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Westlothiana
''Westlothiana'' ("animal from West Lothian") is a genus of reptile-like tetrapod that lived about 338 million years ago during the latest part of the Visean age of the Carboniferous. Members of the genus bore a superficial resemblance to modern-day lizards. The genus is known from a single species, ''Westlothiana lizziae''. The type specimen was discovered in the East Kirkton Limestone at the East Kirkton Quarry, West Lothian, Scotland in 1984. This specimen was nicknamed "Lizzie the lizard" by fossil hunter Stan Wood, and this name was quickly adopted by other paleontologists and the press. When the specimen was formally named in 1990, it was given the specific name "''lizziae''" in homage to this nickname.Smithson, T.R. & Rolfe, W.D.I. (1990): ''Westlothiana'' gen. nov. :naming the earliest known reptile. ''Scottish Journal of Geology'' no 26, pp 137–138. However, despite its similar body shape, ''Westlothiana'' is not considered a true lizard. ''Westlothiana'''s anatomy con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westlothiana Scale
''Westlothiana'' ("animal from West Lothian") is a genus of reptile-like tetrapod that lived about 338 million years ago during the latest part of the Visean age of the Carboniferous. Members of the genus bore a superficial resemblance to modern-day lizards. The genus is known from a single species, ''Westlothiana lizziae''. The type specimen was discovered in the East Kirkton Limestone at the East Kirkton Quarry, West Lothian, Scotland in 1984. This specimen was nicknamed "Lizzie the lizard" by fossil hunter Stan Wood, and this name was quickly adopted by other paleontologists and the press. When the specimen was formally named in 1990, it was given the specific name "''lizziae''" in homage to this nickname.Smithson, T.R. & Rolfe, W.D.I. (1990): ''Westlothiana'' gen. nov. :naming the earliest known reptile. ''Scottish Journal of Geology'' no 26, pp 137–138. However, despite its similar body shape, ''Westlothiana'' is not considered a true lizard. ''Westlothiana'''s anato ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labyrinthodont
"Labyrinthodontia" (Greek, 'maze-toothed') is an informal grouping of extinct predatory amphibians which were major components of ecosystems in the late Paleozoic and early Mesozoic eras (about 390 to 150 million years ago). Traditionally considered a subclass of the class Amphibia, modern classification systems recognize that labyrinthodonts are not a formal natural group (clade) exclusive of other tetrapods. Instead, they consistute an evolutionary grade (a paraphyletic group), ancestral to living tetrapods such as Lissamphibia, lissamphibians (modern amphibians) and Amniote, amniotes (Reptile, reptiles, Mammal, mammals, and kin). "Labyrinthodont"-grade vertebrates evolved from Sarcopterygii, lobe-finned fishes in the Devonian, though a formal boundary between fish and amphibian is difficult to define at this point in time. "Labyrinthodont" generally refers to extinct four-limbed tetrapods with a large body size and a crocodile-like lifestyle. The name describes the pattern o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stan Wood (fossil Hunter)
Stan Wood was a self-taught fossil hunter who dazzled the academic world with his ability to make significant palaeontological discoveries at scale and is arguably most celebrated for refocusing attention on early Carboniferous palaeobiology as the means to closing Romer's gap. Life and works Born Stanley Wood in Edinburgh, 1939, Wood left school aged 14 to work as a dockyard apprentice at Leith Harbour during a period of severe economic hardship, when Leith had acquired the reputation as one of the roughest neighbourhoods in post-war Britain. Wood could put his hand to many things and served in the Merchant Navy as an engineering officer for a time, before being assigned to work for Brown Brothers, an engineering company. He was encouraged to consider white-collar work and changed career to sell insurance with the Prudential. From fossil hunter to palaeontologist As a boy, Wood had been fascinated by Roman Britain, and was convinced that he could calculate the existence of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Lothian
West Lothian ( sco, Wast Lowden; gd, Lodainn an Iar) is one of the 32 council areas of Scotland, and was one of its shires of Scotland, historic counties. The county was called Linlithgowshire until 1925. The historic county was bounded geographically by the River Avon, Falkirk, Avon to the west and the River Almond, Lothian, Almond to the east. The modern council area occupies a larger area than the historic county. It was reshaped following local government reforms in 1975: some areas in the west were transferred to Falkirk (council area), Falkirk; some areas in the east were transferred to Edinburgh; and some areas that had formerly been part of in Midlothian were added to West Lothian. West Lothian lies on the southern shore of the Firth of Forth and is predominantly rural, though there were extensive coal, iron, and shale oil mining operations in the 19th and 20th centuries. These created distinctive red-spoil heaps (locally known as "bing (mining), bings") throughout the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reptiliomorpha
Reptiliomorpha (meaning reptile-shaped; in PhyloCode known as ''Pan-Amniota'') is a clade containing the amniotes and those tetrapods that share a more recent common ancestor with amniotes than with living amphibians ( lissamphibians). It was defined by Michel Laurin (2001) and Vallin and Laurin (2004) as the largest clade that includes ''Homo sapiens'', but not ''Ascaphus truei'' (tailed frog). Laurin and Reisz (2020) defined Pan-Amniota as the largest total clade containing ''Homo sapiens'', but not ''Pipa pipa'', '' Caecilia tentaculata'', and '' Siren lacertina''. The informal variant of the name, "reptiliomorphs", is also occasionally used to refer to stem-amniotes, i.e. a grade of reptile-like tetrapods that are more closely related to amniotes than they are to lissamphibians, but are not amniotes themselves; the name is used in this meaning e.g. by Ruta, Coates and Quicke (2003). An alternative name, "Anthracosauria", is also commonly used for the group, but is confusing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viséan
The Visean, Viséan or Visian is an age in the ICS geologic timescale or a stage in the stratigraphic column. It is the second stage of the Mississippian, the lower subsystem of the Carboniferous. The Visean lasted from to Ma. It follows the Tournaisian age/stage and is followed by the Serpukhovian age/stage. Name and definitions The Viséan Stage was introduced by Belgian geologist André Dumont in 1832. Dumont named this stage after the city of Visé in Belgium's Liège Province. Before being used as an international stage, the Visean Stage was part of the (West) European regional geologic time scale, in which it followed the Tournaisian Stage and is followed by the Namurian Stage. In the North American regional scale, the Visean Stage correlates with the upper Osagean, the Meramecian and lower Chesterian stages. In the Chinese regional time scale, it correlates with the lower and middle Tatangian series.; 2006: ''Global time scale and regional stratigraphic reference sca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lepospondyli
Lepospondyli is a diverse taxon of early tetrapods. With the exception of one late-surviving lepospondyl from the Late Permian of Morocco (''Diplocaulus minumus''), lepospondyls lived from the Early Carboniferous ( Mississippian) to the Early Permian and were geographically restricted to what is now Europe and North America. Five major groups of lepospondyls are known: Adelospondyli; Aïstopoda; Lysorophia; Microsauria; and Nectridea. Lepospondyls have a diverse range of body forms and include species with newt-like, eel- or snake-like, and lizard-like forms. Various species were aquatic, semiaquatic, or terrestrial. None were large (the biggest genus, the diplocaulid ''Diplocaulus'', reached a meter in length, but most were much smaller), and they are assumed to have lived in specialized ecological niches not taken by the more numerous temnospondyl amphibians that coexisted with them in the Paleozoic. Lepospondyli was named in 1888 by Karl Alfred von Zittel, who coined the name t ... [...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] |
East Kirkton Quarry
East Kirkton Quarry is a former limestone quarry in West Lothian, Scotland (East Kirkton Limestone), now better known as a fossil site known for terrestrial fossils from the fossil-poor Romer's gap, a 15 million year period at the beginning of the Carboniferous. The rocks and fossils are of Visean age, about 335 million years old. Best known are the labyrinthodont fossils, as the period coincides with the time where the modern lineages of tetrapods are thought to have evolved. Location The quarry is located in the town of Bathgate in West Lothian, Scotland. Geologically, it sits fairly central to the middle of the fossil-rich Scottish Central Lowlands. The site is dominated by volcanic tuff and limestone, and layered silica deposits, indicating the presence of a hot spring associated with volcanism. Benton, M. (2005): Vertebrate Palaeontology 3rd edition. Blackwell Publishing The land next to the quarry itself is developed for housing. Clack, J.A. (2002): Gaining ground: the or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Casineria
''Casineria'' is an extinct genus of tetrapod which lived about 340-334 million years ago in the Mississippian epoch of the Carboniferous period. Its generic name, ''Casineria'', is a latinization of Cheese Bay, the site near Edinburgh, Scotland where the holotype fossil was found. When originally described in 1999, it was identified as a transitional fossil noted for its mix of basal (amphibian-like) and advanced (reptile-like) characteristics, putting it at or very near the origin of the amniotes, the group containing all mammals, birds, modern reptiles, and other descendants of their reptile-like common ancestor. However, the sole known fossil is lacking key elements such as a skull, making exact analysis difficult. As a result, the classification of ''Casineria'' has been more controversial in analyses conducted since 1999. Other proposed affinities include a placement among the lepospondyls, seymouriamorphs, " gephyrostegids", or as a synonym of '' Caerorhachis'', another ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Kirkton Limestone
The East Kirkton Limestone is a rock unit in the West Lothian Oil-Shale Formation in Scotland. It preserves fossils of the Carboniferous period. The limestone outcrops at East Kirkton Quarry. See also * '' Kirktonecta'' * List of fossiliferous stratigraphic units in Scotland * ''Westlothiana ''Westlothiana'' ("animal from West Lothian") is a genus of reptile-like tetrapod that lived about 338 million years ago during the latest part of the Visean age of the Carboniferous. Members of the genus bore a superficial resemblance to modern ...'' References * Carboniferous System of Europe Carboniferous Scotland Limestone formations Carboniferous southern paleotropical deposits Viséan {{Scotland-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reptile
Reptiles, as most commonly defined are the animals in the class Reptilia ( ), a paraphyletic grouping comprising all sauropsids except birds. Living reptiles comprise turtles, crocodilians, squamates (lizards and snakes) and rhynchocephalians (tuatara). As of March 2022, the Reptile Database includes about 11,700 species. In the traditional Linnaean classification system, birds are considered a separate class to reptiles. However, crocodilians are more closely related to birds than they are to other living reptiles, and so modern cladistic classification systems include birds within Reptilia, redefining the term as a clade. Other cladistic definitions abandon the term reptile altogether in favor of the clade Sauropsida, which refers to all amniotes more closely related to modern reptiles than to mammals. The study of the traditional reptile orders, historically combined with that of modern amphibians, is called herpetology. The earliest known proto-reptiles originated around ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
