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.     

Characterization of the azide-dependent bacteriorhodopsin-like photocycle of salinarum halorhodopsin

The photocycle of salinarum halorhodopsin was investigated in the presence of azide. The azide binds to the halorhodopsin with 150 mM binding constant in the absence of chloride and with 250 mM binding constant in the presence of 1 M chloride. We demonstrate that the azide-binding site is different from that of chloride, and the influence of chloride on the binding constant is indirect. The analysis of the absorption kinetic signals indicates the existence of two parallel photocycles. One belongs to the 13-cis retinal containing protein and contains a single red shifted intermediate. The other photocycle, of the all-trans retinal containing halorhodopsin, resembles the cycle of bacteriorhodopsin and contains a long-living M intermediate. With time-resolved spectroscopy, the spectra of intermediates were determined. Intermediates L, N, and O were not detected. The multiexponential rise and decay of the M intermediate could be explained by the introduction of the "spectrally silent" intermediates M1, M2, and HR', HR, respectively. The electric signal measurements revealed the existence of a component equivalent with a proton motion toward the extracellular side of the membrane, which appears during the M1 to M2 transition. The differences between the azide-dependent photocycle of salinarum halorhodopsin and pharaonis halorhodopsin are discussed.     

Anion uptake in halorhodopsin from Natromonas pharaonis studied by FTIR spectroscopy: consequences for the anion transport mechanism

The uptake of chloride, bromide, iodide, nitrate, and azide by anion-depleted blue halorhodopsin from Natronobacterium pharaonis has been followed by FTIR difference spectroscopy using an ATR sampling device. The spectra are compared with the spectrum of the O intermediate obtained by time-resolved FTIR studies of the photocycle. It is demonstrated that anion-free blue halorhodopsin can be identified with the O intermediate and, thus, that the decay of O is due to the passive uptake of the anion. The great similarity of the anion-binding spectra and their identity in the case of the monoatomic anions indicate a rather unspecific binding site for the different anions dominated by electrostatic interactions. Comparing spectra obtained with 15N nitrate and unlabeled nitrate, the NO-stretching bands could be identified. The small splitting and the small IR intensity of those bands indicate a rather nonpolar binding site with a rather isotropic influence on the nitrate, in contrast to aqueous nitrate. In further experiments on the photocycle of blue halorhodopsin, the all-trans --> 13-cis isomerization can be clearly identified. Up to 100 micros, the isomerization-induced structural changes deduced from amide I changes are similar to those occurring during the anion-transporting photocycle. Compared to these, the molecular changes involved in the release and their reversion during the uptake of anions are considerably larger. They can be reached via two pathways: (1) by reducing the anion concentration and (2) transiently during the anion-transporting photocycle with the formation of the precursor of O with O conformation. Consequences of the anion transport mechanism are discussed.     

Structural characterization of the L-to-M transition of the bacteriorhodopsin photocycle.

Structural intermediates occurring in the photocycle of wild-type bacteriorhodopsin are trapped by illuminating hydrated, glucose-embedded purple membrane at 170 K, 220 K, 230 K, and 240 K. We characterize light-induced changes in protein conformation by electron diffraction difference Fourier maps, and relate these to previous work on photocycle intermediates by infrared (FTIR) spectroscopy. Samples illuminated at 170 K are confirmed by FTIR spectroscopy to be in the L state; a difference Fourier projection map shows no structural change within the 0.35-nm resolution limit of our data. Difference maps obtained with samples illuminated at 220 K, 230 K, and 240 K, respectively, reveal a progressively larger structural response in helix F when the protein is still in the M state, as judged by the FTIR spectra. Consistent with previous structural studies, an adjustment in the position or in the degree of ordering of helix G accompanies this motion. The model of the photocycle emerging from this and previous studies is that bacteriorhodopsin experiences minimal change in protein structure until a proton is transferred from the Schiff base to Asp85. The M intermediate then undergoes a conformational evolution that opens a hydrated "half-channel," allowing the subsequent reprotonation of the Schiff base by Asp96.     

Low-temperature photoreactions of halorhodopsin. 2. Description of the photocycle and its intermediates

Photostationary states of halorhodopsin (HR, a retinal protein in the halobacterial membrane) and their further thermal conversions were investigated at 140-230 K by absorption spectroscopy in the visible. The difference spectra confirm several steps of the all-trans-HR photocycle, in the presence of chloride, proposed earlier on the basis of room temperature flash spectroscopy. Thus, at 140 K, the spectra reveal the HR600----HR520 reaction, and at 170-230 K the HR640----HR578 and the HR520----HR578 reactions can be seen. No evidence for the expected HR520 in equilibrium HR640 process was found, however. From the difference spectra at various temperatures, exact absorption spectra of HR600 and HR520 were calculated, and an estimate of the HR640 spectrum in a mixture also containing HR520 was obtained. The low-temperature absorption maxima of HR578 and its photointermediates relate to the room temperature maxima differently from what is expected from the spectra of the corresponding intermediates in the bacteriorhodopsin photocycle.     

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.     

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.     

Water structural changes involved in the activation process of photoactive yellow protein

Fourier transform infrared (FTIR) spectroscopy was applied to the blue-light photoreceptor photoactive yellow protein (PYP) to investigate water structural changes possibly involved in the photocycle of PYP. Photointermediates were stabilized at low temperature, and difference IR spectra were obtained between intermediate states and the original state of PYP (pG). Water structural changes were never observed in the >3570 cm(-)(1) region for the intermediates stabilized at 77-250 K, such as the red-shifted pR and blue-shifted pB intermediates. In contrast, a negative band was observed at 3658 cm(-)(1) in the pB minus pG spectrum at 295 K, which shifts to 3648 cm(-)(1) upon hydration with H(2)(18)O. The high frequency of the O-H stretch of water indicates that the water O-H group does not form hydrogen bonds in pG, and newly forms these upon pB formation at 295 K, but not at 250 K. Among 92 water molecules in the crystal structure of PYP, only 1 water molecule, water-200, is present in a hydrophobic core inside the protein. The amide N-H of Gly-7 and the imidazole nitrogen atom of His-108 are its possible hydrogen-bonding partners, indicating that one O-H group of water-200 is free to form an additional hydrogen bond. The water band at 3658 cm(-)(1) was indeed diminished in the H108F protein, which strongly suggests that the water band originates from water-200. Structural changes of amide bands in pB were much greater in the wild-type protein at 295 K than at 250 K or in the H108F protein at 295 K. The position of water-200 is >15 A remote from the chromophore. Virtually no structural changes were reported for regions larger than a few angstroms away from the chromophore, in the time-resolved X-ray crystallography experiments on pB. On the basis of the present results, as well as other spectroscopic observations, we conclude that water-200 (buried in a hydrophobic core in pG) is exposed to the aqueous phase upon formation of pB in solution. In neither crystalline PYP nor at low temperature is this structural transition observed, presumably because of the restrictions on global structural changes in the protein under these conditions.     

The prediction of the circular dichroism of the benzene chromophore: TDDFT calculations and sector rules

The CD spectra of the series PhCH(Me)R, with R = Et (1), nPr (2), iPr (3), and tBu (4), are reported (1-3 for the first time) at room temperature in the 185-280 nm range and at 183 K. These purely hydrocarbon compounds represent the simplest chiral systems containing the phenyl chromophore and exhibit Cotton effects exclusively allied with the benzene transitions. The bands in 1La and 1Lb regions were checked against the available sector rules, with discordant outcomes. Time-dependent density-functional theory calculations, with various functionals and basis sets tested, correctly reproduced the prominent CD bands observed for 1-4.     

FTIR study of the L intermediate of Anabaena sensory rhodopsin: structural changes in the cytoplasmic region

Anabaena sensory rhodopsin (ASR) is an archaeal-type rhodopsin found in eubacteria. The gene encoding ASR forms a single operon with ASRT (ASR transducer) that is a 14 kDa soluble protein, suggesting that ASR functions as a photochromic sensor by activating the soluble transducer. One of the characteristics of ASR is that the formation of the M intermediate accompanies a proton transfer from the Schiff base to Asp217 in the cytoplasmic side [Shi, L., Yoon, S. R., Bezerra, A. G., Jr., Jung, K. H., and Brown, L. S. (2006) J. Mol. Biol. 358, 686-700], in remarkable contrast to other archaeal-type rhodopsins such as a light-driven proton-pump, bacteriorhodopsin (BR). In this study, we applied low-temperature Fourier transform infrared (FTIR) spectroscopy to the all- trans form of ASR at 170 K, and compared the structural changes in the L intermediate with those of BR. The ASR L minus ASR difference spectra were essentially similar to those for BR, suggesting common structures for the L state in ASR and BR. On the other hand, unique CO stretching bands of a protonated carboxylic acid were observed at 1722 (+) and 1703 (-) cm (-1) at pH 5 and 7, and assigned to Glu36 by use of mutants. Glu36 is located at the cytoplasmic side, and the distance from the Schiff base is about 20 A. This result shows the structural changes at the cytoplasmic surface in ASR L. pH-dependent frequency change was also observed for a water stretching vibration, suggesting that the water molecule is involved in a hydrogen-bonding network with Glu36 and Asp217. Unique hydrogen-bonding network in the cytoplasmic domain of ASR will be discussed.     

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.     

Thermal equilibrium of two conformations in photosensitive nitrile hydratase probed by the FTIR band of nitric oxide bound to the non-heme iron center

Nitrile hydratase (NHase) from Rhodococcus N-771 is a novel enzyme that is inactive in the dark due to an enodogenous nitric oxide (NO) molecule bound to the non-heme iron center, and is activated by its photodissociation. FTIR spectra in the NO stretching region of the dark-inactive NHase were recorded in the temperature range of 270-80 K. Two NO peaks were observed at 1854 and 1846 cm-1 at 270 K, and both frequencies upshifted as the temperature was lowered, retaining the peak separation of 8-9 cm-1. The relative intensity of the lower-frequency peak increased with decreasing temperature up to ~120 K, whereas it was mostly unchanged below this temperature. This observation indicates that two distinct conformations with slightly different NO structures are thermally equilibrated in the dark-inactive NHase above ~120 K, and the interconversion is frozen-in at lower temperatures. The intensity ratio of the NO bands changed gradually upon increasing the pH from 5.5 to 11.0, but no specific pKa value was found. This result, together with the comparison of the light-induced FTIR difference spectra measured at pH 6.5 and 9.0, suggests that the protonation/deprotonation of a specific amino acid group in the active site of NHase is not a direct cause of the occurrence of the two conformations, although several protonatable groups in the protein may influence the energetics of the two conformers. From the previous observation that the isolated alpha subunit of NHase exhibited a single broad NO peak, it is suggested that interaction of the beta subunit forming the reactive cavity is essential for the double-minimum potential of the active-site structure. The frequencies and widths of the two NO bands changed upon addition of propionamide, 1,4-dioxane, and cyclohexyl isocyanide, indicating that these compounds are bound to the active pocket and change the interactions of the iron center or the dielectric environments around the NO molecule. Thus, the NO bands of NHase can also be a useful probe to monitor the binding of substrates and their analogues to the active pocket.     

Dynamics of dioxygen and carbon monoxide binding to soybean leghemoglobin

The association of dioxygen and carbon monoxide to soybean leghemoglobin (Lb) has been studied by laser flash photolysis at temperatures from 10 to 320 K and times from 50 ns to 100 s. Infrared spectra of the bound and the photodissociated state were investigated between 10 and 20 K. The general features of the binding process in leghemoglobin are similar to the ones found in myoglobin. Below about 200 K, the photodissociated ligands stay in the heme pocket and rebinding is not exponential in time, implying a distributed enthalpy barrier between pocket and heme. At around 300 K, ligands migrate from the solvent through the protein to the heme pocket, and a steady state is set up between the ligands in the solvent and in the heme pocket. The association rate, lambda on, is mainly controlled by the final binding step at the heme, the bond formation with the heme iron. Differences between Lb and other heme proteins show up in the details of the various steps. The faster association rate in Lb compared to sperm whale myoglobin (Mb) is due to a faster bond formation. The migration from the solvent to the heme pocket is much faster in Lb than in Mb. The low-temperature binding (B----A) and the infrared spectra of CO in the bound state A and the photodissociated state B are essentially solvent-independent in Mb, but depend strongly on solvent in Lb. These features can be correlated with the x-ray structure.     

Assignment of the hydrogen-out-of-plane and -in-plane vibrations of the retinal chromophore in the K intermediate of pharaonis phoborhodopsin

pharaonis phoborhodopsin (ppR; also called pharaonis sensory rhodopsin II, psR-II) is a photoreceptor protein for negative phototaxis in Natronomonas pharaonis. Photoisomerization of the retinal chromophore from all-trans to 13-cis initiates conformational changes of the protein leading to activation of the cognate transducer protein (pHtrII). Elucidation of the initial photoreaction, formation of the K intermediate of ppR, is important for understanding the mechanism of storage of photon energy. We have reported the K minus ppR Fourier transform infrared (FTIR) spectra, including several vibrational bands of the retinal, the protein, and internal water molecules. It is interesting that more vibrational bands were observed in the hydrogen-out-of-plane (HOOP) region than for the light-driven proton pump, bacteriorhodopsin. This result implied that the steric constraints on the retinal chromophore in the binding pocket of ppR are distributed more widely upon formation of the initial intermediate. In this study, we assigned the HOOP and hydrogen-in-plane vibrations by means of low-temperature FTIR spectroscopy applied to ppR reconstituted with retinal deuterated at C7, C8, C10-C12, C14, and C15. As a result, the 966 (+)/971 (-) and 958 (+)/961 (-) cm(-1) bands were assigned to the C7=C8 and C11=C12 Au HOOP modes, respectively, suggesting that the structural changes spread to the middle part of the retinal. The positive bands at 1001, 994, 987, and 979 cm(-1) were assigned to the C15-HOOP vibrations of the K intermediate, whose frequencies are similar to those of the K(L) intermediate of bacteriorhodopsin trapped at 135 K. Another positive band at 864 cm(-1) was assigned to the C14-HOOP vibration. Relatively many positive bands of hydrogen-in-plane vibrations supported the wide distribution of structural changes of the retinal as well. These results imply that the light energy was stored mainly in the distortions around the Schiff base region while some part of the energy was transferred to the distal part of the retinal.     

Properties and photochemistry of a halorhodopsin from the haloalkalophile, Natronobacterium pharaonis

Pharaonis halorhodopsin is a light-driven transport system for chloride, similarly to the previously described halorhodopsin, but we find that it transports nitrate as effectively as chloride. We studied the photoreactions of the purified, detergent-solubilized pharaonis pigment with a gated multichannel analyzer. At a physiological salt concentration (4 M NaCl), the absorption spectra and rate constants of rise and decay for intermediates of the photocycle were similar to those for halorhodopsin. In buffer containing nitrate, halorhodopsin exhibits a second, truncated photocycle; this difference in the photoreaction of the pigment occurs when an anion is bound in such a way as to preclude transport. As expected from the lack of anion specificity in the transport, the photocycle of pharaonis halorhodopsin was nearly unaffected by replacement of chloride with nitrate. All presumed buried positively charged residues, which might play a role in anion binding, are conserved in the two pigments. At the extracellular end of the presumed helix C, however, an arginine residue is found in halorhodopsin, but not in pharaonis halorhodopsin, and an arginine-rich segment between the presumed helices A and B in halorhodopsin is replaced by a less positively charged sequence in pharaonis halorhodopsin (Lanyi, J. K., Duschl, A., Hatfield, G. W., May, K., and Oesterhelt, D. (1990) J. Biol. Chem. 265, 1253-1260). One or both of these alterations may explain the difference in the anion selectivity of the two proteins.     

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.     

Low-frequency fourier transform infrared spectroscopy of the oxygen-evolving and quinone acceptor complexes in photosystem II

The low-frequency (<1000 cm-1) region of the IR spectrum has the potential to provide detailed structural and mechanistic insight into the photosystem II/oxygen evolving complex (PSII/OEC). A cluster of four manganese ions forms the core of the OEC and diagnostic manganese-ligand and manganese-substrate modes are expected to occur in the 200-900 cm-1 range. However, water also absorbs IR strongly in this region, which has limited previous Fourier transform infrared (FTIR) spectroscopic studies of the OEC to higher frequencies (>1000 cm-1). We have overcome the technical obstacles that have blocked FTIR access to low-frequency substrate, cofactor, and protein vibrational modes by using partially dehydrated samples, appropriate window materials, a wide-range MCT detector, a novel band-pass filter, and a closely regulated temperature control system. With this design, we studied PSII/OEC samples that were prepared by brief illumination of O2 evolving and Tris-washed preparations at 200 K or by a single saturating laser flash applied to O2 evolving and inhibited samples at 250 K. These protocols allowed us to isolate low-frequency modes that are specific to the QA-/QA and S2/S1 states. The high-frequency FTIR spectra recorded for these samples and parallel EPR experiments confirmed the states accessed by the trapping procedures we used. In the S2/S1 spectrum, we detect positive bands at 631 and 602 cm-1 and negative bands at 850, 679, 664, and 650 cm-1 that are specifically associated with these two S states. The possible origins of these IR bands are discussed. For the low-frequency QA-/QA difference spectrum, several modes can be assigned to ring stretching and bending modes from the neutral and anion radical states of the quinone acceptor. These results provide insight into the PSII/OEC and demonstrate the utility of FTIR techniques in accessing low-frequency modes in proteins.     

Circular dichroism of halorhodopsin: comparison with bacteriorhodopsin and sensory rhodopsin I

Circular dichroic (CD) spectra of three related protein pigments from Halobacterium halobium, halorhodopsin (HR), bacteriorhodopsin (BR), and sensory rhodopsin I (SR-I), are compared. In native membranes the two light-driven ion pumps, HR and BR, exhibit bilobe circular dichroism spectra characteristic of exciton splitting in the region of retinal absorption, while the phototaxis receptor, SR-I, exhibits a single positive band centered at the SR-I absorbance maximum. This indicates specific aggregation of protein monomers of HR, as previously noted [Sugiyama, Y., & Mukohata, Y. (1984) J. Biochem. (Tokyo) 96, 413-420], similar to the well-characterized retinal/retinal exciton interaction in the purple membrane. The absence of this interaction in SR-I indicates SR-I is present in the native membrane as monomers or that interactions between the retinal chromophores are weak due to chromophore orientation or separation. Solubilization of HR and BR with nondenaturing detergents eliminates the exciton coupling, and the resulting CD spectra share similar features in all spectral regions from 250 to 700 nm. Schiff-base deprotonation of both BR and HR yields positive CD bands near 410 nm and shows similar fine structure in both pigments. Removal of detergent restores the HR native spectrum. HR differs from BR in that circular dichroic bands corresponding to both amino acid and retinal environments are much more sensitive to external salt concentration and pH. A theoretical analysis of the exciton spectra of HR and BR that provides a range of interchromophore distances and orientations is performed.(ABSTRACT TRUNCATED AT 250 WORDS)     

Halide dependence of the halorhodopsin photocycle as measured by time-resolved infrared spectra

Time-resolved Fourier transform infrared (FTIR) difference spectra of the halorhodopsin (hR) photocycle have been collected from 3 micros to 100 ms in saturating concentrations of KCl or KBr. Kinetic analysis of these data revealed two decay processes, with time constants of tau(1) approximately 150 micros and tau(2) approximately 16 ms in the presence of either halide, with tau(2) describing the return to the starting (hR) state. Comparison to previous low-temperature FTIR spectra of hR intermediates confirms that characteristic hK and hL spectral features are both present before the tau(1) decay, in a state previously defined as hK(L) (Dioumaev, A., and M. Braiman. 1997. Photochem. Photobiol. 66:755-763). However, the relative sizes of these features depend on which halide is present. In Br-, the hL features are clearly more dominant than in Cl-. Therefore, the state present before tau(1) is probably best described as an hK(L)/hL(1) equilibrium, instead of a single hK(L) state. Different halides affect the relative amounts of hK(L) and hL(1) present, i.e., Cl- produces a much more significant back-reaction from hL(1) to hK(L) than does Br-. The halide dependence of this back-reaction could therefore explain the halide selectivity of the halorhodopsin anion pump.