FTIR difference spectroscopy in combination with isotope labeling for identification of the carbonyl modes of P700 and P700+ in photosystem I

Room temperature, light induced (P700(+)-P700) Fourier transform infrared (FTIR) difference spectra have been obtained using photosystem I (PS I) particles from Synechocystis sp. PCC 6803 that are unlabeled, uniformly (2)H labeled, and uniformly (15)N labeled. Spectra were also obtained for PS I particles that had been extensively washed and incubated in D(2)O. Previously, we have found that extensive washing and incubation of PS I samples in D(2)O does not alter the (P700(+)-P700) FTIR difference spectrum, even with approximately 50% proton exchange. This indicates that the P700 binding site is inaccessible to solvent water. Upon uniform (2)H labeling of PS I, however, the (P700(+)-P700) FTIR difference spectra are considerably altered. From spectra obtained using PS I particles grown in D(2)O and H(2)O, a ((1)H-(2)H) isotope edited double difference spectrum was constructed, and it is shown that all difference bands associated with ester/keto carbonyl modes of the chlorophylls of P700 and P700(+) downshift 4-5/1-3 cm(-1) upon (2)H labeling, respectively. It is also shown that the ester and keto carbonyl modes of the chlorophylls of P700 need not be heterogeneously distributed in frequency. Finally, we find no evidence for the presence of a cysteine mode in our difference spectra. The spectrum obtained using (2)H labeled PS I particles indicates that a negative difference band at 1698 cm(-1) is associated with at least two species. The observed (15)N and (2)H induced band shifts strongly support the idea that the two species are the 13(1) keto carbonyl modes of both chlorophylls of P700. We also show that a negative difference band at approximately 1639 cm(-1) is somewhat modified in intensity, but unaltered in frequency, upon (2)H labeling. This indicates that this band is not associated with a strongly hydrogen bonded keto carbonyl mode of one of the chlorophylls of P700.     

FTIR study of the primary electron donor of photosystem I (P700) revealing delocalization of the charge in P700(+) and localization of the triplet character in (3)P700.

The effect of global (15)N or (2)H labeling on the light-induced P700(+)/P700 FTIR difference spectra has been investigated in photosystem I samples from Synechocystis at 90 K. The small isotope-induced frequency shifts of the carbonyl modes observed in the P700(+)/P700 spectra are compared to those of isolated chlorophyll a. This comparison shows that bands at 1749 and 1733 cm(-)(1) and at 1697 and 1637 cm(-)(1), which upshift upon formation of P700(+), are candidates for the 10a-ester and 9-keto C=O groups of P700, respectively. A broad and relatively weak band peaking at 3300 cm(-)(1), which does not shift upon global labeling or (1)H-(2)H exchange, is ascribed to an electronic transition of P700(+), indicating that at least two chlorophyll a molecules (denoted P(1) and P(2)) participate in P700(+). Comparisons of the (3)P700/P700 FTIR difference spectrum at 90 K with spectra of triplet formation in isolated chlorophyll a or in RCs from photosystem II or purple bacteria identify the bands at 1733 and 1637 cm(-)(1), which downshift upon formation of (3)P700, as the 10a-ester and 9-keto C=O modes, respectively, of the half of P700 that bears the triplet (P(1)). Thus, while the P(2) carbonyls are free from interaction, both the 10a-ester and the 9-keto C=O of P(1) are hydrogen bonded and the latter group is drastically perturbed compared to chlorophyll a in solution. The Mg atoms of P(1) and P(2) appear to be five-coordinated. No localization of the triplet on the P(2) half of P700 is observed in the temperature range of 90-200 K. Upon P700 photooxidation, the 9-keto C=O bands of P(1) and P(2) upshift by almost the same amount, giving rise to the 1656(+)/1637(-) and 1717(+)/1697(-) cm(-)(1) differential signals, respectively. The relative amplitudes of these differential signals, as well as of those of the 10a-ester C=O modes, appear to be slightly dependent on sample orientation and temperature and on the organism used to generate the P700(+)/P700 spectrum. If it is assumed that the charge density on ring V of chlorophyll a, as measured by the perturbation of the 10a-ester or 9-keto C=O IR vibrations, mainly reflects the spin density on the two halves of the oxidized P700 special pair, a charge distribution ranging from 1:1 to 2:1 (in favor of P(2)) is deduced from the measurements presented here. The extreme downshift of the 9-keto C=O group of P(1), indicative of an unusually strong hydrogen bond, is discussed in relation with the models previously proposed for the PSI special pair.     

Time-resolved FTIR difference spectroscopy for the study of photosystem I particles with plastoquinone-9 occupying the A1 binding site

In photosystem I from plants and cyanobacteria a phylloquinone molecule, called A1, functions as the secondary electron acceptor. In cyanobacteria, genes that encode for proteins involved in phylloquinone biosynthesis can be deleted. Here, we have studied three different gene deletion mutants called menB, menD, and menE mutants. In these mutants, plastoquinone-9 occupies the A1 binding site. Using time-resolved, step-scan FTIR difference spectroscopy we have produced A1(-)/A1 FTIR difference spectra for menB, menD, and menE photosystem I particles at 77 K. These difference spectra show that the P700 triplet state ((3)P700) is formed in a large fraction of the particles. Infrared spectral signatures that are not due to (3)P700 are also observed in the spectra and are suggested to be associated with plastoquinone-9 anion formation in a portion of the particles. By subtracting the known (3)P700 spectral signatures, we produce an A1(-)/A1 FTIR difference spectrum for PS I particles with plastoquinone-9 occupying the binding site. This spectrum shows that a band that we have previously assigned to a C:-O mode of the phylloquinone anion in WT A1(-)/A1 FTIR DS down-shifts approximately 8 cm(-1) when plastoquinone-9 occupies the A1 binding site. Using density functional theory type calculations to produce anion minus neutral infrared difference spectra for both phylloquinone and plastoquinone-9, it is shown that such a downshift is reasonable. A1(-)/A1 FTIR difference spectra, obtained using menB mutant photosystem I particles that were incubated in the presence of phylloquinone, are found to be very similar to those obtained using normal WT photosystem I particles. This result indicates that we were able to reincorporate phylloquinone back into the A1 binding site and that the reincorporated phylloquinone and its immediate protein environment, in both the neutral and anion state, are very similar to that found in wild type photosystem I particles. For the reconstituted menB mutant photosystem I particles, no spectral signatures associated with (3)P700 are observed, indicating that phylloquinone occupies the A1 site in all of the reconstituted menB particles.     

Primary donor photo-oxidation in photosystem I: a re-evaluation of (P700(+) - P700) Fourier transform infrared difference spectra.

Light-induced Fourier transform infrared (FTIR) difference spectroscopy has been used to study the photo-oxidation of the primary electron donor (P700) in PS I particles from Chlamydomonas reinhardtii and Synechocystis sp. PCC 6803. To aid in the interpretation of the spectra, PS I particles from a site-directed mutant of C. reinhardtii, in which the axial histidine ligand (HisA676) was changed to serine, were also studied. A high-frequency (3300-2600 cm(-1)) electronic transition is observed for all PS I particles, demonstrating that P700 is dimeric. The electronic band is, however, species-dependent, indicating some differences in the electronic structure of P700 and/or P700(+) in C. reinhardtii and Synechocystis sp. 6803. For PS I particles from C. reinhardtii, substitution of HisA676 with serine has little effect on the ester carbonyl modes of the chlorophylls of P700. However, the keto carbonyl modes are considerably altered. Comparison of (P700(+) - P700) FTIR difference spectra obtained using PS I particles from the wild type (WT) and the HS(A676) mutant of C. reinhardtii indicates that the mutation primarily exerts its influence on the P700 ground state. The 13(1) keto carbonyls of the chlorophylls of P700 of the wild type absorb at similar frequencies, which has previously made these transitions difficult to resolve. However, for the HS(A676) mutant, the 13(1) keto carbonyl of chlorophyll a or chlorophyll a' of P700 on PsaB or PsaA absorbs at 1703.4 or 1694.2 cm(-1), respectively, allowing their unambiguous resolution. Upon P700(+) formation, in both PS I particles from C. reinhardtii, the higher-frequency carbonyl band upshifts by approximately 14 cm(-1) while the lower frequency carbonyl downshifts by approximately 10 cm(-1). The similarity in the spectra for WT PS I particles from C. reinhardtii and Synechocystis sp. 6803 indicates that a similar interpretation is probably valid for PS I particles from both species. The mutant results allow for an interpretation of the behavior of the 13(1) keto carbonyls of P700 that is different from previous work [Breton, J., Nabedryk, E., and Leibl, W. (1999) Biochemistry 38, 11585-11592], in which it was suggested that 13(1) keto carbonyls of P700 absorb at 1697 and 1639 cm(-1), and upshift by 21 cm(-1) upon cation formation. The interpretation of the spectra reported here is more in line with recent results from ENDOR spectroscopy and high-resolution crystallography.     

Photo-oxidation of P740, the primary electron donor in photosystem I from Acaryochloris marina

Fourier transform infrared spectroscopy (FTIR) difference spectroscopy in combination with deuterium exchange experiments has been used to study the photo-oxidation of P740, the primary electron donor in photosystem I from Acaryochloris marina. Comparison of (P740(+)-P740) and (P700(+)-P700) FTIR difference spectra show that P700 and P740 share many structural similarities. However, there are several distinct differences also: 1), The (P740(+)-P740) FTIR difference spectrum is significantly altered upon proton exchange, considerably more so than the (P700(+)-P700) FTIR difference spectrum. The P740 binding pocket is therefore more accessible than the P700 binding pocket. 2), Broad, "dimer" absorption bands are observed for both P700(+) and P740(+). These bands differ significantly in substructure, however, suggesting differences in the electronic organization of P700(+) and P740(+). 3), Bands are observed at 2727(-) and 2715(-) cm(-1) in the (P740(+)-P740) FTIR difference spectrum, but are absent in the (P700(+)-P700) FTIR difference spectrum. These bands are due to formyl CH modes of chlorophyll d. Therefore, P740 consists of two chlorophyll d molecules. Deuterium-induced modification of the (P740(+)-P740) FTIR difference spectrum indicates that only the highest frequency 13(3) ester carbonyl mode of P740 downshifts, indicating that this ester mode is weakly H-bonded. In contrast, the highest frequency ester carbonyl mode of P700 is free from H-bonding. Deuterium-induced changes in (P740(+)-P740) FTIR difference spectrum could also indicate that one of the chlorophyll d 3(1) carbonyls of P740 is hydrogen bonded.     

Modification of the phylloquinone in the A1 binding site in photosystem I studied using time-resolved FTIR difference spectroscopy and density functional theory

A phylloquinone molecule (2-methyl-3-phytyl-1,4-naphthoquinone) occupies the A1 binding site in photosystem I. Previously, we have obtained A1(-)/A1 FTIR difference spectra using labeled and unlabeled photosystem I particles and proposed assignments for many of the bands in the spectra [Sivakumar, V., Wang, R., and Hastings, G. (2005) Biochemistry 44, 1880-1893]. In particular, we suggested that a negative/positive band at 1654/1495 cm(-1) in A1(-)/A1 FTIR DS is due to a C=O/C-:O mode of the neutral/anionic phylloquinone, respectively. To test this hypothesis, we have obtained A1(-)/A1 FTIR DS for menG mutant PS I particles. In menG mutant PS I, phylloquinone in the A1 binding site is replaced with an analogue in which the methyl group at position 2 of the quinone ring is replaced with a hydrogen atom (2-phytyl-1,4-naphthoquinone). In A1(-)/A1 FTIR DS obtained using menG mutant PS I particles, we find that the 1654/1495 cm(-1) bands are upshifted by approximately 6 cm(-1). To test if such upshifts are likely for C=O/C-:O modes of neutral/anionic phylloquinone, we have used density functional theory to calculate the "anion minus neutral" infrared difference spectra for both phylloquinone and its methyl-less analogue. We have also undertaken calculations in which the C4=O carbonyl group of phylloquinone and its methyl-less analogue are hydrogen bonded (to a water or leucine molecule). We find that, irrespective of the hydrogen bonding state of the C4=O group, the C=O/C-:O modes of neutral/reduced phylloquinone are indeed expected to be upshifted by at least 6 cm(-1) upon replacement of the methyl group at position 2 with hydrogen. The calculations also suggest that certain C=C/C-:C modes of neutral/reduced phylloquinone do not shift upon replacement of the methyl group. On the basis of these calculated results, we suggest which bands in the A1(-)/A1 FTIR DS may be associated with C=C/C-:C modes of neutral/reduced phylloquinone, respectively.     

A Fourier transform infrared absorption difference spectrum associated with the reduction of A1 in photosystem I: are both phylloquinones involved in electron transfer?

Photoaccumulated Fourier transform infrared difference spectra associated with P700(+) and P700(+)A(1)(-) formation have been obtained using purified photosystem I particles from Synechocystis sp. PCC 6803. From these spectra, a difference spectrum associated with phylloquinone reduction (A(1)(-) - A(1)) has been calculated. Infrared absorption changes associated with both the loss of the ground state and formation of the anion radical are observed in the difference spectrum. Fourier transform infrared difference spectra obtained in various spectral regions indicate that two, structurally distinct phylloquinones are photoaccumulated. This could indicate that phylloquinones on both the PsaA and PsaB branches are involved in electron transfer, and that electron transfer is bi-directional in photosystem I. It could also indicate an intrinsic structural heterogeneity in the A(1) binding site of the active branch. Several FTIR difference features taken together indicate that a glutamic acid residue (at position 699 or 702 on PsaA and/or 679 or 682 on PsaB) is perturbed upon A(1) anion formation. It is suggested that the protonation state of the perturbed glutamic acid residue is influenced by hydrogen bonding to a nearby tyrosine residue at position 696/676 on PsaA/PsaB.     

Spectroscopic studies of the chlorophyll d containing photosystem I from the cyanobacterium, Acaryochloris marina

Absorbance difference spectroscopy and redox titrations have been applied to investigate the properties of photosystem I from the chlorophyll d containing cyanobacterium Acaryochloris marina. At room temperature, the (P740(+)-P740) and (F(A/B)(-)-F(A/B)) absorbance difference spectra were recorded in the range between 300 and 1000 nm while at cryogenic temperatures, (P740(+)A(1)(-)-P740A(1)) and ((3)P740-P740) absorbance difference spectra have been measured. Spectroscopic and kinetic evidence is presented that the cofactors involved in the electron transfer from the reduced secondary electron acceptor, phylloquinone (A(1)(-)), to the terminal electron acceptor and their structural arrangement are virtually identical to those of chlorophyll a containing photosystem I. The oxidation potential of the primary electron donor P740 of photosystem I has been reinvestigated. We find a midpoint potential of 450+/-10 mV in photosystem I-enriched membrane fractions as well as in thylakoids which is very similar to that found for P700 in chlorophyll a dominated organisms. In addition, the extinction difference coefficient for the oxidation of the primary donor has been determined and a value of 45,000+/-4000 M(-1) cm(-1) at 740 nm was obtained. Based on this value the ratio of P740 to chlorophyll is calculated to be 1 : to approximately 200 chlorophyll d in thylakoid membranes. The consequences of our findings for the energetics in photosystem I of A. marina are discussed as well as the pigment stoichiometry and spectral characteristics of P740.     

Changes of low-frequency vibrational modes induced by universal 15N- and 13C-isotope labeling in S2/S1 FTIR difference spectrum of oxygen-evolving complex

The effects of universal (15)N- and (13)C-isotope labeling on the low- (650-350 cm(-1)) and mid-frequency (1800-1200 cm(-1)) S(2)/S(1) Fourier transform infrared (FTIR) difference spectrum of the photosynthetic oxygen-evolving complex (OEC) were investigated in histidine-tagged photosystem (PS) II core particles from Synechocystis sp. PCC 6803. In the mid-frequency region, the amide II modes were predominantly affected by (15)N-labeling, whereas, in addition to the amide II, the amide I and carboxylate modes were markedly affected by (13)C-labeling. In the low-frequency region, by comparing a light-induced spectrum in the presence of ferricyanide as the electron acceptor, with the double difference S(2)/S(1) spectrum obtained by subtracting the Q(A)(-)/Q(A) from the S(2)Q(A)(-)/S(1)Q(A) spectrum, considerable numbers of bands found in the light-induced spectrum were assigned to the S(2)/S(1) vibrational modes in the unlabeled PS II core particles. Upon (13)C-labeling, changes were observed for most of the prominent bands in the S(2)/S(1) spectrum. Although (15)N-labeling also induced changes similar to those by (13)C-labeling, the bands at 616(-), 605(+), 561(+), 555(-), and 544(-) cm(-1) were scarcely affected by (15)N-labeling. These results indicated that most of the vibrational modes found in the low-frequency spectrum are derived from the coupling between the Mn-cluster and groups containing nitrogen and/or carbon atom(s) in a direct manner and/or through hydrogen bonding. Interestingly, an intensive band at 577(-) cm(-1) was not affected by (15)N- and (13)C-isotope labeling, indicating that this band arises from the mode that does not include either nitrogen or carbon atoms, such as the skeletal vibration of the Mn-cluster or stretching vibrational modes of the Mn-ligand.     

The two histidine axial ligands of the primary electron donor chlorophylls (P700) in photosystem I are similarly perturbed upon P700+ formation

The extent of delocalization of the positive charge in the oxidized dimer of chlorophyll (Chl) constituting P700, the primary electron donor of photosystem I (PSI), has been investigated by analyzing the perturbation upon P700(+) formation of infrared (IR) vibrational modes of the two His axial ligands of the two P700 Chl molecules. Fourier transform IR (FTIR) difference spectra of the photooxidation of P700 in PSI core complexes isolated from Synechocystis sp. PCC 6803 isotopically labeled either globally with (15)N or more specifically with (13)C on all the His residues reveal isotopic shifts of a differential signal at 1102/1108 cm(-)(1). This signal is assigned to a downshift upon P700(+) formation of the predominantly C(5)-Ntau imidazole stretching mode of His residue(s). The amplitude of this signal is reduced by approximately half in FTIR spectra of Synechocystis mutants in which His PsaB 651, the axial ligand to one of the two Chl molecules in P700, is replaced by Cys, Gln, or Leu. These observations provide further evidence that the positive charge in P700(+) is essentially delocalized over the two Chl molecules, in agreement with a previous FTIR study in which the frequency of the vibrational modes of the 9-keto and 10a-ester C=O groups of the two Chl's in P700, P700(+), and (3)P700 were firmly established for the first time [Breton, J., et al. (1999) Biochemistry 38, 11585-11592]. Only limited perturbations of the amplitude and frequency of the 9-keto and 10a-ester C=O bands of the P700 Chl are elicited by the mutations. On the basis of comparable mutational studies of the primary electron donor in purple bacteria, these perturbations are attributed to small molecular rearrangements of the Chl macrocycle and substituents caused by the repositioning of the P700 dimer in the new protein cavity generated by the mutations. It is proposed that the perturbation of the FTIR spectra upon mutation of a His axial ligand of the P700 Chl recently reported in Chlamydomonas reinhardtii [Hastings, G., et al. (2001) Biochemistry 40, 12943-12949] can be explained by the same effect without the need for a new assignment of the C=O bands of P700. The distribution of charge/spin in P700(+) and (3)P700 determined by FTIR spectroscopy is discussed in relation with the contrasting interpretations derived from recent magnetic resonance experiments.     

Mutation induced modulation of hydrogen bonding to P700 studied using FTIR difference spectroscopy

Site-directed mutagenesis in combination with Fourier transform infrared difference spectroscopy has been used to study how hydrogen bonding modulates the electronic and physical organization of P700, the primary electron donor in photosystem I. Wild-type PS I particles from Chlamydomonas reinhardtii and a mutant in which ThrA739 is changed to alanine [TA(A739) mutant] were studied. ThrA739 is thought to provide a hydrogen bond to the chlorophyll-a' molecule of P700 (the two chlorophylls of P700 (P700(+)) will be called P(A) and P(B) (P(A)(+) and P(B)(+))). The mutation considerably alters the (P700(+)-P700) FTIR difference spectra. However, we were able to describe all of the mutation induced changes in the difference spectra in terms of difference band assignments that were proposed recently (Hastings, G., Ramesh, V. M., Wang, R., Sivakumar, V. and Webber, A. (2001) Biochemistry 40, 12943-12949). Upon comparison of mutant and wild type (P700(+)-P700) FTIR difference spectra, it is shown that (1) the 13(3) ester carbonyl modes of P(A) and P(B) are unaltered upon mutation of ThrA739 to alanine. (2) The 13(3) ester carbonyl modes of P(A)(+)/P(B)(+) upshift/downshift upon mutation. These oppositely directed shifts indicate that the mutation modifies the charge distribution over the pigments in the P700(+) state, with charge on P(B) being relocated onto P(A). We also show that the 13(1) keto carbonyl mode of P(B)/P(B)(+) is unaltered/downshifted upon mutation, as is expected for the above-described mutation induced charge redistribution in P700(+). Although the 13(3) ester carbonyl modes of the chlorophylls of P700 in the ground state are unaltered upon mutation, the 13(1) keto carbonyl mode of P(A) upshifts upon mutation, as does the 13(1) keto carbonyl mode of P(A)(+). For P700 in the ground state, bands that we associate with HisA676/HisB656 upshift/downshift upon mutation. For the P700(+) state, bands that we associate with HisA676/HisB656 also upshift/downshift upon mutation. These observations are also consistent with the notion that the mutation leads to the charge on P(B)(+) being relocated onto P(A)(+). In addition, we suggest that a hydrogen bond to the 13(1) keto carbonyl of P(A) is still present in the TA(A739) mutant, probably mediated through an introduced water molecule.     

FTIR detection of structural changes in a histidine ligand during S-state cycling of photosynthetic oxygen-evolving complex

Changes in structural coupling between the Mn cluster and a putative histidine ligand during the S-state cycling of the oxygen-evolving complex (OEC) have been detected directly by Fourier transform infrared (FTIR) spectroscopy in photosystem (PS) II core particles from the cyanobacterium Synechocystis sp. PCC6803, in which histidine residues were selectively labeled with l-[(15)N(3)]histidine. The bands sensitive to the histidine-specific isotope labeling appeared at 1120-1090 cm(-)(1) in the spectra induced upon the first-, second-, and fourth-flash illumination, for the S(2)/S(1), S(3)/S(2), and S(1)/S(0) differences, at similar frequencies with different sign and/or intensity depending on the respective S-state transitions. However, no distinctive band was observed in the third-flash induced spectrum for the S(0)/S(3) difference. The results indicate that a single histidine residue coupled with the structural changes of the OEC during the S-state cycling is responsible for the observed histidine bands, in which the histidine modes changed during the S(0)-to-S(1) transition are reversed upon the S(1)-to-S(2) and S(2)-to-S(3) transitions. The 1186(+)/1178(-) cm(-)(1) bands affected by l-[(15)N(3)]histidine labeling were observed only for the S(2)/S(1) difference, but those affected by universal (15)N labeling appeared prominently showing a clear S-state dependency. Possible origins of these bands and changes in the histidine modes during the S-state cycling are discussed.     

Mutation of the putative hydrogen-bond donor to P700 of photosystem I

The primary electron donor of photosystem I (PS1), called P(700), is a heterodimer of chlorophyll (Chl) a and a'. The crystal structure of photosystem I reveals that the chlorophyll a' (P(A)) could be hydrogen-bonded to the protein via a threonine residue, while the chlorophyll a (P(B)) does not have such a hydrogen bond. To investigate the influence of this hydrogen bond on P(700), PsaA-Thr739 was converted to alanine to remove the H-bond to the 13(1)-keto group of the chlorophyll a' in Chlamydomonas reinhardtii. The PsaA-T739A mutant was capable of assembling active PS1. Furthermore the mutant PS1 contained approximately one chlorophyll a' molecule per reaction center, indicating that P(700) was still a Chl a/a' heterodimer in the mutant. However, the mutation induced several band shifts in the visible P(700)(+) - P(700) absorbance difference spectrum. Redox titration of P(700) revealed a 60 mV decrease in the P(700)/P(700)(+) midpoint potential of the mutant, consistent with loss of a H-bond. Fourier transform infrared (FTIR) spectroscopy indicates that the ground state of P(700) is somewhat modified by mutation of ThrA739 to alanine. Comparison of FTIR difference band shifts upon P(700)(+) formation in WT and mutant PS1 suggests that the mutation modifies the charge distribution over the pigments in the P(700)(+) state, with approximately 14-18% of the positive charge on P(B) in WT being relocated onto P(A) in the mutant. (1)H-electron-nuclear double resonance (ENDOR) analysis of the P(700)(+) cation radical was also consistent with a slight redistribution of spin from the P(B) chlorophyll to P(A), as well as some redistribution of spin within the P(B) chlorophyll. High-field electron paramagnetic resonance (EPR) spectroscopy at 330-GHz was used to resolve the g-tensor of P(700)(+), but no significant differences from wild-type were observed, except for a slight decrease of anisotropy. The mutation did, however, provoke changes in the zero-field splitting parameters of the triplet state of P(700) ((3)P(700)), as determined by EPR. Interestingly, the mutation-induced change in asymmetry of P(700) did not cause an observable change in the directionality of electron transfer within PS1.     

Picosecond transient absorption spectroscopy in the blue spectral region of photosystem I

Picosecond transient absorption difference spectroscopy in the blue wavelength region (380-500 nm) was used to study the early electron acceptors in photosystem I. Samples were photosystem I core particles with about 100 chlorophylls per reaction center isolated from the cyanobacterium Synechocystis sp. PCC 6803. After excitation at 590 nm at room temperature, decay-associated spectra (DAS) were determined from global analysis in the blue region, yielding two transient components and one nondecaying component. A 3 ps decay phase is interpreted as primarily due to antenna excited-state redistribution. A 28 ps decay phase is interpreted as due to overall excited-state decay by electron transfer. The nondecaying component is ascribed to the difference spectrum of P(700) and the quinone or A(1) electron acceptor (P(700)(+)A(1)(-) - P(700)A(1)). Decay curves on the millisecond time scale at different wavelengths were measured with an autoxidizable artificial electron acceptor, benzyl viologen, and the (P(700)(+) - P(700)) difference spectrum was constructed. The (A(1)(-) - A(1)) difference spectrum was obtained by taking the difference between the above two difference spectra. A parallel picosecond experiment under strongly reducing conditions was also done as a control experiment. These conditions stabilize the electron on an earlier acceptor, A(0). The nondecaying component of the DAS at low potential was assigned to (P(700)(+)A(0)(-) - P(700)A(0)) since the electron-transfer pathway from A(0) to A(1) was blocked. The [(P(700)(+)A(0)(-) - P(700)A(0)) - (P(700)(+) - P(700))] subtraction gives a spectrum, interpreted as the (A(0)(-) - A(0)) difference spectrum of a chlorophyll a molecule, consistent with previous studies. The (A(1)(-) - A(1)) spectrum resolved on the picosecond time scale shows significant differences with similar spectra measured on longer time scales. These differences may be due to electrochromic effects and spectral evolution.     

D1-Asp170 is structurally coupled to the oxygen evolving complex in photosystem II as revealed by light-induced Fourier transform infrared difference spectroscopy

We report both mid-frequency (1800-1200 cm(-)(1)) and low-frequency (670-350 cm(-)(1)) S(2)/S(1) FTIR difference spectra of photosystem II (PSII) particles isolated from wild-type and D1-D170H mutant cells of the cyanobacterium Synechocystis sp. PCC 6803. Both mid- and low-frequency S(2)/S(1) spectra of the Synechocystis wild-type PSII particles closely resemble those from spinach PSII samples, which confirms an earlier result by Noguchi and co-workers [Noguchi, T., Inoue, Y., and Tang, X.-S. (1997) Biochemistry 36, 14705-14711] and indicates that the coordination environment of the oxygen evolving complex (OEC) in Synechocystis is very similar to that in spinach. We also found that there is no appreciable difference between the mid-frequency S(2)/S(1) spectra of wild-type and of D1-D170H mutant PSII particles, from which we conclude that D1-Asp170 does not undergo a significant structural change during the S(1) to S(2) transition. This result also suggests that, if D1-Asp170 ligates Mn, it does not ligate the Mn ion that is oxidized during the S(1) to S(2) state transition. Finally, we found that a mode at 606 cm(-)(1) in the low-frequency wild-type S(2)/S(1) spectrum shifts to 612 cm(-)(1) in the D1-D170H mutant spectrum. Because this 606 cm(-)(1) mode has been previously assigned to an Mn-O-Mn cluster mode of the OEC [Chu, H.-A., Sackett, H., and Babcock, G. T. (2000) Biochemistry 39, 14371-14376], we conclude that D1-Asp170 is structurally coupled to the Mn-O-Mn cluster structure that gives rise to this band. Our results suggest that D1-Asp170 either directly ligates Mn or Ca(2+) or participates in a hydrogen bond to the Mn(4)Ca(2+) cluster. Our results demonstrate that combining FTIR difference spectroscopy with site-directed mutagenesis has the potential to provide insights into structural changes in Mn and Ca(2+) coordination environments in the different S states of the OEC.     

FTIR spectroscopy of synechocystis 6803 mutants affected on the hydrogen bonds to the carbonyl groups of the PsaA chlorophyll of P700 supports an extensive delocalization of the charge in P700+

P700, the primary electron donor of photosystem I is an asymmetric dimer made of one molecule of chlorophyll a' (P(A)) and one of chlorophyll a (P(B)). While the carbonyl groups of P(A) are involved in hydrogen-bonding interactions with several surrounding amino acid side chains and a water molecule, P(B) does not engage in hydrogen bonding with the protein. Light-induced FTIR difference spectroscopy of the photooxidation of P700 has been combined with site-directed mutagenesis in Synechocystis sp. PCC 6803 to investigate the influence of these hydrogen bonds on the structure of P700 and P700(+). When the residue Thr A739, which donates a hydrogen bond to the 9-keto C=O group of P(A), is changed to Phe, a differential signal at 1653(+)/1638(-) cm(-1) in the P700(+)/P700 FTIR difference spectrum upshifts by approximately 30-40 cm(-1), as expected for the rupture of the hydrogen bond or, at least, a strong decrease of its strength. The same upshift is also observed in the FTIR spectrum of a triple mutant in which the residues involved in the three main hydrogen bonds to the 9-keto and 10a-carbomethoxy groups of P(A) have been changed to the symmetry-related side chains present around P(B). In addition, the spectrum of the triple mutant shows a decrease of a differential signal around 1735 cm(-1) and the appearance of a new signal around 1760 cm(-1). This is consistent with the perturbation of a bound 10a-ester C=O group that becomes free in the triple mutant. All of these observations support the assignment scheme proposed previously for the carbonyls of P700 and P700(+) [Breton, J., Nabedryk, E., and Leibl, W. (1999) Biochemistry 38, 11585-11592] and therefore reinforce our previous conclusions that the positive charge in P700(+) is largely delocalized over P(A) and P(B).     

Hydrogen bonding to P700: site-directed mutagenesis of threonine A739 of photosystem I in Chlamydomonas reinhardtii

The primary electron donor P700 of photosystem I is a dimer comprised of chlorophyll a (P(B)) and chlorophyll a' (P(A)). P(A) is involved in a hydrogen bond network with several surrounding amino acid residues and a nearby water molecule. To investigate the influence of hydrogen bond interactions on the properties of P700, the threonine at position A739, which donates a putative hydrogen bond to the 13(1)-keto group of P(A), was replaced with valine, histidine, and tyrosine in Chlamydomonas reinhardtii using site-directed mutagenesis. Growth of the mutants was not impaired. (i) The (P700(+)* - P700) FTIR difference spectra of the mutants lack a negative band at 1634 cm(-1) observed in the wild-type spectrum and instead exhibit a new negative band between 1658 and 1672 cm(-1) depending on the mutation. This band can therefore be assigned to the 13(1)-keto group of P(A) which is upshifted to higher frequencies upon removal of the hydrogen bond. (ii) The main bleaching band in the Q(y)() region of the (P700(+)* - P700) and ((3)P700 - P700) absorption difference spectra is blue shifted for the mutants by approximately 6 nm compared to that of the wild type. A blue shift is also observed for the main bleaching in the Soret region. (iii) The (P700(+)* - P700) CD difference spectrum of the wild type reveals two bands at 694 nm (positive CD) and 680 nm (negative CD) of approximately equal area. For each mutant, these two components are blue-shifted to the same extent. The results strongly suggest that a blue shift of the Q(y) absorption band of P(A) is responsible for a blue shift of the exciton bands. (iv) Redox titrations yielded a decrease in the midpoint potential for the oxidation of P700 by 32 mV for the exchange of Thr against Val. (v) ENDOR spectroscopy shows that the hfc of the methyl protons at position 12 of the spin-carrying Chl P(B) is decreased due to the removal of the hydrogen bond to P(A). This indicates a redistribution of spin density in P700(+)* compared to that in the wild type. This gives evidence for an electronic coupling between the two halves of the dimer in the wild type and mutants.     

Fourier transform infrared difference spectroscopy shows no evidence for an enolization of chlorophyll a upon cation formation either in vitro or during P700 photooxidation

Molecular changes associated with the photooxidation of the primary electron donor P700 in photosystem I from cyanobacteria have been investigated with Fourier transform infrared (FTIR) difference spectroscopy. Highly resolved signals are observed in the carbonyl stretching frequency region of the light-induced FTIR spectra. In order to assign and to interpret these signals, the FTIR spectra of isolated chlorophyll a and pyrochlorophyll a (lacking the 10a-ester carbonyl) in both their neutral and cation states were investigated. Comparison of the redox-induced FTIR difference spectra of these two model compounds demonstrates that upon chlorophyll a cation formation in tetrahydrofuran the 7c-ester carbonyl is essentially unperturbed while the 10a-ester carbonyl is upshifted from 1738 to 1751 cm-1. For the 9-keto group, the shift is from 1693 to 1718 cm-1 in chlorophyll a and from 1686 to 1712 cm-1 in pyrochlorophyll a. The 1718-cm-1 band in the difference spectrum of chlorophyll a is thus unambiguously assigned to the 9-keto carbonyl of the cation. Comparison of the light-induced FTIR difference spectrum associated with the photooxidation of P700 in vivo with the difference FTIR spectrum of chlorophyll a cation formation leads to the assignment of the frequencies of the 9-keto carbonyl group(s) at 1700 cm-1 in P700 and at 1717 cm-1 in P700+.(ABSTRACT TRUNCATED AT 250 WORDS)     

Mid- to low-frequency Fourier transform infrared spectra of S-state cycle for photosynthetic water oxidation in Synechocystis sp. PCC 6803

Flash-induced Fourier transform infrared (FTIR) difference spectra for the four-step S-state cycle and the effects of global (15)N- and (13)C-isotope labeling on the difference spectra were examined for the first time in the mid- to low-frequency (1200-800 cm(-1)) as well as the mid-frequency (1700-1200 cm(-1)) regions using photosystem (PS) II core particles from cyanobacterium Synechocystis sp. PCC 6803. The difference spectra clearly exhibited the characteristic vibrational features for each transition during the S-state cycling. It is likely that the bands that change their sign and intensity with the S-state advances reflect the changes of the amino acid residues and protein matrices that have functional and/or structural roles within the oxygen-evolving complex (OEC). Except for some minor differences, the trends of S-state dependence in the 1700-1200 cm(-1) frequency spectra of the PS II cores from Synechocystis were comparable to that of spinach, indicating that the structural changes of the polypeptide backbones and amino acid side chains that occur during the oxygen evolution are inherently identical between cyanobacteria and higher plants. Upon (13)C-labeling, most of the bands, including amide I and II modes and carboxylate stretching modes, showed downward shifts; in contrast, (15)N-labeling induced isotopic shifts that were predominantly observed in the amide II region. In the mid- to low-frequency region, several bands in the 1200-1140 cm(-1) region were attributable to the nitrogen- and/or carbon-containing group(s) that are closely related to the oxygen evolution process. Specifically, the putative histidine ligand exhibited a band at 1113 cm(-1) which was affected by both (15)N- and (13)C-labeling and showed distinct S-state dependency. The light-induced bands in the 900-800 cm(-1) region were downshifted only by (13)C-labeling, whereas the bands in the 1000-900 cm(-1) region were affected by both (15)N- and (13)C-labeling. Several modes in the mid- to low-frequency spectra were induced by the change in protonation state of the buffer molecules accompanied by S-state transitions. Our studies on the light-induced spectrum showed that contributions from the redox changes of Q(A) and the non-heme iron at the acceptor side and Y(D) were minimal. It was, therefore, suggested that the observed bands in the 1000-800 cm(-1) region include the modes of the amino acid side chains that are coupled to the oxidation of the Mn cluster. S-state-dependent changes were observed in some of the bands.     

Analysis of flash-induced FTIR difference spectra of the S-state cycle in the photosynthetic water-oxidizing complex by uniform 15N and 13C isotope labeling

Protein bands in flash-induced Fourier transform infrared (FTIR) difference spectra of the S-state cycle of photosynthetic water oxidation were analyzed by uniform (15)N and (13)C isotopic labeling of photosystem II (PS II). The difference spectra upon first- to fourth-flash illumination were obtained with hydrated (for the 1800-1200 cm(-)(1) region) or deuterated (for the 3500-3100 cm(-)(1) region) films of unlabeled, (15)N-labeled, and (13)C-labeled PS II core complexes from Thermosynechococcus elongatus. Shifts of band frequencies upon (15)N and (13)C labeling provided the assignments of major peaks in the regions of 3450-3250 and 1700-1630 cm(-)(1) to the NH stretches and amide I modes of polypeptide backbones, respectively, and the assignments of some of the peaks in the 1600-1500 cm(-)(1) region to the amide II modes of backbones. Other prominent peaks in the latter region and most of the peaks in the 1450-1300 cm(-)(1) region exhibited large downshifts upon (13)C labeling but were unchanged by (15)N labeling, and hence assigned to the asymmetric and symmetric COO(-) stretching vibrations, respectively, of carboxylate groups in Glu, Asp, or the C-terminus. Peak positions corresponded well with each other among the first- to fourth-flash spectra, and most of the bands in the first- and/or second-flash spectra appeared with opposite signs of intensity in the third- and/or fourth-flash spectra. This observation indicates that the protein movements in the S(1)-->S(2) and/or S(2)-->S(3) transitions are mostly reversed in the S(3)-->S(0) and/or S(0)-->S(1) transitions, representing a catalytic role of the protein moieties of the water-oxidizing complex. Drastic structural changes in carboxylate groups over the S-state cycle suggest that the Asp and/or Glu side chains play important roles in the reaction mechanism of photosynthetic water oxidation.