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We have previously shown that biologically uncommon d-beta-aspartic acids (Asp) were localized with very high contents at Asp-151 and Asp-58 of alpha A-crystallin from aged human lenses. The amounts increased with age, and we have proposed the mechanism of this reaction. In the present study, in order to elucidate the possible relationship between the formation of d-beta-aspartic acids in alpha A-crystallin and cataract formation, we measured the d/l ratio of beta-Asp-151 of alpha A-crystallin from both cataractous and age-matched normal human lenses. alpha A-crystallin from total proteins of cataractous and age-matched normal lenses was prepared, followed by tryptic digestion and quantification of d/l ratios for tryptic fragments containing the alpha- and beta-aspartate forms of Asp-151 residues. The results demonstrate that the d/l ratio of beta-Asp-151 of alpha A-crystallin from normal lenses is not statistically significant from that of alpha A-crystallin from cataractous lenses, suggesting that formation of this biologically uncommon amino acid may not play a role in human cataractogenesis.

The hypothesis derived from models of the multi-oligomeric chaperone complex suggests that partially denatured proteins bind in a central cavity in the aggregate. To test this hypothesis, the molecular chaperone, alpha crystallin, was bound to partially denatured forms of gamma crystallin, and the binding site was visualized by immunogold localization. In an alternative approach, gold particles were directly complexed with gamma crystallin, followed by binding to the alpha crystallin aggregate. In both cases, binding was localized to the central region of the aggregate, confirming for the first time that partially denatured proteins do indeed bind to a central region of the molecular chaperone aggregate.