Taguchi Taketo, Stone Kari L, Gupta Rupal, Kaiser-Lassalle Benedikt, Yano Junko, Hendrich Michael P, Borovik A S
Department of Chemistry, University of California-Irvine, 1102 Natural Sciences II, Irvine, CA 92697-2025, USA.
Department of Chemistry, Benedictine College, Lisle, IL 60532.
Chem Sci. 2014 Aug 1;5(8):3064-3071. doi: 10.1039/C4SC00453A.
Photosynthetic water oxidation is catalyzed by a MnOCa cluster with an unprecedented arrangement of metal ions in which a single manganese center is bonded to a distorted MnOCa cubane-like structure. Several mechanistic proposals describe the unique manganese center as a site for water binding and subsequent formation of a high valent Mn-oxo center that reacts with a M-OH unit (M = Mn or Ca) to form the O-O bond. The conversion of low valent Mn-OH (n = 1,2) to a Mn-oxo species requires that a single manganese site be able to accommodate several oxidation states as the water ligand is deprotonated. To study these processes, the preparation and characterization of a new monomeric Mn-OH complex is described. The Mn-OH complex completes a series of well characterized Mn-OH and Mn-oxo complexes containing the same primary and secondary coordination spheres; this work thus demonstrates that a single ligand can support mononuclear Mn complexes spanning four different oxidation states (II through V) with oxo and hydroxo ligands that are derived from water. Moreover, we have completed a thermodynamic analysis based on this series of manganese complexes to predict the formation of high valent Mn-oxo species; we demonstrated that the conversion of a Mn-OH species to a Mn-oxo complex would likely occur via a stepwise proton transfer-electron transfer mechanism. The large dissociation energy for the MnO-H bond (~95 kcal/mol) diminished the likelihood that other pathways are operative within a biological context. Furthermore, these studies showed that reactions between Mn-OH and Mn-oxo complexes lead to non-productive, one-electron processes suggesting that initial O-O bond formation with the OEC does not involve an Mn-OH unit.
光合水氧化由一个锰氧钙簇催化,该簇具有前所未有的金属离子排列方式,其中单个锰中心与一个扭曲的类锰氧钙立方烷结构相连。有几种机理假说将这个独特的锰中心描述为水结合位点以及随后形成高价锰氧中心的位点,该高价锰氧中心与一个M-OH单元(M = Mn或Ca)反应形成O-O键。低价Mn-OH(n = 1,2)向锰氧物种的转化要求单个锰位点能够在水配体去质子化时容纳几种氧化态。为了研究这些过程,本文描述了一种新型单体Mn-OH配合物的制备与表征。该Mn-OH配合物完善了一系列具有相同一级和二级配位球的、表征充分的Mn-OH和锰氧配合物;这项工作因此表明,单个配体能够支持单核锰配合物跨越四种不同氧化态(II至V),其氧代和羟基配体均衍生自水。此外,我们基于这一系列锰配合物完成了热力学分析,以预测高价锰氧物种的形成;我们证明Mn-OH物种向锰氧配合物的转化可能通过逐步质子转移-电子转移机制发生。MnO-H键的高解离能(约95千卡/摩尔)降低了其他途径在生物环境中起作用的可能性。此外,这些研究表明Mn-OH和锰氧配合物之间的反应会导致非生产性的单电子过程,这表明与放氧复合体的初始O-O键形成不涉及Mn-OH单元。