Summary — Approximately 30 Quercus (oak) species occur in the eastern United States, of which Q alba, Q rubra, Q velutina, Q coccinea, Q stellata and Q prinus are among the most dominant. Quercus distribution greatly increased at the beginning of the Holocene epoch (10 000 years BP), but has exhibited major changes since European settlement in the 18th and 19th centuries. For example, large-scale increases in Quercus species have occurred as a result of fire exclusion in the central tallgrass prairie and savanna regions. In the northern conifer and hardwood forests of New England and the Lake States region, Q rubra exhibited a dramatic increase following early logging and fire. Quercus species have also increased in the mid-Atlantic region from land-clearing, the charcoal iron industry and the eradication of Castanea dentata following European settlement. Studies of the dendroecology and successional dynamics of several old-growth forests indicate that prior to European settlement Quercus grew and regenerated in uneven-aged conditions. At times oak growth was very slow (< 1.0 mm/year) for long periods, which is usually characteristic of highly shade-tolerant species. Quercus