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探究放氧复合体中的锰氧化态。来自光谱、计算和动力学数据的见解。

Probing the Mn oxidation states in the OEC. Insights from spectroscopic, computational and kinetic data.

作者信息

Kuzek D, Pace R J

机构信息

Department of Chemistry, Faculty of Science, The Australian National University, G.P.O. Box 4, A.C.T. 0200, Canberra, Australia.

出版信息

Biochim Biophys Acta. 2001 Jan 5;1503(1-2):123-37. doi: 10.1016/s0005-2728(00)00218-8.

Abstract

Results from a variety of experimental techniques which have been used to define the oxidation levels of Mn and other components in the S states of the water oxidising complex in Photosystem II are reviewed. A self-consistent interpretation of Mn X-ray absorption near edge spectroscopy, UV-visible and near infrared spectroscopic data suggests that Mn oxidation occurs only on the S0-->S1 transition, and that all four Mn centres have formal oxidation state III thereafter. Ligand oxidation occurs on the transitions to S2 and S3. This is supported by high level quantum chemical calculations and an analysis of the kinetics of substrate water exchange, as recently determined by Wydrzynski et al. (this journal). One type of model for the catalytic site structure and water oxidation mechanism, consistent with these conclusions, is discussed. This model invokes magnetically separate oxo bridged dimers with water oxidation occurring by a concerted 2H+/2e- transfer mechanism, with one H transfer to a bridge oxygen on each dimer.

摘要

本文综述了多种实验技术的结果,这些技术用于确定光系统II中析氧复合物S态下锰及其他成分的氧化态。对锰X射线吸收近边光谱、紫外可见光谱和近红外光谱数据的自洽解释表明,锰的氧化仅发生在S0→S1跃迁上,此后所有四个锰中心的形式氧化态均为III。配体氧化发生在向S2和S3的跃迁上。这一观点得到了高水平量子化学计算以及对底物水交换动力学分析的支持,正如Wydrzynski等人(本刊)最近所确定的那样。本文讨论了一种与这些结论一致的催化位点结构和水氧化机制的模型。该模型提出了磁分离的氧桥联二聚体,水氧化通过协同的2H+/2e-转移机制发生,每个二聚体上有一个H转移到桥氧上。

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