Corry Thomas A, O'Malley Patrick J
School of Chemistry , The University of Manchester , Manchester , M13 9PL , U.K.
J Phys Chem Lett. 2018 Nov 1;9(21):6269-6274. doi: 10.1021/acs.jpclett.8b02793. Epub 2018 Oct 18.
A novel mechanism for the final stages of Nature's photosynthetic water oxidation to molecular oxygen is proposed. This is based on a comparison of experimental and broken symmetry density functional theory (BS-DFT) calculated geometries and magnetic resonance properties of water oxidizing complex models in the final metastable oxidation state, S. We show that peroxo models of the S state are in vastly superior agreement with the current experimental structural determinations compared with oxo-hydroxo models. Comparison of experimental and BS-DFT calculated Mn hyperfine couplings for the electron paramagnetic resonance (EPR) visible form shows better agreement for the oxo-hydroxo model. An equilibrium between oxo-hydroxo and peroxo models is proposed for the S state and the major implications for the final steps in the water oxidation mechanism are analyzed and discussed.
提出了一种关于自然界光合作用中水分子最终氧化为分子氧阶段的新机制。这是基于对处于最终亚稳态氧化态S的水氧化复合物模型的实验几何结构、破缺对称性密度泛函理论(BS-DFT)计算的几何结构以及磁共振性质进行比较得出的。我们表明,与羟基氧模型相比,S态的过氧模型与当前的实验结构测定结果更为吻合。对电子顺磁共振(EPR)可见形式的实验和BS-DFT计算的锰超精细耦合进行比较,结果表明羟基氧模型的吻合度更好。本文提出了S态中羟基氧模型和过氧模型之间的平衡,并分析和讨论了其对水氧化机制最终步骤的主要影响。