Azide as a probe of proton transfer reactions in photosynthetic oxygen evolution

Substitution of the D1-Asn87 site in photosystem II of cyanobacteria mimics the chloride-binding characteristics of spinach photosystem II

Photoinduced water oxidation at the O₂-evolving complex (OEC) of photosystem II (PSII) is a complex process involving a tetramanganese-calcium cluster that is surrounded by a hydrogen-bonded network of water molecules, chloride ions, and amino acid residues. Although the structure of the OEC has remained conserved over eons of evolution, significant differences in the chloride-binding characteristics exist between cyanobacteria and higher plants. An analysis of amino acid residues in and around the OEC has identified residue 87 in the D1 subunit as the only significant difference between PSII in cyanobacteria and higher plants. We substituted the D1-Asn⁸⁷ residue in the cyanobacterium Synechocystis sp. PCC 6803 (wildtype) with alanine, present in higher plants, or with aspartic acid. We studied PSII core complexes purified from D1-N87A and D1-N87D variant strains to probe the function of the D1-Asn⁸⁷ residue in the water-oxidation mechanism. EPR spectra of the S₂ state and flash-induced FTIR spectra of both D1-N87A and D1-N87D PSII core complexes exhibited characteristics similar to those of wildtype Synechocystis PSII core complexes. However, flash-induced O₂-evolution studies revealed a decreased cycling efficiency of the D1-N87D variant, whereas the cycling efficiency of the D1-N87A PSII variant was similar to that of wildtype PSII. Steady-state O₂-evolution activity assays revealed that substitution of the D1 residue at position 87 with alanine perturbs the chloride-binding site in the proton-exit channel. These findings provide new insight into the role of the D1-Asn⁸⁷ site in the water-oxidation mechanism and explain the difference in the chloride-binding properties of cyanobacterial and higher-plant PSII.

Detection of an intermediary, protonated water cluster in photosynthetic oxygen evolution

In photosynthesis, photosystem II evolves oxygen from water by the accumulation of photooxidizing equivalents at the oxygen-evolving complex (OEC). The OEC is a Mn4CaO5 cluster, and its sequentially oxidized states are termed the Sn states. The dark-stable state is S1, and oxygen is released during the transition from S3 to S0. In this study, a laser flash induces the S1 to S2 transition, which corresponds to the oxidation of Mn(III) to Mn(IV). A broad infrared band, at 2,880 cm(-1), is produced during this transition. Experiments using ammonia and (2)H2O assign this band to a cationic cluster of internal water molecules, termed "W5(+)." Observation of the W5(+) band is dependent on the presence of calcium, and flash dependence is observed. These data provide evidence that manganese oxidation during the S1 to S2 transition results in a coupled proton transfer to a substrate-containing, internal water cluster in the OEC hydrogen-bonded network.

A hydrogen-bonding network plays a catalytic role in photosynthetic oxygen evolution

In photosystem II, oxygen evolution occurs by the accumulation of photo-induced oxidizing equivalents at the oxygen-evolving complex (OEC). The sequentially oxidized states are called the S(0)-S(4) states, and the dark stable state is S(1). Hydrogen bonds to water form a network around the OEC; this network is predicted to involve multiple peptide carbonyl groups. In this work, we tested the idea that a network of hydrogen bonded water molecules plays a catalytic role in water oxidation. As probes, we used OEC peptide carbonyl frequencies, the substrate-based inhibitor, ammonia, and the sugar, trehalose. Reaction-induced FT-IR spectroscopy was used to describe the protein dynamics associated with the S(1) to S(2) transition. A shift in an amide CO vibrational frequency (1664 (S(1)) to 1653 (S(2)) cm(-1)) was observed, consistent with an increase in hydrogen bond strength when the OEC is oxidized. Treatment with ammonia/ammonium altered these CO vibrational frequencies. The ammonia-induced spectral changes are attributed to alterations in hydrogen bonding, when ammonia/ammonium is incorporated into the OEC hydrogen bond network. The ammonia-induced changes in CO frequency were reversed or blocked when trehalose was substituted for sucrose. This trehalose effect is attributed to a displacement of ammonia molecules from the hydrogen bond network. These results imply that ammonia, and by extension water, participate in a catalytically essential hydrogen bond network, which involves OEC peptide CO groups. Comparison to the ammonia transporter, AmtB, reveals structural similarities with the bound water network in the OEC.

A sensitive multispectroscopic probe for nucleic acids

Azides have recently been used as vibrational probes of proteins, but their incorporation into nucleic acids has been limited to photo-cross-linking or click chemistry applications. The utility of 2'-azido-2'-deoxyuridine (N(3)-dU, 1) as an IR and (15)N NMR spectroscopic probe of the sugar phosphate backbone region of nucleic acids was investigated by measuring the effects of solvent, heterodimer formation, and temperature on peak frequencies and IR bandwidth. The azide IR asymmetric stretching band (nu(N(3))) of N(3)-dU was sensitive to its environment, undergoing a blue shift of 13.5 cm(-1) when changing the solvent from THF to water. The solvent effects on (15)N chemical shifts (delta((15)N)) of each of the nitrogen atoms in the azido group was studied, and the terminal nitrogen atom was the most sensitive to solvent, shifting downfield by 3.8 ppm when changing the solvent from THF-d(8) to D(2)O. Formation of a base-pair-like heterodimer between 3 (a silyl ether analogue of 1) and 2,6-diheptanamidopyridine (4) in chloroform resulted in minimal changes in the IR and (15)N NMR spectral frequency and chemical shift, respectively, as expected given the location of the azido moiety. The intrinsic temperature dependence of nu(N(3)) and delta((15)N) were found to be minimal over the temperature range studied especially compared to the solvent dependence of these spectral observables. The analysis of the experimental studies was complemented by density functional theory (DFT) calculations on model systems.