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Moschognathus
''Moschognathus'' is an extinct genus of dinocephalian therapsid in the family Tapinocephalidae. The genus includes only the type species ''M. whaitsi'', named by palaeontologist Robert Broom in 1914. It was a short-snouted tapinocephalid, closely related to and resembling the well-known genus '' Moschops'', but its skull is less thickened overall has a relatively longer and shallower snout by comparison. Indeed, ''Moschognathus'' has typically been regarded as a junior synonym of ''Moschops'' (e.g. by King, 1988 and Atayman ''et al''., 2009) since 1969 after Lieuwe Dirk Boonstra sunk ''Moschognathus'' into ''Moschops'', albeit retained as its own doubtfully valid species. However, researchers in the 21st century have expressed doubt over this synonymy and suggested that ''Moschognathus'' is a distinct taxon after all, including first by Christian Kammerer in a 2009 Ph.D. thesis A thesis ( : theses), or dissertation (abbreviated diss.), is a document submitted in s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anteosaurus
''Anteosaurus'' (meaning "Antaeus reptile") is an extinct genus of large carnivorous dinocephalian synapsid. It lived at the end of the Guadalupian (= Middle Permian) during the Capitanian stage, about 265 to 260 million years ago in what is now South Africa. It is mainly known by cranial remains and few postcranial bones. With its skull reaching in length and a body size estimated at more than in length, and in weight, ''Anteosaurus'' was the largest known carnivorous non-mammalian synapsid and the largest terrestrial predator of the Permian period. Occupying the top of the food chain in the Middle Permian, its skull, jaws and teeth show adaptations to capture large prey like the giants titanosuchids and tapinocephalids dinocephalians and large pareiasaurs. As in many other dinocephalians the cranial bones of ''Anteosaurus'' are pachyostosed, but to a lesser extent than in tapinocephalid dinocephalians. In ''Anteosaurus'', pachyostosis mainly occurs in the form of horn-sha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anteosaurus & Moschognathus
''Anteosaurus'' (meaning " Antaeus reptile") is an extinct genus of large carnivorous dinocephalian synapsid. It lived at the end of the Guadalupian (= Middle Permian) during the Capitanian stage, about 265 to 260 million years ago in what is now South Africa. It is mainly known by cranial remains and few postcranial bones. With its skull reaching in length and a body size estimated at more than in length, and in weight, ''Anteosaurus'' was the largest known carnivorous non-mammalian synapsid and the largest terrestrial predator of the Permian period. Occupying the top of the food chain in the Middle Permian, its skull, jaws and teeth show adaptations to capture large prey like the giants titanosuchids and tapinocephalids dinocephalians and large pareiasaurs. As in many other dinocephalians the cranial bones of ''Anteosaurus'' are pachyostosed, but to a lesser extent than in tapinocephalid dinocephalians. In ''Anteosaurus'', pachyostosis mainly occurs in the form of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moschops
''Moschops'' (Greek for "calf face") is an extinct genus of therapsids that lived in the Guadalupian epoch, around 265–260 million years ago. They were heavily built plant eaters, and they may have lived partly in water, as hippopotamuses do. They had short, thick heads and might have competed by head-butting each other. Their elbow joints allowed them to walk with a more mammal-like gait rather than crawling. Their remains were found in the Karoo region of South Africa, belonging to the ''Tapinocephalus'' Assemblage Zone. Therapsids, such as ''Moschops'', are synapsids, the dominant land animals in the Permian period, which ended 252 million years ago. Description ''Moschops'' were heavy set dinocephalian synapsids, measuring in length, and weighing on average and in maximum body mass. They had small heads with broad orbits and heavily-built short necks. Like other members of Tapinocephalidae, the skull had a tiny opening for the pineal organ. The occiput was broad and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1914 In Paleontology
References * Trexler, D., 2001, Two Medicine Formation, Montana: geology and fauna: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, pp. 298–309. 1910s in paleontology 1914, Paleontology 1914 in science, Paleontology 4 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 was previously 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 Lop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils Of South Africa
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian South Africa
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 am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guadalupian Synapsids Of Africa
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 was previously 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 Lop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Therapsid Genera
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tapinocephalians
The Tapinocephalia are one of the major groups of dinocephalian therapsids and the major herbivorous group. Tapinocephalia has been found to consist of three clades: Styracocephalidae, Titanosuchidae, and the very successful Tapinocephalidae. Notable tapinocephalians include ''Moschops'', ''Tapinocephalus'', and ''Titanosuchus''. Description Unlike anteosaurs and estemmenosuchids, tapinocephalians are primarily an African group. The estemmenosuchids and pareiasaurs may have occupied this paleo-bovine niche in the north. Only one tapinocephalian, ''Ulemosaurus'', is known from Russia. Earlier tapinocephalians were carnivorous or omnivorous. One such group was Titanosuchidae, which consisted of long-tailed predators that hunted herbivorous therapsids Therapsida is a major group of eupelycosaurian synapsids that includes mammals, their ancestors and relatives. Many of the traits today seen as unique to mammals had their origin within early therapsids, including limbs that wer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albany Museum
The Albany Museum, South Africa is situated in Grahamstown in South Africa, is affiliated to Rhodes University and dates back to 1855,Chinsamy, Anusuya. (1997). "Albany Museum, Grahamstown, South Africa." ''Encyclopedia of Dinosaurs''. Edited by Phillip J. Currie and Kevin Padian. Academic Press. p. 6. making it the second oldest museum in South Africa. The natural history and geology collections of the '' Eastern Province Literary, Scientific and Medical Society'' were used as its nucleus. The herbarium is staffed by the South African National Biodiversity Institute and has material dating back to 1812, collected by William John Burchell, and a collection of 240 specimens donated by Constance Georgina Adams in 1919, as well as geological material gathered by Andrew Geddes Bain and W. G. Atherstone. It also houses a large collection of invertebrate, vertebrate and tetrapod fossils (some of which are from the world renowned Waterloo Farm lagerstätte), and palaeolithic stone tool ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
American Museum Of Natural History
The American Museum of Natural History (abbreviated as AMNH) is a natural history museum on the Upper West Side of Manhattan in New York City. In Theodore Roosevelt Park, across the street from Central Park, the museum complex comprises 26 interconnected buildings housing 45 permanent exhibition halls, in addition to a planetarium and a library. The museum collections contain over 34 million specimens of plants, animals, fossils, minerals, rocks, meteorites, human remains, and human cultural artifacts, as well as specialized collections for frozen tissue and genomic and astrophysical data, of which only a small fraction can be displayed at any given time. The museum occupies more than . AMNH has a full-time scientific staff of 225, sponsors over 120 special field expeditions each year, and averages about five million visits annually. The AMNH is a private 501(c)(3) organization. Its mission statement is: "To discover, interpret, and disseminate—through scientific research and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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