Mecistotrachelos
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Mecistotrachelos
''Mecistotrachelos'' is an extinct genus of gliding reptile believed to be an archosauromorph, distantly related to crocodylians and dinosaurs. The type and only known species is ''M. apeoros''. This specific name translates to "soaring longest neck", in reference to its gliding habits and long neck. This superficially lizard-like animal was able to spread its lengthened ribs and glide on wing-like membranes. ''Mecistotrachelos'' had a much longer neck than other gliding reptiles of the Triassic such as ''Icarosaurus'' and '' Kuehneosaurus''. It was probably an arboreal insectivore. Discovery ''Mecistotrachelos'' is known from several fossil specimens excavated from the Solite quarry from the Cow Branch Formation on the Virginia-North Carolina border. However, only two of these have been formally described in a scientific journal. The first fossil was found in 1994 and the second fossil eight years later by Nick Fraser, a vertebrate paleontologist at the Virginia Museum of N ...
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Mecistotrachelos Holotype Slab
''Mecistotrachelos'' is an extinction, extinct genus of gliding reptile believed to be an Archosauromorpha, archosauromorph, distantly related to Crocodilia, crocodylians and dinosaurs. The type and only known species is ''M. apeoros''. This Specific name (zoology), specific name translates to "soaring longest neck", in reference to its gliding habits and long neck. This superficially lizard-like animal was able to spread its lengthened ribs and glide on wing-like membranes. ''Mecistotrachelos'' had a much longer neck than other gliding reptiles of the Triassic such as ''Icarosaurus'' and ''Kuehneosaurus''. It was probably an arboreal insectivore. Discovery ''Mecistotrachelos'' is known from several fossil specimens excavated from the Solite quarry from the Cow Branch Formation on the Virginia-North Carolina border. However, only two of these have been formally described in a scientific journal. The first fossil was found in 1994 and the second fossil eight years later by Nick F ...
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Cow Branch Formation
The Cow Branch Formation is a Late Triassic (Carnian to Norian, or Tuvalian in the regional stratigraphy) geologic formation in the eastern United States.Cow Branch Formation
at .org
Indeterminate fossil tracks have been reported from the formation.Weishampel et al., 2004, pp.517-607


Fossil content

The following fossils have been reported from the formation: ;Reptiles * ''
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Archosauromorpha
Archosauromorpha (Greek for "ruling lizard forms") is a clade of diapsid reptiles containing all reptiles more closely related to archosaurs (such as crocodilians and dinosaurs, including birds) rather than lepidosaurs (such as tuataras, lizards, and snakes). Archosauromorphs first appeared during the late Middle Permian or Late Permian, though they became much more common and diverse during the Triassic period. Although Archosauromorpha was first named in 1946, its membership did not become well-established until the 1980s. Currently Archosauromorpha encompasses four main groups of reptiles: the stocky, herbivorous allokotosaurs and rhynchosaurs, the hugely diverse Archosauriformes, and a polyphyletic grouping of various long-necked reptiles including ''Protorosaurus'', tanystropheids, and ''Prolacerta''. Other groups including pantestudines (turtles and their extinct relatives) and the semiaquatic choristoderes have also been placed in Archosauromorpha by some authors. A ...
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Late Triassic
The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series (stratigraphy), series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Geologic time scale, Ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich August von Namoh, Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', t ...
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Virginia Museum Of Natural History
The Virginia Museum of Natural History is the state's natural history museum located in Martinsville, Virginia founded in 1984. The museum has several different award-winning publications, is affiliated with the Smithsonian Institution, and has more than 22 million items. This includes the first intact stromatolite head ever found in Virginia, which is one of the largest complete 'heads' in the world, at over 5 feet in diameter and weighing over 2 tons. History The Virginia Museum of Natural History was founded in 1984 as The Boaz Foundation, named after Dr. Noel T. Boaz, Founding Director, along with co-founder Dr. Dorothy Dechant Boaz. The museum was founded as a private institution, but on June 2, 1985, the museum opened to the public with the new and current name. Three years later in 1988, local and statewide leaders such as Speaker of the Virginia General Assembly, A. L. Philpott, helped the museum become an agency of the Commonwealth of Virginia. The first meeting of th ...
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Vertebra
The spinal column, a defining synapomorphy shared by nearly all vertebrates,Hagfish are believed to have secondarily lost their spinal column is a moderately flexible series of vertebrae (singular vertebra), each constituting a characteristic irregular bone whose complex structure is composed primarily of bone, and secondarily of hyaline cartilage. They show variation in the proportion contributed by these two tissue types; such variations correlate on one hand with the cerebral/caudal rank (i.e., location within the backbone), and on the other with phylogenetic differences among the vertebrate taxa. The basic configuration of a vertebra varies, but the bone is its ''body'', with the central part of the body constituting the ''centrum''. The upper (closer to) and lower (further from), respectively, the cranium and its central nervous system surfaces of the vertebra body support attachment to the intervertebral discs. The posterior part of a vertebra forms a vertebral arch ...
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