Abstract
The Devonian-Carboniferous boundary is documented in marine strata from the Appalachian Basin, Michigan Basin, Illinois Basin, Forest City Basin, Williston Basin, Tobosa Basin, southern continental margin, western platform, and several sub-basins of the Antler Foreland in the USA based on conodonts, brachiopods, miospores, carbon isotope data, and magnetic susceptibility data. The boundary is narrowly constrained and conformable in the Illinois Basin and Oklahoma; less well constrained in the Appalachian Basin, Antler Foreland, western platform, and the Alberta Platform, and often developed on an unconformity.
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