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Active internal waters in the bacteriorhodopsin photocycle. A comparative study of the L and M intermediates at room and cryogenic temperatures by infrared spectroscopy.

We present time-resolved room-temperature infrared difference spectra for the bacteriorhodopsin (bR) photocycle at 8 cm (-1) spectral and 5 micros temporal resolution, from 4000 to 800 cm (-1). An in situ hydration method allowed for a controlled and stable sample hydration (92% relative humidity), largely improving the quality of the data without affecting the functionality of bR. Experiments in both H 2 (16)O and H 2 (18)O were conducted to assign bands to internal water molecules. Room-temperature difference spectra of the L and M intermediates minus the bR ground state (L-BR and M-BR, respectively) were comprehensively compared with their low-temperature counterparts. The room-temperature M-BR spectrum was almost identical to that obtained at 230 K, except for a continuum band. The continuum band contains water vibrations from this spectral comparison between H 2 (16)O and H 2 (18)O, and no continuum band at 230 K suggests that the protein/solvent dynamics are insufficient for deprotonation of the water cluster. On the other hand, an intense positive broadband in the low-temperature L-BR spectrum (170 K) assigned to the formation of a water cavity in the cytoplasmic domain is absent at room temperature. This water cavity, proposed to be an essential feature for the formation of L, seems now to be a low-temperature artifact caused by restricted protein dynamics at 170 K. The observed differences between low- and room-temperature FTIR spectra are further discussed in light of previously reported dynamic transitions in bR. Finally, we show that the kinetics of the transient heat relaxation of bR after photoexcitation proceeds as a thermal diffusion process, uncorrelated with the photocycle itself.