Relocation of water molecules between the Schiff base and the Thr46-Asp96 region during light-driven unidirectional proton transport by bacteriorhodopsin: an FTIR study of the N intermediate

A key event in light-driven proton pumping by bacteriorhodopsin is the formation of the L intermediate, whose transition to M is accompanied by the first proton transfer step, from the Schiff base to Asp85 on the extracellular side. Subsequent reprotonation of the Schiff base from the other side of the membrane to form the N intermediate is crucial for unidirectional proton transport. Previous FTIR studies have suggested that the intense water O-D stretching vibration bands which appear in L at 2589, 2605, and 2621 cm(-)(1) are due to a cluster of polarized water molecules connecting the Schiff base to the Thr46-Asp96 region closer to the cytoplasmic surface. In the present study the difference spectrum was obtained of the N intermediate with its photoproduct N', formed after irradiating N at 80 K. The water O-D stretching vibrations of N appear as a broad feature in a similar frequency region with a similar intensity to those of L. This feature is also affected by T46V like in L. However, the intensities of these water vibrations of N nearly returned to the initial unphotolyzed state upon formation of N', unlike those of L which are preserved in L'. An exception was V49A, which preserved the intense water vibrations of N in N'. The results suggest that both L and N have a water cluster extending from the Schiff base to Thr46. The surrounding protein moiety stabilizes the water cluster in L, but in N it is stabilized mostly by interaction with the Schiff base.     

Crystal structure of the L intermediate of bacteriorhodopsin: evidence for vertical translocation of a water molecule during the proton pumping cycle

For structural investigation of the L intermediate of bacteriorhodopsin, a 3D crystal belonging to the space group P622 was illuminated with green light at 160 K and subsequently with red light at 100 K. This yielded a approximately 1:4 mixture of the L intermediate and the ground-state. Diffraction data from such crystals were collected using a low flux of X-rays ( approximately 2 x 10(15) photons/mm2 per crystal), and their merged data were compared with those from unphotolyzed crystals. These structural data, together with our previous data, indicate that the retinal chromophore, which is largely twisted in the K-intermediate, takes a more planar 13-cis, 15-anti configuration in the L intermediate. This configurational change, which is accompanied by re-orientation of the Schiff base N-H bond towards the intracellular side, is coupled with a large rotation of the side-chain of an amino acid residue (Leu93) making contact with the C13 methyl group of retinal. Following these motions, a water molecule, at first hydrogen-bonded to the Schiff base and Asp85, is dragged to a space that is originally occupied by Leu93. Diffraction data from a crystal containing the M intermediate showed that this water molecule moves further towards the intracellular side in the L-to-M transition. It is very likely that detachment of this water molecule from the protonated Schiff base causes a significant decrease in the pKa of the Schiff base, thereby facilitating the proton transfer to Asp85. On the basis of these observations, we argue that the vertical movement of a water molecule in the K-to-L transition is a key event determining the directionality of proton translocation in the protein.     

Changes in hydrogen bonding and environment of tryptophan residues on helix F of bacteriorhodopsin during the photocycle: a time-resolved ultraviolet resonance Raman study

Protein structural changes during the photocycle of bacteriorhodopsin were examined by time-resolved ultraviolet resonance Raman (UVRR) spectroscopy. Most of the 244-nm UVRR difference signals of Trp were assigned to either Trp182 or Trp189 using the Trp182 --> Phe and Trp189 --> Phe mutants. The W17 mode of Trp182 shows a wavenumber downshift in the M(1) --> M(2) transition, indicating an increase in hydrogen bonding strength at the indole nitrogen. On the other hand, Trp189 shows Raman intensity increases of the W16 and W18 modes ascribable to an increased hydrophobic interaction. These observations suggest that the tilt of helix F, which ensures that reprotonation of the Schiff base is from the cytoplasmic side, occurs in the M(1) --> M(2) transition. In the M(2) --> N transition, the environment of Trp189 returns to the initial state, whereas the hydrophobic interaction of Trp182 decreases drastically. The decrease in hydrophobic interaction of Trp182 in the N state suggests an invasion of water molecules that promote the proton transfer from Asp96 to the Schiff base. Structural reorganization of the protein after the tilt of helix F may be important for efficient reprotonation of the Schiff base.     

Relocation of internal bound water in bacteriorhodopsin during the photoreaction of M at low temperatures: an FTIR study

Changes in the FTIR difference spectra upon photoconversion of the M intermediate to its photoproduct(s) M' were studied in wild-type bacteriorhodopsin and several mutants at low temperatures. The studies aimed at examining whether internally bound water molecules interact with the chromophore and the key residues Asp85 and Asp96 in M, and whether these water molecules participate in the reprotonation of the Schiff base. We have found that three water molecules are perturbed by the isomerization of the chromophore in the M --> M' transition at 80 K. The perturbation of one water molecule, detected as a bilobe at 3567(+)/3550(-) cm(-)(1), relaxed in parallel with the relaxation of an Asp85 perturbation upon increasing temperature from 80 to 100 and 133 K (before the reprotonation of the Schiff base). Two water bands of M at 3588 and 3570 cm(-)(1) shift to 3640 cm(-)(1) upon photoconversion at 173 K. These bands were attributed to water molecules which are located in the vicinity of the Schiff base and Asp85 (Wat85). In the M to M' transition at 80 and 100 K, where the Schiff base remained unprotonated, the Wat85 pair stayed in similar states to those in M. The reprotonation of the Schiff base at 133 K occurred without the restoration of the Wat85 band around 3640 cm(-)(1). This band was restored at higher temperatures. Two water molecules in the region surrounded by Thr46, Asp96, and Phe219 (Wat219) were perturbed in the M to M' transition at 80 K and relaxed in parallel with the relaxation of the perturbation of Asp96 upon increasing the temperature. Mutant studies show that upon photoisomerization of the chromophore at 80 K one of the Wat219 water molecules moves closer to Val49 (located near the lysine side chain attached to retinal, and close to the Schiff base). These data along with our previous results indicate that the water molecules in the cytoplasmic domain participate in the connection of Asp96 with the Schiff base and undergo displacement during photoconversions, presumably shuttling between the Schiff base and a site close to Asp96 in the L to M to N transitions.     

Hydrogen-bonding alterations of the protonated Schiff base and water molecule in the chloride pump of Natronobacterium pharaonis

Halorhodopsin is a light-driven chloride ion pump. Chloride ion is bound in the Schiff base region of the retinal chromophore, and unidirectional chloride transport is probably enforced by the specific hydrogen-bonding interaction with the protonated Schiff base and internal water molecules. In this article, we study hydrogen-bonding alterations of the Schiff base and water molecules in halorhodopsin of Natronobacterium pharaonis (pHR) by assigning their N-D and O-D stretching vibrations in D(2)O, respectively. Highly accurate low-temperature Fourier transform infrared spectroscopy revealed that hydrogen bonds of the Schiff base and water molecules are weak in the unphotolyzed state, whereas they are strengthened upon retinal photoisomerization. Halide dependence of the stretching vibrations enabled us to conclude that the Schiff base forms a direct hydrogen bond with Cl(-) only in the K intermediate. Hydrogen bond of the Schiff base is further strengthened in the L(1) intermediate, whereas the halide dependence revealed that the acceptor is not Cl(-), but presumably a water molecule. Thus, it is concluded that the hydrogen-bonding interaction between the Schiff base and Cl(-) is not a driving force of the motion of Cl(-). Rather, the removal of its hydrogen bonds with the Schiff base and water(s) makes the environment around Cl(-) less polar in the L(1) intermediate, which presumably drives the motion of Cl(-) from its binding site to the cytoplasmic domain.     

Water structural changes in the L and M photocycle intermediates of bacteriorhodopsin as revealed by time-resolved step-scan Fourier transform infrared (FTIR) spectroscopy

In previous Fourier transform infrared (FTIR) studies of the photocycle intermediates of bacteriorhodopsin at cryogenic temperatures, water molecules were observed in the L intermediate, in the region surrounded by protein residues between the Schiff base and Asp96. In the M intermediate, the water molecules had moved away toward the Phe219-Thr46 region. To evaluate the relevance of this scheme at room temperature, time-resolved FTIR difference spectra of bacteriorhodopsin, including the water O-H stretching vibration frequency regions, were recorded in the micro- and millisecond time ranges. Vibrational changes of weakly hydrogen-bonded water molecules were observed in L, M, and N. In each of these intermediates, the depletion of a water O-H stretching vibration at 3645 cm-1, originating from the initial unphotolyzed bacteriorhodopsin, was observed as a trough in the difference spectrum. This vibration is due to the dangling O-H group of a water molecule, which interacts with Asp85, and its absence in each of these intermediates indicates that there is perturbation of this O-H group. The formation of M is accompanied by the appearance of water O-H stretching vibrations at 3670 and 3657 cm-1, the latter of which persists to N. The 3670 cm-1 band of M is due to water molecules present in the region surrounded by Thr46, Asp96, and Phe219. The formation of L at 298 K is accompanied by the perturbations of Asp96 and the Schiff base, although in different ways from what is observed at 170 K. Changes in a broad water vibrational feature, centered around 3610 cm-1, are kinetically correlated with the L-M transition. These results imply that, even at room temperature, water molecules interact with Asp96 and the Schiff base in L, although with a less rigid structure than at cryogenic temperatures.     

Localization and orientation of functional water molecules in bacteriorhodopsin as revealed by polarized Fourier transform infrared spectroscopy.

Linear dichroic difference Fourier transform infrared spectra upon formation of the M photointermediate were recorded with oriented purple membranes. The purpose was to determine the angle of the directions of the dipole moments of 1) the water molecule whose O-H stretching vibration appears at 3643 cm-1 for the unphotolyzed state and 3671 cm-1 for the M intermediate, and 2) the C=O bond of protonated Asp85 in the M intermediate. The angle of 36 degrees we find for the C=O of the protonated Asp85 in the M intermediate is not markedly different from 26 degrees for unprotonated Asp85 in the model based on cryoelectron diffraction, indicating the absence of gross orientation changes in Asp85 upon its protonation. The O-H band at 3671 cm-1 of a water molecule in the M intermediate, although its position has not determined, is fixed almost parallel to the membrane plane. For the unphotolyzed state the angle of the water O-H to the membrane normal was determined to be 60 degrees. On the basis of these data and the structural model, we place the water molecule in the unphotolyzed state at a position where it forms hydrogen bonds with the Schiff base, Asp85, Asp212, and Trp86.     

Interaction of internal water molecules with the schiff base in the L intermediate of the bacteriorhodopsin photocycle

In the photocycle of bacteriorhodopsin (BR), the first proton movement, from the Schiff base to Asp85, occurs after the formation of the L intermediate. In L, the C [double bond] N bond of the Schiff base is strained, and the nitrogen interacts strongly with its counterion. The present study seeks to detect the interaction of internal water molecules with the Schiff base in L using difference FTIR spectroscopy at 170 K. The coupled modes of the hydrogen-out-of plane bending vibrations (HOOPs) of the N-H and C(15)-H of the protonated Schiff base are detected as a broad band centered at 911 cm(-1) for BR. A set of bands at 1073, 1064, and 1056 cm(-1) for L is shown to arise from the coupling of the HOOP with the overtones of interacting water O-H vibrations. Interaction with water was shown by the decreased intensity of the HOOPs of L in H(2)(18)O and by the influence of mutants that have been shown to perturb specific internal water molecules in BR. In contrast, the HOOP band of initial BR was not affected by these mutations. In D85N, the coupled HOOP of BR is depleted, while the coupled HOOPs of L are shifted. The results indicate that the Schiff base interacts with water in the L state but in a different manner than in the BR state. Moreover, the effects of mutations suggest that cytoplasmic water close to Thr46 (Wat46) either interacts stronger with the Schiff base in L or that it is important in stabilizing another water that does.     

Fourier transform infrared study of the N intermediate of bacteriorhodopsin

Visible absorption spectroscopic experiments show that the N intermediate is the main photoproduct of a highly hydrated film of the light-adapted bacteriorhodopsin (70% water by weight) at pH 10 and 274 K. The difference Fourier transform infrared spectrum between the N intermediate and unphotolyzed light-adapted bacteriorhodopsin was recorded under these conditions. A small amount of the M intermediate present did not affect this spectrum significantly. The difference spectrum exhibited a positive band at 1755 cm-1 (probably due to Asp-85) and a negative band at 1742 cm-1 (due to Asp-96), neither of which was observed for the M intermediate. The spectrum of the N intermediate at pH 7 was nearly identical with that at pH 10. Spectra at pH 10 also were measured with isotope-substituted samples. A vibrational band at 1692 cm-1 due to the peptide bond disappeared, and a band at 1558 cm-1 emerged upon formation of the N intermediate. The spectrum also displayed bands containing the N-H and C15-H in-plane bending vibrational modes at 1394 and 1303 cm-1. These frequencies are similar to those of the L intermediate while the intensities of these bands are larger than those in the L intermediate, suggesting that the Schiff bases of both the L and N intermediates have a strong hydrogen-bonding interaction with the protein and that the C12-H to C15-H region of the chromophore is less twisted in the N intermediate than in the L intermediate.     

Structural changes due to the deprotonation of the proton release group in the M-photointermediate of bacteriorhodopsin as revealed by time-resolved FTIR spectroscopy

One of the steps in the proton pumping cycle of bacteriorhodopsin (BR) is the release of a proton from the proton-release group (PRG) on the extracellular side of the Schiff base. This proton release takes place shortly after deprotonation of the Schiff base (L-to-M transition) and results in an increase in the pKa of Asp85, which is a crucial mechanistic step for one-way proton transfer for the entire photocycle. Deprotonation of the PRG can also be brought about without photoactivation, by raising the pH of the enzyme (pKa of PRG; approximately 9). Thus, comparison of the FTIR difference spectrum for formation of the M intermediate (M minus initial unphotolyzed BR state) at pH 7 to the corresponding spectrum generated at pH 10 may reveal structural changes specifically associated with deprotonation of the PRG. Vibrational bands of BR that change upon M formation are distributed across a broad region between 2120 and 1685 cm(-1). This broad band is made up of two parts. The band above 1780 cm(-1), which is insensitive to C15-deuteration of the retinal, may be due to a proton delocalized in the PRG. The band between 1725 and 1685 cm(-1), on the lower frequency side of the broad band, is sensitive to C15-deuteration. This band may arise from transition dipole coupling of the vibrations of backbone carbonyl groups in helix G with the side chain of Tyr57 and with the C15H of the Schiff base. In M, these broad bands are abolished, and the 3657 cm(-1) band, which is due to the disruption of the hydrogen bonding of a water molecule, probably with Arg82, appears. Loss of the interaction of the backbone carbonyl groups in helix G with Tyr57 and the Schiff base, and separation of Tyr57 from Arg82, may be causes of these spectral changes, leading to the stabilization of the protonated Asp85 in M.     

FTIR study of the retinal Schiff base and internal water molecules of proteorhodopsin

Proteorhodopsin (PR), an archaeal-type rhodopsin found in marine bacteria, is a light-driven proton pump similar to bacteriorhodopsin (BR). It is known that Asp97, a counterion of the protonated Schiff base, possesses a higher pKa ( approximately 7) compared to that of homologous Asp85 in BR (<3). This suggests that PR has a hydrogen-bonding network different from that of BR. We previously reported that a strongly hydrogen-bonded water molecule is observed only in the alkaline form of PR, where Asp97 is deprotonated (Furutani, Y., Ikeda, D., Shibata, M., and Kandori, H. (2006) Chem. Phys. 324, 705-708). This is probably correlated with the pH-dependent proton pumping activity of PR. In this work, we studied the water-containing hydrogen-bonding network in the Schiff base region of PR by means of Fourier-transform infrared (FTIR) spectroscopy at 77 K. [zeta-15N]Lys-labeling and 18O water were used for assigning the Schiff base N-D and water O-D stretching vibrations in D2O, respectively. The frequency upshift of the N-D stretch in the primary K intermediate is much smaller for PR than for BR, indicating that the Schiff base forms a hydrogen bond after retinal photoisomerization. We then measured FTIR spectra of the mutants of Asp97 (D97N and D97E) and Asp227 (D227N and D227E) to identify the amino acid interacting with the Schiff base in the K state. The PRK minus PR spectra of D97N and D97E were similar to those of the acidic and alkaline forms, respectively, of the wild type implying that the structural changes upon retinal photoisomerization are not influenced by the mutation at Asp97. In contrast, clear spectral differences were observed in D227N and D227E, including vibrational bands of the Schiff base and water molecules. It is concluded that Asp227 plays a crucial role during the photoisomerization process, though Asp97 acts as the primary counterion in the unphotolyzed state of PR.     

Structural changes of water in the Schiff base region of bacteriorhodopsin: proposal of a hydration switch model

In a light-driven proton-pump protein, bacteriorhodopsin (BR), three water molecules participate in a pentagonal cluster that stabilizes an electric quadrupole buried inside the protein. In low-temperature Fourier transform infrared (FTIR) K minus BR spectra, the frequencies of water bands suggest extremely strong hydrogen bonding conditions in BR. The three observed water O-D stretches, at 2323, 2292, and 2171 cm(-1), are probably associated with water that interacts with the negative charges in the Schiff base region. Retinal isomerization weakens these hydrogen bonds in the K intermediate, but not in the later intermediates such as L, M, and N. In these states, spectral changes of water bands appeared only in the >2500 cm(-1) region, which correspond to weak hydrogen bonds. This observation suggests that after the K state the water molecules in the Schiff base region find a hydrogen bonding acceptor. We propose here a model for the mechanism of proton transfer from the Schiff base to Asp85. In the "hydration switch model", hydration of a water molecule is switched in the M intermediate from Asp85 to Asp212. This will have increased the pK(a) of the proton acceptor, and the proton transfer is from the Schiff base to Asp85. The present results also suggest that the deprotonated Asp96 in the N intermediate is stabilized in a manner different from that of Asp85 in BR.     

Chromophore-protein-water interactions in the L intermediate of bacteriorhodopsin: FTIR study of the photoreaction of L at 80 K.

Using FTIR spectroscopy, perturbations of several residues and internal water molecules have been detected when light transforms all-trans bacteriorhodopsin (BR) to its L intermediate having a 13-cis chromophore. Illumination of L at 80 K results in an intermediate L' absorbing around 550 nm. L' thermally converts to the original BR only at >130 K. In this study, we used the light-induced transformation of L to L' at 80 K to identify some amino acid residues and water molecules that closely interact with the chromophore and distinguish them from those residues not affected by the photoreaction. The L minus L' FTIR difference spectrum shows that the chromophore in L' is in the all-trans configuration. The perturbed states of Asp96 and Val49 and of the environment along the aliphatic part of the retinal and Lys216 seen in L are not affected by the L --> L' photoreaction. On the other hand, the environments of the Schiff base of the chromophore, of Asp115, and of water molecules close to Asp85 returned in L' to their state in which they originally had existed in BR. The water molecules that are affected by the mutations of Thr46 and Asp96 also change to a different state in the L --> L' transition, as indicated by transformation of a water O-H vibrational band at 3497 cm-1 in L into an intense peak at 3549 cm-1 in L'. Notably, this change of water bands in the L --> L' transition at 80 K is entirely different from the changes observed in the BR --> K photoreaction at the same temperature, which does not show such intense bands. These results suggest that these water molecules move closer to the Schiff base as a hydrogen bonding cluster in L and L', presumably to stabilize its protonated state during the BR to L transition. They may contribute to the structural constraints that prevent L from returning to the initial BR upon illumination at 80 K.     

Arginine-82 regulates the pKa of the group responsible for the light-driven proton release in bacteriorhodopsin.

In wild-type bacteriorhodopsin light-induced proton release occurs before uptake at neutral pH. In contrast, in mutants in which R82 is replaced by a neutral residue (as in R82A and R82Q), only a small fraction of the protons is released before proton uptake at neutral pH; the major fraction is released after uptake. In R82Q the relative amounts of the two types of proton release, "early" (preceding proton uptake) and "late" (following proton uptake), are pH dependent. The main conclusions are that 1) R82 is not the normal light-driven proton release group; early proton release can be observed in the R82Q mutant at higher pH values, suggesting that the proton release group has not been eliminated. 2) R82 affects the pKa of the proton release group both in the unphotolyzed state of the pigment and during the photocycle. In the wild type (in 150 mM salt) the pKa of this group decreases from approximately 9.5 in the unphotolyzed pigment to approximately 5.8 in the M intermediate, leading to early proton release at neutral pH. In the R82 mutants the respective values of pKa of the proton release group in the unphotolyzed pigment and in M are approximately 8 and 7.5 in R82Q (in 1 M salt) and approximately 8 and 6.5 in R82K (in 150 mM KCl). Thus in R82Q the pKa of the proton release group does not decrease enough in the photocycle to allow early proton release from this group at neutral pH. 3) Early proton release in R82Q can be detected as a photocurrent signal that is kinetically distinct from those photocurrents that are due to proton movements from the Schiff base to D85 during M formation and from D96 to the Schiff base during the M-->N transition. 4) In R82Q, at neutral pH, proton uptake from the medium occurs during the formation of O. The proton is released during the O-->bacteriorhodopsin transition, probably from D85 because the normal proton release group cannot deprotonate at this pH. 5) The time constant of early proton release is increased from 85 microseconds in the wild type to 1 ms in R82Q (in 150 mM salt). This can be directly attributed to the increase in the pKa of the proton release group and also explains the uncoupling of proton release from M formation. 6) In the E204Q mutant only late proton release is observed at both neutral and alkaline pH, consistent with the idea that E204 is the proton release group. The proton release is concurrent with the O-->bacteriorhodopsin transition, as in R82Q at neutral pH.     

Water-mediated hydrogen-bonded network on the cytoplasmic side of the Schiff base of the L photointermediate of bacteriorhodopsin

The L intermediate in the proton-motive photocycle of bacteriorhodopsin is the starting state for the first proton transfer, from the Schiff base to Asp85, in the formation of the M intermediate. Previous FTIR studies of L have identified unique vibration bands caused by the perturbation of several polar amino acid side chains and several internal water molecules located on the cytoplasmic side of the retinylidene chromophore. In the present FTIR study we describe spectral features of the L intermediate in D(2)O in the frequency region which includes the N-D stretching vibrations of the backbone amides. We show that a broad band in the 2220-2080 cm(-1) region appears in L. By use of appropriate (15)N labeling and mutants, the lower frequency side of this band in L is assigned to the amides of Lys216 and Gly220. These amides are coupled to each other, and interact with Thr46 and Val49 in helix B and Asp96 in helix C via weakly H-bonding water molecules that exhibit O-D stretching vibrations at 2621 and 2605 cm(-1). These water molecules are part of a hydrogen-bonded network characteristic of L which includes other water molecules located closer to the chromophore that exhibit an O-D stretching vibration at 2589 cm(-1). This structure, extending from the Schiff base to the internal proton donor Asp96, stabilizes L and affects the L-to-M transition.     

Role of Gln1029 in the photoactivation processes of the LOV2 domain in adiantum phytochrome3

Phototropin (phot) is a blue-light receptor in plants. The molecule has two FMN (flavin mononucleotide)-binding domains named the LOV (light-oxygen-voltage) domain, that is a subset of a PAS (per-arnt-sim) superfamily. Illumination of phot-LOV domains produces a covalent C(4a) flavin-cysteinyl adduct, which is called the S390 intermediate state. According to the crystal structures of the LOV2 domain of Adiantum phytochrome3 (phy3), a fusion protein of phot containing the phytochrome chromophoric domain, in the unphotolyzed and S390 states, and the side chain of Gln1029 switches hydrogen bonds with the FMN chromophore. Gln1029 is the hydrogen-bonding donor of the C(4)=O group of FMN in the unphotolyzed state, whereas Gln1029 is the hydrogen-bonding acceptor of the N(5)-H group of FMN in S390. In this paper, we measured the light-induced structural changes in the Q1029L mutant protein of phy3-LOV2 by means of low-temperature FTIR spectroscopy, and the obtained spectra are compared with those of the wild type. Low-temperature UV-visible spectroscopy of Q1029L detected only one intermediate state, S390, at 77-295 K, as well as the wild type. The C(4)=O stretch of FMN at 1710 cm(-1) is shifted to 1723 cm(-1) in Q1029L, presumably because of the lack of hydrogen bonds between Gln1029 and FMN. Upon formation of S390, the C(4)=O group hydrogen bond is weakened in both wild type and Q1029L. These observations are fully consistent with the X-ray crystal structures of the unphotolyzed and S390 states. On the other hand, the C(4)=O stretch of FMN and amide-I vibrations are temperature-independent in Q1029L, in contrast to wild type, in which highly temperature-dependent FTIR spectra are detected. Amide-I vibrations of Q1029L at room temperature are similar to those of the wild type at 77-150 K but not at room temperature. These facts imply that the Q1029L mutant protein lacks progressive protein structural changes following flavin-cysteinyl adduct formation in the wild type, which eventually alter structures of beta sheet and alpha helix in the protein moiety. Hydrogen-bonding interaction of Gln1029 with the FMN chromophore likely plays an important role in the protein structural changes of phy3-LOV2.     

FTIR spectroscopy of the all-trans form of Anabaena sensory rhodopsin at 77 K: hydrogen bond of a water between the Schiff base and Asp75

Anabaena sensory rhodopsin (ASR) is an archaeal-type rhodopsin found in eubacteria, and is believed to function as a photosensor interacting with a 14 kDa soluble protein. Most of the residues in the retinal binding pocket are similar in ASR except proline 206, where the corresponding amino acid in other archaeal-type rhodopsins is highly conserved aspartate that constitutes the counterion complex of the positively charged protonated Schiff base. The recently determined X-ray crystallographic structure of ASR revealed a water molecule between the Schiff base and Asp75 [Vogeley, L., Sineshchekov, O. A., Trivedi, V. D., Sasaki, J., Spudich, J. L., and Luecke, H. (2004) Science 306, 1390-1393], as well as the case for bacteriorhodopsin (BR), a typical transport rhodopsin working as a proton pump. In this study, we applied low-temperature Fourier transform infrared (FTIR) spectroscopy to the all-trans form of ASR at 77 K, and compared the local structure around the chromophore and their structural changes upon retinal photoisomerization with those of BR. The K intermediate minus ASR difference spectra were essentially similar to those for BR, indicating that photoisomerization yields formation of the distorted 13-cis form. In contrast, little amide I bands were observed for ASR. The presence of the proline-specific vibrational bands suggests that peptide backbone alterations are limited to the Pro206 moiety in the K state of ASR. The N-D stretching of the Schiff base is presumably located at 2163 (-) and 2125 (-) cm(-)(1) in ASR, suggesting that the hydrogen bonding strength of the Schiff base in ASR is similar to that in BR. A remarkable difference between ASR and BR was revealed from water bands. Although ASR possesses a bridged water molecule like BR, the O-D stretching of water molecules was observed only in the >2500 cm(-)(1) region for ASR. We interpreted that the weak hydrogen bond of the bridged water between the Schiff base and Asp75 originates from their geometry. Since ASR does not pump protons, our result supports the working hypothesis that the existence of strongly hydrogen bonded water molecules is essential for proton pumping activity in archaeal rhodopsins.     

Hydration switch model for the proton transfer in the Schiff base region of bacteriorhodopsin

In a light-driven proton-pump protein, bacteriorhodopsin (BR), protonated Schiff base of the retinal chromophore and Asp85 form ion-pair state, which is stabilized by a bridged water molecule. After light absorption, all-trans to 13-cis photoisomerization takes place, followed by the primary proton transfer from the Schiff base to Asp85 that triggers sequential proton transfer reactions for the pump. Fourier transform infrared (FTIR) spectroscopy first observed O-H stretching vibrations of water during the photocycle of BR, and accurate spectral acquisition has extended the water stretching frequencies into the entire stretching frequency region in D(2)O. This enabled to capture the water molecules hydrating with negative charges, and we have identified the water O-D stretch at 2171 cm(-1) as the bridged water interacting with Asp85. We found that retinal isomerization weakens the hydrogen bond in the K intermediate, but not in the later intermediates such as L, M, and N. On the basis of the observation particularly on the M intermediate, we proposed a model for the mechanism of proton transfer from the Schiff base to Asp85. In the "hydration switch model", hydration of a water molecule is switched in the M intermediate from Asp85 to Asp212. This will have raised the pK(a) of the proton acceptor, and the proton transfer is from the Schiff base to Asp85.     

Structural changes of water molecules during the photoactivation processes in bovine rhodopsin

Internal water molecules of rhodopsins play an important role in stabilizing the crucial ion pair comprised by the protonated retinal Schiff base and its counterion. Previous low-temperature FTIR spectroscopy of archaeal rhodopsins observed water O-D stretching vibrations at 2400-2100 cm(-1) in D(2)O, corresponding to strong hydrogen bonds. Since a water molecule bridges the protonated Schiff base and an aspartate in archaeal rhodopsins, the observed water molecules presumably hydrate the negative charges in the Schiff base region. In contrast, the FTIR spectroscopy data of bovine rhodopsin presented here revealed that there are no spectral changes of water molecules under strongly hydrogen-bonding conditions (in the range <2400 cm(-1) for O-D stretch) during the photoactivation processes. The only observed water bands were located in the >2500 cm(-1) region that corresponds to weak hydrogen bonding. These results imply that the ion pair state in vertebrate visual rhodopsins is stabilized in a manner different from that in archaeal rhodopsins. In addition, the internal water molecules that hydrate the negative charges do not play important role in the photoactivation processes of rhodopsin that involve proton transfer from the Schiff base to Glu113 upon formation of Meta II. Structural changes of the H-D exchangeable peptide amide of a beta-sheet are observed upon formation of metarhodopsin II, suggesting that motion of a beta-sheet is coupled to the proton transfer reaction from the Schiff base to its counterion.     

Kinetics and pH Dependence of Light-Induced Deprotonation of the Schiff Base of Rhodopsin: Possible Coupling to Proton Uptake and Formation of the Active Form of Meta II

In this paper we first review what is known about the kinetics of Meta II formation, the role and stoichiometry of protons in Meta II formation, the kinetics of the light-induced changes of proton concentration, and the site of proton uptake. We then go on to compare the processes that lead to the deprotonation of the Schiff base in bacteriorhodopsin with rhodopsin. We point out that the similarity of the signs of the light-induced electrical signals from the two kinds of oriented pigment molecules could be explained by bacteriorhodopsin releasing a proton from its extracellular side while rhodopsin taking up a proton on its cytoplasmic side. We then examined the pH dependence of both the absorption spectrum of the unphotolyzed state and the amplitude and kinetics of Meta II formation in bovine rhodopsin. We also measured the effect of deuteration and azide on Meta II formation. We concluded that the pK _a of the counter-ion to the Schiff base of bovine rhodopsin and of a surface residue that takes up a proton upon photolysis are both less than 4 in the unphotolyzed state. The data on pH dependence of Meta II formation indicated that the mechanisms involved are more complicated than just two sequential, isospectral forms of Meta II in the bleaching sequence. Finally we examined the evidence that, like in bacteriorhodopsin, the protonation of the Schiff bases's counter-ion (Glu113) is coupled to the changing of the pK _a of a protonatable surface group, called Z for rhodopsin and tentatively assigned to Glu134. We conclude that there probably is such a coupling, leading to the formation of the active form of Meta II.