Renaturation of denatured, covalently closed circular DNA.

The rate of renaturation of denatured, covalently closed, circular DNA (form Id DNA) of the phi X174 replicative form has been investigated as a function of pH, temperature, and ionic strength. The rate at a constant temperature is a sharply peaked function of pH in the range of pH 9 to 12. The position on the pH scale of the maximum rate decreases as the temperature is increased and as the ionic strength is increased. The kinetic course of renaturation is pseudo-first order: it is independent of DNA concentration, but falls off in rate from a first order relationship as the reaction proceeds. The rate of renaturation depends critically on the temperature at which the denaturation is carried out. Form Id, prepared at an alkaline pH at 0 degrees C, renatures from 5 to more than 100 times more rapidly than that similarly prepared at 50 degrees C. Both the heterogeneity in rate and the effect of the temperature of denaturation depend, in part, on the degree of supercoiling of the form I DNA from which the form Id is prepared. However, it is concluded that a much larger contribution to both arises from a configurational heterogeneity introduced in the denaturation reaction. The renaturation rate was determined by neutralization of the alkaline reaction and analytical ultracentrifugal analysis of the amounts of forms I and Id. The nature of the proximate renatured species at the temperature and alkaline pH of renaturation was investigated by spectrophotometric titration and analytical ultracentrifugation. It is concluded that the proximate species are the same as the intermediate species defined by an alkaline sedimentation titration of the kind first done by Vinograd et al. ((1965) Proc. Natl. Acad. Sci. U. S. A. 53, 1104-1111). Observations are included on the buoyant density of form Id and on depurination of DNA at alkaline pH values and high temperatures.