The oxidized Fe,S, ferredoxin from the hyperthermophilic bacterium Thermotoga maritima has been investigated by one-and two-dimensional NMR in order to characterize its hyperfine-shifted resonances originating from the cysteinyl cluster ligands and to assign its resonances in the diamagnetic shift range. The chemical shift and relaxation time pattern of the hyperfine-shifted signals is very similar to other oxidized Fe,S, ferredoxins. A tentative sequence-specific assignment of these resonances according to a general pattern of chemical shift of cysteine protons versus sequence position of cluster ligand is presented. Furthermore, sequence-specific assignments for 85 Yo of the amino acid residues that were obtained without any guidance by known X-ray structures of ferredoxins are given. They reveal the formation of at least two elements of secondary structure by the polypeptide chain of 7: maritima ferredoxin:an a-helix comprising residues C43-D49 and a double-stranded antiparallel p-sheet consisting of the N- Keywords. Ferredoxin ; hyperthermophilic ; NMR ; secondary structure ; Thermotoga maritima. Thermotoga maritima is a hyperthermophilic microorganism (Stetter et al., 1990) with an optimal growth temperature of 80°C. It was isolated from geothermally heated marine sediments where it lives as a strictly anaerobic heterotroph by the fermentation of carbohydrates (Huber et al., 1986). As an exception of the rule that hyperthermophiles belong to the phylogenetic domain of the Archaea, 7: maritima is a bacterium (Woese et al., 1990). Based on their 16s rRNA sequences, 7: maritima and the recently discovered Aquifex pyrophilus (Huber et al., 1992) represent the most ancient and most slowly evolving branches of the bacterial phylogenetic tree. They are supposed to be more similar to the common ancestor of life than any other known organism (Achenbach-Richter et al., 1987 ;Burggraf et al., 1992). Thus, proteins from 7: maritima are of considerable interest from an evolutionary point of view and with regard to their thermostability.Ferredoxins are ubiquitous iron-sulfur proteins that participate in important biological electron-transfer reactions, e.g. in the respiratory chain, in photosynthesis and in nitrogen fixation [see Matsubara and Saeki (1992) and Beinert (1990) of Florence, Via Gino Capponi, 7, 1-50121 Florence, Italy reviews]. The prosthetic groups that render redox activity to these proteins are Fe-S clusters of the Fe,S, type (mostly in plants and animals) or of the Fe,S, (Fe,S,) type (mostly in prokaryotes). Their redox potential is strongly dependent on the protein environment of the cluster (Backes et al., 1991 ;Langen et al., 1992;Jensen et al., 1994). According to the chemo-autotrophic theory for the origin of life in which pyrite formation provides the energy for the first autocatalytic reproduction cycle (Wachtershauser, 1992), small iron-sulfur proteins such as ferredoxins may be remnants of a pyrite surface metabolism during the first steps of biological evolution.The 60-residue ferredoxin (Fd...