Temporal range: Middle Triassic to Upper Cretaceous
Mary Anning was the first to discovere a plesiosaur. She found it on the 'Jurassic Coast' of Dorset, England in the winter of 1820-21. The fossil was missing its skull, but in 1823 she found another one, this time complete with its skull. The name Plesiosaurus was given to it by the Rev. William Conybeare.
The earliest plesiosaur remains are from the Middle Triassic period,p128 and the group was important through the Jurassic and Cretaceous. They had two large pairs of paddles, short tails, short or long necks, and broad bodies. They died out at the K/T extinction event, 65 million years ago.
Description[change | change source]
Plesiosaurs had many bones in their flippers, making them flexible. No modern animal has this four-paddle anatomy: modern turtles use their forelimbs for swimming. They were mainly piscivorous (fish-eaters).
Pliosaurs[change | change source]
The pliosaurs were a group of mostly large submarine predators with short necks and large heads. Their sizes ranged from two to 15 metres, and they were predators of large fish and other reptiles. Their streamlined body shape suggests they swam and ate under water.
Long-necked plesiosaurs[change | change source]
There were three families of long-necked plesiosaurs, who evidently had a different life-style from the pliosaurs. It was suggested by D.M.S. Watson that their method was as surface swimmers, mostly eating with their head above water, darting down to snatch smaller fish which were feeding on plankton. It is hard to see the benefit of a long neck under water; aquatic mammals operating under water all have a streamlined torpedo-shape, as did pliosaurs and ichthyosaurs. All the longer-necked familiers were, from the setting of the teeth and jaws, eaters of small fish. However, some at least were bottom-feeders, consuming various prey. Digestion of shellfish was aided by gastroliths.
- Plesiosaurids: neck not so long as the other two families, and not so flexible: a more general all-round plesiosaur. Head of medium size, neck fairly thick and strong, up to 30 vertebrae.
- Cryptoclidids: longer necks, with more than 30 vertebrae.
- Elasmosaurids: very long necks; some later forms have as many as 76 cervical (neck) vertebrae and quite small skulls.p30 Watson and Alexander's ideas apply especially to this group.
Gastroliths[change | change source]
Plesiosaurs have been found with fossils of belemnites (squid-like animals), and ammonites (giant nautilus-like molluscs) associated with their stomachs. But plesiosaurs could not crack shells. Instead, they probably swallowed them whole. In the belly of a plesiosaur were "stomach stones", which are called gastroliths. These stones moved around in the plesiosaur's stomach and cracked or crushed the shells of the animals it ate. One plesiosaur fossil found in South Dakota had 253 gatroliths weighing a total of 29 pounds.
Live birth?[change | change source]
Live birth has been proved for ichthyosaurs, but is uncertain for plesiosaurs.
References[change | change source]
|Wikispecies has information on: Plesiosauria.|
- Benton M.J. 1990. The reign of the reptiles. Quarto N.Y.
- Carroll R.L. 1988. Vertebrate paleontology and evolution. Freeman N.Y.
- Other classifications are possible: O'Keefe F.R. 2001. A cladistic analysis and taxonomic revision of the Plesiosauria (Reptilia: Sauropterygia); Acta Zool. Fennica 213: 1-63.
- Watson D.M.S. 1951. Palaeontology and modern biology. Yale, CT.
- Watson D.M.S. 1958. Studies on fossil vertebrates. London.
- Alexander, R. McNeill 1989. Dynamics of dinosaurs and other extinct giants. Columbia N.Y. p137
- BBC NEWS | Science/Nature | Plesiosaur bottom-feeding shown
- Benton M.J. 2004. Vertebrate palaeontology. 3rd ed, Blackwell, Oxford.
- Hiller N. Mannering A.A. Jones C.M. Cruickshank A.R.I. 2005. The nature of Mauisaurus haasti Hector, 1874 (Reptilia: Plesiosauria). Journal of Vertebrate Paleontology 25:588-601.
- Everhart, M.J. 2005. "Gastroliths associated with plesiosaur remains in the Sharon Springs Member (Late Cretaceous) of the Pierre Shale, Western Kansas" on-line, updated from article in Kansas Acad. Sci. Trans. 103(1-2):58-69