Photosynthetic
water-splitting generates electrons, protons, and oxygen, which are the sources
for energy and oxygen indispensible for maintaining almost all life forms on
the earth. This reaction is catalyzed by photosystem II (PSII), a large
membrane-protein complex consisting of 20 subunits with a total molecular mass
of 350 kDa for a monomer. We have solved the crystal structure of dimeric PSII
from a thermophilic cyanobacterium
Thermosynechococcus
vulcanus at 1.9 Å resolution (Umena Y. et al. Nature
, 2011,
473, 55-60),
which revealed a clear picture of the catalytic center for photosynthetic
water-splitting, namely, a Mn
4CaO
5-cluster organized into
a distorted chair form. This feature of the distorted shape suggested a
remarkable flexibility in the structure, which would be needed for structural
changes expected to occur during the catalytic water-splitting cycle (S-state
cycle). Some of the inter-atomic distances within the metal cluster revealed by
the X-ray structural analysis, however, were shown to be slightly longer than
those obtained by previous EXAFS studies as well as theoretical studies. Among
these, the position of O5 has received particular attention, since it connects
Mn1 and Mn4 with bond distances unusually longer compared with typical Mn-O
bond distances. This unusual property implied that this oxo-bridge may
participate in the O-O bond formation during O
2 release. In order to
reveal the role of the Ca
2+ ion in the Mn
4CaO
5-cluster,
we replace it with Sr
2+ and solved the Sr
2+-substituted PSII
structure at 2.1 Å resolution (Koua HMK, et al. PNAS, 2013, 110, 3889-3894),
which had an oxygen-evolving activity half of native PSII. Based on the results
obtained, I will discuss the possible mechanism for photosynthetic water-splitting.