Chlorite dismutases (Clds) are heme b-containing
prokaryotic oxidoreductases that catalyze the reduction of chlorite
to chloride with the concomitant release of molecular oxygen. Over
time, they are irreversibly inactivated. To elucidate the mechanism
of inactivation and investigate the role of the postulated intermediate
hypochlorite, the pentameric chlorite dismutase of “Candidatus Nitrospira defluvii” (NdCld) and
two variants (having the conserved distal arginine 173 exchanged with
alanine and lysine) were recombinantly produced in Escherichia
coli. Exchange of the distal arginine boosts the extent of
irreversible inactivation. In the presence of the hypochlorite traps
methionine, monochlorodimedone, and 2-[6-(4-aminophenoxy)-3-oxo-3H-xanthen-9-yl]benzoic acid, the extent of chlorite degradation
and release of molecular oxygen is significantly increased, whereas
heme bleaching and oxidative modifications of the protein are suppressed.
Among other modifications, hypochlorite-mediated formation of chlorinated
tyrosines is demonstrated by mass spectrometry. The data obtained
were analyzed with respect to the proposed reaction mechanism for
chlorite degradation and its dependence on pH. We discuss the role
of distal Arg173 by keeping hypochlorite in the reaction sphere for
O–O bond formation.