| Literature DB >> 25347729 |
Mikhail Askerka1, Jimin Wang, Gary W Brudvig, Victor S Batista.
Abstract
The S1 → S2 transition of the oxygen-evolving complex (OEC) of photosystem II does not involve the transfer of a proton to the lumen and occurs at cryogenic temperatures. Therefore, it is commonly thought to involve only Mn oxidation without any significant change in the structure of the OEC. Here, we analyze structural changes upon the S1 → S2 transition, as revealed by quantum mechanics/molecular mechanics methods and the isomorphous difference Fourier method applied to serial femtosecond X-ray diffraction data. We find that the main structural change in the OEC is in the position of the dangling Mn and its coordination environment.Entities:
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Year: 2014 PMID: 25347729 PMCID: PMC4230327 DOI: 10.1021/bi5011915
Source DB: PubMed Journal: Biochemistry ISSN: 0006-2960 Impact factor: 3.162
Figure 1QM/MM S1 and S2 models and difference Fourier maps. (A) Simulated S2-minus-S1 difference Fourier maps calculated using the QM/MM S1 and S2 models and phases derived from multicrystal noncrystallographic symmetry averaging (see the text for computational procedures and contour levels). The highest peak near the OEC results from the displacement of Mn4. (B) Comparison of the simulated S2-minus-S1 (from panel A) and X-ray-observed S2-minus-S1 (from panel C) difference Fourier maps with color codes according to panels A and C. (C) Observed S2-minus-S1 difference Fourier maps calculated from ref (7).