of hydrogen bonds at the different transition states of the different reactions.

Chlorine kinetic isotope effects on enzymatic dehalogenations

Enzymatic dehalogenation reactions are important for the bioremediation of the environment because of the increasing anthropogenic pollution with halogen-containing organic compounds. Chlorine kinetic isotope effects have been measured for four hydrolytic dehalogenases. On the basis of these isotope effects, several details of the mechanisms of the enzymatic dehalogenation reactions have been revealed.