The Campanian is the fifth of six ages of the Late Cretaceous epoch on the geologic timescale of the International Commission on Stratigraphy (ICS). In chronostratigraphy, it is the fifth of six stages in the Upper Cretaceous Series. Campanian spans the time from 83.6 (± 0.2) to 72.1 (± 0.2) million years ago. It is preceded by the Santonian and it is followed by the Maastrichtian.
The Campanian was an age when a worldwide sea level rise covered many coastal areas. The geomorphology of some of these areas has been preserved: it is an unconformity beneath a cover of marine .
Etymology
The Campanian was introduced in scientific literature by
Henri Coquand in 1857. It is named after the French village of Champagne in the department of Charente-Maritime. The original type locality was a series of
near the village of Aubeterre-sur-Dronne in the same region.
Definition
The base of the Campanian Stage is defined as a place in the stratigraphic column where the
extinction of
crinoid species
Marsupites testudinarius is located. A GSSP was ratified for the base of the Campanian in October 2022, having been placed in Bottaccione,
Gubbio,
Italy.
The top of the Campanian stage is defined as the place in the stratigraphic column where the
ammonite Pachydiscus neubergicus first appears.
Subdivisions
The Campanian can be subdivided into Lower, Middle and Upper Subages. In the western interior of the United States, the base of the Middle Campanian is defined as the first occurrence of the ammonite
Baculites obtusus (80.97 Ma) and the base of the Upper Campanian defined as the first occurrence of the ammonite
Didymoceras nebrascense (76.27 Ma).
In the
Tethys Ocean, the Campanian encompasses six ammonite
. They are, from young to old:
Paleontology
During the Campanian age, a radiation among
dinosaur species occurred. In North America, for example, the number of known dinosaur
genera rises from four at the base of the Campanian to forty-eight in the upper part. This development is sometimes referred to as the "Campanian Explosion". However, it is not yet clear if the event is artificial, i.e. the low number of genera in the lower Campanian can be caused by a lower preservation chance for fossils in deposits of that age. The generally warm climates and large continental area covered in shallow sea during the Campanian probably favoured the dinosaurs. In the following Maastrichtian stage, the number of North American dinosaur genera found is 30% less than in the upper Campanian.
[See Weishampel et al. (2004)]
See also
Further reading
-
Varricchio, D. J. 2001. Late Cretaceous oviraptorosaur (Theropoda) dinosaurs from Montana. pp. 42–57 in D. H. Tanke and K. Carpenter (eds.), Mesozoic Vertebrate Life. Indiana University Press, Indianapolis, Indiana.
-
; 2004: Dinosaur distribution, in: ( eds.): The Dinosauria, University of California Press, Berkeley (2nd ed.), , pp 517–606.
External links
