The Campanian is, in the ICS' geologic timescale, the fifth of six ages of the Late Cretaceous epoch (or, in chronostratigraphy: the fifth of six stages in the Upper Cretaceous series). The Campanian spans the time from 83.6 ± 0.7 Ma to 72.1 ± 0.6 Ma (million years ago). It is preceded by the Santonian and it is followed by the Maastrichtian.[1]
Stratigraphic definition
The Campanian was introduced in scientific literature by Henri Coquand in 1857. It is named after the French village of Champagne in the département Charente-Maritime. The original type locality was an outcrop near the village of Aubeterre-sur-Dronne in the same region. Due to changes of the stratigraphic definitions, this section is now part of the Maastrichtian stage.
The base of the Campanian stage is laid at the extinction of crinoid species Marsupites testudinarius. A GSSP had not yet been ratified in 2009. One possible candidate is in a section near a dam at Waxahachie, Texas.
The top of the Campanian is defined as the place in the stratigraphic column were the ammonite Pachydiscus neubergicus first appears.
Subdivision
The Campanian is sometimes subdivided into Lower, Middle and Upper subages. In the Tethys domain, the Campanian encompasses six ammonite biozones. 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 4 at the base of the Campanian to 48 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.[2]
Animals that lived in the Campanian include:
†Ankylosaurs
Ankylosaurs of the Campanian |
Taxa |
Presence |
Location |
Description |
Images |
Aletopelta |
|
Point Loma Formation, California, USA |
A medium-sized ankylosaurid, estimated to be around 6 m (20 ft) long. |
|
Antarctopelta |
|
Santa Marta Formation, James Ross Island, Antarctica |
A stocky ankylosaur protected by armor plates embedded in the skin. Although a complete skeleton has not been found, the species is estimated to have reached a maximum length of 4 meters (13 ft). Displays characteristics of both ankylosaurids and nodosaurids. |
Edmontonia |
Campanian to Maastrichtian |
Horseshoe Canyon Formation, Alberta, Canada |
A bulky nodosaurid at roughly 6.6 m (22 ft) long. It had small, ridged bony plates on its back and many sharp spikes along its body sides. The four largest spikes jutted out from the shoulders on each side, two of which were split into subspines in some specimens. Its skull had a pear-like shape when viewed from above. |
Euoplocephalus |
|
|
Nodocephalosaurus |
|
|
|
Panoplosaurus |
|
Judith River Formation, Alberta, Canada; Montana, USA |
A 5.5–7 m long nodosaurid. |
Pinacosaurus |
|
|
|
Saichania |
|
|
|
Shanxia |
|
|
|
Struthiosaurus |
|
|
|
Tarchia |
|
|
|
Tianzhenosaurus |
|
|
|
Birds (avian theropods)
Bony Fish
Cartilaginous Fish
†Ceratopsians
Crocodylomorphs
Mammals
†Ornithopods
Ornithopods of the Campanian |
Taxa |
Presence |
Location |
Description |
Images |
Aralosaurus |
85.8 mya |
Asia |
Aralosaurus was about the size of an elephant. Although very little is known about Aralosaurus (only one near complete skull has been found); it was identified by a beak with nearly 1,000 small teeth in 30 rows. These teeth were used for breaking up plant matter by chewing, a feature common in herbivorous dinosaurs, but unusual for reptiles.The back of an Aralosaurus skull was wide, a feature suggestive of large jaw muscles used to power its chewing apparatus. |
|
Brachylophosaurus |
76.5 mya |
Montana, USA; Alberta, Canada |
Brachylophosaurus was a typical hadrosaur which reached an adult length of 9 meters (30 ft). |
Corythosaurus |
77-76.5 mya |
Alberta, Canada |
Corythosaurus weighed in at 4 tonnes and measured roughly 10 metres (33 ft) from nose to tail. Like other hadrosaurs it had a toothless beak, the back of the jaws contained a dental battery composed of hundreds of small, interlocking teeth. These were used to crush and grind plant matter and were continually replaced as they wore away. |
Diclonius |
75 mya |
Montana, USA |
|
Edmontosaurus |
73.0-76.5 mya |
Canada |
Edmontosaurus included some of the largest hadrosaurid species, measuring up to 12 metres (39 ft) long and weighing around 4.0 metric tons (4.4 short tons). |
Gasparinisaura |
85 mya |
Argentina |
Gasparinisaura was a small bipedal herbivore. In 2010 Gregory S. Paul estimated the length at 1.7 metres, the weight at thirteen kilogrammes. |
Gilmoreosaurus |
70 mya |
Mongolia |
|
Gryposaurus |
83-75.5 mya |
Alberta, Canada |
Gryposaurus was a hadrosaurid of typical size and shape. |
Hadrosaurus |
79.5 mya |
New Jersey, USA |
It was likely bipedal for the purposes of running, but could use its forelegs to support itself while feeding. |
Hypacrosaurus |
75-67 mya |
Alberta, Canada |
Hypacrosaurus is most easily distinguished from other hollow-crested duckbills by its tall neural spines and the form of its crest. The neural spines, which project from the top of the vertebrae, are 5 to 7 times the height of the body of their respective vertebrae in the back,[4] which would have given it a tall back in profile. The skull's hollow crest is like that of Corythosaurus, but is more pointed along its top, not as tall, wider side to side, and has a small bony point at the rear |
Hypsibema |
|
North Carolina and Missouri, USA |
|
Kritosaurus |
73 mya |
North America |
The type specimen of Kritosaurus navajovius is only represented by a partial skull and lower jaws, and associated postcranial remains. |
Lambeosaurus |
76-75 mya |
Alberta, Canada |
|
Lophorhothon |
80 mya |
Alabama, USA |
|
Maiasaura |
76.7 mya |
Montana, USA |
Maiasaura was large, attaining an adult length of about 9 metres (30 ft) and had the typical hadrosaurid flat beak and a thick nose. It had a small, spiky crest in front of its eyes. The crest may have been used in headbutting contests between males during the breeding season. |
Mandschurosaurus |
|
Asia |
|
Microhadrosaurus |
|
China |
|
Mochlodon |
|
Austria |
A rhabdodontid. |
Naashoibitosaurus |
73 mya |
New Mexico, USA |
Naashoibitosaurus, based as it is on a single partial skeleton, is not well known in terms of anatomy. Its skull, the most thoroughly described portion, has a low nasal crest that peaks in front of the eyes, but does not strongly arch as in Gryposaurus. |
Nipponosaurus |
|
Russia |
|
Orodromeus |
76.7 mya |
Montana, USA |
Orodromeus was a small fast bipedal herbivore that probably coexisted with dinosaurs such as Daspletosaurus and Einiosaurus. Its length was estimated by Horner & Weishampel at 2.5 metres. |
Parasaurolophus |
76.5-73 mya |
Alberta, Canada; New Mexico and Utah, USA |
|
Prosaurolophus |
76-75 mya |
Alberta, Canada |
Prosaurolophus was a large-headed duckbill; the most complete described specimen has a skull around 0.9 meters long (2.9 ft) on a ~8.5 meter long skeleton (~28 ft).[2] It had a small, stout, triangular crest in front of the eyes; the sides of this crest were concave, forming depressions. The upper arm was relatively short. |
Pteropelyx |
|
Montana, USA |
|
Rhabdodon |
70 mya |
France; Spain; Haţeg Island, Romania |
It is unclear whether it was an iguanodont or a hypsilophodont, and may be a "missing link" between the two. Current evidence indicates it is an iguanodont similar to Tenontosaurus. |
Saurolophus |
69.5-68.5 mya |
North America, Asia |
Saurolophus is known from material including nearly complete skeletons, giving researchers a clear picture of its bony anatomy. S. osborni, the rarer Albertan species, was around 9.8 meters long (32 feet), with its skull a meter long (3.3 feet). Its weight is estimated at 1.9 tonnes (2.1 tons). S. angustirostris, the Mongolian species, was larger; the type skeleton is roughly 12 meters long (39.4 ft), and larger remains are reported. |
Shantungosaurus |
70 mya |
China |
It is one of the longest and largest known hadrosaurids; the composite skeleton of a medium-sized individual mounted at the Geological Institute of China in Beijing measures 14.72 metres (48.3 ft) in length. |
Tanius |
|
China |
|
Trachodon |
77 mya |
Montana, USA |
|
Tsintaosaurus |
70 mya |
Southern China |
|
Velafrons |
72 mya |
Mexico |
|
†Pachycephalosaurs
Pachycephalosaurs of the Campanian |
Taxa |
Presence |
Location |
Description |
Images |
Alaskacephale |
|
Prince Creek Formation, Alaska, USA |
|
|
Colepiocephale |
|
Alberta, Canada |
The oldest known pachycephalosaurid. |
Goyocephale |
|
Mongolia |
|
Gravitholus |
|
|
|
Hanssuesia |
|
Alberta, Canada; Montana, USA |
Distinguished from other pachycephalosaurs by having a depressed parietal region, wide frontoparietal dome, broad nasal characteristics, reduced prefontal lobes, and a reduced parietosquamosal shelf. |
?Heishansaurus |
|
|
|
Homalocephale |
|
Mongolia |
Sporting a flat, wedge-shaped skull roof, Homalocephale was different from other pachycephalosaurs. |
?Micropachycephalosaurus |
|
|
|
Ornatotholus |
|
|
|
Prenocephale |
|
|
|
Sphaerotholus |
|
|
|
Stegoceras |
|
|
|
Tylocephale |
|
|
|
Wannanosaurus |
|
|
|
†Plesiosaurs
†Pterosaurs
Pterosaurs of the Campanian |
Taxa |
Presence |
Location |
Description |
Images |
Geosternbergia |
|
USA, North America |
Geosternbergia was originally a species of Pteranodon and is famous for its oddly shaped crest. |
Nyctosaurus |
|
mid-western United States |
Nyctosaurus is a genus of pterodactyloid pterosaur. |
|
Pteranodon |
|
Kansas, USA, North America |
Pteranodon is a genus of pterosaurs which included some of the largest known flying reptiles, with wingspans over 6 metres |
Quetzalcoatlus |
|
Texas, USA |
Quetzalcoatlus was a pterodactyloid pterosaur known from the Late Cretaceous of North America and one of the largest known flying animals of all time. |
Piksi |
|
Montana, USA |
Piksi is a genus of pterosaurs containing the single species Piksi barbarulna. |
Navajodactylus |
|
New Mexico, USA, and Alberta, Canada |
Known primarily from forearm elements; tentatively assigned to Azhdarchidae, though most likely not part of it. |
Montanazhdarcho |
|
Montana, USA |
Small azhdarchoid pterosaur, probably a tapejarid |
Volgadraco |
|
Saratov, Russia |
Azhdarchid pterosaur. |
†Sauropods
Squamates
Testudines
†Theropods (non-avian)
David J. Varrichio observes that during the late Campanian Alberta and Montana had very similar theropods despite significant differences in the types of herbivorous dinosaur faunas.[3]
Footnotes
- ↑ See Gradstein et al. (2004) for a detailed version of the geological timescale
- ↑ See Weishampel et al. (2004)
- ↑ "Abstract," in Varricchio (2001). Page 42.
References
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- 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.
- Weishampel, D.B.; Barrett, P.M.; Coria, R.A.; Le Loueff, J.; Xu, X.; Zhao, X.; Sahni, A.; Gomani, E.M.P. & Noto, C.N.; 2004: Dinosaur distribution, in: Weishampel, D.B.; Dodson, P. & Osmólska, H. (eds.): The Dinosauria, University of California Press, Berkeley (2nd ed.), ISBN 0-520-24209-2, pp 517–606.
External links