In the geologic timescale, the Callovian is an age or stage in the Middle Jurassic, lasting between 164.7 ± 4.0 Ma (million years ago) and 161.2 ± 4.0 Ma. It is the last stage of the Middle Jurassic, following the Bathonian and preceding the Oxfordian.[1]
Stratigraphic definitions [edit]
The Callovian stage was first described by French palaeontologist Alcide d'Orbigny in 1852. Its name derives from the latinized name for Kellaways Bridge, a small hamlet 3 km north-east of Chippenham, Wiltshire, England.
The base of the Callovian is defined as the place in the stratigraphic column where the ammonite genus Kepplerites first appears, which is the base of the biozone of Macrocephalites herveyi. A global reference profile (a GSSP) for the base had in 2009 not yet been assigned.
The top of the Callovian (the base of the Oxfordian) is at the first appearance of ammonite species Brightia thuouxensis.
Subdivision [edit]
Matmor Formation (Callovian,
Peltoceras athleta Zone) in Makhtesh Gadol, Israel.
The Callovian is often subdivided into three substages (or subages): Lower/Early, Middle and Upper/Late Callovian. In the Tethys domain, the Callovian encompasses six ammonite biozones:
Palaeogeography [edit]
During the Callovian, Europe was an Archipelago of a dozen or so large islands. Between them were extensive areas of continental shelf. Consequently, there are shallow marine Callovian deposits in Russia and from Belarus, through Poland and Germany, into France and eastern Spain and much of England. Around the former island coasts are frequently, land-derived sediments. These are to be found, for example, in western Scotland.[2]
The Louann Salt and the southern Campeche Salt of the Gulf of Mexico are thought to have formed by an embayment of the Pacific Ocean across modern-day Mexico.[3]
Palaeontology [edit]
Crocodylomorphs [edit]
†Ornithischians [edit]
| Ornithischia of the Callovian |
| Taxa |
Presence |
Location |
Description |
Images |
| Agilisaurus |
|
Dashanpu Formation, Sichuan, China |
A 4-foot-long (1.2 m) bipedal herbivore that was built for speed. It was discovered in one of China's many Callovian deposits. |
|
| Callovosaurus |
|
England |
A primitive camptosaurid iguanodont, estimated to have been 3.5 meters long |
| Ferganocephale |
|
Kyrgyzstan |
Possibly an early pachycephalosaurid |
Hexinlusaurus
- Hexinlusaurus multidens
|
Bathonian to Callovian |
Lower Shaximiao Formation, Sichuan, China |
A small ornithischian dinosaur distinguished from all other basal ornithischians by a single autapomorphy, the presence of a marked concavity that extends over the lateral surface of the postorbital. |
†Plesiosaurs [edit]
†Sauropods [edit]
†Stegosauria [edit]
| Stegosaurs of the Callovian |
| Taxa |
Presence |
Location |
Description |
Images |
| Huayangosaurus |
Bathonian to Callovian |
Lower Shaximiao Formation, Sichuan, China |
A 4.5 meters in length quadrupedal herbivore with a small skull and a spiked tail. Bore the distinctive double row of plates, rising vertically along its arched back, of all the stegosaurians and two pairs of long spikes extending horizontally near the end of its tail |
|
| Lexovisaurus |
|
Lisieux, France; Northern England |
Traditionally, Lexovisaurus was depicted as having either large spines over the hips or shoulders, with a selection of flat plates and round pointed spines that ran along the back and tail. It was probably about 5 m long. |
| Loricatosaurus |
|
France; England |
Known from remains previously assigned to Lexovisaurus. |
Theropods [edit]
†Ammonitida [edit]
Members of the Order Ammonitida are known as ammonitic ammonites. They are distinguished primarily by their suture lines. In ammonitic suture patterns, the lobes and saddles are much subdivided (fluted) and subdivisions are usually rounded instead of saw-toothed. Ammonoids of this type are the most important species from a biostratigraphical point of view. This suture type is characteristic of Jurassic and Cretaceous ammonoids but extends back all the way to the Permian.
†Belemnites [edit]
| Belemnites of the Callovian |
| Taxa |
Presence |
Location |
Description |
Images |
| Produvalia |
|
|
|
Callovian belemnite from the Zohar Formation, northern Israel
|
Nautiloids [edit]
| Nautiloids of the Callovian |
| Taxa |
Presence |
Location |
Description |
Images |
| Somalinautilus |
|
|
|
An illustration of a variety of fossil nautiloids.
|
Neocoleoids [edit]
References [edit]
Literature [edit]
- Elmi, S. & Babin, C.; 2002: Histoire de la Terre, Dunod, Paris (2nd ed.), ISBN 2-10-006631-5. (French)
- Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
- d'Orbigny, A.C.V.M.D.; 1842: Paléontologie française. 1. Terrains oolitiques ou jurassiques. 642 p, Bertrand, Paris. (French)
External links [edit]
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In horizontal bars are eras; in left column are periods; right column: bold are epochs; not bold not italic are ages; italic are chrons:
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kya = thousands years ago. Mya = millions years ago. * Not officially recognized by the I.C.S.
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