A new binding site for anions which inhibit the water oxidizing comple
x (WOC) of Photosystem II in spinach has been identified. Anions which
bind to this site inhibit the flash-induced S-2/S-0 catalase reaction
(2H(2)O(2) --> 2H(2)O + O-2) of the WOC by displacing hydrogen peroxi
de. Using a mass spectrometer and gas permeable membrane to detect the
O-32(2) product, the yield and lifetime of the active state of the fl
ash-induced catalase (to be referred to simply as 'flash-catalase') re
action were measured after forming the S-2 or S-0-states by a short fl
ash. The increase in flash-catalase activity with H2O2 concentration e
xhibits a K-m = 10-20 mM, and originates from an increase in the lifet
ime by 20-fold of the active state. The increased lifetime in the pres
ence of peroxide is ascribed to formation of the long-lived S-0-state
at the expense of the unstable S-2-state. The anion inhibition site di
ffers from the chloride site involved in stimulating the photolytic wa
ter oxidation reaction (2H(2)O --> O-2 + 4e(-) + 4H(+)). Whereas water
oxidation requires Cl- and is inhibited with increasing effectiveness
by F- << CN- << N-3(-), the flash-catalase reaction is weakly inhibit
ed by Cl-, and with increasing effectiveness by F- << CN-, N-3(-). Unl
ike water oxidation, chloride is unable to suppress or reverse inhibit
ion of the flash-catalase reaction caused by these anions. The inhibit
or effectiveness correlates with the pK(a) of the conjugate acid, sugg
esting that the protonated species may be the active inhibitor. The re
duced activity arises from a shortening of the lifetime of the flash-i
nduced catalase active state by 3-10 fold owing to stronger anion bind
ing in the flash-induced states, S-2 and S-0, than in the dark S-state
s, S-1 and S--1. To account for the paradoxical result that higher ani
on concentrations are required to inhibit at lower H2O2 concentrations
, where S-2 forms initially after the flash, than at higher H2O2 conce
ntrations, where S-0 forms initially after the flash, stronger anion b
inding to the S-0-state than to the S-2-state is proposed. A kinetic m
odel is given which accounts for these equilibria with anions and H2O2
. The rate constant for the formation/release of O-2 by reduction of S
-2 in the WOC is < 0.4 s(-1).