Nature’s water splitting cofactor passes through a series of catalytic intermediates (S0-S4) before O-O bond formation and O2 release. In the second last transition (S2 to S3) cofactor oxidation is coupled to water molecule binding to Mn1. It is this activated, water-enriched all MnIV form of the cofactor that goes on to form the O-O bond, after the next light-induced oxidation to S4. How cofactor activation proceeds remains an open question. Here, we report a so far not described intermediate (S3') in which cofactor oxidation has occurred without water insertion. This intermediate can be trapped in a significant fraction of centers (>50%) in (i) chemical-modified cofactors in which Ca2+ is exchanged with Sr2+; the Mn4O5Sr cofactor remains active, but the S2-S3 and S3-S0 transitions are slower than for the Mn4O5Ca cofactor; and (ii) upon addition of 3% vol/vol methanol; methanol is thought to act as a substrate water analog. The S3' electron paramagnetic resonance (EPR) signal is significantly broader than the untreated S3 signal (2.5 T vs. 1.5 T), indicating the cofactor still contains a 5-coordinate Mn ion, as seen in the preceding S2 state. Magnetic double resonance data extend these findings revealing the electronic connectivity of the S3' cofactor is similar to the high spin form of the preceding S2 state, which contains a cuboidal Mn3O4Ca unit tethered to an external, 5-coordinate Mn ion (Mn4). These results demonstrate that cofactor oxidation regulates water molecule insertion via binding to Mn4. The interaction of ammonia with the cofactor is also discussed.
Biological water oxidation, performed by a single enzyme, photosystem II, is a central research topic not only in understanding the photosynthetic apparatus but also for the development of water splitting catalysts for technological applications. Great progress has been made in this endeavor following the report of a high-resolution X-ray crystallographic structure in 2011 resolving the cofactor site (Umena et al. in Nature 473:55–60, 2011), a tetra-manganese calcium complex. The electronic properties of the protein-bound water oxidizing Mn4OxCa complex are crucial to understand its catalytic activity. These properties include: its redox state(s) which are tuned by the protein matrix, the distribution of the manganese valence and spin states and the complex interactions that exist between the four manganese ions. In this short review we describe how magnetic resonance techniques, particularly EPR, complemented by quantum chemical calculations, have played an important role in understanding the electronic structure of the cofactor. Together with isotope labeling, these techniques have also been instrumental in deciphering the binding of the two substrate water molecules to the cluster. These results are briefly described in the context of the history of biological water oxidation with special emphasis on recent work using time resolved X-ray diffraction with free electron lasers. It is shown that these data are instrumental for developing a model of the biological water oxidation cycle.
In biological water oxidation, a redox-active tyrosine residue (D1-Tyr161 or Y Z ) mediates electron transfer between the Mn 4 CaO 5 cluster of the oxygen-evolving complex and the charge-separation site of photosystem II (PSII), driving the cluster through progressively higher oxidation states S i ( i = 0–4). In contrast to lower S-states (S 0 , S 1 ), in higher S-states (S 2 , S 3 ) of the Mn 4 CaO 5 cluster, Y Z cannot be oxidized at cryogenic temperatures due to the accumulation of positive charge in the S 1 → S 2 transition. However, oxidation of Y Z by illumination of S 2 at 77–190 K followed by rapid freezing and charge recombination between Y Z • and the plastoquinone radical Q A •– allows trapping of an S 2 variant, the so-called S 2 trapped state (S 2 t ), that is capable of forming Y Z • at cryogenic temperature. To identify the differences between the S 2 and S 2 t states, we used the S 2 t Y Z • intermediate as a probe for the S 2 t state and followed the S 2 t Y Z • /Q A •– recombination kinetics at 10 K using time-resolved electron paramagnetic resonance spectroscopy in H 2 O and D 2 O. The results show that while S 2 t Y Z • /Q A •– recombination can be described as pure electron transfer occurring in the Marcus inverted region, the S 2 t → S 2 reversion depends on proton rearrangement and exhibits a strong kinetic isotope effect. This suggests that Y Z oxidation in the S 2 t state is facilitated by favorable proton redistribution in the vicinity of Y Z , most likely within the hydrogen-bonded Y Z –His190–Asn298 triad. Computational models show that tautomerization of Asn298 to its imidic acid form enables proton translocation to an adjacent asparagine-rich cavity of water molecules that functions as a proton reservoir and can further participate in proton egress to the lumen.
The oxygen evolving complex of Photosystem II undergoes four light-induced oxidation transitions, S(0)-S(1),...,S(3)-(S(4))S(0) during its catalytic cycle. The oxidizing equivalents are stored at a (Mn)(4)Ca cluster, the site of water oxidation. EPR spectroscopy has yielded valuable information on the S states. S(2) shows a notable heterogeneity with two spectral forms; a g=2 (S=1/2) multiline, and a g=4.1 (S=5/2) signal. These oscillate in parallel during the period-four cycle. Cyanobacteria show only the multiline signal, but upon advancement to S(3) they exhibit the same characteristic g=10 (S=3) absorption with plant preparations, implying that this latter signal results from the multiline configuration. The fate of the g=4.1 conformation during advancement to S(3) is accordingly unknown. We searched for light-induced transient changes in the EPR spectra at temperatures below and above the half-inhibition temperature for the S(2) to S(3) transition (ca 230K). We observed that, above about 220K the g=4.1 signal converts to a multiline form prior to advancement to S(3). We cannot exclude that the conversion results from visible-light excitation of the Mn cluster itself. The fact however, that the conversion coincides with the onset of the S(2) to S(3) transition, suggests that it is triggered by the charge-separation process, possibly the oxidation of tyr Z and the accompanying proton relocations. It therefore appears that a configuration of (Mn)(4)Ca with a low-spin ground state advances to S(3).
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