Huang Hao-Li, Brudvig Gary W
Department of Chemistry, Yale University, New Haven, CT 06520, USA.
BBA Adv. 2021 May 11;1:100014. doi: 10.1016/j.bbadva.2021.100014. eCollection 2021.
We derive a model that provides an exact solution to the substrate-water exchange kinetics in a double-conformation system and use this model to interpret recently published data for Ca- and Sr-containing PSII in the S state, in which the g = 2.0 and g = 4.1 conformations coexist. The component concentrations derived from the kinetic model provide an analytic description of the substrate-water exchange kinetics, allowing us to more accurately interpret the results. Based on this model and the previously reported data on the S state g = 2.0 conformation, we obtain the substrate-water exchange rates of the g = 4.1 conformation and the conformational change rates. Two conclusions are made from the analyses. First, contrary to previous reports, there is no significant effect of substituting Sr for Ca on any of the exchange rate constants. Second, the exchange rate of the slowly-exchanging water (W) in the S state g = 4.1 conformation is much faster than that in the S state g = 2.0 conformation. The second conclusion is consistent with the assignment of W to W1 or W2 bound as terminal ligands to Mn4; Mn4 has been proposed to undergo an oxidation state change from Mn(IV) in the g = 2.0 conformation to Mn(III) in the g = 4.1 conformation.
我们推导了一个模型,该模型为双构象系统中的底物 - 水交换动力学提供了精确解,并使用此模型来解释最近发表的关于处于S态的含Ca和Sr的光系统II的数据,其中g = 2.0和g = 4.1构象共存。从动力学模型得出的组分浓度提供了底物 - 水交换动力学的解析描述,使我们能够更准确地解释结果。基于此模型和先前报道的关于S态g = 2.0构象的数据,我们获得了g = 4.1构象的底物 - 水交换速率和构象变化速率。分析得出两个结论。第一,与先前的报道相反,用Sr替代Ca对任何交换速率常数均无显著影响。第二,S态g = 4.1构象中缓慢交换的水(W)的交换速率比S态g = 2.0构象中的快得多。第二个结论与将W指定为作为末端配体与Mn4结合的W1或W2一致;有人提出Mn4的氧化态从g = 2.0构象中的Mn(IV)变为g = 4.1构象中的Mn(III)。