Denaturation of covalently closed circular DNA. Kinetics, comparison of several DNAs, mechanism and ionic effects

The rates of the alkaline denaturation of the covalently closed, circular DNAs (form I) of the replicative forms (RF) of phages G4, phi X174, and fd, and of plasmid pBR322 and phage PM2 have been measured at 0 degrees C and some at higher temperatures. These rates are orders of magnitude slower than the denaturation of linear DNA because of the increased stability of the helix to deprotonation that results from the accumulating positive superhelicity during denaturation. Denaturation reactions were initiated by rapid, infrasonic mixing (Camien, M.N., and Warner, R.C. (1984) Anal. Biochem. 138, 329-334), and their progress was measured by analytical ultracentrifugal analysis for the amounts of form I and denatured (Id) DNA after neutralization of the alkaline reaction. The comparative rates of the five DNAs varied over a wide range; the fastest, G4-RF, denatured at 500-fold the rate of the slowest, fd-RF. The differences are accounted for by the interaction of positive superhelicity with the sequence-dependent regions of relative helix stability in the various DNAs. Renaturation rates of Id DNAs varied similarly for Ids prepared at 0 degrees C, but only a few-fold for Ids prepared at 50 degrees C. The rate of denaturation of G4-RF was determined over a wide range of NaOH and NaCl concentrations at 0 degrees C, and the pHm was determined as a function of ionic strength and temperature. The effects of ionic strength have been analyzed in an application of the Manning ion condensation-screening theory (Manning, G.S. (1978) Q. Rev. Biophys. 11, 179-246) which is shown to account for the large destablizing effect of salts on the helix. The pH region of transition at 50 degrees C from renaturation to denaturation was examined, and it was found that the maximum rate of renaturation occurred at a pH about 0.05 units below the pHm.