Pliensbachian

The Pliensbachian is an age of the geologic timescale and stage in the stratigraphic column. It is part of the Early or Lower Jurassic epoch or series and spans the time between 190.8 ± 1.5 Ma and 182.7 ± 1.5 Ma (million years ago).[3] The Pliensbachian is preceded by the Sinemurian and followed by the Toarcian.[4]

Pliensbachian
190.8 ± 1.0 – 182.7 ± 0.7 Ma
Chronology
Key events in the Jurassic
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-190 
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how to approximate the timescale of key Jurassic events.
Vertical axis: millions of years ago.
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFAD of the Ammonite species Bifericeras donovani and genus Apoderoceras
Lower boundary GSSPRobin Hood's Bay, Yorkshire, England, UK
54.4069°N 0.4975°W / 54.4069; -0.4975
GSSP ratifiedMarch 2005[1]
Upper boundary definitionPeniche, Portugal
Upper boundary GSSPFAD of the Ammonite D. (E.) simplex
39.3708°N 9.3853°W / 39.3708; -9.3853
GSSP ratified2014[2]

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.

Stratigraphic definitions

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).[5]

The top of the Pliensbachian (the base of the Toarcian stage) is at the first appearance of ammonite genus Eodactylites.

Biostratigraphy

Pleuroceras spinatum Museum of Toulouse

The Pliensbachian contains five ammonite biozones in the boreal domain:

In the Tethys domain, the Pliensbachian contains six biozones:

Palaeontology

Amphibians

Amphibians of the Pliensbachian
Taxa Presence Location Description Images
Pliensbachian-Toarcian Evergreen Formation, Australia

Crocodylomorpha

Crocodylomorphs of the Pliensbachian
Taxa Presence Location Description Images
Pliensbachian-Toarcian Kayenta Formation, Arizona

†Ichthyosaurs

Ichthyosaurs of the Pliensbachian
Taxa Presence Location Description Images
Europe
Hettangian to Toarcian All over Europe An ichthyosaur that exceeded 12 metres (39 ft) in length

†Plesiosaurs

Plesiosaurs of the Pliensbachian
Taxa Presence Location Description Images
Calcaire à Bélemnites, France A moderate-sized pliosaurid.
Early Pliensbachian Westphalia, Germany A basal plesiosauroid, possible a microcleidid.

Ornithischians

Ornithischians of the Pliensbachian
Taxa Presence Location Description Images
Lower Lufeng Formation, Yunnan, China A dubious basal thyreophoran.

†Sauropodomorphs

Sauropodomorphs of the Pliensbachian
Taxa Presence Location Description Images
San Juan County, Utah A basal sauropodiform.

Theropods

Theropods of the Pliensbachian
Taxa Presence Location Description Images
Hettangian to Pliensbachian Elliot Formation, South Africa The species was a small to medium-sized, lightly built, ground-dwelling, bipedal carnivore, that could grow up to 3 m (9.8 ft) long. It was formerly called Syntarsus, but that name was already taken by a beetle, and was subsequently given the name Megapnosaurus though many subsequent studies have classified it in the genus Coelophysis.
Sinemurian to Pliensbachian Hanson Formation, Antarctica A dilophosaurid. About 7 meters (23 feet) long with a high, narrow skull and a peculiar nasal crest just over the eyes.
Sinemurian to Pliensbachian Arizona, USA 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.
Pliensbachian Kayenta Formation, Arizona, USA A possible tetanuran originally assigned to the coelophysoid Syntarsus kayentakatae (now Megapnosaurus kayentakatae or Coelophysis kayentakatae). The holotype specimen is a juvenile and would have stood about 0.5 metres (1.6 ft) high at the hip. The adult size of Kayentavenator is unknown).
Pliensbachian to Toarcian Navajo Sandstone, Arizona, USA Segisaurus was small coelophysoid theropod dinosaur and probably a close relative of Procompsognathus.

References

Notes

  1. Meister, Christian; Aberhan, Martin; Blau, Joachim; Dommergues, Jean-Louis; Feist-Burkhardt, Susanne; Hailwood, Ernie; Hart, Malcolm; Hesselbo, Stephen; Hounslow, Mark; Hylton, Mark; Martin, Nicol; Page, Kevin; Price, Greg (June 2006). "The Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic), Wine Haven, Yorkshire, UK". Episodes. 29 (2): 93–106. doi:10.18814/epiiugs/2006/v29i2/003. Retrieved 23 December 2020.
  2. da Rocha, Rogério Bordalo; Mattioli, Emanuela; Duarte, Luís Vítor; Pittet, Bernard; Elmi, Serge; Mouterde, René; Cabral, Maria Cristina; Comas-Rengifo, Maria José; Gómez, Juan José; Goy, António; Hesselbo, Stephen P.; Jenkyns, Hugh C.; Littler, Kate; Mailliot, Samuel; Veiga de Oliveira, Luiz Carlos; Osete, Maria Luisa; Nicola, Perilli; Pinto, Susana; Ruget, Christiane; Suan, Guillaume (September 2016). "Base of the Toarcian Stage of the Lower Jurassic defined by the Global Boundary Stratotype Section and Point (GSSP) at the Peniche section (Portugal)". Episodes. 39 (3): 460–481. doi:10.18814/epiiugs/2016/v39i3/99741. Retrieved 29 August 2020.
  3. Benton, Michael J. (2012). Prehistoric Life. Edinburgh, Scotland: Dorling Kindersley. pp. 44–45. ISBN 978-0-7566-9910-9.
  4. See Gradstein et al. (2004) for a detailed geologic timescale
  5. Meister et al. (2006)

Literature

  • Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
  • Howart, M.K.; 2002: The Lower Lias of Robin Hood's Bay, Yorkshire, and the work of Leslie Bairstow, Bulletin of the Natural History Museum. Geology Series 58, p. 81–152, Cambridge University Press, The Natural History Museum, (abstract)
  • Meister, C.; Aberhan, M.; Blau, J.; Dommergues, J.-L.; Feist-Burkhardt, S.; Hailwood, E.A.; Hart, M.; Hesselbo, S.P.; Hounslow, M.W.; Hylton, M.; Morton, N.; Page, K & Price, G.D.; 2006: The Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic), Wine Haven, Yorkshire, UK, Episodes 29(2), pp. 93–106.
  • Oppel, C.A.; 1856-1858: Die Juraformation Englands, Frankreichs und des südwestlichen Deutschlands: nach ihren einzelnen Gliedern engetheilt und verglichen, 857 pp., Ebner & Seubert, Stuttgart. (in German)
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