Interaction of histone f2al fragments with deoxyribonucleic acid. Circular dichroism and thermal denaturation studies.

The glycine-arginine-rich histone, f2al (IV) (102 amino acids), from calf thymus was cleaved at residue 84 with cyanogen bromide. Complexes containing homologous DNA and each f2al fragment were reconstituted by means of Gdn-HC1 gradient dialysis. The circular dichroic (CD) spectra of these complexes were all examined in 0.14 M NaC1. The CD spectra of the DNA-f2al fragment complexes did not differ appreciably from that of DNA alone in the wavelength region above 240 nm. However, intact f2al-DNA complexes yield CD spectra which differ significantly (enhanced, blue-shifted, 273-nm band) from that of native DNA (Shih and Fasman, 1971). The small C-terminal fragment (85-102) was bound weakly to DNA under the conditions used. However, the large basic N-terminal fragment (1-83) was bound as well to DNA as was whole f2al, but produced no CD distortion. The conformation of the N-terminal fragment, unlike intact f2al, was not changed upon increasing the ionic strength to 0.14 M NaF. These results complement previous studies on f2al and its N-terminal CNBr fragment (Ziccardi and Schumaker, 1973). Thermal denaturation of the complexes in 2.5 X 10(-4) M EDTA was monitored simultaneously by changes in the absorption and CD spectra. All complexes showed a thermal transition at 45 degrees (Tml), attributable to the melting of free, double-stranded DNA. In addition, f2al-DNA and N fragment-DNA complexes displayed melting phenomena at 88 and 78 degrees (Tm2), respectively, caused by the denaturation of the histone-bound DNA. This difference in Tm2 constitutes further evidence that loss of the 18-amino-acid carboxyl end segment of f2al prohibits the unique type of interaction which occurs between DNA and the intact histone.