Differential scanning calorimetry was used to determine thermodynamic parameters of decondensation of intranuclear rat liver chromatin was induced by a decrease in the concentration of magnesium ions from 5 mM to 0 mM. The process of chromatin melting in the temperature range of 70-100°C occurs in the following order: melting of core-histones, melting of relaxed DNA, and melting of topologically constrained DNA. It was found that Tm and Д H of individual peaks also depend on the concentration of Mg2+ ions in the buffer. In nuclei with condensed chromatin, Mg2+ ions at a concentration of 5 mM increased significantly the Tm of core histones (by ~7°C), as compared to that in unfolded chromatin but at the same time lowered the Tm of nuclear DNA both in the relaxed and constrained state (by ~2.5°С and ~7.5°С, respectively). In the presence of Mg2+ ions, melting enthalpy for peaks increased significantly. At the same time, a decrease in molecular weights of intranuclear DNA levels out a stabilizing effect of Mg2+ ions on core histones. A rise in the concentration of Mg2+ ions above 5 mM leads to the appearance of a new peak with Tm above 100°С, which probably reflects the thermal behavior of some Mg-induced aggregates. Possible mechanisms underlying thermal behavior of chromatin inside the nucleus are discussed.