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Molecular Identification of a High-Spin Deprotonated Intermediate during the S2 to S3 Transition of Nature’s Water-Oxidizing Complex
Author(s) -
Thomas A. Corry,
Patrick J. O’Malley
Publication year - 2020
Publication title -
journal of the american chemical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 7.115
H-Index - 612
eISSN - 1520-5126
pISSN - 0002-7863
DOI - 10.1021/jacs.0c01351
Subject(s) - chemistry , deprotonation , electron paramagnetic resonance , cubane , ligand (biochemistry) , density functional theory , crystallography , spin (aerodynamics) , computational chemistry , nuclear magnetic resonance , crystal structure , ion , biochemistry , physics , organic chemistry , receptor , engineering , aerospace engineering
The identity of a key intermediate in the S 2 o S 3 ransition of nature's water-oxidizing complex (WOC) in Photosystem 2 is presented. Broken-symmetry density functional theory (BS-DFT) calculations and Heisenberg-Dirac-van Vleck (HDvV) spin ladder calculations show that an S 2 state open cubane model of the WOC containing a μ-hydroxo O4 changes from an S = 5 / 2 form to an S = 7 / 2 , form upon deprotonation of W1. Combined with X-band electron paramagnetic resonance (EPR) spectral analysis, this indicates that the g = 4.1 EPR signal corresponds to an S = 5 / 2 form of the WOC with W1 present as a water ligand to Mn 4 , while the g = 4.8/4.9 form observed at high pH values corresponds to an S = 7 / 2 form, with W1 as a hydroxo ligand. The latter is also likely to represent the form needed to progress to S 3 in the functioning enzyme.

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