[No authors listed]
The tryptophan synthase alpha2beta2 complex catalyzes the last two steps in the biosynthesis of l-tryptophan in bacteria, plants, and fungi, the conversion of indole-3-glycerol phosphate and l-serine to l-tryptophan, glyceraldehyde 3-phosphate, and water. The beta-subunit binds pyridoxal 5'-phosphate and catalyzes the beta-replacement reaction with serine and indole. Structural, spectral, and kinetic studies indicate that different monovalent cations stabilize the alternative enzyme conformations and equilibrium distribution of the internal, external, and alpha-aminoacrylate Schiff base. To improve our understanding of the role of monovalent cations, the pH dependence of steady-state and pre-steady-state kinetic parameters and primary kinetic deuterium isotope effects were measured in the presence of l-serine and [alpha-2H]-l-serine in the absence and presence of Na+, K+, and Cs+. For the interpretation of the data obtained in this study, it was necessary to re-interpret a number of results published previously. Overall, data suggest that the enzyme exists in two conformers that equilibrate slowly either in the absence of substrates and monovalent cations or in the presence of K+ or Cs+, whereas they equilibrate faster in the presence of Na+. The rate of interconversion of the conformers increases as a group on the enzyme with a pKa of approximately 8 becomes deprotonated. The pH dependence of deuterium isotope effects is suggestive of a mechanism in which a pH-dependent conformational change that closes the active site precedes the chemical steps, likely a result of formation of one or more salt bridges. As the pH increases, the reaction becomes more committed to proceed to products, which causes the deuterium isotope effect to decrease to a value of unity at high pH. The closure of the site is modulated by the different monovalent cations and is fastest in the presence of Na+, which exhibits the maximum isotope effect of 5.7 (likely the intrinsic effect) on V/Kserine, and slowest in the presence of Cs+, which exhibits the smallest isotope effect of approximately 1.5. The isotope effect on V, in all cases, indicates a contribution to rate limitation from steps in the second half of the reaction. Finally, in the presence of Na+, the steady-state isotope effect on V is greater than that on the pre-steady-state rate constant for decay of the external Schiff base, suggesting that the rate of conversion of the two conformers of the internal aldimine contributes to the pre-steady-state rate, but not the steady-state rate because the high serine concentration traps the enzyme in the active E-serine complex before it can decay to the less active form.
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