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