EXTENT AND RATE OF PROTON RELEASE BY PHOTOSYNTHETIC WATER OXIDATION IN THYLAKOIDS - ELECTROSTATIC RELAXATION VERSUS CHEMICAL PRODUCTION

Authors
Citation
M. Haumann et W. Junge, EXTENT AND RATE OF PROTON RELEASE BY PHOTOSYNTHETIC WATER OXIDATION IN THYLAKOIDS - ELECTROSTATIC RELAXATION VERSUS CHEMICAL PRODUCTION, Biochemistry, 33(4), 1994, pp. 864-872
Citations number
60
Categorie Soggetti
Biology
Journal title
ISSN journal
00062960
Volume
33
Issue
4
Year of publication
1994
Pages
864 - 872
Database
ISI
SICI code
0006-2960(1994)33:4<864:EAROPR>2.0.ZU;2-3
Abstract
The detailed chemical mechanism of the four steps of photosynthetic ox idation of two molecules of water to yield molecular oxygen plus four protons is under contention. The observed release of protons is a comp osite of the chemical production and more indirect reactions such as e lectrostatically induced shifts of acid/base equilibria of peripheral amino acids. In thylakoids we studied the extent and the rate (at micr osecond time resolution) of proton release and uptake by each of the f our oxidation steps. The pattern of net proton release in thylakoids v aried drastically (between 0.3 and 2 H+/e-) as a function of pH. It di ffered substantially from the pH-dependent patterns of PSII-enriched m embrane fragments and core particles, but the stepped progression towa rd release of dioxygen (the Kok parameter triple) was about the same. This implied an electrostatic origin of this variation and, with in th e observed limits, a lack of (inhibitory) feedback of the uncompensate d charge on the electrontransfer from the catalytic Mn cluster to Tyr( z)+. The rate of rapid proton transfer to the amphiphilic, surface-ads orbed indicator neutral red was proportional to its concentration. The shortest half-transfer time was 12 mus, substantially shorter than th e time for electron transfer from Mn to Tyr(z)+ at any oxidation step. Rapid deprotonation thus occurred at the level of Tyr(z)+. By rapid d eprotonation acts the four light-driven oxidation steps S0 double-line arrow pointing right S1 double-line arrow pointing right S2 double-li ne arrow pointing right S3 double-line arrow pointing right S4 created between 3.4 (at pH 7.4) and 4.5 (pH 6.3) bases per photosystem II. On the last step there was a compensating slow release of 0.6 proton (pH 7.4) and slow uptake of 0.5 proton (pH 6.3) in milliseconds, respecti vely. The slow event was attributed to the oxygen-evolving step, S4 -- > S0. Our results are in favor of a concerted electron-proton transfer mechanism from water to a manganese-base cluster and are also in favo r of one reaction step with water (S4 --> S0) as opposed to two two-el ectron reactions with a peroxide intermediate formed upon S1 double-li ne arrow pointing right S2.