Ci. Deluca et al., THE EFFECTS OF STERIC MUTATIONS ON THE STRUCTURE OF TYPE-III ANTIFREEZE PROTEIN AND ITS INTERACTION WITH ICE, Journal of Molecular Biology, 275(3), 1998, pp. 515-525
The interaction of proteins with ice is poorly understood and difficul
t to study, partly because ice is transitory and can present many bind
ing surfaces, and partly because structures have been determined for o
nly two ice-binding proteins. This paper focuses on one of these, a 66
-residue antifreeze protein (AFP) from eel pout. The high resolution X
-ray structure of this fish AFP demonstrated that the proposed ice-bin
ding surface is remarkably flat for such a small protein. The residues
on the planar surface thought to be involved in ice binding are restr
ained by hydrogen bonds or by tight packing of their side-chains. To p
robe the requirement for a flat binding surface, a conserved alanine i
n the center of the AFP planar surface was substituted with larger res
idues. Six alanine replacement mutants (Ala16 > Cys, Thr, Met, Arg, Hi
s and Tyr), designed to disrupt the planarity of the surface and steri
cally block binding to ice, were characterized by X-ray crystallograph
y and compared with the wild-type AFP. In each case, the detail provid
ed by these crystal structures has helped explain the effects of the m
utation on antifreeze activity. The substitutions, Ala16 > His and Ala
16 > Tyr, were large enough to shield Gln44, one of the putative ice-b
inding residues, contributing to their very low thermal hysteresis act
ivity. In addition to sterically hindering the putative ice-binding si
te, the bulkier residues also caused shifts in the putative ice-bindin
g residues owing to the tight packing of side-chains on the planar sur
face. This unexpected consequence of the mutations helps account for t
he severely reduced antifreeze activity. One explanation for residual
antifreeze activity in some of the mutants lies in the possibility tha
t AFPs have a role in shaping the site on the ice to which they bind.
Thus, side-chain dislocations might be partially accommodated by ice t
hat can freeze around them. It is evident that the disruption of the p
lanarity, by introducing larger residues at the center of the proposed
ice-binding site, is not the only factor responsible for the loss of
antifreeze activity. There are multiple causes including positional ch
ange and steric blockage of some putative ice-binding residues. (C) 19
98 Academic Press Limited.