D1-Asp170 is structurally coupled to the oxygen evolving complex in photosystem II as revealed by light-induced Fourier transform infrared differencespectroscopy
Ha. Chu et al., D1-Asp170 is structurally coupled to the oxygen evolving complex in photosystem II as revealed by light-induced Fourier transform infrared differencespectroscopy, BIOCHEM, 40(7), 2001, pp. 2312-2316
We report both mid-frequency (1800-1200 cm(-1)) and low-frequency (670-350
cm(-1)) S-2/S-1 FTIR difference spectra of photosystem II (PSII) particles
isolated from wild-type* and D1-D170H mutant cells of the cyanobacterium Sy
nechocystis sp. PCC 6803. Both mid- and low-frequency S-2/S-1 spectra of th
e Synechocystis wild-type* PSII particles closely resemble those from spina
ch PSII samples, which confirms an earlier result by Noguchi and co-workers
[Noguchi, T., Inoue, Y., and Tang, X.-S. (1997) Biochemistry 36, 14705-147
11] and indicates that the coordination environment of the oxygen evolving
complex (OEC) in Synechocystis is very similar to that in spinach. We also
found that there is no appreciable difference between the mid-frequency S-2
/S-1 spectra of wild-type* and of D1-D170H mutant PSII particles, from whic
h we conclude that D1-Asp170 does not undergo a significant structural chan
ge during the S-1 to S-2 transition. This result also suggests that, if D1-
Asp170 ligates Mn, it does not ligate the Mn ion that is oxidized during th
e S-1 to S-2 State transition. Finally, we found that a mode at 606 cm(-1)
in the low-frequency wild-type* S-2/S-1 spectrum shifts to 612 cm(-1) in th
e D1-D170H mutant spectrum. Because this 606 cm(-1) mode has been previousl
y assigned to an Mn-O-Mn cluster mode of the OEC [Chu, H.-A., Sackett, H.,
and Babcock, G. T. (2000) Biochemistry 39, 14371-14376], we conclude that D
1-Asp170 is structurally coupled to the Mn-O-Mn cluster structure that give
s rise to this band. Our results suggest that D1-Asp170 either directly Lig
ates Mn or Ca2+ or participates in a hydrogen bond to the Mn4Ca2+ cluster.
Our results demonstrate that combining FTIR difference spectroscopy with si
te-directed mutagenesis has the potential to provide insights into structur
al changes in Mn and Ca2+ coordination environments in the different S stat
es of the OEC.