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Placodont
Placodonts (" Tablet teeth") are an extinct order of marine reptiles that lived during the Triassic period, becoming extinct at the end of the period. They were part of Sauropterygia, the group that includes plesiosaurs. Placodonts were generally between in length, with some of the largest measuring long. The first specimen was discovered in 1830. They have been found throughout central Europe, North Africa, the Middle East and China. Palaeobiology The earliest forms, like ''Placodus'', which lived in the early to middle Triassic, resembled barrel-bodied lizards superficially similar to the marine iguana of today, but larger. In contrast to the marine iguana, which feeds on algae, the placodonts ate molluscs and so their teeth were flat and tough to crush shells. In the earliest periods, their size was probably enough to keep away the top sea predators of the time: the sharks. However, as time passed, other kinds of carnivorous reptiles began to colonize the seas, such as ...
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Placodontoidea
Placodonts (" Tablet teeth") are an extinct order of marine reptiles that lived during the Triassic period, becoming extinct at the end of the period. They were part of Sauropterygia, the group that includes plesiosaurs. Placodonts were generally between in length, with some of the largest measuring long. The first specimen was discovered in 1830. They have been found throughout central Europe, North Africa, the Middle East and China. Palaeobiology The earliest forms, like ''Placodus'', which lived in the early to middle Triassic, resembled barrel-bodied lizards superficially similar to the marine iguana of today, but larger. In contrast to the marine iguana, which feeds on algae, the placodonts ate molluscs and so their teeth were flat and tough to crush shells. In the earliest periods, their size was probably enough to keep away the top sea predators of the time: the sharks. However, as time passed, other kinds of carnivorous reptiles began to colonize the seas, such as ich ...
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Cyamodontoidea
Cyamodontoidea is an extinct superfamily of placodont marine reptiles from the Triassic period. It is one of the two main groups of placodonts, the other being Placodontoidea. Cyamodontoids are distinguished from placodontoids by their large shells, formed from fused bony plates called osteoderms and superficially resembling the shells of turtles. Cyamodontoids also have distinctive skulls with narrow, often toothless jaws and wide, flaring temporal regions behind the eyes. Two large temporal openings are positioned at the top of the back of the skull, an arrangement that is known as the euryapsid condition and seen throughout Sauropterygia, the marine reptile group to which placodonts belong. Cyamodontoids are also distinguished by their large crushing teeth, which grow from the palatine bones on the roof of the mouth. Description Shell The shells of cyamodontoids differ from those of turtles in several ways. Turtle shells are fused to their skeletons in several regions, includin ...
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Macroplacus Raeticus
''Macroplacus'' is an extinct genus of placodont reptiles. The type species is ''M. raeticus''Schubert-Klempnauer, H., 1975, Macroplacus raeticus n. g. n. sp.-ein neuer Placodontier aus dem Rat der Bayerischen Alpen: Mitteilungen der Bayerischen Staatssammlung fur Palaontologie und historishce Geologie, v. 15, p. 33-55. and the fossil record of this species dates back to the upper Triassic, Rhaetian age (age range: 205.6 to 201.6 million years ago). These fossils have been found in Germany, at Hinterstein near Hindelang im Allgäu. Taxonomy The classification of ''Macroplacus'' is controversial but it is usually placed in the Cyamodontidae or in the Placochelyidae. These reptiles are placodonts, a group of animal probably related to diapsids, but that look similar to the turtles. ''Macroplacus'', in particular, was a representative of cyamodontoidea, characterized by heavy armor and narrow snouts. Description ''Macroplacus raeticus'', the only known species, possessed a re ...
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Paraplacodontidae
''Paraplacodus broilli'' is an extinct placodont sauropterygian from the middle Triassic period, from the Anisian until Ladinian stages. The fossils were uncovered in Northern Italy and the species was named in 1931 by Bernhard Peyer. ''Paraplacodus'' means "Almost ''Placodus''", in reference to its similarity to ''Placodus''. Like the majority of described placodonts, ''Paraplacodus'' was an aquatic reptile that fed almost exclusively on shellfish. Most known Placodont species can be divided into two groups - the unarmored placodontoids, which would resemble a large, scaly, tooth-filled newt, or the armored cyamodontids, which would resemble a heavily armored turtle; ''Paraplacodus'' belonged to the former family. It was a small reptile, measuring about in total body length. The jaws of ''Paraplacodus'' were adapted to eat shellfish, with three pairs of protruding teeth in the top row and two rows of protruding teeth in the front of the jaw, with rounded crushing teeth in t ...
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Sauropterygia
Sauropterygia ("lizard flippers") is an extinct taxon of diverse, aquatic reptiles that developed from terrestrial ancestors soon after the end-Permian extinction and flourished during the Triassic before all except for the Plesiosauria became extinct at the end of that period. The plesiosaurs would continue to diversify until the end of the Mesozoic. Sauropterygians are united by a radical adaptation of their pectoral girdle, adapted to support powerful flipper strokes. Some later sauropterygians, such as the pliosaurs, developed a similar mechanism in their pelvis. Uniquely among reptiles, sauropterygians moved their tail vertically like modern cetaceans and sirenians. Origins and evolution The earliest sauropterygians appeared about 247 million years ago (Ma), at the start of the Middle Triassic: the first definite sauropterygian with exact stratigraphic datum lies within the Spathian division of the Olenekian era in South China. Early examples were small (around 60 c ...
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Henodontidae
Henodontidae is an extinct family of superficially turtle-like placodonts belonging to the superfamily Cyamodontoidea Cyamodontoidea is an extinct superfamily of placodont marine reptiles from the Triassic period. It is one of the two main groups of placodonts, the other being Placodontoidea. Cyamodontoids are distinguished from placodontoids by their large sh .... Fossils have been found in Germany and Spain.Huene F von 1936. Henodus chelyops, ein neuer Placodontier. Palaeontographica A, 84, 99-147. References Placodonts Prehistoric reptile families Triassic sauropterygians Late Triassic first appearances {{triassic-reptile-stub ...
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Placochelyidae
Placochelyidae is an extinct family of placodonts belonging to the superfamily Cyamodontoidea. Genus *''Glyphoderma'' *''Placochelys'' *''Psephosauriscus'' *''Psephochelys ''Psephochelys (meaning "pebbly turtle")'' is an extinct genus of placodont reptile from the Late Triassic of China. It is represented by a single species, ''Psephochelys polyosteoderma'', named in 2002 on the basis of a single partial skeleton ...'' *'' Psephoderma'' References Placodonts Prehistoric reptile families Triassic sauropterygians Middle Triassic first appearances Late Triassic first appearances {{triassic-reptile-stub ...
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Pararcus
''Pararcus'' is an extinct genus of placodont marine reptile from the Middle Triassic of the Netherlands. The genus is monotypic and the type species is ''Pararcus diepenbroeki''. ''Pararcus'' is known from a holotype skeleton about long from the Lower Muschelkalk of Winterswijk Winterswijk (; also known as ''Winterswiek'' or ''Wenters'') is a municipality and a town in the eastern Netherlands. It has a population of and is situated in the Achterhoek, which lies in the easternmost part of the province of Gelderland in th .... References Placodonts Ladinian genera Middle Triassic reptiles of Europe Fossils of the Netherlands Fossil taxa described in 2013 Sauropterygian genera {{triassic-reptile-stub ...
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Cyamodontidae
Cyamodontidae is an extinct family of superficially turtle-like placodonts belonging to the superfamily Cyamodontoidea. Fossils have been found in Germany and Italy. It is named after ''Cyamodus'', the namesake of the family. Meyer (1863) originally created the family solely for ''Cyamodus''. However, the naming of ''Protenodontosaurus ''Protenodontosaurus'' is an extinct genus of placodont Placodonts ("Tablet teeth") are an extinct order of marine reptiles that lived during the Triassic period, becoming extinct at the end of the period. They were part of Sauropterygia, th ...'' in 1990 by Pinna regrouped the two genera under one family. {{Taxonbar, from=Q2316620 Placodonts Prehistoric reptile families ...
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Atopodentatus
''Atopodentatus'' is an extinct genus of basal sauropterygian known from the early Middle Triassic (Pelsonian substage, Anisian to Ladinian stage) of Luoping County, Yunnan Province, southwestern China. It contains a single species, ''Atopodentatus unicus''. It is thought to have lived between 247 and 240 million years ago, during the Middle Triassic period, about six million years after the Permian extinction. ''Atopodentatus'' was an herbivorous marine reptile, although marine reptiles are usually omnivores or carnivores. A near complete skeleton along with a left lateral portion of the skull were discovered near Daaozi village, Yunnan, China. The scientific name derives from the peculiar zipper-shaped morphology of the holotype specimen's jaws and unique dentition. However, two fossil skulls discovered in 2016 indicate that the holotype skull was badly damaged, and that the living animal actually had a hammer-shaped head with shovel-like jaws. Description ''Atopodentatus'' ...
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Late Triassic
The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series (stratigraphy), series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Geologic time scale, Ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich August von Namoh, Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', t ...
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Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ...
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