Dimetrodon (; meaning "two measures of teeth") was a predatory synapsid genus that flourished during the Permian period, living between 280–265 million years ago (during the Artinskian to Capitanian stages).
As a synapsid it was more closely related to mammals than to true reptiles such as lizards and snakes. It is classified as a pelycosaur. Fossils of Dimetrodon have been found in North America and Europe. Dimetrodon had a sail on its back, which is thought to have been used for regulating body temperature, or for display.
The structure of the bones indicate that it was cold-blooded and had low metabolism . There are few channels in the bones, which indicates limited circulation. For proper metabolism, Dimetrodon needed external heat. The growth pattern of Dimetrodon is unclear. Analysis based on the length and ossification of the thigh, the ulna and the humerus, shows a poor correlation between the size and relative age of individuals. There was a difference in habitat between juveniles and adults in Dimetrodon. Younger animals lived mainly in habitats with plenty of shelter, such as swamps and reed-lined banks. The adults preferred the open areas of flood plains. This is the finding of fossils from the Wichita Group of Texas. The length of the upper arm and thigh, the main measure that was used to distinguish between young and adult specimens, were examined and it was determined what type of sediment the fossils occurred. A similar difference in distribution between young and adult specimens, was also found for Ophiacodon and Eryops and is also known from modern crocodiles and water turtles.
In a 2001 study on the biomechanics of the dinosaur Albertosaurus's teeth, William L. Abler observed that examined Dimetrodon teeth possessed serrations so fine they resembled a crack in the tooth. Though Albertosaurus had similar serrations, the base of each serration included a round void which would have functioned to distribute force over a larger surface area. These voids, termed an ampulla, would hinder the ability of the "crack" formed by the serration to propagate through the tooth. Dimetrodon was found to lack adaptations for preventing "crack" propagation.
Many suggestions have been made about the function of the sail; as camouflage among reeds while it waited for prey, for sexual display, or literally as a sail while swimming. Romer and Price first suggested that it served a mechanical function and strengthened the backbone, but Romer later realized that the sail had evolved with features strongly suggesting an early attempt at temperature regulation. The fact that these spines are present in both Dimetrodon and Edaphosaurus, two animals in similar geological periods, would suggest that the spines had a significant value in the survival as result of environmental factors. In a study of the relationship between body temperature and blood pressure, Rodbard analyzed the evolution of thermoregulation, which he thought was a one possible function of the sails of Dimetrodon and Edaphosaurus. The spines of Dimetrodon have grooves on the base that were presumably ingested by blood vessels and thus ensured good bloodflow through the skin of the sail. The theory is that Dimetrodon was active in the early morning when the sun rose. The sail would be pointed towards the sun and would absorb heat allowing rapid warming. This allowed Dimetrodon to hunt at a time when other animals were not sufficiently warmed up and were slow. The sail increased body surface area by 50%. According to calculations by Bramwell Fellgett, it took a Dimetrodon approximately one and a half hours for its body temperature to go from A study by Haack concluded that warming was slower than previously thought and that the process probably took four hours. In order to cool its body in the hot midday sun, Dimetrodon turned its sail away from the sun, causing the heat to drain. The rapid warming using the sail give Dimetrodon an edge over larger animals, weighing over 55 kg. Smaller animals had higher body surface-to-mass ratio, making them hotter than Dimetrodon. The prey of Dimetrodon would therefore have been mostly large animals like Diadectes, Eryops and Ophiacodon. The changing climate during the Permian period, when the temperature increased, is a possible reason for the extinction of Dimetrodon since the sail meant no benefit over other animals and was rather a disadvantage due to its fragility.
The significance of this classification of Dimetrodon depends on the system used. In the classical Linnaeïsche system, it belongs to the genus order Pelycosauria. Since this classification, the Therapsida and mammals traditionally been placed in the order Pelycosauria, this order is in fact paraphyletic as not all descendants belong to it. Not only the order as a whole is paraphyletic but the family within that order which contains the ancestor of the later therapsiden and mammals. Now it is the family Sphenacodontidae to which Dimetrodon belongs.
In the cladistic system, only monophyletic groups are used: that is taxa that include all the descendants. The monophyletic group that Dimetrodon belongs to also includes close relatives Ctenospondylus, Neosaurus, Secodontosaurus, Sphenacodon and Steppesaurus. Within Sphenacodontidae Secodontosaurus is the closest relative of Dimetrodon. The Sphenacodontidae is classified, together with Tetraceratops and Therapsida (which now includes the mammals) in the clade Sphenacodontoidea. The Sphenacodontoidea together with a few basal (bottom the tree upright) forms Haptodus the clade Sphenacodontia.
Many species have been described by Edward Drinker Cope during his expeditions in 1880. Romer Alfred Sherman described a few species in the 1930s and 1940s. Most of the type specimens from the collection of which Cope based his descriptions were not released from the matrix. Reassessment after his death led to different conclusions on these specimens, including on the construction of the skull. The status of some of the species described by Cope is questionable, namely D. fritillus, D. gigas, D. incisivus, D. rectiformis and D. semiradicatus. There is a broad subdivision into species with a long skull from the Early Permian and species with a short head from the later parts of the Permian.
Category:Permian synapsids Category:Prehistoric synapsids of Europe Category:Prehistoric synapsids of North America Category:Sphenacodonts Category:Transitional fossil
ar:ديميترودون br:Dimetrodon bg:Диметродон ca:Dimetrodon cs:Dimetrodon da:Dimetrodon de:Dimetrodon el:Διμετρόδοντας es:Dimetrodon fa:دیمترودون fr:Dimétrodon ko:디메트로돈 hr:Dimetrodon id:Dimetrodon it:Dimetrodon he:דימטרודון jv:Dimetrodon ka:დიმეტროდონი hu:Dimetrodon ml:ഡൈമെട്രോഡോൺ nl:Dimetrodon ja:ディメトロドン no:Dimetrodon pl:Dimetrodon pt:Dimetrodon ro:Dimetrodon ru:Диметродон simple:Dimetrodon sk:Dimetrodon sl:Dimetrodon sr:Диметредон fi:Dimetrodon sv:Dimetrodon vi:Dimetrodon zh:异齿龙This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
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