The quaternary structure of bovine alpha-crystallin. Effects of variation in alkaline pH, ionic strength, temperature and calcium ion concentration

Abstract

The stability of the native quaternary structure of bovine alpha-crystallin was studied, by sedimentation analysis and electron microscopy, as a function of pH (7--11), ionic strength (0.01--0.5), temperature (6--60 degrees C) and calcium ion concentration (0 and 10 mM). Three successive transitions are distinguished at 20 degrees C. Firstly, a slow transconformation step, which is independent of pH, ionic strength or calcium ions. Secondly, an irreversible primary dissociation step, favoured by increasing pH above 8 and/or a lower ionic strength, with formation of 'alkali-modified alpha-crystallin', which is spherically shaped like the native protein but has a smaller average diameter, sedimentation coefficient and molecular weight. Thirdly, with further increase of pH above 9, a rapidly reversible dissociation of alkali-modified alpha-crystallin characterized by a single reaction boundary in sedimentation velocity analysis. In the presence of calcium ions the quaternary structure is stabilized to the extent that no dissociation is observed up to at least pH 10.3. Upon increase of temperature, at pH 7.3, a slow irreversible dissociation and swelling run parallel until a limit is reached around 37 degrees C with formation of 'temperature-modified alpha-crystallin', which is indistinguishable from the native protein by electron microscopy, but has a higher relative viscosity and lower sedimentation coefficient and molecular weight. Calcium ions have little or no effect on this transition. Above 37 degrees C a reversal of this transition or aggregation is indicated. These findings, together with previous structural data on microheterogeneity, reassociation from urea, and aging of alpha-crystallin in vivo, are incorporated into a hypothetical scheme of transitions, based on a three-layer model for the quaternary structure.