MECHANISM OF ASSEMBLY OF THE TYROSYL RADICAL-DIIRON(III) COFACTOR OF ESCHERICHIA-COLI RIBONUCLEOTIDE REDUCTASE .1. MOSSBAUER CHARACTERIZATION OF THE DIFERRIC RADICAL PRECURSOR
N. Ravi et al., MECHANISM OF ASSEMBLY OF THE TYROSYL RADICAL-DIIRON(III) COFACTOR OF ESCHERICHIA-COLI RIBONUCLEOTIDE REDUCTASE .1. MOSSBAUER CHARACTERIZATION OF THE DIFERRIC RADICAL PRECURSOR, Journal of the American Chemical Society, 116(18), 1994, pp. 8007-8014
The R2 subunit of Escherichia coli ribonucleotide reductase (RNR) cont
ains a cofactor which consists of a stable tyrosyl radical (Y122) adj
acent to a mu-oxo-bridged diiron(III) cluster. This cofactor assembles
spontaneously when apo R2 is treated with Fe2+ and O-2. By using rapi
d kinetic techniques, two kinetically competent intermediates in this
assembly process were recently identified (Bollinger, J. M., Jr. et al
. Science 1991, 253, 292-298). One of the intermediates is a paramagne
tic iron species. By using the rapid freeze-quench technique and a mut
ant R2 subunit in which Y122 is replaced with F, 1 equiv of this inter
mediate per R2 subunit can be trapped. Previous electron paramagnetic
resonance (EPR) and Mossbauer studies suggested that this species isa
spin coupled system involving two high-spin ferric ions and a free rad
ical (a ''diferric radical species'') (Bollinger, J. M., Jr. et al. J.
Am. Chem. Sec. 1991, 113, 6289-6291). In the present study, Mossbauer
spectra have been recorded over a wide range of applied fields (60 mT
-8 T), and detailed analysis of the Mossbauer data consolidates the in
itial finding. The observed isomer shifts (0.55 mm/s for iron site 1 a
nd 0.36 mm/s for site 2) and quadrupole splittings (similar to 1 mm/s)
are typical for high-spin ferric species. The magnetic hyperfine coup
ling tensors, A, for the two iron sites are relatively isotropic (with
in 20%), a feature which is unique to high-spin Fe(III). By using a si
mple three-spin coupling model (S-1 = 5/2 and S-2 = 5/2 for the two ir
on sites, and S-3 = 1/2 for the radical), both the signs and magnitude
s of the observed A values for the iron sites (A(1)/g(m) beta(n) = -52
.5 T and A(2)/g(m) beta(n) = +24 T) can be explained with an intrinsic
A value that is consistent with high-spin Fe(III). The asymmetry in t
he A values for the two iron sites is a result of the spin orientation
s: the Spin of the radical is parallel to that of the negative-A-value
Fe site and antiparallel to that of the positive-A-value Fe site. Sin
ce it has been suggested on the basis of functional analogy with heme-
iron-dependent peroxidases that generation of Y122 in RNR-R2 may invo
lve a high-valent iron-oxo intermediate, the possibility that this par
amagnetic iron species contains Fe(IV) has also been carefully examine
d. Both the EPR and the Mossb;auer data are incompatible with such a p
ossibility.