Analysis of outcropping Upper Carboniferous (Virgilian, Wabaunsee Group) strata in the North American Mid-Continent suggests a hierarchy of stratigraphic forcing. Fourth order depositional sequences from -the Wabaunsee Group represent the latest highstand sequence sets of a composite third order sequence (1-10m.y.) that encompasses strata from the Douglas, Shawnee, Wabaunsee, and Admire Groups.
The composite third order sequence (1-10m.y) is composed of fifteen composite fourth order depositional sequences (0.1 - 1m.y.). The composite fourth order depositional sequences of the Wabaunsee Group contain between two and three fifth order cycles (0.01-0.1m.y.). These fifth order cycles form retrogradational transgressive system tracks and aggradational to progradational highstand system tracks.
Lowstand units are comprised of incised valley fill deposits
or laterally extensive paleosols. The fifth order cycles are separated
by poorly developed, laterally discontinuous paleosols or marginal
marine units. These poorly developed paleosols are expressed as
coals, coaly shales, or underclays.