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氨与光合作用系统 II 放氧复合物的结合鉴定了锰四聚体的可交换溶剂氧桥(μ-氧)。

Ammonia binding to the oxygen-evolving complex of photosystem II identifies the solvent-exchangeable oxygen bridge (μ-oxo) of the manganese tetramer.

机构信息

Max-Planck-Institut für Chemische Energiekonversion, D-45470 Mülheim an der Ruhr, Germany.

出版信息

Proc Natl Acad Sci U S A. 2013 Sep 24;110(39):15561-6. doi: 10.1073/pnas.1304334110. Epub 2013 Sep 10.

Abstract

The assignment of the two substrate water sites of the tetra-manganese penta-oxygen calcium (Mn4O5Ca) cluster of photosystem II is essential for the elucidation of the mechanism of biological O-O bond formation and the subsequent design of bio-inspired water-splitting catalysts. We recently demonstrated using pulsed EPR spectroscopy that one of the five oxygen bridges (μ-oxo) exchanges unusually rapidly with bulk water and is thus a likely candidate for one of the substrates. Ammonia, a water analog, was previously shown to bind to the Mn4O5Ca cluster, potentially displacing a water/substrate ligand [Britt RD, et al. (1989) J Am Chem Soc 111(10):3522-3532]. Here we show by a combination of EPR and time-resolved membrane inlet mass spectrometry that the binding of ammonia perturbs the exchangeable μ-oxo bridge without drastically altering the binding/exchange kinetics of the two substrates. In combination with broken-symmetry density functional theory, our results show that (i) the exchangable μ-oxo bridge is O5 {using the labeling of the current crystal structure [Umena Y, et al. (2011) Nature 473(7345):55-60]}; (ii) ammonia displaces a water ligand to the outer manganese (MnA4-W1); and (iii) as W1 is trans to O5, ammonia binding elongates the MnA4-O5 bond, leading to the perturbation of the μ-oxo bridge resonance and to a small change in the water exchange rates. These experimental results support O-O bond formation between O5 and possibly an oxyl radical as proposed by Siegbahn and exclude W1 as the second substrate water.

摘要

两个底物水位点在光合作用 II 系统的四锰五氧钙(Mn4O5Ca)簇中的分配对于阐明生物 O-O 键形成的机制以及随后设计生物启发的水分解催化剂至关重要。我们最近使用脉冲 EPR 光谱证明,五个氧桥之一(μ-氧)与体相水交换异常迅速,因此可能是其中一个底物的候选者。氨,一种水类似物,以前被证明可以与 Mn4O5Ca 簇结合,可能取代一个水/底物配体[Britt RD 等人,(1989)J Am Chem Soc 111(10):3522-3532]。在这里,我们通过 EPR 和时间分辨膜入口质谱的组合表明,氨的结合会扰乱可交换的μ-氧桥,而不会剧烈改变两个底物的结合/交换动力学。结合broken-symmetry 密度泛函理论,我们的结果表明:(i)可交换的μ-氧桥是 O5{使用当前晶体结构的标记[Umena Y 等人,(2011)自然 473(7345):55-60]};(ii)氨取代外锰(MnA4-W1)上的一个水配体;(iii)由于 W1 与 O5 反式,氨的结合会拉长 MnA4-O5 键,导致μ-氧桥共振的扰动和水交换速率的微小变化。这些实验结果支持 Siegbahn 提出的 O5 与可能的氧自由基之间的 O-O 键形成,并排除 W1 作为第二个底物水。

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