Light-dependent production of dioxygen in photosynthesis.

Junko Yano, Jan Kern, Vittal K Yachandra, Håkan Nilsson, Sergey Koroidov, Johannes Messinger
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Abstract

Oxygen, that supports all aerobic life, is abundant in the atmosphere because of its constant regeneration by photosynthetic water oxidation, which is catalyzed by a Mn₄CaO₅ cluster in photosystem II (PS II), a multi subunit membrane protein complex. X-ray and other spectroscopy studies of the electronic and geometric structure of the Mn₄CaO₅ cluster as it advances through the intermediate states have been important for understanding the mechanism of water oxidation. The results and interpretations, especially from X-ray spectroscopy studies, regarding the geometric and electronic structure and the changes as the system proceeds through the catalytic cycle will be summarized in this review. This review will also include newer methodologies in time-resolved X-ray diffraction and spectroscopy that have become available since the commissioning of the X-ray free electron laser (XFEL) and are being applied to study the oxygen-evolving complex (OEC). The femtosecond X-ray pulses of the XFEL allows us to outrun X-ray damage at room temperature, and the time-evolution of the photo-induced reaction can be probed using a visible laser-pump followed by the X-ray-probe pulse. XFELs can be used to simultaneously determine the light-induced protein dynamics using crystallography and the local chemistry that occurs at the catalytic center using X-ray spectroscopy under functional conditions. Membrane inlet mass spectrometry has been important for providing direct information about the exchange of substrate water molecules, which has a direct bearing on the mechanism of water oxidation. Moreover, it has been indispensable for the time-resolved X-ray diffraction and spectroscopy studies and will be briefly reviewed in this chapter. Given the role of PS II in maintaining life in the biosphere and the future vision of a renewable energy economy, understanding the structure and mechanism of the photosynthetic water oxidation catalyst is an important goal for the future.

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光合作用中依靠光产生二氧。
支持所有有氧生命的氧气在大气中含量丰富,这是因为氧气通过光合作用水氧化作用不断再生,而光合作用水氧化作用是由光合系统 II(PS II)(一种多亚基膜蛋白复合体)中的 Mn₄CaO₅簇催化的。对 Mn₄CaO₅簇在中间状态时的电子和几何结构进行的 X 射线和其他光谱研究,对于了解水氧化的机理非常重要。本综述将总结有关几何和电子结构以及系统在催化循环过程中的变化的结果和解释,特别是 X 射线光谱研究的结果和解释。本综述还将包括自 X 射线自由电子激光器(XFEL)投入使用以来出现的时间分辨 X 射线衍射和光谱学的最新方法,这些方法正被用于研究氧演变复合物(OEC)。XFEL 的飞秒 X 射线脉冲使我们能够在室温下超越 X 射线损伤,并且可以在 X 射线探针脉冲之后使用可见激光泵探查光诱导反应的时间演变。XFEL 可用来同时测定结晶学中光诱导的蛋白质动力学,以及功能条件下催化中心的 X 射线光谱所发生的局部化学反应。膜入口质谱法对于提供底物水分子交换的直接信息非常重要,这直接关系到水氧化的机理。此外,它对于时间分辨 X 射线衍射和光谱研究也是不可或缺的,本章将对其进行简要回顾。鉴于 PS II 在维持生物圈生命方面的作用以及未来可再生能源经济的愿景,了解光合作用水氧化催化剂的结构和机理是未来的一个重要目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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