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首页> 外文期刊>Philosophical Transactions of the Royal Society of London, Series B. Biological Sciences >QM/MM computational studies of substrate water binding to the oxygen-evolving centre of photosystem II
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QM/MM computational studies of substrate water binding to the oxygen-evolving centre of photosystem II

机译:底物水与光系统II的析氧中心结合的QM / MM计算研究

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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 μ4-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 18O-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.
机译:本文报道了对底物水与光系统II(PSII)的氧演化中心(OEC)结合的计算研究,该结合完全由氨基酸残基,水,氢氧化物和氯化物连接。该计算基于PSII的OEC的量子力学/分子力学的混合模型,该模型是最近与来自蓝藻嗜热嗜热球菌的PSII的X射线晶体结构一起开发的。 OEC模型包括一个长方体Mn3CaO4Mn金属簇,该簇具有三个紧密相连的锰离子,这些锰离子与一个通过μ4氧连接的Mn离子相连,通常称为“悬锰”。假定两个与钙和悬挂的锰结合的水分子是底物分子,负责形成双氧。发现与Mn(4)结合的水的能垒与模型配合物的能垒很好地吻合。然而,与钙结合的水的屏障大得多。水的结合不仅仅与金属中心的形式氧化态相关,而且还与它们各自的静电势原子电荷相关,如电荷转移相互作用所调节。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的18O标记水的交换速率应比悬挂锰的水分子的交换速率小。这些模型还预测,S1→S2的过渡应该对两种水交换速率产生相反的影响。

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