Dromomeron

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Dromomeron
Fossil range: Late Triassic
Hypothetical reconstruction of Dromomeron romeri
Hypothetical reconstruction of Dromomeron romeri
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Sauropsida
Infraclass: Archosauromorpha
(unranked) Ornithodira
Genus: Dromomeron
Irmis et al., 2007
Species

D. romeri Irmis et al., 2007

Dromomeron (meaning "running femur") is a genus of dinosauromorph archosaur from Late Triassic-age Chinle Formation rocks at Ghost Ranch, New Mexico (USA). It is known from partial remains including a thigh bone,[1] belonging to an animal less than 1.0 meters (3.3 ft) long.[2] It is described as most closely related to the earlier Lagerpeton of Argentina, but was found among remains of true dinosaurs like Chindesaurus, indicating that the first dinosaurs did not immediately replace related groups. The species name honors influential 20th century vertebrate paleontologist Alfred Sherwood Romer.[1]

[edit] Discovery and history

Dromomeron is based on GR 218, a complete left thigh bone from the Hayden Quarry at Ghost Ranch. The rocks there are in the lower portion of the Petrified Forest Member of the Chinle Formation, and are Norian in age (between 216 and 203 million years old). Additional hindlimb bones, some probably from the same individual, are also known. These bones are most similar to those of the older dinosauromorph Lagerpeton.[1] Other specimens, from the Chinle Formation of Arizona and a roughly contemporaneous part of the Dockum Group of Texas, also have been assigned to this genus.[3]

Also found at Hayden Quarry are the remains of phytosaurs, aetosaurs, rauisuchians, and several types of dinosaurs and dinosaur relatives, including a Silesaurus-like animal, the herrerasaurid Chindesaurus, and an unnamed coelophysoid theropod. Finding the remains of four types of dinosaurus and dinosaur relatives (including Dromomeron itself) is noteworthy because it shows that dinosaurs did not immediately replace related groups; that some of these groups, like the lagerpetonids, persisted for longer than previously known and diversified; and that dinosaurian replacement may have occurred at different times in different areas.[1]

[edit] References

  1. ^ a b c d Irmis, Randall B.; Nesbitt, Sterling J.; Padian, Kevin; Smith, Nathan D.; Turner, Alan H.; Woody, Daniel; and Downs, Alex (2007). "A Late Triassic dinosauromorph assemblage from New Mexico and the rise of dinosaurs". Science 317: 358–361. doi:10.1126/science.1143325. 
  2. ^ Estimate after the scale diagram at the article's press fact sheet.
  3. ^ Irmis, Randall B.; Nesbitt, Sterling J.; Padian, Kevin; Smith, Nathan D.; Turner, Alan H.; Woody, Daniel; and Downs, Alex (2007). Supporting online material for A Late Triassic dinosauromorph assemblage from New Mexico and the rise of dinosaurs (PDF). Science. DOI:10.1126/science.1143325. Retrieved on 2007-07-22.

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