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Cenomanian
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The Cenomanian age (also known as Woodbinian [depreciated by the ICS]) is the first or earliest or oldest Geochronological "geologic age" of the Late Cretaceous Epoch. Like all geological time units the Cenomanian age is associated with a Chronostratigraphic stratum or "geologic stage" (or faunal stage—see biostratigraphy and geobiology) of the same name, the "Cenomanian stage" (and its relationship to the parents epochs' strata, called a series, is that it is one of many in the series).

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Encyclopedia
The Cenomanian age (also known as Woodbinian [depreciated by the ICS]) is the first or earliest or oldest Geochronological "geologic age" of the Late Cretaceous Epoch. Like all geological time units the Cenomanian age is associated with a Chronostratigraphic stratum or "geologic stage" (or faunal stage—see biostratigraphy and geobiology) of the same name, the "Cenomanian stage" (and its relationship to the parents epochs' strata, called a series, is that it is one of many in the series). Each belong to the Cretaceous period and Cretaceous system as well.
Terminology
The strata characteristic of the geological stage were identified by various means as having been laid down during the corresponding age. The terms upper and lower refer to the strata and stage (or other larger chronostratigraphic units) whereas 'late' and 'early' generally refer to relative time measures, which is to say late or middle or early modify when within 'the age' (or hierarchically larger) time unit.
The Cenomanian units
As a unit of geologic time measure, the Cenomanian age spans the time between) as formally accepted by the International Union of Geological Sciences. The Cenomanian stage is the sequence of rock strata and its fossil record which have been studied by many disciplines and are used in geochronology to date findings within the geologic age. Excepting chronozones, which are outside the hierarchy organization, stages are the smallest unit and type of chronostratigraphic layers used in the earth sciences for dating comparisons and determination.
Characteristics in the Cenomanian
The late Cenomanian represents the highest mean sea-level observed in 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 and what few lands rose above the waves were made of old mountains and hills, upland plateaus, all much weathered. Tectonic mountain building was minimal, for today's configuration of continents was far from complete, so 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 depositions of strata in water regions at fast rate.
Invertebrate Fauna
Belemnites
| Belemnites of the Cenomanian |
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| Taxa | Presence | Location | Description | Images |
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Hibolites | | | | | |
Vertebrate Fauna
Ankylosauria
| Ankylosaurs of the Cenomanian |
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| Taxa | Presence | Location | Description | Images |
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| Albian or Aptian to Cenomanian | Greesand Formation, 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. | | | Animantarx | Cenomanian to Turonian | Cedar Mountain Formation, Utah, USA | thought of as a nodosaurid ankylosaur, although its precise relationships within that family are uncertain | | Nodosaurus | | 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. | | Stegopelta | Late Albian to early Cenomanian | Frontier Formation, Wyoming, USA | A poorly known genus of nodosaurid | | Tsagantegia | | Baynshiree Svita Formation, Dzun-Bayan, Mongolia | An ankylosaurid known from the remains of its skull | | Zhejiangosaurus | | Chaochuan Formation, Zhejiang, China | Nodosaurid | | Zhongyuansaurus | | Ruyang, Henan, China | Nodosaurid |
Ornithopoda
| Ornithopods of the Cenomanian |
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| Taxa | Presence | Location | Description | Images |
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Anabisetia | | Cerro Lisandro Formation, Neuquén, Argentina | A small bipedal herbivore, almost seven feet (2 meters) long | | |
Bihariosaurus | | Bihor, Romania | An iguanodont similar to Camptosaurus | |
Eolambia | Albian-Cenomanian | Utah, USA | An iguanodont | |
Gadolosaurus | | Mongolia | | |
Notohypsilophodon | 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 | |
Protohadros | | Flower Mound, Texas, USA | A primitive hadrosauroid, Protohadros reached 6 m (19.5 ft) in length and had many hadrosaur-like features | |
Shuangmiaosaurus | Cenomanian-Turonian | China | A poorly known iguanodont |
Sauropoda
| Sauropods of the Cenomanian |
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| Taxa | Presence | Location | Description | Images |
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Argentinosaurus | | Río Limay Formation, Neuquén, Argentina | | | |
Brachiosaurus | ? Brachiosaurus nougaredi | Wargla, Algeria | |
Theropoda
Geologic Formations
Related other topics
External links
- : overview
- : chart
- displaying geologic time periods compared to the fossil record.
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