H. Zhang et al., CONFORMATIONAL TRANSITIONS IN PEPTIDES CONTAINING 2 PUTATIVE ALPHA-HELICES OF THE PRION PROTEIN, Journal of Molecular Biology, 250(4), 1995, pp. 514-526
Prions are composed largely, if not entirely, of the scrapie isoform o
f the prion protein (PrP5c). Conversion of the cellular isoform (PrPC)
to PrPSc is accompanied by a diminution in the alpha-helical content
and an increase in the beta-sheet structure. To investigate the struct
ural basis of this transition, peptide fragments corresponding to Syri
an hamster PrP residues 90 to 145 and 109 to 141, which contain the mo
st conserved residues of the prion protein and the first two putative
alpha-helical regions in a PrPC model, were studied using infrared spe
ctroscopy and circular dichroism. The peptides could be induced to for
m alpha-helical structures in aqueous solutions in the presence of org
anic solvents, such as trifluoroethanol and hexafluoroisopropanol, or
detergents, such as sodium dodecyl sulfate and dodecyl phosphocholine.
NaCl at physiological concentration or acetonitrile induced the pepti
des to acquire substantial beta-sheet. The intermolecular nature of th
e beta-sheet was evident in the formation of rod-shaped polymers as de
tected by electron microscopy. Resistance to hydrolysis by proteinase
K and epitope mapping argue that the beta-sheet structures were formed
by the interaction of residues lying between 109 and 141. A similar r
ange of residues was shown by nuclear magnetic resonance spectroscopy
to be capable of forming alpha-helices. The alpha-helical structures s
eem to require a hydrophobic support from either intermolecular intera
ctions or the hydrophobic environment provided by micelles, in agreeme
nt with the predicted hydrophobic nature of the packing surface among
the four putative helices of PrPC and the outer surfaces of the first
two helices. Our results suggest that perturbation of the packing envi
ronment of the highly conserved residues is a possible mechanism for t
riggering the conversion of PrPC to PrPSc where alpha-helices appear t
o be converted into beta-sheets.