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The decay of the light-induced spin-correlated radical pair [P700+ A1-] and the associated electron spin echo envelope modulation (ESEEM) have been studied in either thylakoid membranes, cellular membranes, or purified photosystem I prepared from the wild-type strains of Synechocystis sp. PCC 6803, Chlamydomonas reinhardtii, and Spinaceae oleracea. The decay of the spin-correlated radical pair is described in the wild-type membrane by two exponential components with lifetimes of 2-4 and 16-25 micros. The proportions of the two components can be altered by preillumination of the membranes in the presence of reductant at temperatures lower than 220 K, which leads to the complete reduction of the iron-sulfur electron acceptors F(A), F(B), and F(X) and partial photoaccumulation of the reduced quinone electron acceptor A1A-. The "out-of-phase" (OOP) ESEEM attributed to the [P700+ A1-] radical pair has been investigated in the three species as a function of the preillumination treatment. Values of the dipolar (D) and the exchange (J) interactions were extracted by time-domain fitting of the OOP-ESEEM. The results obtained in the wild-type systems are compared with two site-directed mutants of C. reinhardtii [Santabarbara et al. (2005) Biochemistry 44, 2119-2128], in which the spin-polarized signal on either the PsaA- or PsaB-bound electron transfer pathway is suppressed so that the radical pair formed on each electron transfer branch could be monitored selectively. This comparison indicates that when all of the iron-sulfur centers are oxidized, only the echo modulation associated with the A branch [P700+ A1A-] radical pair is observed. The reduction of the iron-sulfur clusters and the quinone A1 by preillumination treatment induces a shift in the ESEEM frequency. In all of the systems investigated this observation can be interpreted in terms of different proportions of the signal associated with the [P700+ A1A-] and [P700+ A1B-] radical pairs, suggesting that bidirectionality of electron transfer in photosystem I is a common feature of all species rather than being confined to green algae.

We have used pulsed electron paramagnetic resonance (EPR) measurements of the electron spin polarised (ESP) signals arising from the geminate radical pair P700(z.rad;+)/A(1)(z.rad;-) to detect electron transfer on both the PsaA and PsaB branches of redox cofactors in the photosystem I (PSI) reaction centre of Chlamydomonas reinhardtii. We have also used electron nuclear double resonance (ENDOR) spectroscopy to monitor the electronic structure of the bound phyllosemiquinones on both the PsaA and PsaB polypeptides. Both these spectroscopic assays have been used to analyse the effects of site-directed mutations to the axial ligands of the primary chlorophyll electron acceptor(s) A(0) and the conserved tryptophan in the PsaB phylloquinone (A(1)) binding pocket. Substitution of histidine for the axial ligand methionine on the PsaA branch (PsaA-M684H) blocks electron transfer to the PsaA-branch phylloquinone, and blocks photoaccumulation of the PsaA-branch phyllosemiquinone. However, this does not prevent photoautotrophic growth, indicating that electron transfer via the PsaB branch must take place and is alone sufficient to support growth. The corresponding substitution on the PsaB branch (PsaB-M664H) blocks kinetic electron transfer to the PsaB phylloquinone at 100 K, but does not block the photoaccumulation of the phyllosemiquinone. This transformant is unable to grow photoautotrophically although PsaA-branch electron transfer to and from the phyllosemiquinone is functional, indicating that the B branch of electron transfer may be essential for photoautotrophic growth. Mutation of the conserved tryptophan PsaB-W673 to leucine affects the electronic structure of the PsaB phyllosemiquinone, and also prevents photoautotrophic growth.

Previous work in many laboratories has established that hydroxylamine reduces the S(1) state of the water oxidizing complex (WOC) in one-electron steps. Significant levels of what can now be defined as the S(-1)* state are achieved by specific (concentration and incubation length) hydroxylamine treatments. This state has already been studied by electron paramagnetic resonance spectrometry (EPR), and unusual EPR signals were noted (for example, see Sivaraja, M., and Dismukes, G. C. (1988) Biochemistry 27, 3467-3475). We have now reinvestigated these initial experiments and confirmed many of the original observations. We then utilized more recent EPR markers for the S(0) and S(1) states to further explore the S(-1)* state. The broad radical "split" type EPR signal, produced by 200 K illumination of samples prepared to give a high yield of the S(-1)* state, is shown to most likely reflect a trapped intermediate state between S(-1)* and S(0)*, since samples where this signal is present can be warmed in the dark to produce S(0)*. The threshold for advancement from S(-1)* to S(0)* is near 200 K, as the yield of broad radical decreases and S(0)* multiline EPR signal increases with length of 200 K illumination. Advancement of S(0)* to S(1) is limited at 200 K, but S(1) can be restored by 273 K illumination. Illumination of these hydroxylamine-treated samples at temperatures below 77 K gives a second broad radical EPR signal. The line shape, decay, and other properties of this new radical signal suggest that it may arise from an interaction in the S(-2)* or lower S states, which are probably present in low yield in these samples. Illumination below 20 K of S(0)* state samples containing methanol, and therefore exhibiting the S(0) multiline signal, gives rise to a third broad radical with distinctive line shape. The characteristics of the three broad radicals are similar to those found from interactions between Y(Z)(*) and other S states. The evidence is presented that they do represent intermediate states in S state turnover. Further work is now needed to identify these radicals.

Intra-subunit interactions in the environment of the iron-sulfur cluster F(X) in Photosystem I (PS I) of Synechocystis sp. PCC 6803 were studied by site-directed and second site suppressor mutations. In subunit PsaB, the cysteine ligand (C565) of F(X) and a conserved aspartate (D566) adjacent to C565 were modified. The resulting mutants D566E, C556S/D566E, C556H/D566E and C565H/D566E did not assemble PS I in the thylakoids of the cyanobacterium. Yet, this is the first report of cells of the second site-suppressor mutant (D566E/L416P) and of second site-directed mutant (C565S/D566E) in PsaB that could grow autotrophically in light and were found to assemble a stable functional PS I containing all three iron-sulfur centers, F(X) and F(A/B). The newly resolved structure of PS I (PDB 1JB0) was used to interpret the functional interactions among the amino acid residues. It is suggested that the stability of F(X) is supported by a salt bridge formed between D566, which is adjacent to the cysteine ligand C565 of the iron-sulfur cluster located on loop hi, and R703 located at the start of loop jk. Hydrogen bond between R703 and D571 at the start of loop hi further stabilizes the arginine. Lengthening of the side by 1.2 A chain in mutation D566E caused destabilization of F(X). The extended side-chain was compensated for by the Fe-O, which is 0.3 A shorter than the Fe-S bond resulting in stabilization of the F(X) in the double mutations C565S/D566E. The suppressor mutation D566E/L416P allowed greater freedom for the salt bridge E566-R703, thus relieving the pressure introduced by the D566E replacement and enabling the formation of F(X). F(X) and R703 are therefore stabilized through short- and long-range interactions of the inter-helical loops between h-i, j-k and f-g, respectively.

Photoaccumulation of membrane preparations of Chlamydomonas reinhardtii at pH 8 and 220 K reduces the primary and secondary electron acceptors in the Photosystem I (PSI) reaction centre, and produces a maximum of two spins per P700(z.rad;+). Proton electron nuclear double resonance (ENDOR) spectra demonstrate that the phyllosemiquinone produced is that attributed to the PsaA branch of electron transfer. Photoaccumulation at pH 10 and 220 K produces a maximum of four spins per P700(z.rad;+), and proton ENDOR spectra indicate that a second phyllosemiquinone is being photoaccumulated, with markedly different proton hyperfine couplings (hfcs). This phyllosemiquinone is unaffected by mutation of PsaAW693, confirming that it does not arise from the PsaA branch of electron transfer, and we therefore attribute it to the PsaB phyllosemiquinone.

To investigate the environment of the phylloquinone secondary electron acceptor A(1) within the photosystem I reaction center, we have carried out site-directed mutagenesis of two tryptophan residues (W693 and W702) in the PsaA subunit of Chlamydomonas reinhardtii. One of these conserved tryptophans (W693) is predicted to be close to the phylloquinone and has been implicated in the interaction of A(1) with an aromatic residue through pi--pi stacking. We find that replacement of W702 with either histidine or leucine has no effect on the electronic structure of A(1)(*-) or on forward electron transfer from A(1)(*-) to the iron--sulfur center F(x). In contrast, the same mutations of W693 alter the electronic structure of the photoaccumulated A(1)(*-) and slow forward electron transfer as measured by the decay of the electron spin-polarized signal arising from the P700(*+)/A(1)(*-) radical pair. These results provide support for the hypothesis that W693 has a role in poising the redox potential of A(1)/A(1)(*-) so it can reduce F(x), and they indirectly provide evidence for electron transfer along the PsaA-side branch of cofactors in PSI.

This mini-review outlines the current theories on the mechanism of electron transfer from water to P680, the location and structure of the water oxidising complex and the role of the manganese cluster. We discuss how our data fit in with current theories and put forward our ideas on the location and mechanism of water oxidation.

The interaction of water oxidising photosystem II preparations with the aqueous environment has been investigated using electron spin echo envelope modulation spectroscopy in the presence of 2H(2)O. The spectra show interaction of 2H of 2H(2)O with the preparation in the S(2) state. The component interacting with water decays during 1-4 weeks storage at 77 K. No interaction of water with the classical multiline S(2) Mn signal, which is more stable on storage at 77 K, was detected. The results show that a component of the water oxidation complex, possibly involving the Mn centre, is accessible to water and may be the water binding site for photosynthetic water oxidation.

Photoaccumulation at 205 K in the presence of dithionite produces EPR signals in anaerobically prepared membranes from Chlorobium limicola and Heliobacterium chlorum that resemble the EPR spectrum of phyllosemiquinone (A1*-) photoaccumulated in photosystem I. We have used ENDOR and special TRIPLE resonance spectroscopy to demonstrate conclusively that these signals arise from menasemiquinone electron acceptors reduced by photoaccumulation. Hyperfine couplings to two protons H-bonded to the semiquinone oxygens have been identified by exchange of H. chlorum into D2O, and hyperfine couplings to the methyl group, and the methylene group of the phytyl side chain, of the semiquinone have also been assigned. The electronic structure of these menasemiquinones in these reaction centers is very similar to that of phyllosemiquinone in PSI, and shows a distorted electron spin density distribution relative to that of phyllosemiquinone in vitro. Special TRIPLE resonance spectrometry has been used to investigate the effect of detergents and oxygen on membranes of C. limicola. Triton X-100 and oxygen affect the menaquinone binding site, but n-dodecyl beta-D-maltoside preparations exhibit a relatively unaltered special TRIPLE spectrum for the photoaccumulated menasemiquinone.

Interaction of the water oxidising manganese complex of photosystem II with the aqueous environment has been investigated using electron paramagnetic resonance spectroscopy and electron spin echo envelope modulation spectroscopy to detect interaction of [2H]methanol with the complex in the S2 state. The experiments show that the classical S2 multiline signal is associated with a manganese environment which is not exposed to the aqueous medium. An electron paramagnetic resonance spectroscopy signal, also induced by 200 K illumination, showing 2H modulation by methanol in the medium and a modified multiline electron paramagnetic resonance spectroscopy signal formed in parallel to it, are suggested to be associated with a second manganese environment exposed to the medium.

The S0* state was generated by incubation of dark-adapted (S1 state) photosystem II membranes either with the exogenous two electron reductant hydrazine and subsequent 273 K illumination in the presence of DCMU or by dark incubation with low amounts of the one electron reductant hydroxylamine. In agreement with earlier reports, the S1 and S-1 states were found to be electron paramagnetic resonance (EPR) silent. However, in the presence of 0.5-1.5% methanol, a weak EPR multiline signal centered around g = 2.0 was observed at 7 K for the S0* states generated by both procedures. This signal has a similar average line splitting to the well-characterized S2 state multiline EPR signal, but can be clearly distinguished from that and other modified S2 multiline signals by differences in line position and intensities. In addition, at 4 K it can be seen that the S0* multiline has a greater spectral breadth than the S2 multilines and is composed of up to 26 peaks. The S0* signal is not seen in the absence of methanol and is not affected by 1 mM EDTA in the buffer medium. We assign the S0* multiline signal to the manganese cluster of the oxygen evolving complex in a mixed valence state of the form MnIIMnIIIMnIIIMnIII,MnIIMnIIIMnIVMnIV, or MnIIIMnIIIMnIIIMnIV. Addition of methanol may be helpful in future to find an EPR signal originating form the natural S0 state.

Experiments are described which allow the detection and characterization of new EPR signals in photosystem II (PSII). PSII has been extensively studied with the water oxidising complex (WOC) poised in the S1 and S2 states. Other stages in the cycle of water oxidation lack characteristic EPR signals for use as probes. In this study, experiments use multiple turnovers of PSII from an initial S1 state to allow new states of PSII to be studied. The first EPR signal detected, centered at g = 4.85 and termed the g = 5 signal, is suggested to be a new form of S2 probably formed by decay of S3 at cryogenic temperatures, but a novel form of oxidized non-heme iron cannot be fully excluded at present. The second signal is split around g = 2 and shows characteristics of signals formed by spin-spin interaction between two paramagnetic species. The split g = 2 signal is reversibly formed by illumination at <30 K of a sample containing the g = 5 signal. The g = 2 signal may be a form of the "S3" EPR signal previously only found in a variety of PSII preparations where oxygen evolution has been inhibited. Those "S3" signals are thought to arise from the interaction of an oxidized amino acid radical and the S2 state, i.e., S2X+. Illumination at higher temperatures or illumination at <30 K, followed by dark-adaptation at 77 K, removes the g = 5 signal and prevents subsequent detection of the g = 2 signal on illumination at <30 K. The most likely explanation of our data is that illumination at <30 K of centers containing the g = 5 species allows accumulation of an oxidized intermediate and that at higher temperatures electron transfer proceeds to re-form an EPR-silent S state equivalent to that initially trapped during sample preparation. Study of these signals should provide an important new insight into the WOC and PSII.

The association of water with the Mn of the water oxidizing complex was investigated using H2(17)O- and 2H2O-reconstituted lyophilized photosystem II particles. The pulsed electron paramagnetic resonance (EPR) technique of electron spin echo envelope modulation (ESEEM) was used to investigate the interaction of the magnetic 2H and 17O nuclei with the paramagnetic S2 state of the Mn complex and other photosystem II components. ESEEM offers a much more specific and sensitive detection of this type of interaction than continuous wave (CW) EPR. Unlike earlier reports using CW EPR, these experiments did not detect any interaction of water with the multiline EPR signal from the S2 state of the Mn complex. No signals indicating specific interaction of either H or O with the multiline signal were detected. Signals due to 2H and 17O were detected only at the Larmour frequency, indicating nonspecific "distant ENDOR" effects. A weak interaction with 17O was detected both in S1, when the Mn is EPR silent, and in S2, but only on the high-field side of g = 2. This interaction may be with the Rieske iron-sulfur center in the cytochrome b6f complex. The results were the same whether the multiline signal was generated by 200 K illumination of dark-frozen samples, or by room temperature illumination in the presence of the inhibitor 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). Illumination at room temperature in the presence of an electron acceptor to allow multiple turnovers of the system with cycling of the S states did not result in the appearance of any new interactions. These results appear to exclude close (less than 6 A) binding of water to the Mn center giving rise to the multiline signal, and also to exclude mechanisms in which water oxidation involves the breaking and re-formation of the mu-oxo bridges of the Mn complex. They cannot, however, exclude models in which water binding to the manganese complex and direct oxidation by the manganese complex occur in the higher S states, or are catalyzed by one bis(mu-oxo) Mn dimer while oxidizing equivalents are accumulated in the S2 state by a second bis(mu-oxo) Mn dimer.

Previous work has challenged the assignment of a photoaccumulated EPR signal to the phylloquinone electron acceptor in photosystem I, A1.-. Biosynthetic deuteration of the phylloquinone in the cyanobacterium Anabaena variabilis has been shown to narrow this photoaccumulated signal, demonstrating that the signal arises from A1.-. The ESP signal attributed to P700.+A1.- is also narrowed by this deuteration, showing that the photoaccumulated EPR signal and the ESP signal are monitoring the same redox component. Confirmation that the photoaccumulated EPR signal comes from deuterated phylloquinone was obtained by exchanging the deuterated for protonated phylloquinone, which broadened the photoaccumulated EPR signal.

The photoaccumulated radical state of the photosystem 1 secondary electron acceptor A1, A1.-, has been studied in spinach and the cyanobacterium Anabaena variabilis strain Met27 using electron nuclear double resonance (ENDOR) and electron--nuclear--nuclear special triple (ST) resonance spectroscopies. Spectra of A1.- in both these species are very similar. ENDOR spectra of the phylloquinone anion radical in solvent glass were also obtained. Comparison of the spectra of the in vivo and in vitro radicals shows that A1.- is a phylloquinone anion radical with a distorted electron spin density distribution. Hyperfine couplings to the A1.- methyl group and to two protons hydrogen bonded to the quinone oxygens have been identified using biosynthetic deuteration in A. variabilis. Possible hyperfine coupling to a methylene proton of the phytyl side chain of the quinone has also been identified. These results are compared with those from previous studies of protein-bound semiquinones in the light of the unusual redox potential of A1.

ENDOR and special TRIPLE spectroscopies have been used to study the electron spin density distribution and hydrogen bonding of the plastosemiquinone anion radical, QA.-, of photosystem 2. The semiquinone radical was made accessible to ENDOR through the use of exogenous cyanide, which decouples the radical from the ferrous iron of the photosystem 2 ferroquinone acceptor complex [Sanakis, Y., et al. (1994) Biochemistry 33, 9922]. H2O/D2O exchange was used to assign hyperfine couplings to hydrogen-bonded protons, and orientation-selected special TRIPLE spectroscopy has revealed the orientation of hydrogen bonds relative to the quinone ring. Methyl group resonances have also been assigned. ENDOR spectra of the decylplastosemiquinone anion radical in vitro are presented for comparison. This shows that interaction with the protein leads to changes in the electron spin density distribution and the hydrogen bond orientation; both hydrogen bonds are parallel to the quinone ring plane in vitro, whereas QA.- has one parallel and one perpendicular to the plane. These results are discussed in the light of previous ENDOR studies of the ubiquinone radical QA.- of Rhodobacter sphaeroides and the predicted structure of the QA-binding region of photosystem 2.

Using EPR and EXAFS spectroscopies we show that high concentrations of ammonium cations at alkaline pH are required for (1) inhibition of oxygen evolution: (2) an alteration of the EPR properties of the oxygen evolving complex: (3) the ability to detect YZ; and (4) the slow reduction of the Mn complex leading to the appearance of EPR detectable Mn2+. The inhibition of S state cycling, slowing of YZ reduction, appearance of Mn2+ and the yield of a Hpp < 10 mT S3 type EPR signal are decreased by calcium addition. This indicates that these effects were probably associated with calcium depletion arising from the high concentration of ammonium cation. The ammonia-induced changes to the S2 multiline EPR signal are not affected by calcium addition. The appearance of Mn2+ is shown to be reversible on illumination, suggesting that the Mn reduced from the native state is located at or near the native site. Simulations of the interaction which give rise to the S3 EPR signal are also presented and discussed. These indicate that lineshape differences occur through small changes in the exchange component of the interaction between the manganese complex and organic radical, probably through minor structural changes between the variously treated samples.

Pulsed EPR spectroscopy and selective removal of the iron-sulfur centers in photosystem 1 have been used to study forward electron transfer from the secondary electron acceptor A1. At cryogenic temperatures where forward electron transfer is inhibited, we have observed a g = 2.003 electron spin-echo signal presenting a characteristic phase shift. This out-of-phase signal is attributed to the electron spin-polarized pair P700+/A1-, it decays with t1/e = 23 microseconds, reflecting the recombination reaction. At room temperature the out-of-phase signal is also observed, but it decays with t1/c = 200 ns in untreated photosystem 1, due to forward electron transfer from A1- to one of the iron-sulfur centers. This rate is unchanged in Fe-SA/B-depleted PS1 but is lost when the iron-sulfur center Fe-Sx is removed. In the preparations depleted of all iron-sulfur centers the out-of-phase signal decays with t1/c = 1.3 microseconds, reflecting either the back reaction or the decay of polarization. These results demonstrate that the electron transfer pathway in photosystem 1 is P700-->A1-->Fe-SX-->Fe-SA/B.

The radical cation P840+. was studied in frozen suspensions of Chlorobium limicola f. sp. thiosulphatophilum membranes using ENDOR and Special TRIPLE spectroscopies. The spectra show that P840+. arises from a bacteriochlorophyll a 'special' pair with a highly symmetrical distribution of electron spin density between the constituent bacteriochlorophylls. Special TRIPLE spectroscopy has resolved the separate contributions of the two halves of the pair and revealed small deviations from a 1:1 electron spin density distribution. Nevertheless P840+. appears to come the closest yet to the symmetrical 'dimer' originally proposed for the structure of the primary donor radical cation (P870+.) in purple non-sulphur photosynthetic bacteria.

Manganese K-edge X-ray spectra have been obtained for Photosystem II samples isolated using Triton X-100 detergent and samples further purified by n-heptyl beta-D-thioglucoside detergent treatment to remove light-harvesting polypeptides and low-affinity calcium. The structure of the manganese complex is very similar for the two detergent preparations used. Analysis of the e.x.a.f.s. spectra for samples in the S1 and S2 states indicate changes in bond lengths for the shells of oxygen/nitrogen atoms. For the S1 state, oxygen shells at 0.181 and 0.193 nm (1.81 and 1.93 A) were observed and one manganese shell at 0.270 nm (2.70A). In the S2 state the oxygen bond lengths are longer at 0.184 and 0.200 nm (1.84 and 2.00 A). Additionally a shell of scatterers at 0.37 nm (3.7 A) was observed in both states which could be fitted to models with calcium scatterers at this distance.

The origin of the "S3" EPR signal from calcium-depleted photosystem 2 samples has been investigated. This signal is observed after freezing samples under illumination and has been assigned to an interaction between the manganese cluster and an oxidized histidine radical [Boussac et al. (1990) Nature 347; 303-306]. In calcium-depleted samples prepared by three different methods, we observed the trapping of the tyrosine radical YZ+ under conditions which also formed the "S3" signal. An "S3"-type signal and YZ+ were also formed in PS2 samples treated with the water analogue ammonia. Following illumination at 277 K, the "S3" and YZ+ signals decayed at the same rate at 273 K in the dark. Both the YZ+ and "S3" signals decayed on storage at 77 K and could be subsequently regenerated by illumination at 8-77 K. No evidence to support histidine oxidation was found. The effects of DCMU, chelators, and alkaline pH on the dark-stable multiline S2 and the "S3" signals from calcium-depleted samples were determined. Both signals required the presence of EGTA or citrate for maximum yield. The addition of DCMU caused a reduction in the yield of "S3" generated by freezing under illumination. Incubation at pH 7.5 resulted in the loss of both signals. We propose that a variety of treatments which affect calcium and chloride binding cause a stabilization of the S2 state and slow the reduction of YZ+. This allows the trapping of YZ+, the interaction with the manganese cluster (probably in the S2 state) resulting in the "S3" signal. The data allow the position of the manganese cluster to be estimated as within 10 A of tyrosine Z (D1-161).