The multiphasic thermal denaturation profile of histone-H1-depleted chromatin was studied by using a nucleoprotein preparation which lacked the first high temperature transition at about 72°C. Such a preparation was obtained by heating at 72 "C HI-depleted chromatin, the DNA of which was cross-linked with psoralen to ensure a complete renaturation of DNA upon cooling. When this nucleoprotein was redenatured, its melting profile was found to be significantly altered: only one high temperature peak centered at about 82 "C was observed in addition to the low temperature transition at about 53 "C. The kinetics of digestion of this material with micrococcal nuclease showed a limit digest equal to that found for the 'native' HI-depleted chromatin but the rate of hydrolysis was higher. The monomer particles prepared from this nucleoprotein were found similar to the 'native' monosomes in respect to protein:DNA ratio and size of DNA but showed an altered melting profile: the premelt area was broader, bigger, and centered at lower temperature; the main peak was reduced in size with no change in its melting temperature. On the basis of these data, the following conclusions were drawn: (a) the last two thermal transitions in HI-depleted chromatin most likely reflect the presence within each nucleosome of two regions with different stability of DNA; (b) DNA involved in the first high thermal transition of HI-depleted chromatin belongs to nuclease-accessible DNA, and (c) the main peak in the biphasic melting profile of the monomer particles reflects the denaturation of DNA regions which in the polymer nucleoprotein are involved in the two high temperature transitions.The thermal denaturation of nucleoproteins is one of the most frequently used physical methods for studying the interactions between DNA and chromosomal proteins (for recent reviews see [3,2]). The denaturation profile of intact or histone-Hl-depleted chromatin was found to be multiphasic [3-61. The two high temperature transitions at 72°C and 82 "C (see [4]) are generally ascribed to the binding of histones to DNA [4,7] but different explanations of their origin were suggested [3 -5,8]. On the other hand, the melting profile of monomers lacking histone H1 shows a low temperature transition (premelt) at about 60 "C and a main transition at about 74-76 "C [9 -1 I]. The question arises, therefore, about the relationship between the melting pattern of the polymer material and that of the monosomes. Recently, Bryan et al. [12] forwarded the idea that the premelt and the main thermal transition of the monosomes corresponded to the 72 "C and 82 "C transitions of the polymer nucleoprotein, respectively, the transitions of the monomers being shifted to a lower temperature by the free DNA ends.In the present study on H1-depleted chromatin we developed an experimental approach which allowed us to obtain a material lacking the transition at 72 "C and to investigate some properties of this material as well as the melting profile of the monomer particles isolated from it. Th...