Temporal range: Permian
|An artist's illustration of Dimetrodon loomisi|
| †Dimetrodon limbatus|
(Cope, 1877) (originally Clepsydrops limbatus)
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 individuals lived mainly in habitats with plenty of shelters, 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. Dimetrodon may have had 'scales' on its belly like that of a rat on its tail.
Dimetrodon has two types of teeth, shearing teeth, and sharp canine teeth. Its name, in fact, means "two measures of teeth". Dimetrodon was one of the first animals with differentiated teeth and the teeth were suitable for killing animals then tearing them to pieces. Dimetrodon has a large skull with a temporal fenestra behind each eye orbit on the lateral surface, a distinguishing feature of the synapsid skull. This made possible new attachment sites for jaw muscles, which could run faster and create mastication. Based on the osteology of the temporal region, the posterior part of the palate and mandible, powerful jaw muscles of Dimetrodon was found to have differentiated. Two groups of muscles have been reconstructed: the adductors and the pterygoids. The adductors were from temporal to the inside of the lower jaw and caused the closing of the jaws. The pterygoids ran from the Pterygoid processes of the sphenoid and the sphenoid bone to the articular, one of the bones in the lower jaw, and caused a backward movement of the mandible. The development of the coronoid process in Dimetrodon compared with other quadrupeds led to an increase in the length of the moment of external muscular and thus greater bite force. The construction of the inner ear and the vestibular system of Dimetrodon were described by Case, but he drew no conclusions about the possible function of these organs. 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.
The sturdy legs of Dimetrodon were spread beside the body. Judging from the construction of the legs, it was a relatively fast and smoothly moving animal, especially compared to its solid build herbivorous relatives. The shape of the hip bones, the hind legs and the joints between the vertebrae can be seen.
The most striking feature of Dimetrodon has been the one-meter long protrusions at the back of the spine, the spinous processes also referred to as spines. This feature is also found on the dinosaur Spinosaurus, as these spines have a wide base and then his long and slender with a pointed tip. It is believed that the spines were connected by a solid skin and thus formed a sail on the back. 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, or for display, 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 survival as a 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 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 blood flow 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 200 kg (440 lb) Dimetrodon approximately one and a half hours for its body temperature to go from 26 to 32 °C (79 to 90 °F) A study by Haack concluded that warming was slower than previously thought and that the process probably took four hours. Therefore 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 gives 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. More recent research supports Haack's findings and leads some scientists to conclude that the sail was an inefficient way to regulate body temperature and makes it more likely that the sail was used for sexual display. 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 genus Dimetrodon currently includes several more or less recognized types:
- D. platensis (Olson, 1962)
- D. booneorum (Romer, 1937)
- D. dollovianus (Cope, 1888)
- D. fritillus (Cope, 1878)
- D. gigas (Cope, 1878)
- D. grandis (Case, 1907)
- D. incisivus (Cope, 1878)
- D. kempae (Romer, 1937)
- D. limbatus (Cope, 1877)
- D. loomisi (Romer, 1937)
- D. macrospondylus (Cope, 1884)
- D. milleri (Romer, 1937)
- D. natalis (Cope, 1877)
- D. occidentalis (Berman, 1977)
- D. platycentrus (Case, 1907)
- D. rectiformis (Cope, 1878)
- D. semiradicatus (Cope, 1881)
- D. teutonis (Berman et al, 2001)
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.
Relationship with modern mammals
As a synapsid, Dimetrodon was distantly related to modern mammals. Synapsids were the first tetrapods to evolve differentiated, or heterodont, teeth. While reptiles barely chew their food, essentially gulping it down, synapsids like Dimetrodon developed teeth to help shear meat into smaller pieces for easier digestion. These "two-measure teeth" eventually gave rise to the various kinds of teeth present in modern mammals.
Fossils are known from the United States (Texas, Oklahoma, New Mexico, Arizona, Utah, and Ohio) and Germany, areas that the first parts of the Permian were part of the supercontinent Euramerica. Most fossil finds are part of lowland ecosystems, during the Permian would have been vast wetlands. In particular, the Red Beds of Texas is an area ofthe great diversity of fossils of Dimetrodon species and other species from the Early Permian. The fossils date from 290 to 270 million years ago, which means it lived from the Cisuralian to the Guadalupian period. Dimetrodon probably developed from a Sphenacodon-like ancestor. The climate of the Late Carboniferous (Pennsylvanaen) and Early Permian (Asse Lien, Sakmarien, Arti Skiing) resulted in warm, humid ecosystems in subtropical and tropical zones, consisting of vast wetland areas. In additio,n there were large ice sheets on the Southern Hemisphere that stretched to about 30° south. The fauna was concentrated in this period therefore in tropical and subtropical zones. Aquatic and semi-aquatic tetrapods dominated, while land predators as Dimetrodon were largely water-fed animals. The Early Permian had a drier and hotter climate where deserts began to develop. This led a climate change causing major extinction of the tetrapods, thus clearing the way for the development of therapsids. Dimetrodon was replaced as an apex predator by carnivores as Biarmosuchia and Dinocephalia.
In popular culture
- Dimetrodon appeared in BBC's Walking with Monsters depicted as an apex predator though being shown in an arid environment when in reality it lived in a more lush and tropical environment. A female mother is shown to be the main character of the second segment of the second episode whilst protecting her eggs.
- Dimetrodon appears in Jurassic World: The Game.
- Dimetrodon itself doesn't appear in the movies, although a statue of Dimetrodon is seen in Benjamin Lockwood's museum in the Lockwood Manor in Jurassic World: Fallen Kingdom.
- Dimetrodon also appeared in the Zoo Tycoon 2 expansion pack Zoo Tycoon 2: Extinct Animals
- A Dimetrodon made a cameo appearance in Don Bluth's The Land Before Time (1988). It based on its outdated lizard-like appearance, and also sported a forked tongue repeatedly sticking it out.
- Dimetrodon appears in ARK: Survival Evolved, where it is one of many creatures that the player can tame.
- Dimetrodon made heavily brief cameos while the sitcom Dinosaurs were on the air.
- The Dimetrodon appears in Toy Story That Time Forgot.
- †Dimetrodon sincillis made a cameo in the Poo-inators
- A cyan auxiliary zord based on the Dimetrodon appeared in Power Rangers: Dino Thunder.
- Journey to the Center of the Earth 1959 played by Rhinoceros Iguanas.