Histones H3 and H4 are components of upstream activation factor required for the high-level transcription of yeast rDNA by RNA polymerase I

RNA polymerase I (Pol I) transcription in the yeast Saccharomyces cerevisiae is greatly stimulated in vivo and in vitro by the multiprotein complex, upstream activation factor (UAF). UAF binds tightly to the upstream element of the rDNA promoter, such that once bound (in vitro), UAF does not readily exchange onto a competing template. Of the polypeptides previously identified in purified UAF, three are encoded by genes required for Pol I transcription in vivo: RRN5, RRN9, and RRN10. Two others, p30 and p18, have remained uncharacterized. We report here that the N-terminal amino acid sequence, its mobility in gel electrophoresis, and the immunoreactivity of p18 shows that it is histone H3. In addition, histone H4 was found in UAF, and myc-tagged histone H4 could be used to affinity-purify UAF. Histones H2A and H2B were not detectable in UAF. These results suggest that histones H3 and H4 probably account for the strong binding of UAF to DNA and may offer a means by which general nuclear regulatory signals could be transmitted to Pol I.

Intercellular mobility and homing of an archaeal rDNA intron confers a selective advantage over intron- cells of Sulfolobus acidocaldarius.

Some intron-containing rRNA genes of archaea encode homing-type endonucleases, which facilitate intron insertion at homologous sites in intron- alleles. These archaeal rRNA genes, in contrast to their eukaryotic counterparts, are present in single copies per cell, which precludes intron homing within one cell. However, given the highly conserved nature of the sequences flanking the intron, homing may occur in intron- rRNA genes of other archaeal cells. To test whether this occurs, the intron-containing 23S rRNA gene of the archaeal hyperthermophile Desulfurococcus mobilis, carried on nonreplicating bacterial vectors, was electroporated into an intron- culture of Sulfolobus acidocaldarius. PCR experiments demonstrated that the intron underwent homing and spread through the culture. By using a double drug-resistant mutant of S. acidocaldarius, it was shown that spreading resulted partly from a selective advantage of intron+ cells and partly from intercellular mobility of the intron and homing.

Evidence from molecular systematics for decreased avian diversification in the pleistocene Epoch.

Pleistocene glaciations have been suggested as major events influencing speciation rates in vertebrates. Avian paleontological studies suggest that most extant species evolved in the Pleistocene Epoch and that species' durations decreased through the Pleistocene because of heightened speciation rates. Molecular systematic studies provide another data base for testing these predictions. In particular, rates of diversification can be determined from molecular phylogenetic trees. For example, an increasing rate of speciation (but constant extinction) requires shorter intervals between successive speciation events on a phylogenetic tree. Examination of the cumulative distribution of reconstructed speciation events in mtDNA phylogenies of 11 avian genera, however, reveals longer intervals between successive speciation events as the present time is approached, suggesting a decrease in net diversification rate through the Pleistocene Epoch. Thus, molecular systematic studies do not indicate a pulse of Pleistocene diversification in passerine birds but suggest, instead, that diversification rates were lower in the Pleistocene than for the preceding period. Documented habitat shifts likely led to the decreased rate of diversification, although from molecular evidence we cannot discern whether speciation rates decreased or extinction rates increased.