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. |
The Pliensbachian is an age of the geologic timescale or stage in the stratigraphic column. It is part of the Early or Lower Jurassic epoch or series and spans the time between 189.6 ± 1.5 Ma and 183 ± 1.5 Ma (million years ago). The Pliensbachian is preceded by the Sinemurian and followed by the Toarcian.[1]
The Pliensbachian ended with the extinction event called the Toarcian turnover. During the Pliensbachian, the middle part of the Lias was deposited in Europe. The Pliensbachian is roughly coeval with the Charmouthian regional stage of North America.
Contents |
The Pliensbachian takes its name from the hamlet of Pliensbach in the community of Zell unter Aichelberg in the Swabian Alb, some 30 km east of Stuttgart in Germany. The name was introduced into scientific literature by German palaeontologist Albert Oppel in 1858.
The base of the Pliensbachian is at the first appearances of the ammonite species Bifericeras donovani and genera Apoderoceras and Gleviceras. The Wine Haven profile near Robin Hood's Bay (Yorkshire, England) has been appointed as global reference profile for the base (GSSP).[2]
The top of the Pliensbachian (the base of the Toarcian stage) is at the first appearance of ammonite genus Eodactylites.
The Pliensbachian contains five ammonite biozones in the boreal domain:
In the Tethys domain, the Pliensbachian contains six biozones:
Ornithischians of the Pliensbachian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
Lower Lufeng Formation, Yunnan, China | A dubious basal thyreophoran | |||
Lower Lufeng Formation, Yunnan, China | Description based on only a partial left mandible with teeth, a dubious basal thyreophoran |
Theropods of the Pliensbachian | ||||
---|---|---|---|---|
Taxa | Presence | Location | Description | Images |
Hanson Formation, Antarctica | The earliest known tetanuran. About 6 to 8 meters (20 to 26 feet) long with a high, narrow skull and a peculiar nasal crest just over the eyes | |||
Sinemurian to Pliensbachian | Arizona, USA; Yunnan, China | Measured around six meters (20 ft) long and may have weighed half a ton. The most distinctive characteristic of Dilophosaurus is the pair of rounded crests on its skull, possibly used for display. |
Jurassic Period | ||
---|---|---|
Lower/Early Jurassic | Middle Jurassic | Upper/Late Jurassic |
Hettangian | Sinemurian Pliensbachian | Toarcian |
Aalenian | Bajocian Bathonian | Callovian |
Oxfordian | Kimmeridgian Tithonian |