Proamphiuma | |
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Scientific classification | |
Kingdom: | |
Phylum: | |
Class: | |
Genus: | †Proamphiuma |
Species: | †P. cretacea |
Type species | |
†Proamphiuma cretacea |
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Proamphiuma is an extinct genus of prehistoric amphibian found in the Bug Creek Anthills in the Hell Creek Formation. [1] [2]
The Caudata are a group of amphibians containing the extant salamanders and all extinct species of amphibians more closely related to salamanders than to frogs. They are typically characterized by a superficially lizard-like appearance, with slender bodies, blunt snouts, short limbs projecting at right angles to the body, and the presence of a tail in both larvae and adults.
The Batrachia are a clade of amphibians that includes frogs and salamanders, but not caecilians nor the extinct allocaudates. The name Batrachia was first used by French zoologist Pierre André Latreille in 1800 to refer to frogs, but has more recently been defined in a phylogenetic sense as a node-based taxon that includes the last common ancestor of frogs and salamanders and all of its descendants. The idea that frogs and salamanders are more closely related to each other than either is to caecilians is strongly supported by morphological and molecular evidence; they are, for instance, the only vertebrates able to raise and lower their eyes. However, an alternative hypothesis exists in which salamanders and caecilians are each other's closest relatives as part of a clade called the Procera, with frogs positioned as the sister taxon of this group.
Apodops is an extinct genus of early caecilians from the Early Eocene Itaboraí Formation of Brazil. The type species of the genus is A. pricei, described based on an isolated and broken trunk vertebra.
The Albanerpetontidae are an extinct family of small amphibians, native to the Northern Hemisphere during the Mesozoic and Cenozoic. The only members of the order Allocaudata, they are thought to be allied with living amphibians belonging to Lissamphibia. Despite a superficially salamander-like bodyform, their anatomy is strongly divergent from modern amphibians in numerous aspects. The fossil record of albanerpetontids spans over 160 million years from the Middle Jurassic to the beginning of the Pleistocene, about 2.13–2 million years ago.
Batrachosauroides is an extinct genus of prehistoric salamander known from several sites across the United States. The two identified species are Batrachosauroides dissimulans and Batrachosauroides gotoi. A proposed, unidentified third species has been proposed by paleontologist James Gardner based on the discovery of a dental fossil in the Bushy Tailed Blowout area of the Lance Formation fossil grounds, but has not been definitively identified as a new species or as part of either of the two identified species.
Comonecturoides is an extinct genus of prehistoric caudate amphibians, possibly a salamander, from Reed's Quarry 9 of the Morrison Formation, near Como Bluff, Wyoming; the type species is C. marshi. It is considered a nomen dubium because the name is based on non-distinctive remains which cannot be classified in detail.
Galverpeton is an extinct genus of prehistoric salamander. It lived during the Barremian-Aptian stages in the Early Cretaceous, in what is now Western Europe. The type species, Galverpeton ibericum, was described by Estes and Sanchíz in 1982. It was found in the Castellar Formation, part of the Galve fossil assemblage. The fossil is in the Institut Paleontologic Miquel Crusafont, Sabadell.
Doleserpeton is an extinct, monospecific genus of dissorophoidean temnospondyl within the family Amphibamidae that lived during the Upper Permian, 285 million years ago. Doleserpeton is represented by a single species, Doleserpeton annectens, which was first described by John R. Bolt in 1969. Fossil evidence of Doleserpeton was recovered from the Dolese Brothers Limestone Quarry in Fort Sill, Oklahoma. The genus name Doleserpeton is derived from the initial discovery site in Dolese quarry of Oklahoma and the Greek root "herp-", meaning "low or close to the ground". This transitional fossil displays primitive traits of amphibians that allowed for successful adaptation from aquatic to terrestrial environments. In many phylogenies, lissamphibians appear as the sister group of Doleserpeton.
Iridotriton is an extinct genus of prehistoric salamander known from a fossil found in stratigraphic zone 6 of the late Jurassic Morrison Formation in the Dinosaur National Monument. One species has been described, Iridotriton hechti. It is likely a member of Cryptobranchoidea.
Horezmia is an extinct Mesozoic genus of prehistoric salamanders. The fossils have been found in Russia. It is comparable to modern advanced salamanders, though its phylogenetic placement within Salamandroidea is uncertain.
Lisserpeton is an extinct genus of prehistoric salamander of the Hell Creek Formation. Its closest living relatives are the mole salamanders.
Kokartus is an extinct genus of prehistoric stem-group salamander (Caudata) from the Middle Jurassic Balabansai Formation of Kyrgyzstan.
Opisthotriton is an extinct genus of prehistoric salamanders that lived in North America between at least the Upper Cretaceous and the Paleocene.
Mioproteus is an extinct genus of prehistoric salamanders from Neogene Europe. Its living relatives are the olm and the mudpuppies. The species M. caucasicus is from the Middle Miocene. The species M. wezei first appears in the fossil record during the Pliocene, then disappears during the Middle Pleistocene.
Prodesmodon is an extinct genus of prehistoric salamander, first described from the Lance Formation.
Paleoamphiuma is an extinct genus of prehistoric salamanders known from the Green River Formation in Wyoming, the United States. It was initially classified within the family Amphiumidae, but Gardner (2003) suggested that it be better placed within the family Sirenidae. The single known specimen measures 39 cm in length. It was named in reference to the extant salamander Amphiuma.
Pangerpeton is an extinct genus of salamanders. Its monotypic species is Pangerpeton sinensis.
Scapherpeton is an extinct genus of prehistoric amphibian. Fossils of it have been found in the Hell Creek Formation.
Eobatrachus is a dubious genus of extinct frog known only from the holotype, YPM 1862, part of the right humerus, found in Reed's Quarry 9 near Como Bluff, Wyoming in the Late Jurassic-aged Morrison Formation. The type, and only species, E. agilis, was named by Othniel Charles Marsh in 1887 and he initially interpreted it as a mammal, although it was later re-classified as a genus of frog related to Comobatrachus and Eobatrachus is now seen as a dubious amphibian genus, possibly belonging to Anura (frogs) according to Foster (2007).
Triassurus is an extinct genus of amphibian, and the oldest member of Caudata. It is known from the Middle to Upper Triassic (Ladinian-Carnian) aged Madygen Formation in Kyrgyzstan. The type species is T. sixtelae.