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Relative stability of the S2 isomers of the oxygen evolving complex of photosystem II.

Authors :
Kaur, Divya
Szejgis, Witold
Mao, Junjun
Amin, Muhamed
Reiss, Krystle M.
Askerka, Mikhail
Cai, Xiuhong
Khaniya, Umesh
Zhang, Yingying
Brudvig, Gary W.
Batista, Victor S.
Gunner, M. R.
Source :
Photosynthesis Research; Sep2019, Vol. 141 Issue 3, p331-341, 11p
Publication Year :
2019

Abstract

The oxidation of water to O<subscript>2</subscript> is catalyzed by the Oxygen Evolving Complex (OEC), a Mn<subscript>4</subscript>CaO<subscript>5</subscript> complex in Photosystem II (PSII). The OEC is sequentially oxidized from state S<subscript>0</subscript> to S<subscript>4</subscript>. The S<subscript>2</subscript> state, (Mn<superscript>III</superscript>)(Mn<superscript>IV</superscript>)<subscript>3</subscript>, coexists in two redox isomers: S<subscript>2,g=2</subscript>, where Mn4 is Mn<superscript>IV</superscript> and S<subscript>2,g=4.1</subscript>, where Mn1 is Mn<superscript>IV</superscript>. Mn4 has two terminal water ligands, whose proton affinity is affected by the Mn oxidation state. The relative energy of the two S<subscript>2</subscript> redox isomers and the protonation state of the terminal water ligands are analyzed using classical multi-conformer continuum electrostatics (MCCE). The Monte Carlo simulations are done on QM/MM optimized S<subscript>1</subscript> and S<subscript>2</subscript> structures docked back into the complete PSII, keeping the protonation state of the protein at equilibrium with the OEC redox and protonation states. Wild-type PSII, chloride-depleted PSII, PSII in the presence of oxidized Y<subscript>Z</subscript>/protonated D1-H190, and the PSII mutants D2-K317A, D1-D61A, and D1-S169A are studied at pH 6. The wild-type PSII at pH 8 is also described. In qualitative agreement with experiment, in wild-type PSII, the S<subscript>2,g=2</subscript> redox isomer is the lower energy state; while chloride depletion or pH 8 stabilizes the S<subscript>2,g=4.1</subscript> state and the mutants D2-K317A, D1-D61A, and D1-S169A favor the S<subscript>2,g=2</subscript> state. The protonation states of D1-E329, D1-E65, D1-H337, D1-D61, and the terminal waters on Mn4 (W1 and W2) are affected by the OEC oxidation state. The terminal W2 on Mn4 is a mixture of water and hydroxyl in the S<subscript>2,g=2</subscript> state, indicating the two water protonation states have similar energy, while it remains neutral in the S<subscript>1</subscript> and S<subscript>2,g=4.1</subscript> states. In wild-type PSII, advancement to S<subscript>2</subscript> leads to negligible proton loss and so there is an accumulation of positive charge. In the analyzed mutations and Cl<superscript>−</superscript> depleted PSII, additional deprotonation is found upon formation of S<subscript>2</subscript> state. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
01668595
Volume :
141
Issue :
3
Database :
Complementary Index
Journal :
Photosynthesis Research
Publication Type :
Academic Journal
Accession number :
138397337
Full Text :
https://doi.org/10.1007/s11120-019-00637-6