EXPLORATION OF THE STRUCTURAL ENVIRONMENT OF THE IRON-SULFUR CLUSTER IN PUTIDAREDOXIN BY N-15 NMR-SPECTROSCOPY OF SELECTIVELY LABELED CYSTEINE RESIDUES
N. Sari et al., EXPLORATION OF THE STRUCTURAL ENVIRONMENT OF THE IRON-SULFUR CLUSTER IN PUTIDAREDOXIN BY N-15 NMR-SPECTROSCOPY OF SELECTIVELY LABELED CYSTEINE RESIDUES, Biochemical and biophysical research communications (Print), 249(3), 1998, pp. 773-780
Putidaredoxin is a di-iron protein whose paramagnetic region is not we
ll characterized by H-1 detected NMR. We have studied the structure of
this region in greater detail by directly observed N-15 NMR of oxidiz
ed and reduced putidaredoxin preparations in which the six cysteine re
sidues are selectively labeled with N-15. A new method for preparation
of a stable form of reduced putidaredoxin has been developed for use
in NMR. The N-15 NMR spectra of the oxidized and reduced forms are cha
racteristically different, and we have measured and compared N-15 chem
ical shifts, spin-lattice relaxation times (T-1), and chemical shift/t
emperature dependences for both forms. Evidence for localized valencie
s of the iron atoms in the reduced form is presented. From the N-15 T-
1 values of the oxidized form, reduced distances of the cysteine backb
one N-15 nuclei from the center of the Fe2S2 cluster have been calcula
ted. These distances are consistent with those calculated from X-ray c
rystal structure data for five ferredoxins, and confirm the structural
similarity of the Fe2S2 clusters in putidaredoxin and in these ferred
oxins in the oxidized state. (C) 1998 Academic Press.