H. Sticht et al., AN NMR-DERIVED MODEL FOR THE SOLUTION STRUCTURE OF OXIDIZED THERMOTOGA-MARITIMA 1[FE-4-S-4] FERREDOXIN, European journal of biochemistry, 237(3), 1996, pp. 726-735
The solution structure of the 60-residue 1[Fe-4-S-4] ferredoxin from t
he hyperthermophilic bacterium Thermotoga maritima was determined base
d on 683 distance and 35 dihedral angle restraints that were obtained
from NMR data. In addition, data known from crystallographic studies o
f ferredoxins was used for modeling of the iron-sulfur cluster and its
environment. The protein shows a globular fold very similar to the fo
ld of the related 1[Fe-4-S-4] ferredoxins from Desulfovibrio gigas and
Desulfovibrio africanus, and elements of regular secondary structure
similar to those in other ferredoxins were found in the T. maritima pr
otein. In particular, the T. maritima protein displayed a beta-sheet s
tructure made up of strands located at the very NH2 and COOH termini o
f the protein, and an internal alpha-helix. The internal beta-sheet ob
served in the D. gigas and D. africanus ferredoxins could not be confi
rmed in T. maritima ferredoxin and is thus suggested to be only weakly
present or even absent in this protein. This result suggests that the
rmostability in ferredoxins is not necessarily correlated with the con
tent of stable elements of regular secondary structure.