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''Dromomeron'' (meaning "running femur") is a genus of lagerpetonid dinosauromorph archosaur containing species known from Late Triassic-age rocks of the Southwestern United States and northwestern Argentina. It is known from partial remains, largely from the hindlimbs, which indicate an animal with an overall length of less than 1.0 meters (3.3 ft).〔Estimate after the scale diagram at (the article's press fact sheet ).〕 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.〔 ==Discovery and history== ''Dromomeron'' and type species ''D. romeri'' is based on GR 218, a complete left thigh bone from the Hayden Quarry at Ghost Ranch, New Mexico. The rocks there are in the lower portion of the Petrified Forest Member of the Chinle Formation, and are Norian in age. Additional hindlimb bones, some probably from the same individual, are also known,〔 and a partial skeleton has been recovered from Hayden Quarry, but has not yet been fully prepared. A few other specimens have been recovered from nearby localities, including the Snyder Quarry.〔 The bones of ''Dromomeron'' are most similar to those of the older dinosauromorph ''Lagerpeton'',〔 and the two animals have been classified together in a clade Lagerpetonidae.〔 The species name ''romeri'' honors influential 20th century vertebrate paleontologist Alfred Sherwood Romer.〔 Also found at the 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 the basal theropod ''Tawa''. Finding the remains of four types of dinosaurs 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.〔 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. These have been assigned to second species ''D. gregorii'', named in 2009.〔 ''D. gregorii'', named for Joseph T. Gregory, is based on TMM 31100–1306, a right femur (thigh bone) from the Otis Chalk Quarry, Colorado City Formation, (Dockum Group), near Otis Chalk, Texas. Several other limb bones from the quarry, and a partial femur (thigh bone) from the ''Placerias'' Quarry of eastern Arizona have been assigned to this species. The rocks ''D. gregorii'' is known from are older than those ''D. romeri'' has been found in. As with ''D. romeri'', the Otis Chalk Quarry also has at least one specimen of the early dinosaur ''Chindesaurus''.〔 Third species, ''D. gigas'', was described by Martínez ''et al''. (2015) on the basis of fossils recovered from the Norian Quebrada del Barro Formation in northwestern Argentina. Based on the study of the overlapping material of ''Dromomeron'' and ''Tawa hallae'', Christopher Bennett proposed that the two taxa were conspecific, forming a single growth series of ''Dromomeron''. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Dromomeron」の詳細全文を読む スポンサード リンク
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