Role of D1-His190 in the proton-coupled oxidation of tyrosine Y-Z in manganese-depleted photosystem II

Citation
Ama. Hays et al., Role of D1-His190 in the proton-coupled oxidation of tyrosine Y-Z in manganese-depleted photosystem II, BIOCHEM, 38(37), 1999, pp. 11851-11865
Citations number
147
Categorie Soggetti
Biochemistry & Biophysics
Journal title
BIOCHEMISTRY
ISSN journal
00062960 → ACNP
Volume
38
Issue
37
Year of publication
1999
Pages
11851 - 11865
Database
ISI
SICI code
0006-2960(19990914)38:37<11851:RODITP>2.0.ZU;2-Q
Abstract
TO further characterize the role of D1-His190 in the oxidation of tyrosine Y-Z in photosystem II, the pH dependence of P-680(.+) reduction was measure d in H190A and Mn-depleted wild-type* PSII particles isolated from the cyan obacterium, Synechocystis sp. PCC 6803. Measurements were conducted in the presence and absence of imidazole and other small organic bases. In H190A P SII particles, rapid reduction of P-680(.+) attributed to electron transfer from Y-Z increased dramatically above pH 9, with an apparent pK(A) of simi lar to 10.3. In the presence of ethanolamine and imidazole, this dramatic i ncrease occurred at lower pH values, with the efficiency of YZ oxidation co rrelating with the solution pK(A) value of the added base. We conclude that the pK(A) of Y-Z is similar to 10.3 in D1-H190A PSII particles. In Mn-depl eted wild type* PSII particles, P-680(.+) reduction was accelerated by all exogenous bases examined (substituted imidazoles, histidine, Tris, and 1,4- diazabicyclo[2.2.2] octane). We conclude that Y-Z is solvent accessible in Mn-depleted wild-type* PSII particles and that its pK(A) is near that of ty rosine in solution. In Mn-depleted wild-type* PSII particles, over 80% of t he kinetics of P680.+ reduction after a flash could be described by three k inetic components. The individual rate constants of these components varied slightly with pH, but their relative proportions varied dramatically with pH, showing apparent pK(A) values of 7.5 and 6.25 (6.9 and 5.8 in the prese nce of Ca2+ and Mg2+ ions). An additional pKA value (pK(A) < 4.5) may also be present. To describe these data, we propose (1) the pKA of His190 is 6.9 -7.5, depending on buffer ions, (2) the deprotonation of Y-Z is facilitated by the transient formation of a either a hydrogen bond or a hydrogen-bonde d water bridge between Y-Z and D1-His190, and (3) when protonated, D1-His19 0 interacts with nearby residues having pK(A) values near 6 and 4. Because Y-Z and D1-His190 are located near the Mn cluster, these residues may inter act with the Mn cluster in the intact system.