|Subdivision of the Cretaceous system|
according to the ICS, as of 2017.
The Cenomanian is, in the ICS' geological timescale the oldest or earliest age of the Late Cretaceous epoch or the lowest stage of the Upper Cretaceous series. An age is a unit of geochronology: it is a unit of time; the stage is a unit in the stratigraphic column deposited during the corresponding age. Both age and stage bear the same name.
As a unit of geologic time measure, the Cenomanian age spans the time between 100.5 ± 0.9 Ma and 93.9 ± 0.8 Ma (million years ago). In the geologic timescale it is preceded by the Albian and is followed by the Turonian. The Upper Cenomanian starts approximately at 95 M.a.
The Cenomanian was introduced in scientific literature by French palaeontologist Alcide d'Orbigny in 1847. Its name comes from the New Latin name of the French city of Le Mans (département Sarthe), Cenomanum.
The base of the Cenomanian stage (which is also the base of the Upper Cretaceous series) is placed at the first appearance of foram species Rotalipora globotruncanoides in the stratigraphic record. An official reference profile for the base of the Cenomanian (a GSSP) is located in an outcrop at the western flank of Mont Risou, near the village of Rosans in the French Alps (département Hautes-Alpes, coordinates: 44°23'33"N, 5°30'43"E). The base is, in the reference profile, located 36 meters below the top of the Marnes Bleues Formation.
Sequence stratigraphy and palaeoclimatology
The late Cenomanian represents the highest mean sea-level observed in the Phanerozoic eon, the past six hundred million years (approximately one hundred and fifty meters above present day sea-levels). A corollary is that the highlands were at all time lows, so the landscape on Earth was one of warm broad shallow seas inundating low-lying land areas on the precursors to today's continents. What few lands rose above the waves were made of old mountains and hills, upland plateaus, all much weathered. Tectonic mountain building was minimal and most continents were isolated by large stretches of water. Without highlands to brake winds, the climate would have been windy and waves large, adding to the weathering and fast rate of sediment deposition.
The crown-group Crocodylia, the true-crocodiles, first appear during the Cenomanian.
|Belemnites of the Cenomanian|
|Ankylosaurs of the Cenomanian|
|Albian or Aptian to Cenomanian||Upper Greensand Group, Cambridgeshire, England||A nodosaurid with an armor of oval plates set almost horizontally into the skin, with spikes protruding from the neck and shoulder area, along the spine. Its size has been estimated to be in the range of 3 to 5.5 meters (10 to 18 ft) long and approximately 380 kilograms (840 lb) in weight.|
|Cenomanian to Turonian||Cedar Mountain Formation, Utah, USA||thought of as a nodosaurid ankylosaur, although its precise relationships within that family are uncertain|
|Wyoming, Kansas, USA||A nodosaurid ankylosaur about 4 to 6 meters (13 to 20 feet) long with bony dermal plates covering the top of its body. It may have had spikes along its side as well. It had four short legs, five-toed feet, a short neck, and a long, stiff, clubless tail.|
|Late Albian to early Cenomanian||Dakota Formation, Kansas, USA||A genus of nodosaurid known from a nearly complete skull.|
|Late Albian to early Cenomanian||Frontier Formation, Wyoming, USA||A poorly known genus of nodosaurid|
|Baynshiree Svita Formation, Dzun-Bayan, Mongolia||An ankylosaurid known from the remains of its skull|
|Chaochuan Formation, Zhejiang, China||Ankylosaurid|
|Ruyang, Henan, China||Ankylosaurid|
|Ornithopods of the Cenomanian|
|Cerro Lisandro Formation, Neuquén, Argentina||A small bipedal herbivore, almost seven feet (2 meters) long|
|Bihor, Romania||An iguanodont similar to Camptosaurus|
|Albian-Cenomanian||Utah, USA||A basal hadrosaur|
|Fostoria||Australia||A new iguanodont|
|Albian-Cenomanian||Australia||A large ornithopod that stood about 5 metres high known from about 60% of its skeleton|
|Cenomanian-Turonian||Bajo Barreal Formation, Chubut, Argentina||A hypsilophodontid or other basal ornithopod, Notohypsilophodon would have been a bipedal herbivore. Its size has not been estimated|
|Blackleaf Formation, Montana, and Wayan Formation, Idaho, USA||A burrowing hypsilophodont|
|Flower Mound, Texas, USA||A primitive hadrosauroid, Protohadros reached 6 m (19.5 ft) in length and had many hadrosaur-like features|
|Cenomanian-Turonian||China||A poorly known iguanodont|
|Pari Aike Formation, Lake Viedma, Santa Cruz||A 4 metres (13 ft) long elasmarian|
|Plesiosaurs of the Cenomanian|
|Belle Fourche Shale, Wyoming, USA||A pliosaurid characterized by a moderately long symphysis bearing 8 pairs of teeth, teeth that are nearly circular in cross-section and which are smooth on the outer surface (except near the base), ribs of the neck vertebrae being singled-headed (double-headed in Jurassic pliosaurs), and a long slender interpectoral bar on the coracoid|
|Graneros Shale Formation, Colorado and Belle Fourche Formation, Montana||Thalassomedon is among the largest elasmosaurids, with a total length of 10.86 metres (35.6 ft) for the holotype.|
|Pterosaurs of the Cenomanian|
|Brazil||An Ornithocheirid pterosaur|
|Albian-Turonian||Chalk Formation and Cambridge Greensand, England|
|Sauropods of the Cenomanian|
|Andesaurus||Candeleros Formation, Argentina|
|Argentinosaurus||Huincul Formation, Neuquén, Argentina|
|Diamantinasaurus||Winton Formation, Queensland, Australia|
|Paralititan||Bahariya Formation, Egypt|
|Puertasaurus||Pari Aike Formation, Patagonia, Argentina||Originally believed to be from Maastrichtian age.|
|Sibirosaurus||Kiya River, Russia|
|Theropods of the Cenomanian|
|Winton Formation, Queensland, Australia||A megaraptoran.|
|Bahariya Oasis, Egypt; Niger||A large theropod of dubious classification. May be synonymous with Deltadromeus.|
|Kem Kem Formation, Eckhar Formation, Bahariya Formation, Morocco; Niger; Egypt||A large carcharodontosaurid. Original specimens destroyed in World War II, new remains uncovered in 1990's. Two species known; C. saharicus and C. iguidensis. Contemporaneous with Rugops, Spinosaurus and Deltadromeus/Bahariasaurus.|
|Morocco||A ceratosaur or possible neovenatorid carnosaur. May be synonymous with Bahariasaurus. Contemporaneous with Spinosaurus, Rugops, and Carcharodontosaurus.|
|Candeleros Formation, Argentina||A carcharodontosaurid. One of the largest theropods currently known to science.|
|Huincul Formation, Argentina||A carcharodontosaurid. Known from multiple specimens in a single bone bed.|
|Moreno Hill Formation, Zuni Basin, New Mexico; Tropic Shale, Utah, USA||A therizinosaur. Two species known; N. mckinleyi and N. graffmani.|
|Brasil||A spinosaurid. Largest theropod thus far recovered from Brazil.|
|Pari Aike Formation, Patagonia, Argentina; South America||A megaraptoran. Originally thought to have been from Maastrichtian deposits.|
|Niger||An abelisaurid. Contemporaneous with Spinosaurus, Carcharodontosaurus, and Deltadromeus/Bahariasaurus.|
|Mongolia||A theropod belonging to the Therizinosauridae family.|
|Cenomanian||Mussentuchit Member, Cedar Mountain Formation, Utah, USA||An 11-12 meter neovenatorid carcharodontosaur known from juvenile remains. Youngest known allosauroid known from North America.|
|Tafilalt, Morocco||A spinosaurid. Known from fragmentary remains.|
|Bahariya Oasis, Egypt; Tunisia; Morocco||A spinosaurid. Currently considered one of the largest known theropods if not the largest at an estimated 15 m (49 ft).|
|Comahue, Argentina||A unenlagiine dromaeosaurid.|
|Nammoura, Ouadi al Gabour, Lebanon|
|Bajo Barreal Formation, Chubut Province, Argentina||An abelisaurid.|
- Super User. "ICS - Chart/Time Scale". www.stratigraphy.org.
- See for a detailed geologic timescale Gradstein et al. (2004)
- International Commission on Stratigraphy. "International Stratigraphic Chart" (PDF). Archived from the original (PDF) on 2008-05-29. Retrieved 2008-06-17.
- The GSSP for the Cenomanian was established by Kennedy et al. (2004)
- Mateus, O., Callapez P. M., & Puértolas-Pascual E. (2017). The oldest Crocodylia? a new eusuchian from the Late Cretaceous (Cenomanian) of Portugal. Journal of Vertebrate Paleontology, Program and Abstracts. 2017, 160.
- Vecchia, F. M. D.; Chiappe, L. M. (2002). "First avian skeleton from the Mesozoic of northern Gondwana". Journal of Vertebrate Paleontology. 22 (4): 856. doi:10.1671/0272-4634(2002)022[0856:FASFTM]2.0.CO;2.
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- Kennedy, W.J.; Gale, A.S.; Lees, J.A. & Caron, M.; 2004: The Global Boundary Stratotype Section and Point (GSSP) for the base of the Cenomanian Stage, Mont Risou, Hautes-Alpes, France, Episodes 27, pp. 21–32.
- GeoWhen Database - Cenomanian
- Late Cretaceous timescale, at the website of the subcommission for stratigraphic information of the ICS
- Stratigraphic chart of the Lower Cretaceous (including the Cenomanian), at the website of Norges Network of offshore records of geology and stratigraphy
- Cenomanian Microfossils: 20+ images of Foraminifera