Abstract

Ferredoxin from the haloarchaeon Halobacterium salinarum is a 14.6-kDa protein with a [Fe2-S2] center and is involved in the oxidative decarboxylation of 2-oxoacids. It possesses a high molar excess of acidic amino acid residues and is stable at high salt concentration. We have purified the protein from this extreme haloarchaeon and investigated its salt-dependent stability by circular dichroism, fluorescence, and absorption techniques. The predominantly β-sheeted protein is stable in salt concentrations of ≥1.5 M NaCl. At lower concentrations a time-dependent increase in fluorescence intensity ratio ( I 360: I 330), a decrease in the absorption at 420 nm, and a decrease in ellipticity values are observed. The rate of fluorescence intensity change at any low salt concentration is the highest, followed by absorption and ellipticity. This suggests that at low salt the unfolding of ferredoxin starts with the loss of tertiary structure, which leads to the disruption of the [Fe2-S2] center, resulting in the loss of secondary structural elements.

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