Tapinocephalids
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Tapinocephalids
Tapinocephalidae was an advanced family (biology), family of tapinocephalians. It is defined as the clade containing ''Ulemosaurus'', ''Tapinocaninus'', and the Tapinocephalinae. They are known from both Russia and South Africa. In all probability, the Tapinocephalidae had a worldwide (Pangean) distribution. They flourished briefly during the Wordian and Capitanian ages, radiating into several lineages, existing simultaneously, and differing mainly in details of the skull and, to an even lesser degree, the skeleton. It is not clear how such similar animals could each find their own ecological niche, but such was obviously the case. There is a parallel here with the hadrosaur and ceratopsian dinosaurs of the Late Cretaceous. The cause of their abrupt extinction is not clear, since other smaller animals, and even the pareiasaurs, were not affected. Quite probably, like the extinction of the late Pleistocene megafauna, a number of factors were involved. Description The body is deep ...
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Criocephalosaurus
''Criocephalosaurus'' (Greek for “ram head lizard”) is an extinct genus of tapinocephalian therapsids that lived in Southern Africa during the Guadalupian epoch of the Permian. They are the latest surviving dinocephalians, extending past the Abrahamskraal Formation into the lowermost Poortjie Member of the Teekloof Formation in South Africa. They are also regarded as the most derived of the dinocephalians, alongside ''Tapinocephalus'', and the most abundant in the fossil record. Discovery and naming ''Criocephalus vanderbyli'' was the first discovered species of the genus and was named by Broom in 1928 following discovery of a weathered skull cap by W. Van der Byl at the Abrahamskraal Formation of the Karoo Basin in South Africa. The specimen found was a skull cap featuring the frontals, parietals, postfrontals, and one pre frontal. ''Criocephalus gunyankaensis'' is the second named species of the genus and it was figured from four skull-caps described in 1946 by Boonstra. ...
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Tapinocephalidae - Moschops Capensis
Tapinocephalidae was an advanced family of tapinocephalians. It is defined as the clade containing ''Ulemosaurus'', ''Tapinocaninus'', and the Tapinocephalinae. They are known from both Russia and South Africa. In all probability, the Tapinocephalidae had a worldwide (Pangean) distribution. They flourished briefly during the Wordian and Capitanian ages, radiating into several lineages, existing simultaneously, and differing mainly in details of the skull and, to an even lesser degree, the skeleton. It is not clear how such similar animals could each find their own ecological niche, but such was obviously the case. There is a parallel here with the hadrosaur and ceratopsian dinosaurs of the Late Cretaceous. The cause of their abrupt extinction is not clear, since other smaller animals, and even the pareiasaurs, were not affected. Quite probably, like the extinction of the late Pleistocene megafauna, a number of factors were involved. Description The body is deep and capacious, all ...
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Tapinocaninus
''Tapinocaninus'' (Greek for "humble"- tapino, and "canine"- caninus) is an extinct genus of therapsids in the family Tapinocephalidae, of which it is the most basal member. Only one species is known, ''Tapinocaninus pamelae'' (meaning "Pamela's humble canine"). The species is named in honor of Rubidge's mother, Pamela. Fossils have been found dating from the Middle Permian ( Wordian age). Discovery ''Tapinocaninus'' fossils were first found in the Eodicynodon Assemblage Zone of the Karoo deposits, in the Lower Beaufort Beds in Beaufort West. Five specimens are known, four found at Modderdrift farm and one found on Swartgrond farm. A holotype (NMQR 2987) and four paratypes (NMQR 2985, 2986, 3097 and ROZ K95). Two specimens were found by the director of the Bernard Price Institute for Paleontological Research (now the Evolutionary Studies Institute), Professor Bruce Rubidge. Three were found by John Nyaphuli of the National Museum Bloemfontein in the same sandstone. The excavat ...
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Tapinocephalus
''Tapinocephalus'' ("low, depressed head") is an extinct genus of large herbivorous dinocephalians that lived during the Middle Permian Period in what is now South Africa. Only the type species, ''Tapinocephalus atherstonei'' is now considered valid for this genus. Discovery and naming Fossils of ''Tapinocephalus atherstonii'' were collected and donated to the British Museum by William Guybon Atherstone. They were described by Richard Owen, who described and named the species in 1876. He initially considered it a close relative of ''Pareiasaurus'' and classified both as members of Dinosauria. Based on the only remains of the skull known at the time—a poorly-preserved partial snout—he believed it had a low, broad skull similar to labyrinthodonts. Owen accordingly named it ''Tapinocephalus'', from Greek ταπεινός "low, depressed" and κεφαλή "head". Description These stocky, barrel-bodied animals were characterised by a massive bony skull roof and short weak sn ...
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Struthiocephalus
''Struthiocephalus'' ("ostrich head") is an extinct genus of dinocephalian therapsids from the Permian of South Africa. It was a large animal, reaching in body mass. Ecology This animal has the largest head of any tapinocephalid. Brink (1956) suggests that ''Struthiocephalus'' fed in or near water, the teeth being used for rooting up, gathering and grasping plant matter. Boonstra (1965) likewise considered that ''Struthiocephalus'' fed on soft vegetation, possibly under water. He suggested the postcranial skeleton possibly showed adaptations to living in marshy conditions, and the bone surface around the nostril might indicate the presence of a fleshy valve present used for closing off the nostril under water. Classification The long-snouted ''Struthiocephalus whaitsi'' would seem to be the only genus and species of this taxon. There are a large number of synonyms. ''Struthiocephalellus'' is apparently a juvenile of ''Struthiocephalus''. Boonstra showed that the seven named sp ...
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Middle Permian
The Guadalupian is the second and middle series/epoch of the Permian. The Guadalupian was preceded by the Cisuralian and followed by the Lopingian. It is named after the Guadalupe Mountains of New Mexico and Texas, and dates between 272.95 ± 0.5 – 259.1 ± 0.4 Mya. The series saw the rise of the therapsids, a minor extinction event called Olson's Extinction and a significant mass extinction called the end-Capitanian extinction event. The Guadalupian is also known as the Middle Permian. Name and background The Guadalupian is the second and middle series or epoch of the Permian. Previously called Middle Permian, the name of this epoch is part of a revision of Permian stratigraphy for standard global correlation. The name "Guadalupian" was first proposed in the early 1900s, and approved by the International Subcommission on Permian Stratigraphy in 1996. References to the Middle Permian still exist. The Guadalupian was preceded by the Cisuralian and followed by the Lopingian. ...
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Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ...
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Ulemosaurus22DB
''Ulemosaurus'' is an extinct genus of dinocephalian therapsids that lived 265 to 260 million years ago, at Isheevo in Russian Tatarstan. It was a tapinocephalid, a group of bulky herbivores which flourished in the Middle Permian. ''Ulemosaurus'' and other tapinocephalians disappeared at the end of the Middle Permian. Description Only several partial skeletons and skulls have been found. ''Ulemosaurus'' grew to 4-5 meters in length and weighed up to one ton.https://ar.culture.ru/en/subject/ulemozavr The skull bones are extremely dense: about at its thickest. This thickening is possibly related to head-butting behavior, as some researchers suggest. The species is considered a herbivore, but because the mandible is heavily constructed some palaeontologists consider it a carnivore, with the species being able to use muscle power to cut prey up with its incisors. Classification ''Ulemosaurus'' is a large ''Moschops''-like form from Russia; it is probably similar enough to be inc ...
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Dicynodont
Dicynodontia is an extinct clade of anomodonts, an extinct type of non-mammalian therapsid. Dicynodonts were herbivores that typically bore a pair of tusks, hence their name, which means 'two dog tooth'. Members of the group possessed a horny, typically toothless beak, unique amongst all synapsids. Dicynodonts first appeared in Southern Pangaea during the mid-Permian, ca. 270–260 million years ago, and became globally distributed and the dominant herbivorous animals in the Late Permian, ca. 260–252 Mya. They were devastated by the end-Permian Extinction that wiped out most other therapsids ca. 252 Mya. They rebounded during the Triassic but died out towards the end of that period. They were the most successful and diverse of the non-mammalian therapsids, with over 80-90 genera known, varying from rat-sized burrowers to elephant-sized browsers. Characteristics The dicynodont skull is highly specialised, light but strong, with the synapsid temporal openings at the rear o ...
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Eocene
The Eocene ( ) is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''Ēṓs'', 'Eos, Dawn') and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch.See: *Letter from William Whewell to Charles Lyell dated 31 January 1831 in: * From p. 55: "The period next antecedent we shall call Eocene, from ήως, aurora, and χαινος, recens, because the extremely small proportion of living species contained in these strata, indicates what may be considered the first commencement, or ''dawn'', of the existing state of the animate creation." The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isoto ...
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Pachycephalosauria
Pachycephalosauria (; from Greek παχυκεφαλόσαυρος for 'thick headed lizards') is a clade of ornithischian dinosaurs. Along with Ceratopsia, it makes up the clade Marginocephalia. With the exception of two species, most pachycephalosaurs lived during the Late Cretaceous Period, dating between about 85.8 and 66 million years ago. They are exclusive to the Northern Hemisphere, all of them being found in North America and Asia. They were all bipedal, herbivorous/omnivorous animals with thick skulls. Skulls can be domed, flat, or wedge-shaped depending on the species, and are all heavily ossified. The domes were often surrounded by nodes and/or spikes. Partial skeletons have been found of several pachycephalosaur species, but to date no complete skeletons have been discovered. Often isolated skull fragments are the only bones that are found. Candidates for the earliest-known pachycephalosaur include ''Ferganocephale adenticulatum'' from Middle Jurassic Period strata ...
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Dinosaurs
Dinosaurs are a diverse group of reptiles of the clade Dinosauria. They first appeared during the Triassic Geological period, period, between 243 and 233.23 million years ago (mya), although the exact origin and timing of the #Evolutionary history, evolution of dinosaurs is a subject of active research. They became the dominant terrestrial vertebrates after the Triassic–Jurassic extinction event 201.3 mya and their dominance continued throughout the Jurassic and Cretaceous periods. The fossil record shows that birds are feathered dinosaurs, Evolution of birds, having evolved from earlier Theropoda, theropods during the Late Jurassic epoch, and are the only dinosaur lineage known to have survived the Cretaceous–Paleogene extinction event approximately 66 mya. Dinosaurs can therefore be divided into avian dinosaurs—birds—and the extinct non-avian dinosaurs, which are all dinosaurs other than birds. Dinosaurs are varied from taxonomy (biology), taxonomic, ...
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