We analyze calcareous nannofossils in the Late Cretaceous Niobrara Formation of the Western Interior Seaway.
Base of the Campanian lies between the last occurrences of Helicolithus trabeculatus >7 μm and Zeugrhabdotus biperforatus
The base of the Scaphites leei III ammonite Zone appears to be slightly younger than the base of paleomagnetic chron C33r.