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Biophys J, July 2000, p. 501-510, Vol. 79, No. 1
Department of Chemical Sciences, Tata Institute of Fundamental Research, Mumbai 400 005, India
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
-sheeted protein is stable in salt concentrations of
1.5 M NaCl.
At lower concentrations a time-dependent increase in fluorescence
intensity ratio
(I360:I330), 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.
Biophys J, July 2000, p. 501-510, Vol. 79, No. 1
© 2000 by the Biophysical Society 0006-3495/00/07/501/10 $2.00
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