The distribution of H1 histone is nonuniform in chromatin and correlates with different degrees of condensation.

Salt induces aggregation of large chromatin fragments maximally at 150-200 mM NaCl. The soluble fragments are depleted of H1 histones while the aggregated fragments are enriched. H1 histones did not equilibrate between the soluble and insoluble chromatin fractions when they were recycled through the process of salt-induced aggregation. The chromatin fragments that resisted aggregation retained more H1c subtype than they did H1 ab, correlating with previous results which showed complexes of H1c with DNA resisted salt-induced aggregation much more than complexes of DNA with other subtypes. The chromatin that was soluble at physiological concentrations of NaCl was DNase I sensitive and enriched in acetylated core histones. We conclude that H1 histone is nonuniformly distributed in chromatin in a stable pattern that probably correlates with the different degrees of condensation known to exist in vivo.