Physicochemical properties of salt-soluble, unsheared chromatin. Molecular weight studies

Viscosity of chromatin solutions increases with increasing ionic strength

Increasing the ionic strength of rat liver chromatin solutions above 0.4 M causes increasing viscosity. This indicates transformation of the compact chromatin molecules to more elongated forms. In the range of 0.4-0.5 M ionic strength histone H1 is dissociating continuously from the chromatin and the quaternary structure chromatin unravels. At ionic strength higher than 0.5 M the viscosities of chromatin solutions are furthermore increasing due to structural deformation. Near 0.7 M ionic strength the core histones H2A and H2B begin to dissociate from the chromatin, and the opening of the nucleosome cores leads to increasing elongation of the chromatin molecules.

Viscosity as an additional physico-chemical parameter for studying chromatin structure

The viscosity values of chromatin in higher order structures, which range from 0.1 to 0.4 dl/g, are considerably lower than those of isolated DNA. These low values are consistent with other physico-chemical parameters, such as sedimentation and diffusion coefficients. When deducing molecular mass and compact shape of chromatin molecules in solvents of nearly physiological ionic strength, all these parameters are in general agreement. A decrease in ionic strength increases viscosity and decreases s-value. Both effects are consistent with a chromatin model postulating a very compact quaternary structure which unravels in low ionic environment to an unfolded but not completely extended tertiary structure.

Interaction of histone H1 with superhelical DNA. Conformational studies and influence of ionic strength

The interaction of histone H1 with superhelical SV40 DNA at low ionic strength (approximately 0.02 M NaCl) results in the formation of DNP double-fibers and bundle- and cablelike twisted side-by-side associates of several of these double-fibers. On the basis of simple cylindrical or ellipsoidal models the sedimentation properties of these structures can be calculated in accordance with the experiment allowing a direct assignment of electron microscopical and hydrodynamic results. Sedimentation measurements in dependence on the ionic strength indicate a redistribution of H1 resulting in the formation of associates at 0.04 M NaCl and of aggregates at higher salt concentration. Double-fibers are present up to physiological salt concentrations.