Abstract
Polynucleosomes with poly(dG-m5dC) .cntdot. poly(dG-m5dC) have been reconstituted, and well-defined nucleosome core particles from these have been prepared. Upon addition of MgCl2 to the levels used to induce the B to Z transition in this highly methylated DNA, significant changes in the circular dichroism spectrum are observed in solutions of these particles. However, such core particles also exhibit a noticeable instability when compared to chicken erythrocyte core particles under the same conditions. The change in circular dichroism can be entirely accounted for on the assumption that only free nucleotide, released by core particle dissociation, undergoes the B .fwdarw. Z transition. Therefore, no evidence has been found for "Z nucleosomes" in these solutions. In fact, the histone-DNA interaction in the nucleosome seems to partially inhibit the B to Z transition of the DNA. The analysis of our results is consistent with a model in which all of the DNA that remains bound to the histone octamer retains the B form.