Origins of deuterium kinetic isotope effects on the proton transfers of the bacteriorhodopsin photocycle

Deuterium kinetic isotope effects (KIE) were measured, and proton inventory plots were constructed, for the rates of reactions in the photocycles of wild-type bacteriorhodopsin and several site-specific mutants. Consistent with earlier reports from many groups, very large KIEs were observed for the third land largest) rise component for the M state and for the decay of the O state, processes both linked to proton transfers in the extracellular region. The proton inventory plots (ratio of reaction rates in mixtures of H2O and D2O to that in H2O vs mole fraction of D2O) were approximately linear for the first and second M rise components and for M decay, as well as for O decay, indicating that the rates of these reactions are limited by simple proton transfer. Uniquely, the third rise component of M land in the D96N mutant also a fourth rise component) exhibited a strongly curved proton inventory plot, suggesting that its rate, which largely accounts for the rate of deprotonation of the retinal Schiff base, depends on a complex multiproton process. This curvature is observed also in the E194Q, E204Q, and Y57F mutants but not in the R82A mutant. From these findings, and from the locations of bound water in the extracellular region in the crystal structure of the protein [Luecke, Schobert, Richter, Cartailler, and Lanyi (1999) J. Mol. Biol. 291, 899-911], we suspect that the effects of deuterium substitution on the formation of the M state originate from cooperative rearrangements of the extensively hydrogen-bonded water molecules 401, 402, and 406 near Asp-85 and Arg-82.