Zatrachydidae
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Zatrachydidae
Zatracheidae (sometimes mistakenly spelled Zatrachydidae or Zatrachysdidae) is a family of Late Carboniferous and Early Permian temnospondyl amphibians known from North America and Europe. Zatracheidids are distinguished by lateral (sideways) bony protuberances of the quadratojugal bone of the skull, and a large opening in the snout called the internarial fontanelle (sometimes the internarial fenestra) that is bordered by enlarged premaxillae. The skull is flattened, with small orbits or eye sockets set far back. The opening in the snout may have housed a gland for producing a sticky substance so that prey would adhere to the tongue. If so, this indicates that these animals spent a large part of their time on land. History of study There are three genera of zatracheidids: '' Acanthostomatops'' Kuhn, 1961; '' Dasyceps'' Huxley 1859; and '' Zatrachys'' Cope, 1878. Only ''Dascyeps'' is represented by a species in addition to the type species. The name Zatracheidae was first coin ...
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Zatracheidae
Zatracheidae (sometimes mistakenly spelled Zatrachydidae or Zatrachysdidae) is a family of Late Carboniferous and Early Permian temnospondyli, temnospondyl amphibians known from North America and Europe. Zatracheidids are distinguished by lateral (sideways) bony protuberances of the quadratojugal bone of the skull, and a large opening in the snout called the internarial fontanelle (sometimes the internarial fenestra) that is bordered by enlarged premaxillae. The skull is flattened, with small Orbit (anatomy), orbits or eye sockets set far back. The opening in the snout may have housed a gland for producing a sticky substance so that prey would adhere to the tongue. If so, this indicates that these animals spent a large part of their time on land. History of study There are three genera of zatracheidids: ''Acanthostomatops'' Kuhn, 1961; ''Dasyceps'' Huxley 1859; and ''Zatrachys'' Cope, 1878. Only ''Dascyeps'' is represented by a species in addition to the type species. The name ...
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Zatrachys
''Zatrachys'' is an extinct genus of large and flat-headed zatracheidid temnospondyl from the early Permian of North America. History of study ''Zatrachys'' was named by American paleontologist Edward Drinker Cope in 1878 for the type species, ''Z. serratus'', based on a partial skull from the early Permian of Texas. Additional material has been reported from the early Permian of New Mexico and Oklahoma. Urban et al. (2007) reported material attributed to ''Z. serratus'' from the late Carboniferous and the early Permian of West Virginia. This is the only record of ''Zatrachys'' in the Carboniferous. ''Zatrachys microphthalmus'' is now placed within '' Dasyceps''. Anatomy Like all zatracheidids, ''Zatrachys'' is easily recognized by the presence of a large opening in the snout, the internarial fontanelle or fenestra. Of the three genera of zatracheidids, that of ''Zatrachys'' is the largest, extending as far back as to fully divide the nasals and to partially divide the fro ...
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Temnospondyli
Temnospondyli (from Greek τέμνειν, ''temnein'' 'to cut' and σπόνδυλος, ''spondylos'' 'vertebra') is a diverse order of small to giant tetrapods—often considered primitive amphibians—that flourished worldwide during the Carboniferous, Permian, and Triassic periods. A few species continued into the Jurassic and Cretaceous periods. Fossils have been found on every continent. During about 210 million years of evolutionary history, they adapted to a wide range of habitats, including freshwater, terrestrial, and even coastal marine environments. Their life history is well understood, with fossils known from the larval stage, metamorphosis, and maturity. Most temnospondyls were semiaquatic, although some were almost fully terrestrial, returning to the water only to breed. These temnospondyls were some of the first vertebrates fully adapted to life on land. Although temnospondyls are considered amphibians, many had characteristics, such as scales and armour-like bon ...
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Acanthostomatops
''Acanthostomatops'' is an extinct genus of zatracheidid temnospondyl Temnospondyli (from Greek language, Greek τέμνειν, ''temnein'' 'to cut' and σπόνδυλος, ''spondylos'' 'vertebra') is a diverse order (biology), order of small to giant tetrapods—often considered Labyrinthodontia, primitive amphi ... from the Lower Permian Döhlen Basin of Saxony. History of study ''Acanthostomatops'' was originally named as the type species ''Acanthostoma vorax,'' in 1883. However, the genus name ''Acanthostoma'' was previously used for a polychaete worm back in 1813, and the present name was given in 1961. Detailed descriptions of the taxon were given by Steen & Brough (1937), with an emphasis on the ontogeny of the taxon based on the large sample size given by Boy (1989) and Witzmann & Schoch (2006). Werneburg (1998) described a larval specimen of ''A. vorax'', but this was later proven to be a specimen of the micromelerpetid '' Branchierpeton amblystomum''. Anatomy ...
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Dasyceps
''Dasyceps'' is an extinct genus of zatracheidid temnospondyl from the early Permian of England. History of study ''Dasyceps'' was originally named in 1850 for the type species, ''D. bucklandi'', which honors English paleontologist William Buckland, but under the now defunct genus "''Labyrinthodon''," which is now regarded as a junior synonym of the Triassic capitosaur ''Mastodonsaurus''. The new genus name for the species was created by Thomas Huxley in 1859. A detailed description of the taxon was given in German by the German paleontologist Friedrich von Huene Friedrich von Huene, born Friedrich Richard von Hoinigen, (March 22, 1875 – April 4, 1969) was a German paleontologist who renamed more dinosaurs in the early 20th century than anyone else in Europe. He also made key contributions about v ... in 1910. The most recent description is that of Paton (1975). A second species from Texas, ''D. microphthalmus'', was originally named as a species of ''Zatrachys'' b ...
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Edward Drinker Cope
Edward Drinker Cope (July 28, 1840 – April 12, 1897) was an American zoologist, paleontologist, comparative anatomist, herpetologist, and ichthyologist. Born to a wealthy Quaker family, Cope distinguished himself as a child prodigy interested in science; he published his first scientific paper at the age of 19. Though his father tried to raise Cope as a gentleman farmer, he eventually acquiesced to his son's scientific aspirations. Cope married his cousin and had one child; the family moved from Philadelphia to Haddonfield, New Jersey, although Cope would maintain a residence and museum in Philadelphia in his later years. Cope had little formal scientific training, and he eschewed a teaching position for field work. He made regular trips to the American West, prospecting in the 1870s and 1880s, often as a member of United States Geological Survey teams. A personal feud between Cope and paleontologist Othniel Charles Marsh led to a period of intense fossil-finding competition ...
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Late Carboniferous
Late may refer to: * LATE, an acronym which could stand for: ** Limbic-predominant age-related TDP-43 encephalopathy, a proposed form of dementia ** Local-authority trading enterprise, a New Zealand business law ** Local average treatment effect, a concept in econometrics Music * ''Late'' (album), a 2000 album by The 77s * Late!, a pseudonym used by Dave Grohl on his ''Pocketwatch'' album * Late (rapper), an underground rapper from Wolverhampton * "Late" (song), a song by Blue Angel * "Late", a song by Kanye West from ''Late Registration'' Other * Late (Tonga), an uninhabited volcanic island southwest of Vavau in the kingdom of Tonga * "Late" (''The Handmaid's Tale''), a television episode * LaTe, Oy Laivateollisuus Ab, a defunct shipbuilding company * Late may refer to a person who is Dead See also * * * ''Lates'', a genus of fish in the lates perch family * Later (other) * Tardiness * Tardiness (scheduling) In scheduling, tardiness is a measure of a delay in exe ...
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Cisuralian Extinctions
The Cisuralian is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 272.3 ± 0.5 Mya. The Cisuralian is often synonymous with the informal terms early Permian or lower Permian. It corresponds approximately with the Wolfcampian in southwestern North America. The series saw the appearance of beetles and flies and was a relatively stable warming period of about 21 million years. Name and background The Cisuralian is the first series or epoch of the Permian. The Cisuralian was preceded by the last Pennsylvanian epoch (Gzhelian) and is followed by the Permian Guadalupian Epoch. The name "Cisuralian" was proposed in 1982, and approved by the International Subcommission on Permian Stratigraphy in 1996. The Cisuralian Epoch is named after the western slopes of the Ural Mountain ...
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Pennsylvanian First Appearances
Pennsylvanian may refer to: * A person or thing from Pennsylvania * Pennsylvanian (geology), a geological subperiod of the Carboniferous Period * Pennsylvanian (train), ''Pennsylvanian'' (train), an Amtrak train {{disambiguation ...
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Rhachitomes
Rhachitomi is a group of temnospondyl amphibians that includes all temnospondyls except edopoids and dendrerpetontids. It was established as a clade name by German paleontologist Rainer R. Schoch in 2013, although the name had first been established in 1919 by British paleontologist D. M. S. Watson to encompass an evolutionary grade of temnospondyls leading to the group Stereospondyli. American paleontologist Alfred Romer used the term in a similar sense, grouping most Permian and Triassic temnospondyls under Rhachitomi. A similar name that appeared earlier in the scientific literature is Rachitomi, which was named by American paleontologist Edward Drinker Cope in 1882. Rachitomi was commonly used in the late nineteenth and early twentieth century to include early amphibians such as ''Eryops'' and ''Archegosaurus'' that had rhachitomous vertebrae. Many early tetrapods have vertebrae that are split into two parts below the notochord: a pleurocentrum and an intercentrum. In rhach ...
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Permian Temnospondyls
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids (reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their amphibia ...
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Carboniferous Temnospondyls
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian lineages ...
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