PhnZ
utilizes a mixed valence diiron(II/III) cofactor and O2 to oxidatively cleave the carbon–phosphorus bond of
(R)-2-amino-1-hydroxyethylphosphonic acid to form
glycine and orthophosphate. The active site residues Y24 and E27 are
proposed to mediate induced-fit recognition of the substrate and access
of O2 to one of the active site Fe ions. H62 is proposed
to deprotonate the C1-hydroxyl of the substrate during catalysis.
Kinetic isotope effects (KIEs), pH–rate dependence, and site-directed
mutagenesis were used to probe the rate-determining transition state
and the roles of these three active site residues. Primary deuterium
KIE values of 5.5 ± 0.3 for D(V)
and 2.2 ± 0.4 for D(V/K) were measured
with (R)-2-amino[1-2H1]-1-hydroxyethylphosphonic
acid, indicating that cleavage of the C1–H bond of the substrate
is rate-limiting. This step is also rate-limiting for PhnZ Y24F, as
shown by a significant deuterium KIE value of 2.3 ± 0.1 for D(V). In contrast, a different reaction step
appears to be rate-limiting for the PhnZ E27A and H62A variants, which
exhibited D(V) values near unity. A solvent
KIE of 2.2 ± 0.3 for D2O(V) is observed for PhnZ. Significant solvent KIE values are also observed
for the PhnZ Y24F and E27A variants. In contrast, the PhnZ H62A variant
does not show a significant solvent KIE, suggesting that H62 is mediating
proton transfer in the transition state. A proton inventory study
with PhnZ indicates that 1.5 ± 0.6 protons are in flight in the
rate-determining step. Overall, the rate-determining transition state
for oxidative C–P bond cleavage by PhnZ is proposed to involve
C–H bond cleavage that is coupled to deprotonation of the substrate
C1-hydroxyl by H62