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Anomodont Genera
Anomodontia is an extinct group of non-mammalian therapsids from the Permian and Triassic periods. By far the most speciose group are the dicynodonts, a clade of beaked, tusked herbivores.Chinsamy-Turan, A. (2011) ''Forerunners of Mammals: Radiation - Histology - Biology''p.39.Indiana University Press, . Retrieved May 2012 Anomodonts were very diverse during the Middle Permian, including primitive forms like ''Anomocephalus'' and ''Patranomodon'' and groups like Venyukovioidea and Dromasauria. Dicynodonts became the most successful and abundant of all herbivores in the Late Permian, filling ecological niches ranging from large browsers down to small burrowers. Few dicynodont families survived the Permian–Triassic extinction event, but one lineage (Kannemeyeriiformes) evolved into large, stocky forms that became dominant terrestrial herbivores right until the Late Triassic, when changing conditions caused them to decline, finally going extinct during the Triassic-Jurassic ext ... [...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] |
Patranomodon
''Patranomodon'' (from Greek ''patr-'' “father”, thus “father of anomodonts”) is an extinct genus belonging to the group of Anomodontia. Rubidge and Hopson named this anomodont in 1990 after discovering its skull.Rubidge, B. S., & Hopson, J. A. (1990). A new anomodont therapsid from South Africa and its bearing on the ancestry of Dicynodontia. ''South African Journal of Science'', ''86''(1), 43-45. ''Patranomodon'' is known to have ranged in the Karoo of Southern Africa. Discovery and history The skull fossil of ''Patranomodon'' was found in the ''Eodicynodon'' Assemblage Zone of South Africa, belonging to the lowest biozone of the Beaufort Group. The Beaufort Group time period extends from the middle of the Permian to the early Triassic period. It is one of the three main subdivisions of the Karoo Supergroup in what today is southern Africa. Rubidge and Hopson were the first to discover the skull of ''Patranomodon''. These paleobiologists also named ''Patranomodon'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suminia
''Suminia'' is an extinct genus of basal anomodont that lived during the Tatarian age of the late Permian, spanning approximately from 268-252 Ma.Rybczynski N. 2000. Cranial anatomy and phylogenetic position of Suminia getmanovi, a basal anomodont (Amniota: Therapsida) from the Late Permian of Eastern Europe. Zool. J. Linn. Soc. 130:329–73 ''Suminia'' is recognized the youngest non-dicynodont anomodont.Ivachnenko MF. 1994. A new Late Permian dromasaurian (Anomodontia) from Eastern Europe. Paleontological Journal 28: 96- 103. Its fossil localities are primarily derived from the Kotel’nich locality of the Kirov region in Russia. However, there have been some isolated specimen found in a few different localities, all from eastern European regions of Russia.Fröbisch, J. and Reisz, R. R. 2011. The postcranial anatomy of Suminia getmanovi (Synapsida: Anomodontia), the earliest known arboreal tetrapod. Zoological Journal of the Linnean Society, 162: 661–698. ''Suminia'', along wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otsheria
''Otsheria'' is an extinct genus of anomodont from the Permian of Russia.Modesto, S. P. & Rybcynski, N''The amniote faunas of the Russian Permian: implications for Late Permian terrestrial vertebrate biogeography'' ''In'' Benton, M. J.; Shishkin, M. A.; Unwin, D. M.; Kurochkin, E. N. The Age of Dinosaurs in Russia and Mongolia. Cambridge University Press, 2001. 672 p. ''Otsheria'' had a long skull. See also * List of therapsids References Further reading *''The Origin and Evolution of Mammals (Oxford Biology)'' by T. S. Kemp *''The Age of Dinosaurs in Russia and Mongolia'' by Michael J. Benton, Mikhail A. Shishkin, David M. Unwin, and Evgenii N. Kurochkin *''Origins of the Higher Groups of Tetrapods: Controversy and Consensus'' by Hans-Peter Schultze and Linda Trueb *''Reptiles and Herbivory'' by G.M. King Anomodont genera Guadalupian synapsids Guadalupian genus first appearances Guadalupian genus extinctions Prehistoric synapsids of Europe Permian Russia Fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otsheridae
Otsheriidae is an extinct family of small herbivorous anomodont therapsids that are known from the Permian of Russia. See also * List of synapsids These lists of synapsids collectively include every genus that has ever been included in the clade Synapsida- the mammals and their evolutionary precursors. The lists includes accepted genera along with those now considered invalid, doubtful (''nom ... References Anomodonts Permian synapsids Extinct animals of Russia Prehistoric synapsids of Europe Guadalupian first appearances Lopingian extinctions Prehistoric therapsid families {{anomodont-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tiarajudens
''Tiarajudens'' (" Tiaraju tooth") is an extinct genus of saber-toothed herbivorous anomodonts which lived during the Middle Permian period (Capitanian stage) in what is now Rio Grande do Sul, Brazil. It is known from the holotype UFRGS PV393P, a nearly complete skull. The type species ''T. eccentricus'' was named in 2011. Description ''Tiarajudens'' is a member of Anomodontia, a suborder of therapsids. Like other anomodonts, it was a quadrupedal herbivore about the size of a wild boar. The single fragmented holotype skull is short and robust at about in length. The most prominent features of ''Tiarajudens'' are its two large saber-like canine teeth. These teeth are unlike the tusks of dicynodonts, a later group of anomodonts. Twenty-one high- crowned teeth are present on either side of the upper jaw, including spoon-shaped incisors. Wide palatal teeth are also present. The top and bottom sets of teeth fit closely together, much like the teeth of mammals, allowing it to e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anomocephaloidea
Anomocephaloidea is a clade (evolutionary grouping) of anomodont therapsids that existed in Gondwana during the Middle Permian and includes two species, ''Anomocephalus africanus'' from South Africa and ''Tiarajudens eccentricus'' from Brazil, both of which are characterized by large body size and teeth that fit tightly together or occlude. Anomocephaloidea is among the most basal groups of anomodonts, the other being Venyukovioidea, which differs in being a Laurasian clade of mostly small-bodied species. Anomocephaloidea was named in 2011 with the discovery of ''Tiarajudens''; ''Anomocephalus'' had been known since 1999, but was unique among anomodonts until ''Tiarajudens'' was described. Both ''Anomocephalus'' and ''Tiarajudens'' were herbivores, although the latter possessed a pair of saber-like canine teeth that may have been used in display or combat with other individuals of the same species. Although Anomocephaloidea was short-lived and had a limited geographic distribut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biseridens
''Biseridens'' ("two rows of teeth") is an extinct genus of anomodont therapsid, and one of the most basal anomodont genera known. Originally known from a partial skull misidentified as an eotitanosuchian in 1997, another well-preserved skull was found in the Qingtoushan Formation in the Qilian Mountains of Gansu, China, in 2009 that clarified its relationships to anomodonts, such as the dicynodonts. Among tetrapod taxa, the therapsid clade anomodontia in which ''Biseridens'' belong has one of the largest population sizes, highest levels of diversity, and longest stratigraphic range (Middle Permian to the Triassic, possibly into the Cretaceous), as well as being one of the only clades known from all the continents. Primarily understood from the recently discovered, most-well preserved specimen, ''Biseridens'' is most notably distinguishable as an anomodont due to its short snout, dorsally elevated zygomatic arch, and presence of a septomaxilla that distinctly lacks a facial ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Therapsid
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 were oriented more underneath the body, as opposed to the sprawling posture of many reptiles and salamanders. Therapsids evolved from "pelycosaurs", specifically within the Sphenacodontia, more than 279.5 million years ago. They replaced the "pelycosaurs" as the dominant large land animals in the Middle Permian through to the Early Triassic. In the aftermath of the Permian–Triassic extinction event, therapsids declined in relative importance to the rapidly diversifying reptiles during the Middle Triassic. The therapsids include the cynodonts, the group that gave rise to mammals ( Mammaliaformes) in the Late Triassic, around 225 million years ago. Of the non-mammalian therapsids, only cynodonts survived beyond the end of the Triassic, with the only other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kannemeyeriiformes
Kannemeyeriiformes is a group of large-bodied Triassic dicynodonts. As a clade, Kannemeyeriiformes has been defined to include the species ''Kannemeyeria simocephalus'' and all dicynodonts more closely related to it than to the species '' Lystrosaurus murrayi''. Evolutionary history Despite being the most species-rich group of dicynodonts in the Triassic Period, kannemeyeriiforms exhibit much less diversity in terms of their anatomy and ecological roles than the dicynodonts from the Permian Period. Lystrosauridae is thought to be the most closely related group (sister taxon) to Kannemeyeriiformes, and since the earliest lystrosaurids are known from the Late Permian, the divergence of these two groups must have occurred at least as far back as this time, implying that a long ghost lineage must exist. Although no kannemeyeriiforms have been found in the Late Permian yet, the recent discovery of ''Sungeodon'' helps fill a gap in the early fossil record of the group by showing that k ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian–Triassic Extinction Event
The Permian–Triassic (P–T, P–Tr) extinction event, also known as the Latest Permian extinction event, the End-Permian Extinction and colloquially as the Great Dying, formed the boundary between the Permian and Triassic geologic periods, as well as between the Paleozoic and Mesozoic eras, approximately 251.9 million years ago. It is the Earth's most severe known extinction event, with the extinction of 57% of biological families, 83% of genera, 81% of marine species and 70% of terrestrial vertebrate species. It was the largest known mass extinction of insects. There is evidence for one to three distinct pulses, or phases, of extinction. The scientific consensus is that the main cause of extinction was the large amount of carbon dioxide emitted by the volcanic eruptions that created the Siberian Traps, which elevated global temperatures, and in the oceans led to widespread anoxia and acidification. Proposed contributing factors include: the emission of much addition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
