Ubiquitinated histones uH2A.1, uH2A.Z, and uH2B have been identified in the basic nuclear proteins of the slime mold Physarum polycephalum by three methods: peptide mapping, cross-reaction with anti-ubiquitin antibody, and uH2A and uH2B isopeptidase cleavage. In microplasmodia, uH2A amounts to 7% of H2A and uH2B amounts to 6% of H2B. Detailed studies of mitosis in Physarum polycephalum macroplasmodia show that in early prophase, which last 15 min, the uH2As and uH2B are both strongly present, whereas minutes later in metaphase, which lasts 7 min, they disappear. When the nuclei enter anaphase, which lasts 3 min, both the uH2As and uH2B reappear. These precise studies suggest that cleavage of ubiquitin from the uH2As and uH2B is a very late, possibly final event in chromosome condensation to metaphase chromosomes and that ubiquitination is an early event in their decondensation. It is proposed that the uH2A and uH2B mark specific regions of the genome which have to be deubiquitinated prior to packaging into metaphase chromosomes; after metaphase these regions are the first to be decondensed and ubiquitinated. This modification, however, is not thought to be a general factor in chromosome condensation but labels a specific subcomponent of chromatin containing the expressed genes of a particular cell type or an important subset of these genes required by the cell to be available for activation, e.g. stress genes.