Siegbahn Per E M
Department of Organic Chemistry, Arrhenius Laboratory, Stockholm University, SE-106 91, Stockholm, Sweden.
Phys Chem Chem Phys. 2014 Jun 28;16(24):11893-900. doi: 10.1039/c3cp55329a.
The main parts of the water oxidation mechanism in photosystem II have now been established both from theory and experiments. Still, there are minor questions remaining. One of them concerns the charge and the protonation state of the oxygen evolving complex (OEC). Previously, theory and experiments have agreed that the two water derived ligands on the outer manganese should be one hydroxide and one water. In the present study it is investigated whether both of them could be water. This question is addressed by a detailed study of energy diagrams, but in this context it is more conclusive to compare the redox potential of the OEC to the one of TyrZ. Both procedures lead to the conclusion that one of the ligands is a hydroxide. Another question concerns the protonation of the second shell His337, where the results are more ambiguous. The final part of the present study describes results when calcium is removed from the OEC. Even though protons enter to compensate the charge of the missing Ca(2+), the redox potential and the pKa value of the OEC change dramatically and prevent the progress after S2.
目前,通过理论和实验已经确定了光系统II中析氧机制的主要部分。不过,仍存在一些小问题。其中之一涉及放氧复合体(OEC)的电荷和质子化状态。此前,理论和实验一致认为,外层锰上两个源自水的配体应该是一个氢氧根和一个水。在本研究中,探讨了它们是否都可以是水。通过对能量图的详细研究来解决这个问题,但在这种情况下,将OEC的氧化还原电位与TyrZ的氧化还原电位进行比较更具决定性。两种方法都得出一个配体是氢氧根的结论。另一个问题涉及第二壳层His337的质子化,其结果更具模糊性。本研究的最后部分描述了从OEC中去除钙后的结果。尽管质子进入以补偿缺失的Ca(2+)的电荷,但OEC的氧化还原电位和pKa值发生了巨大变化,并阻止了S2之后的进程。