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Limnoscelis
''Limnoscelis'' (\ limˈnäsələ̇s \, meaning "marsh footed") was a genus of large diadectomorph tetrapods from the Late Carboniferous of western North America. It includes two species: the type species ''Limnoscelis paludis'' from New Mexico, and ''Limnoscelis dynatis'' from Colorado, both of which are thought to have lived concurrently. No specimens of ''Limnoscelis'' are known from outside of North America. ''Limnoscelis'' was carnivorous, and likely semiaquatic, though it may have spent a significant portion of its life on land. ''Limnoscelis'' had a combination of derived amphibian and primitive reptilian features, and its placement relative to Amniota has significant implications regarding the origins of the first amniotes. Discovery and naming The type species ''Limnoscelis paludis'' was collected by the fossil hunter David Baldwin between 1877 and 1880 from the El Cobre Canyon beds of the Cutler Formation, New Mexico. Baldwin was collecting fossils in service of the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limnoscelis Paludis 2
''Limnoscelis'' (\ limˈnäsələ̇s \, meaning "marsh footed") was a genus of large diadectomorph tetrapods from the Late Carboniferous of western North America. It includes two species: the type species ''Limnoscelis paludis'' from New Mexico, and ''Limnoscelis dynatis'' from Colorado, both of which are thought to have lived concurrently. No specimens of ''Limnoscelis'' are known from outside of North America. ''Limnoscelis'' was carnivorous, and likely semiaquatic, though it may have spent a significant portion of its life on land. ''Limnoscelis'' had a combination of derived amphibian and primitive reptilian features, and its placement relative to Amniota has significant implications regarding the origins of the first amniotes. Discovery and naming The type species ''Limnoscelis paludis'' was collected by the fossil hunter David Baldwin between 1877 and 1880 from the El Cobre Canyon beds of the Cutler Formation, New Mexico. Baldwin was collecting fossils in service of the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limnoscelis
''Limnoscelis'' (\ limˈnäsələ̇s \, meaning "marsh footed") was a genus of large diadectomorph tetrapods from the Late Carboniferous of western North America. It includes two species: the type species ''Limnoscelis paludis'' from New Mexico, and ''Limnoscelis dynatis'' from Colorado, both of which are thought to have lived concurrently. No specimens of ''Limnoscelis'' are known from outside of North America. ''Limnoscelis'' was carnivorous, and likely semiaquatic, though it may have spent a significant portion of its life on land. ''Limnoscelis'' had a combination of derived amphibian and primitive reptilian features, and its placement relative to Amniota has significant implications regarding the origins of the first amniotes. Discovery and naming The type species ''Limnoscelis paludis'' was collected by the fossil hunter David Baldwin between 1877 and 1880 from the El Cobre Canyon beds of the Cutler Formation, New Mexico. Baldwin was collecting fossils in service of the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diadectomorpha
Diadectomorpha is a clade of large tetrapods that lived in Euramerica during the Carboniferous and Early Permian periods and in Asia during Late Permian (Wuchiapingian), They have typically been classified as advanced reptiliomorphs (transitional between "amphibians" ''sensu lato'' and amniotes) positioned close to, but outside of the clade Amniota, though some recent research has recovered them as the sister group to the traditional Synapsida within Amniota, based on inner ear anatomy and cladistic analyses. They include both large (up to 2 meters long) carnivorous and even larger (to 3 meters) herbivorous forms, some semi-aquatic and others fully terrestrial. The diadectomorphs seem to have originated during late Mississippian times, although they only became common after the Carboniferous rainforest collapse and flourished during the Late Pennsylvanian and Early Permian periods. Anatomy Diadectomorphs possessed both amphibian-like and amniote-like characteristics. Originall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Redpath Museum
The Redpath Museum (french: Musée Redpath) is a museum of natural history belonging to McGill University and located on the university's campus at 859, rue Sherbrooke Ouest (859 Sherbrooke Street West) in Montreal, Quebec. It was built in 1882 as a gift from the sugar baron Peter Redpath. It houses collections of interest to ethnology, biology, paleontology, and mineralogy/geology. The collections were started by some of the same individuals who founded the Smithsonian and Royal Ontario Museum collections. The current director is Hans Larsson. Commissioned by Redpath to mark the 25th anniversary of Sir John William Dawson's appointment as Principal, the Museum was designed by A.C. Hutchison and A.D. Steele. McGill University's Redpath Museum website characterizes it as an "idiosyncratic expression of eclectic Victorian Classicism" as well as "an unusual and late example of the Greek Revival in North America." It is the oldest building built specifically to be a museum in Can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
El Cobre Canyon Formation
The El Cobre Canyon Formation is a geologic formation in New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian periods. Description The El Cobre Canyon Formation consists of siliciclastic red beds with a total thickness of roughly . These lie on Proterozoic basement and are in turn overlain by the Arroyo del Agua Formation. At its type section, the formation is 66% siltstone and 21% sandstone, with minor conglomerate (9%) sandy shale (2%), and calcrete (1%). The beds are pale reddish brown in color, and can readily be distinguished from the orange beds of the overlying Arroyo del Agua Formation. The siltstone beds contain many rhizoliths, while the sandstone beds are coarse grained, arkosic, and micaceous, with trough crossbedding. The sandstones form thick cliffs and benches. The conglomerates are composed mostly of fragments of basement rock. The formation correlates with the Atrasado Formation and lower Abo Formation to the south. Fossils Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amniote
Amniotes are a clade of tetrapod vertebrates that comprises sauropsids (including all reptiles and birds, and extinct parareptiles and non-avian dinosaurs) and synapsids (including pelycosaurs and therapsids such as mammals). They are distinguished from the other tetrapod clade — the amphibians — by the development of three extraembryonic membranes ( amnion for embryoic protection, chorion for gas exchange, and allantois for metabolic waste disposal or storage), thicker and more keratinized skin, and costal respiration (breathing by expanding/constricting the rib cage). All three main features listed above, namely the presence of an amniotic buffer, water-impermeable cutes and a robust respiratory system, are very important for amniotes to live on land as true terrestrial animals – the ability to reproduce in locations away from water bodies, better homeostasis in drier environments, and more efficient air respiration to power terrestrial locomotions, although the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sangre De Cristo Formation
The Sangre de Cristo Formation is a geologic formation in Colorado and New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian. Description The formation is divided into an informal lower member and an upper Crestone Conglomerate Member. The lower informal member consists of about of red arkosic sandstone, conglomeratic sandstone, siltstone, and shale. These are arranged into fining upwards cycles. The Crestone Conglomerate Member consists of about of red conglomerate, conglomeratic sandstone, sandstone, and minor siltstone and shale.Lindsey ''et al.'' 1985 The formation is exposed in the Sangre de Cristo Mountains in both southern Colorado and northern New Mexico. However, the exposures in the southeastern Sangre de Cristo Mountains were deposited in a distinct basin (the Rowe-Mora basin) rather than the central Colorado basin, lack the marine beds found in Colorado, and should probably be assigned instead to the Abo Formation.Lucas ''et al.'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsh
A marsh is a wetland that is dominated by herbaceous rather than woody plant species.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes provide habitats for many kinds of invertebrates, fish, amphibians, waterfowl and aquatic mammals. This biological productivity means that marshes contain 0.1% of global sequestered terrestrial carbon. Moreover, they have an outsized influence on climate resi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhachitomi
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 rhac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Postcrania
Postcrania (postcranium, adjective: postcranial) in zoology and vertebrate paleontology is all or part of the skeleton apart from the skull. Frequently, fossil remains, e.g. of dinosaurs or other extinct tetrapods, consist of partial or isolated skeletal elements; these are referred to as ''postcrania''. There is some disagreement over whether the skull and skeleton belong to the same or different animals. One example is the case of a Cretaceous sauropod skull of ''Nemegtosaurus'' found in association with the postcranial skeleton ''Opisthocoelicaudia ''Opisthocoelicaudia'' is a genus of sauropod dinosaur of the Late Cretaceous Period discovered in the Gobi Desert of Mongolia. The type species is ''Opisthocoelicaudia skarzynskii''. A well-preserved skeleton lacking only the head and neck wa ...''. In paleoanthropological studies, reconstruction of relationship between various species/remains is considered to be better supported by cranial characters rather than postcranial c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yale College
Yale College is the undergraduate college of Yale University. Founded in 1701, it is the original school of the university. Although other Yale schools were founded as early as 1810, all of Yale was officially known as Yale College until 1887, when its schools were confederated and the institution was renamed Yale University. It is ranked as one of the top colleges in the United States. Originally established to train Congregationalist ministers, the college began teaching humanities and natural sciences by the late 18th century. At the same time, students began organizing extracurricular organizations: first literary societies, and later publications, sports teams, and singing groups. By the middle of the 19th century, it was the largest college in the United States. In 1847, it was joined by another undergraduate school at Yale, the Sheffield Scientific School, which was absorbed into the college in 1956. These merged curricula became the basis of the modern-day liberal arts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peabody Museum Of Natural History
The Peabody Museum of Natural History at Yale University is among the oldest, largest, and most prolific university natural history museums in the world. It was founded by the philanthropist George Peabody in 1866 at the behest of his nephew Othniel Charles Marsh, the early paleontologist. Most known to the public for its Great Hall of Dinosaurs, which includes a mounted juvenile ''Brontosaurus'' and the mural '' The Age of Reptiles,'' it also has permanent exhibits dedicated to human and mammal evolution; wildlife dioramas; Egyptian artifacts; and the birds, minerals and Native Americans of Connecticut. Description The Peabody Museum is located at 170 Whitney Avenue in New Haven, Connecticut, United States, and is operated by almost one hundred staff members. While the original building was demolished in 1917, it moved to its current location in 1925, and has since expanded to occupy the Peabody Museum, the attached Kline Geology Laboratory and the Class of 1954 Environmental ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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