Named By: Edward Drinker Cope - 1868.
Classification: Chordata, Reptilia, Sauropterygia, Plesiosauria, Elasmosauridae.
Species: E. platyurus (type).
Size: Upper size of up to 13-14 meters long.
Known locations: USA, particularly associated with Kansas - Pierre Shale.
Time period: Campanian of the Cretaceous.
Fossil representation: Many specimens.
Elasmosaurus is one of the best known plesiosaurs
the world, and
is the type genus for the Elasmosauridae. This group is noted for
having particularly long necks, proportionately even longer than the
more standard plesiosaurs. These long necks are composed of a large
number of cervical vertebrae that in Elasmosaurus
more than other plesiosaurs including fellow elasmosaurids. The
sheer number of vertebrae not only extend the length of the neck but
also provide greater flexibility for fine control of the head,
although very early reconstructions of Elasmosaurus
being able to coil
its neck like a snake are today considered to be very inaccurate and
impossible for a living Elasmosaurus to do.
Instead the neck would
have been held quite straight when resting with sideward movements
only occurring when necessary.
It was the long neck of Elasmosaurus that was key to its feeding method. All Elasmosaurus would have to do was swim up to a shoal of fish, possibly from below so that it could hide its body in the slightly darker depths, and use its neck to dart its head in and pluck out a mouthful of fish. Approaching prey like a shoal of fish from below would also silhouette themselves against the brighter surface water, making them easier to define as well as removing the defence method of flashing light off their shiny scales to confuse predators as they turned and swam through the water. Such a method would have been a reasonably efficient form of feeding as Elasmosaurus would just have to move its head and neck and not waste energy swimming after fast moving individuals.
Key to prey capture were the long and thin teeth that protruded from the mouth of Elasmosaurus. These intermeshed together so that when a fish was caught between the jaws it was impaled upon the teeth so that it could not wriggle free and escape. This kind of dentition is common among other elasmosaurids as well as other piscivorous (fish eating) animals such as skim feeding pterosaurs. A defining characteristic of Elasmosaurus is the fact that it has six teeth in each premaxilla. Because the teeth of Elasmosaurus were adapted for prey capture rather than biting clean through flesh, prey would need to have been swallowed whole. Gastroliths have been found in association to Elasmosaurus remains and its thought that the grinding action of these stones in its gut tenderised food for easier digestion.
Elasmosaurus probably was not a fast swimmer, although if it used stalking tactics to approach its prey from below it would not need to be. The flipper-like limbs were rigid and well suited for providing efficient locomotion through the water. Skeletal elements of the main body such as the pectoral girdles were also well adapted to provide efficient musculature support for the flippers so that that Elasmosaurus could paddle itself through the water with ease.
While Elasmosaurus was beautifully adapted for an aquatic life, the price of these adaptations is that Elasmosaurus would have almost certainly been restricted to the marine environment. Because the paddle-shaped limbs were so stiff they would at best been only just better than useless for pushing its body along. Even when if Elasmosaurus was ever active in the shallows, it would still need to have kept its body totally immersed so that the water could support its body weight.
More ‘classic’ depictions of Elasmosaurus shooting its neck out of the water are also unlikely as the longer the neck got, the more body tissue such as bone and muscle was used to make up the neck meaning more weight was added to it. More weight means that stronger muscles would have been needed to support the neck when out of the water, and study of the cervical vertebrae where the muscles attach indicates that Elasmosaurus just did not have the muscles to move its neck when it did not have water to support the weight. Instead the muscles were only strong enough to provide basic neck movements, which would be all that was required of them when the neck was immersed in water.
While no hard evidence currently exists for Elasmosaurus either laying eggs on land or giving birth to live young, most palaeontologists believe that Elasmosaurus, and similar marine reptiles would have given birth to live young. The precedent is known to exist for other marine reptiles like the ichthyosaurs and nothosaurs as far abck as the Triassic and given the problems that Elasmosaurus would have had just moving its body if it ever found itself out of the water make it extremely unlikely it could have laid eggs on land. Today marine reptiles such as sea snakes can also be observed giving birth to live young which indicates that as a group the reptiles are capable of adapting to new methods to thrive in different environments.
reconstruction and classification
The palaeontological history of Elasmosaurus is a turbulent one. First discovered in 1868 by Dr. Theophilus Turner, the fossils were sent to Edward Drinker Cope for study and identification. Cope had never assembled a plesiosaur before but he had the idea the large number of vertebrae mostly belonged in the tail which resulted in a long tail and short neck. To Cope this made sense as the proportions were similar to those of many modern lizards that also have short necks and incredibly long tails.
The next part of this story is a little hazy for exact details, but the popular retelling of it has Othniel Charles Marsh realising that the head was on the wrong end and ridiculed Cope for placing it in the wrong place. However it seems that it was actually Joseph Leidy who pointed this error out in a meeting in 1870, although given the animosity already between Marsh and Cope at the time, its quite possible that Marsh continued to use this case as an example to discredit Cope’s work, hence the confusion. It is this criticism that poured fuel onto the already burning fire that would become the ‘bone wars’, a fierce rivalry between Cope and Marsh that saw them trying to out compete one another in terms of discovering new species.
Since its naming back in 1868 many new specimens of Elasmosaurus have been recovered, and many of these were assigned their own species within the genus. Many of these species continue to be mentioned despite the fact that in 1999 the palaeontologist Ken Carpenter conducted a study of the known Elasmosaurus fossils at this point and found that some of these did not belong as individual species, and some of them even represented different genera. Today most palaeontologists only recognise the original type species, E. platyurus, as being valid.
- On a new large enaliosaur. - The American Journal of Science, series 2 46(137):263-264. - E. D. Cope - 1868.
- Remarks on a new enaliosaurian, Elasmosaurus platyurus. - Proceedings of the Academy of Natural Sciences of Philadelphia. 20: 92–93. - E. D. Cope - 1868.
- Remarks on Elasmosaurus platyurus. - Proceedings of the Academy of Natural Sciences of Philadelphia. 22: 9–10. - J. Liedy - 1870.
- North American plesiosaurs Elasmosaurus, Cimoliasaurus, and Polycotylus. - American Journal of Science. 4. 21 (123): 221–236. - S. W. Williston - 1906.
- Elasmosaurus platyurus and a page from the Cope-Marsh war. - Discovery. 17 (2): 25–27.- G. W. Storrs - 1984.
- Revision of North American elasmosaurs from the Cretaceous of the western interior. - Paludicola. 2 (2): 148–173. - K. Carpenter - 1999.
- Bonehead mistakes: The background in scientific literature and illustrations for Edward Drinker Cope's first restoration of Elasmosaurus platyurus. - Proceedings of the Academy of Natural Sciences of Philadelphia. 152 (1): 215–240. - J. P. Davidson - 2002.
- Elasmosaurid remains from the Pierre Shale (Upper Cretaceous) of western Kansas. Possible missing elements of the type specimen of Elasmosaurus platyurus Cope 1868?. - PalArch's Journal of Vertebrate Palaeontology. 4 (3). - M. J. Everhart - 2005.
- Postscript to Everhart, M.J. 2005. "Elasmosaurid remains from the Pierre Shale (Upper Cretaceous) of western Kansas. Possible missing elements of the type specimen of Elasmosaurus platyurus Cope 1868?" – PalArch's Journal of Vertebrate Palaeontology 4, 3: 19–32. - PalArch's Journal of Vertebrate Palaeontology. 2 (1). - L. F. Noč & M. Gómez–Pérez - 2007.
- Revised Vertebral Count in the "Longest-Necked Vertebrate" Elasmosaurus platyurus Cope 1868, and Clarification of the Cervical-Dorsal Transition in Plesiosauria. - PLOS ONE. 8 (8). - S. Sachs, B. P. Kear & M. Everhart - 2013.
- Captain Theophilus H. Turner and the Unlikely Discovery of Elasmosaurus platyurus. - Transactions of the Kansas Academy of Science. 120 (3–4): 233–246. - M. J. Everhart - 2017.
- Scattered and Shattered: A Brief History of the Early Methods of Digging, Preserving and Transporting Kansas Fossils. - Transactions of the Kansas Academy of Science. 120 (3–4): 247–258. - J. P. Davidson & M. J. Everhart - 2017.
- The Mystery of Elasmosaurus platyurus Cope 1868 – Where is the rest of the type specimen?. - Transactions of the Kansas Academy of Science. 121 (3–4): 335–345. - J. P. Davidson & M. J. Everhart - 2018.