Simultaneous interpretation of Mossbauer, EPR and Fe-57 ENDOR spectra of the [Fe4S4] cluster in the high-potential iron protein I from Ectothiorhodospira halophila
Awe. Dilg et al., Simultaneous interpretation of Mossbauer, EPR and Fe-57 ENDOR spectra of the [Fe4S4] cluster in the high-potential iron protein I from Ectothiorhodospira halophila, J BIOL I CH, 4(6), 1999, pp. 727-741
Mossbauer spectra of the oxidized [Fe4S4](3+) and the reduced Fe4S4](2+) cl
usters in the high-potential iron protein I from Ectothiorhodospira halophi
la were measured in a temperature range from 5 K to 240 K. EPR measurements
and Fe-57 electron-nuclear double resonance (ENDOR) experiments were carri
ed out with the oxidized protein. In the oxidized state the cluster has a n
et spin S=1/2 and is paramagnetic. As common in [Fe4S4](3+) clusters, the M
ossbauer spectrum was simulated with two species contributing equally to th
e absorption area: two Fe3+ atoms couple to the "ferric-ferric" pair, and o
ne Fe2+ and one Fe3+ atom give the "ferric-ferrous pair". For the simulatio
n of the Mossbauer spectrum, g-values were taken from EPR measurements. A-t
enser components were determined by Fe-57 ENDOR experiments that turned out
to be a necessary source of estimating parameters independently. In order
to obtain a detailed agreement of Mossbauer and ENDOR data, electronic rela
xation has to be taken into account. Relaxing the symmetry condition in a w
ay that the electric field gradient tensor does not coincide with g- and A-
tensors yielded an even better agreement of experimental and theoretical Mo
ssbauer spectra. Spin-spin and spin-lattice relaxation times were estimated
by pulsed EPR; the former turned out to be the dominating mechanism at T=5
K, Relaxation times measured by pulsed EPR and obtained from the Mossbauer
fit were compared and yield nearly identical values. The reduced cluster h
as one additional electron and has a diamagnetic (S=0) ground state. All th
e four irons are indistinguishable in the Mossbauer spectrum, indicating a
mixed-valence state of Fe2.5+ for each.