Oak opening is an open savanna community with a heavy prairie component. Oak openings tend to be dominated by members of the white oak group, especially bur oak (Quercus macrocarpa), sometimes white oak (Q. alba), and locally in southwestern Wisconsin, chinquapin oak (Q. muhlenbergii). Black oak (Q. velutina) and shagbark hickory (Carya ovata) may also be present. Canopy closure can vary widely. The best quality sites have a canopy with 5-40% closure but can be as high as 60% closure, often with large canopy gaps in between trees. "Canopy closure" is the proportion of shrub and ground layer that is covered in shade or shade flecks at noon on a sunny day. Canopy trees tend to have short, thick trunks with wide-spreading crowns, unlike the tall straight trunks and narrower crowns of forest-grown trees.
Oak openings historically experienced near-annual surface fires. As a result, the subcanopy is essentially absent in good quality sites. Tall shrubs are also sparse, though may include American hazelnut (Corylus americana) and shrubby oak saplings, also known as oak grubs. The ground layer of oak openings is typically dominated by a matrix of native grasses and sedges, especially little bluestem (Schizachyrium scoparium), big bluestem (Andropogon gerardii), needlegrass (Hesperostipa spartea), and Leiberg’s panic grass (Dichanthelium leibergii). Where oak openings occur on wet-mesic sites, sedges (e.g., Carex pellita) or bluejoint grass (Calamagrostis canadensis) may dominate.
Typical forbs are numerous and have significant overlap with prairies, barrens, bedrock glades, and oak woodlands. Some of the best indicators include leadplant (Amorpha canescens), white camas (Anticlea elegans), Canada milkvetch (Astragalus canadensis), kitten-tails (Besseya bullii), bastard toadflax (Comandra umbellata), prairie coreopsis (Coreopsis palmata), veiny pea (Lathyrus venosus), whorled loosestrife (Lysimachia quadrifolia), prairie phlox (Phlox pilosa), Seneca snakeroot (Polygala senega), eastern shooting-star (Primula meadia), and early buttercup (Ranunculus fascicularis). Additional oak opening indicator species can be found in the Coarse-level Monitoring Protocol for Oak Openings (Carter et al, 2023).
Today, oak opening is one of the rarest plant communities in the Upper Midwest with very few high-quality sites in existence. Sites that were not converted to agriculture or settlements were quickly degraded by grazing resulting in the loss of prairie and savanna flora. When grazing declined fire suppression became the norm, causing a rapid growth of trees and shrubs. Oak openings historically occurred in a variety of landscape settings. The best remaining sites are found in the Driftless Region on steep west- to south-facing slopes where they are associated with dry prairies on bluffs. In glaciated southern Wisconsin, they occur on gravelly kames, eskers, and along end moraines, especially in the southern Kettle Moraine region. A variant of oak openings can also occur on sandy alluvial terraces and islands associated with large river systems, such as the Wisconsin, Black, and Chippewa Rivers, where they are sometimes also referred to as floodplain savannas. Historically, oak openings also occurred on mesic sites, but these have essentially been extirpated by fire suppression, intense grazing, and conversion to other land uses.