In this series of articles, the board members of ChemSusChem discussrecent research articles that they consider of exceptional quality and importance for sustainability.T his entry features Prof. L. Sun, who proposes as pecialm echanismf or OÀOb ond formationi np hotosystem II with involvement of an Mn VII -oxo speciesi nduced by charge-a nd structural rearrangements. In this viewpoint, Proton transfer is involved in changes of the first coordination spheres around the Mn VII -oxo site on the dangling Mn4 with de-and re-coordination of carboxylates (Glu333 and Asp170).
Mechanism of OÀOB ond Formation in Photosystem IIPhotosynthesis in plants, algae, and cyanobacteria is significant to the aerobic life on Earth. The mechanism of water oxidation in photosystem II (PSII), whichi sakey point in photosynthesis, becomes more and more intriguing, owing not only to curiosity towards uncovering the mystery of nature but also to the strong desire to provide ab lueprint to guide the development of man-made water-oxidation catalysts for artificial photosynthesis. [1] Since the proposal of Kok's five-state S-cycle in 1970, extensive investigations on the photosynthetic oxygen evolution have been performed with complex interplay between numerous different disciplines including biochemistry,m olecular and structural biology,b iophysics, physicalc hemistry,a nd quantum chemistry. [1c,d, 2] The structure of the oxygen evolution complex (OEC), the catalytic centerf or water oxidation in PSII, has been well studied in the past decades by high-resolutionX -ray crystallography,s howing ac lear picture of the Mn 4 CaO 5 cluster with surrounding amino-acid residues (Y Z ,D 1-H190, D1-D61, etc.), two Cl À ions, and many H 2 Om olecules ( Figure 1a). [3] Moreover, severalb reakthroughsh ave been made to understand the catalytic water-oxidation mechanism by the OEC. Kineticso ft he S-statet ransitions have been estimated by different in situ physical measurements, as shown in Figure 1b. [4] Amazingly, structures of all four meta-stable states S 0 ,S 1 ,S 2 ,a nd S 3 have been crystallographically characterized recently. [5] In the transitions S 0 !S 1 andS 1 !S 2 ,the Mn 4 CaO 5 cluster undergoes no significant structural changes. Insertion of an ew oxygen (O6 found by Suga et al. [5a] or Ox found by Kern et al. [5b] )t oM n1 from W3 H 2 Oo nC awas clearly observed in the S 2 !S 3 transition with two transients tates, revealing the previously proposed structural changes in this step. At present, the first three transitions (S 0 !S 1 !S 2 !S 3 )a re close to be cleared with plenty of experimental results.H owever,t he steps of S 3 !(S 4 )!S 0 , which directly involve an active state S 4 ,O ÀOb ond formation, and O 2 release, are poorly understood. There is no direct experimental identification of the hypothetical transients tate S 4 . Lack of characterization of these steps has greatly restricted the proposal of ac omplete catalytic cycle for water oxidation by the OEC in nature.Twoe xtensive hypotheses that have been discussed his...