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底物氧的早期结合导致了光系统II中一个光谱特征不同的S态。

Early Binding of Substrate Oxygen Is Responsible for a Spectroscopically Distinct S State in Photosystem II.

作者信息

Pushkar Yulia, K Ravari Alireza, Jensen Scott C, Palenik Mark

机构信息

Department of Physics and Astronomy, Purdue University, West Lafayette, Indiana 47907, United States.

Code 6189, Chemistry Division, Naval Research Laboratory, Washington, DC 20375, United States.

出版信息

J Phys Chem Lett. 2019 Sep 5;10(17):5284-5291. doi: 10.1021/acs.jpclett.9b01255. Epub 2019 Aug 27.

Abstract

The biological generation of oxygen by the oxygen-evolving complex (OEC) in photosystem II (PS II) is one of nature's most important reactions. The OEC is a MnCa cluster that has multiple Mn-O-Mn and Mn-O-Ca bridges and binds four water molecules. Previously, binding of an additional oxygen was detected in the S to S transition. Here we demonstrate that early binding of the substrate oxygen to the five-coordinate Mn center in the S state is likely responsible for the S high-spin EPR signal. Substrate binding in the Mn-OH form explains the prevalence of the high-spin S state at higher pH and its low-temperature conversion into the S state. The given interpretation was confirmed by X-ray absorption spectroscopic measurements, DFT, and broken symmetry DFT calculations of structures and magnetic properties. Structural, electronic, and spectroscopic properties of the high-spin S state model are provided and compared with the available S state models. New interpretation of the high-spin S state opens opportunity for analysis of factors controlling the oxygen substrate binding in PS II.

摘要

光系统II(PS II)中由析氧复合物(OEC)进行的氧气生物生成是自然界最重要的反应之一。OEC是一个锰钙簇,具有多个Mn-O-Mn和Mn-O-Ca桥,并结合四个水分子。此前,在S到S的转变中检测到了额外一个氧的结合。在此我们证明,底物氧在S态时与五配位锰中心的早期结合可能是S高自旋电子顺磁共振(EPR)信号的原因。以Mn-OH形式存在的底物结合解释了在较高pH下高自旋S态的普遍存在及其在低温下向S态的转变。通过X射线吸收光谱测量、密度泛函理论(DFT)以及结构和磁性的破缺对称性DFT计算,证实了上述解释。提供了高自旋S态模型的结构、电子和光谱性质,并与现有的S态模型进行了比较。对高自旋S态的新解释为分析控制PS II中氧底物结合的因素提供了机会。

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