C. Tommos et al., STEPWISE DISINTEGRATION OF THE PHOTOSYNTHETIC OXYGEN-EVOLVING COMPLEX, Journal of the American Chemical Society, 120(40), 1998, pp. 10441-10452
Photosynthetic water oxidation catalyzed by Photosystem II takes place
at a site that comprises a redox-active tyrosine, Y-z, a tetramangane
se cluster, and, in addition to its redox components, two inorganic co
factors, calcium and chloride. Recent work suggests that Y-z and the m
etal site are intimately linked in the oxidation and deprotonation rea
ctions of substrate water. The metal cluster stores oxidizing equivale
nts and provides binding sites for the substrate from which Y-z(.) is
proposed to abstract hydrogen atoms during the catalytic cycle of phot
osystem II. Intrinsic to this hydrogen-abstraction mechanism for water
oxidation is an intimate structural and functional relationship betwe
en the metal site and Y-z, which predicts that the local Y-z environme
nt will be sensitive to the composition and integrity of the metal clu
ster. To test this postulate, we have examined the Y-z site and its st
atus with respect to solvent exposure under varying degrees of disasse
mbly of the oxygen-evolving complex. H-1/H-2-isotope exchange was carr
ied out for various times in samples devoid of Mn, Ca2+, and Cl-, and
in samples depleted exclusively of Ca2+. The Y-z(.) andS(2)Y(z)(.) spe
cies were cryotrapped to high yield in these two preparations, respect
ively, and the radical site was characterized by using electron spin-e
cho envelope modulation spectroscopy. The isotope exchange at the Yz s
ite was completed with an upper limit on the minutes time scale in bot
h the (Mn)(4)-depleted and the Ca-depleted samples. The number of isot
ope-exchangeable protons in the site and their distances to Yi were fo
und to be different in the two systems, indicating that Yz is shielded
from the solvent in the Ca-depleted system and, upon removal of the (
Mn)(4) cluster, becomes accessible to bulk water. The results from an
electron spin-echo analysis of S2Yz., in the weak-coupling limit, sugg
est that Y-z(.) in samples that retain the (Mn)(4) cluster, but lack C
a2+, is involved in a bifurcated hydrogen bond. The data for both clas
ses of samples are consistent with a hydrogen-abstraction function for
Y-z in water oxidation and provide insight into the light-driven asse
mbly of the (Mn)4 cluster.