(geology) Southern European equivalent of the Portlandian stage (uppermost Jurassic) of geologic time.
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(geology) Southern European equivalent of the Portlandian stage (uppermost Jurassic) of geologic time.
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| System | Series | Stage | Age (Ma) | |
|---|---|---|---|---|
| Cretaceous | Lower | Berriasian | younger | |
| Jurassic | Upper | Tithonian | 145.5–150.8 | |
| Kimmeridgian | 150.8–155.7 | |||
| Oxfordian | 155.7–161.2 | |||
| Middle | Callovian | 161.2–164.7 | ||
| Bathonian | 164.7–167.7 | |||
| Bajocian | 167.7–171.6 | |||
| Aalenian | 171.6–175.6 | |||
| Lower | Toarcian | 175.6–183.0 | ||
| Pliensbachian | 183.0–189.6 | |||
| Sinemurian | 189.6–196.5 | |||
| Hettangian | 196.5–199.6 | |||
| Triassic | Upper | Rhaetian | older | |
| Subdivision of the Jurassic system according to the IUGS, as of July 2009. | ||||
In the geologic timescale the Tithonian is the latest age of the Late Jurassic epoch or the uppermost stage of the Upper Jurassic series. It spans the time between 150.8 ± 4 Ma and 145.5 ± 4 Ma (million years ago). It is preceded by the Kimmeridgian and followed by the Berriasian stage (part of the Cretaceous).[1]
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The Tithonian was introduced in scientific literature by German stratigrapher Albert Oppel in 1865. The name Tithonian is unusual in geological stage names because it is derived from Greek mythology. Tithonus was the son of Laomedon of Troy. He fell in love with Eos, the Greek goddess of dawn and finds his place in the stratigraphy because this stage, the Tithonian, finds itself hand in hand with the dawn of the Cretaceous.
The base of the Tithonian stage is at the base of the ammonite biozone of Hybonoticeras hybonotum. A global reference profile (a GSSP or golden spike) for the base of the Tithonian had in 2009 not yet been established.
The top of the Tithonian stage (the base of the Berriasian stage and the Cretaceous system) is at the first appearance of fossils of ammonite species Berriasella jacobi in the stratigraphic record.
The Tithonian is often subdivided into Lower/Early, Middle and Upper/Late substages or subages. The Late Tithonian is coeval with the Portlandian stage of British stratigraphy.
The Tithonian stage contains seven ammonite biozones in the Tethys domain, from top to base:
In the Tethys domain, the Tithonian has a calcareous facies with a typical cephalopod fauna. The Solnhofen limestone of southern Germany, which is known for its fossils (especially Archaeopteryx), is of Tithonian age.
| Ankylosauria of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Morrison Formation, Wyoming, USA | The smallest and the earliest well-known ankylosaur. Its skull measures only 29 cm in length, and its total body length is an estimated three to four meters. | |||
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Morrison Formation, Colorado, USA | A poorly known early ankylosaurian. | ||
| Ceratopsia of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| ? | Chaoyang area, Liaoning, China | One of the earliest ceratopsians | ||
| Hebei, China | A member of the family Chaoyangsauridae, it was one of the earliest ceratopsians | |||
| Ornithopoda of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Kimmeridgian to ?Berriasian | Wyoming, USA; England; France | Camptosaurus could be more than 7.9 meters long (26 ft), and 2.0 meters tall (6.7 ft) at the hips. They had heavy bodies but, as well as walking on four legs (quadrupedal), could also rear up to walk on two legs (bipedal). This genus is probably closely related to the ancestor of the later iguanodontid and hadrosaurid dinosaurs. It probably ate cycads with its parrot-like beak. | ||
| Lourinhã, Portugal | A camptosaurid iguanodont | |||
| Plesiosaurs of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
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| Stegosaurs of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Kimmeridgian to Early Tithonian | Morrison Formation, Colorado, Utah, Wyoming, USA | Averaging around 9 metres (30 ft) long and 4 metres (14 ft) tall, the quadrupedal Stegosaurus is one of the most easily identifiable dinosaurs, due to the distinctive double row of kite-shaped plates rising vertically along its arched back and the two pairs of long spikes extending horizontally near the end of its tail. | ||
| Sauropoda of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Thalattosuchians of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
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A large genus of metriorhynchid, that was a high order predator which fed on other marine reptiles
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A relatively small metriorhynchid genus. No known species of Geosaurus attained lengths in excess of 3 meters (10 feet). There were multiple Geosaurus species alive during the Tithonian.
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An opportunistic carnivore that fed on fish, belemnites and other marine animals and possible carrion. Metriorhynchus grew to an average adult length of 3 meters (9.6 feet). | |||
| Belemnites of the Tithonian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Jurassic period | ||
|---|---|---|
| Lower/Early Jurassic | Middle Jurassic | Upper/Late Jurassic |
| Hettangian | Sinemurian Pliensbachian | Toarcian |
Aalenian | Bajocian Bathonian | Callovian |
Oxfordian | Kimmeridgian Tithonian |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Comodactylus | |
| Nannopterygius | |
| Pleurosauridae |
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