Abstract
The molten globule model for the beginning of the folding process, which originated with Kuwajima's studies of alpha-lactalbumin (Kuwajima, K., 1989, Proteins Struct. Funct. Genet. 6, 87-103, and references therein), states that, for those proteins that exhibit equilibrium molten globule intermediates, the molten globule is a major kinetic intermediate near the start of the folding pathway. Pulsed hydrogen-deuterium exchange measurements confirm this model for apomyoglobin (Jennings, P.A. & Wright, P.E., in prep.). The energetics of the acid-induced unfolding transition, which have been determined by fitting a minimal three-state model (N<-->I<-->U; N = native, I = molten globule intermediate, U = unfolded) show that I is more stable than U at neutral pH (Barrick, D. & Baldwin, R.L., 1993, Biochemistry 32, in press), which provides an explanation for why I is formed from U at the start of folding. Hydrogen exchange rates measured by two-dimensional NMR for individual peptide NH protons, taken together with the CD spectrum of I, indicate that moderately stable helices are present in I at the locations of the A, G, and H helices of native myoglobin (Hughson, F.M., Wright, P.E., & Baldwin, R.L., 1990, Science 249, 1544-1548). Directed mutagnesis experiments indicate that the interactions between the A, G, and H helices in I are loose (Hughson, F.M., Barrick, D., & Baldwin, R.L., 1991, Biochemistry 30, 4113-4118), which can explain why I is formed rapidly from U at the start of folding.(ABSTRACT TRUNCATED AT 250 WORDS)
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