Kimmeridgian
System/ Period |
Series/ Epoch |
Stage/ Age |
Age (Ma) | |
---|---|---|---|---|
Cretaceous | Lower/ Early |
Berriasian | younger | |
Jurassic | Upper/ Late |
Tithonian | 145.0–152.1 | |
Kimmeridgian | 152.1–157.3 | |||
Oxfordian | 157.3–163.5 | |||
Mid/ Middle |
Callovian | 163.5–166.1 | ||
Bathonian | 166.1–168.3 | |||
Bajocian | 168.3–170.3 | |||
Aalenian | 170.3–174.1 | |||
Lower/ Early |
Toarcian | 174.1–182.7 | ||
Pliensbachian | 182.7–190.8 | |||
Sinemurian | 190.8–199.3 | |||
Hettangian | 199.3–201.3 | |||
Triassic | Upper/ Late |
Rhaetian | older | |
Subdivision of the Jurassic system according to the IUGS, as of July 2012. |
In the geologic timescale, the Kimmeridgian is an age or stage in the Late or Upper Jurassic epoch or series. It spans the time between 157.3 ± 1.0 Ma and 152.1 ± 0.9 Ma (million years ago). The Kimmeridgian follows the Oxfordian and precedes the Tithonian.[1]
Stratigraphic definition
The Kimmeridgian stage takes its name from the village of Kimmeridge on the Dorset coast, England. The name was introduced in literature by Swiss geologist Jules Thurmann in 1832. The Kimmeridge Clay Formation has its name from the same type location. It is the source for about 95% of the petroleum in the North Sea.
Historically the term Kimmeridgian has been used in two different ways. The base of the interval is the same but the top was defined by British stratigraphers as the base of the Portlandian (sensu anglico) whereas in France the top was defined as the base of the Tithonian (sensu gallico). The differences have not yet been fully resolved; As of 2004 Tithonian is has been seen as the uppermost stage of the Jurassic in the timescale of the ICS.[2]
The base of the Kimmeridgian is at the first appearance of ammonite species Pictonia baylei in the stratigraphic column. A global reference profile for the base (the GSSP of the Kimmeridgian stage) had in 2009 not yet been assigned. The top of the Kimmeridgian (the base of the Tithonian) is at the first appearance of ammonite species Hybonoticeras hybonotum. It also coincides with the top of magnetic anomaly M22An.
Subdivision
The Kimmeridgian is sometimes subdivided into Upper and Lower substages. In the Tethys domain, the Kimmeridgian contains seven ammonite biozones:
- zone of Hybonoticeras beckeri
- zone of Aulacostephanus eudoxus
- zone of Aspidoceras acanthicum
- zone of Crussoliceras divisum
- zone of Ataxioceras hypselocyclum
- zone of Sutneria platynota
- zone of Idoceras planula
Palaeontology
†Ankylosaurs
Ankylosaurs of the Kimmeridgian | ||||
---|---|---|---|---|
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. | | |
|
Morrison Formation, Colorado, USA | A poorly known early ankylosaurian. | ||
Birds
Birds of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
| |||
†Ornithopods
Ornithopoda of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
Kimmeridgian to Tithonian | Wyoming, USA | Camptosaurus could be more than 7.9 meters (26 feet) long, and 2.0 meters (6.6 feet) tall at the hips. It had heavy bodies but, as well as walking on four legs (quadrupedal), they could 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. |
| |
†Plesiosaurs
Plesiosaurs of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
†Sauropods
†Sauropods of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
| |||
|
||||
†Stegosaurs
Stegosaurs of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
England and France | A large stegosaurid | |||
Upper Shaximiao Formation, Sichuan, China | Had relatively small dorsal plates and greatly enlarged shoulder spines, twice the length of the shoulder blades. Estimated to have been about 4 metres long. | |||
Morrison Formation, Wyoming, USA | Had alternating plates on its back and four spikes on its tail. Appears more closely related to Dacentrurus than Stegosaurus. | |||
Tanzania | A 4 meter long stegosaurian with spikes on its flanks. The length of the thigh bone compared with the rest of the leg indicates that Kentrosaurus was a slow and inactive dinosaur. | |||
Loe-ein Formation, Tibet, China | The fragmentary condition of the only known skeleton places doubt on the validity of this genus | |||
Kimmeridgian to Early Tithonian | Morrison Formation, Colorado, Utah, Wyoming, USA | Averaging around 9 metres (30 feet) long and 4 metres (13 feet) 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. | ||
†Thalattosuchians
Thalattosuchians of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
Germany | type species of the genus, is known from Western Europe (England, France, Switzerland and Germany) of the Late Jurassic (Late Kimmeridgian-Early Tithonian). | ||
|
Germany | A relatively small metriorhynchid genus. | ||
|
England, France and Switzerland | 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 (9.8 feet). | ||
†Theropods (non-avian)
†Non-avian theropods of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
Guimarota Mine, Portugal | Small 5 kg tyrannosauroid. Avityrannis along with Stokesosaurus represents the oldest known tyrannosauroids. | ||
|
Morrison Formation, Wyoming | Small theropod about 2 metres in length | ||
|
Tendaguru Beds, Tanzania | Probably a ceratosaur about 6 meters long | ||
|
||||
|
||||
Nautiloids
Nautiloids of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
| |||
†Ammonites
Ammonites of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
|
| |||
†Belemnites
Belemnites of the Kimmeridgian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
| ||||
Palaeontological sites
References
Notes
- ↑ For a detailed version of the ICS' timescale, see Gradstein et al. (2004)
- ↑ INTERNATIONAL SUBCOMMISSION ON JURASSIC STRATIGRAPHY, Newsletter 31, Edited by Nicol Morton and Paul Bown, August 2004
Literature
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- Thurmann, J.; 1832: Sur Les Soulèvemens Jurassiques Du Porrentruy: Description Géognostique de la Série Jurassique et Théorie Orographique du Soulèvement, Mémoires de la Société d'histoire naturelle de Strasbourg 1: pp 1–84, F. G. Levrault, Paris.(French)
External links
- GeoWhen Database - Kimmeridgian
- Jurassic-Cretaceous timescale, at the website of the subcommission for stratigraphic information of the ICS
- Stratigraphic chart of the Upper Jurassic, at the website of Norges Network of offshore records of geology and stratigraphy
Jurassic Period | ||
---|---|---|
Lower/Early Jurassic | Middle Jurassic | Upper/Late Jurassic |
Hettangian | Sinemurian Pliensbachian | Toarcian |
Aalenian | Bajocian Bathonian | Callovian |
Oxfordian | Kimmeridgian Tithonian |