Sproviero Eduardo M, Shinopoulos Katherine, Gascón José A, McEvoy James P, Brudvig Gary W, Batista Victor S
Department of Chemistry, Yale University, PO Box 208107, New Haven, CT 06520-8107, USA.
Philos Trans R Soc Lond B Biol Sci. 2008 Mar 27;363(1494):1149-56; discussion 1156. doi: 10.1098/rstb.2007.2210.
This paper reports computational studies of substrate water binding to the oxygen-evolving centre (OEC) of photosystem II (PSII), completely ligated by amino acid residues, water, hydroxide and chloride. The calculations are based on quantum mechanics/molecular mechanics hybrid models of the OEC of PSII, recently developed in conjunction with the X-ray crystal structure of PSII from the cyanobacterium Thermosynechococcus elongatus. The model OEC involves a cuboidal Mn3CaO4Mn metal cluster with three closely associated manganese ions linked to a single mu4-oxo-ligated Mn ion, often called the 'dangling manganese'. Two water molecules bound to calcium and the dangling manganese are postulated to be substrate molecules, responsible for dioxygen formation. It is found that the energy barriers for the Mn(4)-bound water agree nicely with those of model complexes. However, the barriers for Ca-bound waters are substantially larger. Water binding is not simply correlated to the formal oxidation states of the metal centres but rather to their corresponding electrostatic potential atomic charges as modulated by charge-transfer interactions. The calculations of structural rearrangements during water exchange provide support for the experimental finding that the exchange rates with bulk 18 O-labelled water should be smaller for water molecules coordinated to calcium than for water molecules attached to the dangling manganese. The models also predict that the S1-->S2 transition should produce opposite effects on the two water-exchange rates.
本文报道了对与光系统II(PSII)的析氧中心(OEC)结合的底物水的计算研究,该OEC完全由氨基酸残基、水、氢氧化物和氯离子连接。计算基于PSII的OEC的量子力学/分子力学混合模型,该模型是最近结合来自嗜热栖热放线菌的PSII的X射线晶体结构开发的。模型OEC包含一个长方体状的Mn3CaO4Mn金属簇,其中三个紧密相连的锰离子与一个单μ4-氧连接的锰离子相连,该锰离子通常被称为“悬空锰”。假定与钙和悬空锰结合的两个水分子是底物分子,负责形成二氧。发现与Mn(4)结合的水的能垒与模型配合物的能垒非常吻合。然而,与钙结合的水的能垒要大得多。水的结合不仅仅与金属中心的形式氧化态相关,而是与它们相应的静电势原子电荷相关,该电荷由电荷转移相互作用调节。水交换过程中结构重排的计算为实验发现提供了支持,即与钙配位的水分子与大量18O标记水的交换速率应比与悬空锰相连的水分子的交换速率小。模型还预测S1→S2跃迁应该对两种水交换速率产生相反的影响。