FTIR detection of water reactions in the oxygen-evolving centre of photosystem II

Flash-induced Fourier transform infrared (FTIR) difference spectroscopy has been used to study the water-oxidizing reactions in the oxygen-evolving centre of photosystem II. Reactions of water molecules were directly monitored by detecting the OH stretching bands of weakly H-bonded OH of water in the 3700-3500 cm(-1) region in FTIR difference spectra during S-state cycling. In the S1-->S2 transition, a band shift from 3588 to 3617 cm(-1) was observed, indicative of a weakened H-bond. Decoupling experiments using D2O:H2O (1:1) showed that this OH arose from a water molecule with an asymmetric H-bonding structure and this asymmetry became more significant upon S2 formation. In the S2-->S3, S3-->S0 and S0-->S1 transitions, negative bands were observed at 3634, 3621 and 3612 cm(-1), respectively, representing formation of a strong H-bond or a proton release reaction. In addition, using complex spectral features in the carboxylate stretching region (1600-1300 cm-(1)) as 'fingerprints' of individual S-state transitions, pH dependency of the transition efficiencies and the effect of dehydration were examined to obtain the information of proton release and water insertion steps in the S-state cycle. Low-pH inhibition of the S2-->S3, S3-->S0 and S0-->S1 transitions was consistent with a view that protons are released in the three transitions other than S1-->S2, while relatively high susceptibility to dehydration in the S2-->S3 and S3-->S0 transitions suggested the insertion of substrate water into the system during these transitions. Thus, a possible mechanism of water oxidation to explain the FTIR data is proposed.     

X-ray spectroscopy of the Mn4Ca cluster in the water-oxidation complex of Photosystem II

The water-oxidation complex of Photosystem II (PS II) contains a heteronuclear cluster of 4 Mn atoms and a Ca atom. Ligands to the metal cluster involve bridging O atoms, and O and N atoms from amino acid side-chains of the D1 polypeptide of PS II, with likely additional contributions from water and CP43. Although moderate resolution X-ray diffraction-based structures of PS II have been reported recently, and the location of the Mn₄Ca cluster has been identified, the structures are not resolved at the atomic level. X-ray absorption (XAS), emission (XES), resonant inelastic X-ray scattering (RIXS) and extended X-ray absorption fine structure (EXAFS) provide independent and potentially highly accurate sources of structural and oxidation-state information. When combined with polarized X-ray studies of oriented membranes or single-crystals of PS II, a more detailed picture of the cluster and its disposition in PS II is obtained.     

Calcium controls the assembly of the photosynthetic water-oxidizing complex: a cadmium(II) inorganic mutant of the Mn4Ca core

Perturbation of the catalytic inorganic core (Mn4Ca1OxCly) of the photosystem II-water-oxidizing complex (PSII-WOC) isolated from spinach is examined by substitution of Ca2+ with cadmium(II) during core assembly. Cd2+ inhibits the yield of reconstitution of O2-evolution activity, called photoactivation, starting from the free inorganic cofactors and the cofactor-depleted apo-WOC-PSII complex. Ca2+ affinity increases following photooxidation of the first Mn2+ to Mn3+ bound to the 'high-affinity' site. Ca2+ binding occurs in the dark and is the slowest overall step of photoactivation (IM1-->IM1* step). Cd2+ competitively blocks the binding of Ca2+ to its functional site with 10- to 30-fold higher affinity, but does not influence the binding of Mn2+ to its high-affinity site. By contrast, even 10-fold higher concentrations of Cd2+ have no effect on O2-evolution activity in intact PSII-WOC. Paradoxically, Cd2+ both inhibits photoactivation yield, while accelerating the rate of photoassembly of active centres 10-fold relative to Ca2+. Cd2+ increases the kinetic stability of the photooxidized Mn3+ assembly intermediate(s) by twofold (mean lifetime for dark decay). The rate data provide evidence that Cd2+ binding following photooxidation of the first Mn3+, IM1-->IM1*, causes three outcomes: (i) a longer intermediate lifetime that slows IM1 decay to IM0 by charge recombination, (ii) 10-fold higher probability of attaining the degrees of freedom (either or both cofactor and protein d.f.) needed to bind and photooxidize the remaining 3 Mn2+ that form the functional cluster, and (iii) increased lability of Cd2+ following Mn4 cluster assembly results in (re)exchange of Cd2+ by Ca2+ which restores active O2-evolving centres. Prior EPR spectroscopic data provide evidence for an oxo-bridged assembly intermediate, Mn3+(mu-O2(-))Ca2+, for IM1*. We postulate an analogous inhibited intermediate with Cd2+ replacing Ca2+.     

Disorganization of the Mn4Ca complex of photosystem II by ruthenium red: a thermoluminescence study

Ruthenium red (RR) is known to be an inhibitor that binds to Ca²⁺ sites. It releases Ca²⁺ and Cl^? together with the extrinsic polypeptide of 17 kDa associated with the oxygen evolving complex of photosystem II. In this work we used thermoluminescence to study S_2/3Q_B^? and S₂Q_A^? charge recombination. It is shown that RR produced a deeper inhibition of oxygen evolution compared with the effect of extrinsic polypeptide or Ca²⁺/Cl^? depletion. Even though Mn is not released, the Mn cluster is disorganized by RR and the S₁ → S₂ transition is inhibited. Copyright © 2008 John Wiley & Sons, Ltd.     

Light-induced FTIR difference spectroscopy as a powerful tool toward understanding the molecular mechanism of photosynthetic oxygen evolution

The molecular mechanism of photosynthetic oxygen evolution remains a mystery in photosynthesis research. Although recent X-ray crystallographic studies of the photosystem II core complex at 3.0-3.5 A resolutions have revealed the structure of the oxygen-evolving center (OEC), with approximate positions of the Mn and Ca ions and the amino acid ligands, elucidation of its detailed structure and the reactions during the S-state cycle awaits further spectroscopic investigations. Light-induced Fourier transform infrared (FTIR) difference spectroscopy was first applied to the OEC in 1992 as detection of its structural changes upon the S(1)-->S(2) transition, and spectra during the S-state cycle induced by consecutive flashes were reported in 2001. These FTIR spectra provide extensive structural information on the amino acid side groups, polypeptide chains, metal core, and water molecules, which constitute the OEC and are involved in its reaction. FTIR spectroscopy is thus becoming a powerful tool in investigating the reaction mechanism of photosynthetic oxygen evolution. In this mini-review, the measurement method of light-induced FTIR spectra of OEC is introduced and the results obtained thus far using this technique are summarized.     

Drastic changes in the ligand structure of the oxygen-evolving Mn cluster upon Ca depletion as revealed by FTIR difference spectroscopy

A Fourier transform infrared (FTIR) difference spectrum of the oxygen-evolving Mn cluster upon the S₁-to-S₂ transition was obtained with Ca²⁺-depleted photosystem II (PSII) membranes to investigate the structural relevance of Ca²⁺ to the Mn cluster. Previously, Noguchi et al. [Biochim. Biophys. Acta 1228 (1995) 189] observed drastic changes in the carboxylate stretching region of the S₂/S₁ FTIR spectrum upon Ca²⁺ depletion, whereas Kimura and co-workers [Biochemistry 40 (2001) 14061; ibid. 41 (2002) 5844] later claimed that these changes were not ascribed to Ca²⁺ depletion itself but caused by the interaction of EDTA to the Mn cluster and/or binding of K⁺ at the Ca²⁺ site. In the present study, the preparation of the Ca²⁺-depleted PSII sample and its FTIR measurement were performed in the absence of EDTA and K⁺. The obtained S₂/S₁ spectrum exhibited the loss of carboxylate bands at 1587/1562 and 1364/1403 cm^− 1 and diminished amide I intensities, which were identical to the previous observations in the presence of EDTA and K⁺. This result indicates that the drastic FTIR changes are a pure effect of Ca²⁺ depletion, and provides solid evidence for the general view that Ca²⁺ is strongly coupled with the Mn cluster.     

Specific interaction of chalcone-protein: cardamonin binding site II on the human serum albumin molecule

Cardamonin (2',4'-dihydroxy-6'-methoxychalcone), one of the main constituents from the seeds of Alpinia katsumadai Hayata, belongs to chalcone with its antibacterial, antiinflammatory and other important therapeutic activities of significant potency and low systemic toxicity. In this article, the interaction of cardamonin to human serum albumin (HSA) has been studied for the first time by spectroscopic methods including Fourier transform infrared (FTIR) spectroscopy, circular dichroism (CD), and UV-absorption spectroscopy in combination with fluorescence quenching under physiological conditions with drug concentrations of 0.67-4.0 microM. The results of the spectroscopic measurements and the thermodynamic parameters obtained (the enthalpy change DeltaH(0) and the entropy change DeltaS(0) were calculated to be -25.312 and 7.040 J.mol(-1).K(-1) according to the van't Hoff equation) suggest that hydrophobic interaction is the predominant intermolecular forces stabilizing the complex, which is also in good agreement with the results of the molecule modeling study. The alterations of protein secondary structure in the presence of cardamonin in aqueous solution were quantitatively calculated by the evidence from CD and FTIR spectroscopes with reductions of alpha-helices of about 20%, decreases of beta-sheet structures of about 14%, and increases of beta-turn structures of about 15%. The quenching mechanism and the number of binding sites (n approximately 1) were obtained by fluorescence titration data. Fluorescent displacement measurements confirmed that cardamonin binds HSA on site II. In addition, the effects of common ions on the constants of the cardamonin-HSA complex were also discussed.     

Interaction of N,N,N′,N′-tetramethyl-p-phenylenediamine with photosystem II as revealed by thermoluminescence: Reduction of the higher oxidation states of the Mn cluster and displacement of plastoquinone from the QB niche

The flash-induced thermoluminescence (TL) technique was used to investigate the action of N,N,N′,N′-tetramethyl-p-phenylenediamine (TMPD) on charge recombination in photosystem II (PSII). Addition of low concentrations (μM range) of TMPD to thylakoid samples strongly decreased the yield of TL emanating from S₂Q_B⁻ and S₃Q_B⁻ (B-band), S₂Q_A⁻ (Q-band), and Y_D⁺Q_A⁻ (C-band) charge pairs. Further, the temperature-dependent decline in the amplitude of chlorophyll fluorescence after a flash of white light was strongly retarded by TMPD when measured in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). Though the period-four oscillation of the B-band emission was conserved in samples treated with TMPD, the flash-dependent yields (Y_n) were strongly declined. This coincided with an upshift in the maximum yield of the B-band in the period-four oscillation to the next flash. The above characteristics were similar to the action of the ADRY agent, carbonylcyanide m-chlorophenylhydrazone (CCCP). Simulation of the B-band oscillation pattern using the integrated Joliot-Kok model of the S-state transitions and binary oscillations of Q_B confirmed that TMPD decreased the initial population of PSII centers with an oxidized plastoquinone molecule in the Q_B niche. It was deduced that the action of TMPD was similar to CCCP, TMPD being able to compete with plastoquinone for binding at the Q_B-site and to reduce the higher S-states of the Mn cluster.     

Stepwise Transition of the Tetra-Manganese Complex of Photosystem II to a Binuclear Mn2(μ-O)2 Complex in Response to a Temperature Jump: A Time-Resolved Structural Investigation Employing X-Ray Absorption Spectroscopy

In oxygenic photosynthesis, water is oxidized at a protein-cofactor complex comprising four Mn atoms and, presumably, one calcium. Using multilayers of Photosystem II membrane particles, we investigated the time course of the disassembly of the Mn complex initiated by a temperature jump from 25°C to 47°C and terminated by rapid cooling after distinct heating periods. We monitored polarographically the oxygen-evolution activity, the amount of the Y_D^ox radical and of released Mn²⁺ by EPR spectroscopy, and the structure of the Mn complex by x-ray absorption spectroscopy (XAS, EXAFS). Using a novel approach to analyze time-resolved EXAFS data, we identify three distinct phases of the disassembly process: (1) Loss of the oxygen-evolution activity and reduction of Y_D^ox occur simultaneously (k₁ = 1.0 min⁻¹). EXAFS spectra reveal the concomitant loss of an absorber-backscatterer interaction between heavy atoms separated by ~3.3 Å, possibly related to Ca release. (2) Subsequently, two Mn(III) or Mn(IV) ions seemingly separated by ~2.7 Å in the native complex are reduced to Mn(II) and released (k₂ = 0.18 min⁻¹). The x-ray absorption spectroscopy data is highly suggestive that the two unreleased Mn ions form a di-μ-oxo bridged Mn(III)₂ complex. (3) Finally, the tightly-bound Mn₂(μ-O)₂ unit is slowly reduced and released (k₃ = 0.014 min⁻¹).     

Time-resolved step-scan FTIR difference spectroscopy for the study of photosystem I with different benzoquinones incorporated into the A1 binding site

Time-resolved step-scan FTIR difference spectroscopy has been used to study photosystem I (PSI) with plastoquinone-9 (PQ) and two other benzoquinones (2,6-dimethyl-1,4-benzoquinone and 2,3,5,6-tetrachloro-1,4-benzoquinone) incorporated into the A₁ binding site. By subtracting a (P700⁺A₁^????P700A₁) FTIR difference spectrum for PSI with the native phylloquinone (PhQ) incorporated from corresponding spectra for PSI with different benzoquinones (BQs) incorporated, FTIR double difference spectra are produced, that display bands associated with vibrational modes of the quinones, without interference from features associated with protein vibrational modes.Molecular models for BQs involved in asymmetric hydrogen bonding were constructed and used in vibrational mode frequency calculations. The calculated data were used to aid in the interpretation and assignment of bands in the experimental spectra. We show that the calculations capture the general trends found in the experimental spectra.By comparing four different FTIR double difference spectra we are able to verify unambiguously bands associated with phyllosemiquinone in PSI at 1495 and 1415?cm^?1. We also resolve a previously unrecognized band of phyllosemiquinone at 1476?cm^?1 that calculations suggest is due in part to a C₄$\stackrel{?}{?}$O stretching mode.For PSI with PQ incorporated, calculations and experiment taken together indicate that the C₁$\stackrel{?}{?}$O and C₄$\stackrel{?}{?}$O vibrational modes of the semiquinone give rise to bands at 1487 and 1444?cm^?1, respectively. This is very distinct compared to PSI with PhQ incorporated.From the calculated and experimental spectra, we show that it is possible to distinguish between two possible orientations of PQ in the A₁ protein binding site.