Batrachosauroididae

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Batrachosauroididae
Temporal range: Campanian–Miocene
Batrachosauroididae.png
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Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Amphibia
Subclass: Lissamphibia
Superorder: Batrachia
Clade: Caudata
Family: Batrachosauroididae
Auffenberg, 1958
Synonyms

Batrachosauridae

Batrachosauroididae is an extinct family of prehistoric salamanders with holarctic distribution. They were paedomorphic and presumably aquatic. They are possibly the sister taxon of Proteidae, an extant family of aquatic salamanders. [1] They are definitively known from the Late Cretaceous to Miocene of North America and Europe. Remains from the earliest Cretaceous (Berriasian) Lulworth Formation of England have tenatively been attributed to this family. [2]

The following genera are included: [3]

See also

Related Research Articles

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<span class="mw-page-title-main">Giant salamander</span> Family of amphibians

The Cryptobranchidae are a family of fully aquatic salamanders commonly known as the giant salamanders. They include some of the largest living amphibians. The family is native to China, Japan, and the eastern United States. Giant salamanders constitute one of two living families—the other being the Asiatic salamanders belonging to the family Hynobiidae—within the Cryptobranchoidea, one of two main divisions of living salamanders.

<span class="mw-page-title-main">Podocnemididae</span> Family of turtles

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<span class="mw-page-title-main">Proteidae</span> Family of amphibians

The family Proteidae is a group of aquatic salamanders found today in the Balkan Peninsula and North America. The range of the genus Necturus runs from southern central Canada, through the midwestern United States, east to North Carolina and south to Georgia and Mississippi. The range of the olm, the only extant member of the genus Proteus, is limited to the Western Balkans. The fossil record of the family extends into the end of the Late Cretaceous, with Paranecturus being known from the Maastrichtian of North America.

<span class="mw-page-title-main">Choristodera</span> Extinct order of reptiles

Choristodera is an extinct order of semiaquatic diapsid reptiles that ranged from the Middle Jurassic, or possibly Triassic, to the Miocene. Choristoderes are morphologically diverse, with the best known members being the crocodile-like neochoristoderes such as Champsosaurus. Other choristoderans had lizard-like or long necked morphologies. Choristoderes appear to have been confined to the Northern Hemisphere, having been found in North America, Asia, and Europe, and possibly also North Africa. Choristoderes are generally thought to be derived neodiapsids that are close relatives or members of Sauria.

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<i>Necturus</i> Genus of amphibians

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Opisthotriton is an extinct genus of prehistoric salamanders that lived in North America between at least the Upper Cretaceous and the Paleocene.

Piceoerpeton is an extinct genus of prehistoric amphibian, containing species known from the latest Cretaceous, Paleocene and Eocene of North America. It is one of the largest known salamanders at 1.8 metres, and would have approached the cryptobranchid Andrias in size. However, Piceoerpeton is unrelated to the Cryptobranchidae; instead it appears to be a member of the extinct family Scapherpetontidae.

Enneabatrachus is an extinct genus of prehistoric frogs known from the late Jurassic Morrison Formation of the United States and also the Late Jurassic-Early Cretaceous Ksar Metlili Formation of Morocco. The type species is E. hechti, whose remains have been recovered from stratigraphic zone 5.

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<span class="mw-page-title-main">Ellisdale Fossil Site</span>

The Ellisdale Fossil Site is located near Ellisdale in the valley of the Crosswicks Creek, in Monmouth County, New Jersey, United States. The site has produced the largest and most diverse fauna of Late Cretaceous terrestrial animals from eastern North America, including the type specimens of the teiid lizard Prototeius stageri and the batrachosauroidid salamander Parrisia neocesariensis. The site occurs within the basal portion of the Marshalltown Formation, and dates from the Campanian Stage of the Late Cretaceous. The site is classified as a Konzentrat-Lagerstätten resulting from a prehistoric coastal storm.

The geological history of North America comprises the history of geological occurrences and emergence of life in North America during the interval of time spanning from the formation of the Earth through to the emergence of humanity and the start of prehistory. At the start of the Paleozoic Era, what is now "North" America was actually in the Southern Hemisphere. Marine life flourished in the country's many seas, although terrestrial life had not yet evolved. During the latter part of the Paleozoic, seas were largely replaced by swamps home to amphibians and early reptiles. When the continents had assembled into Pangaea, drier conditions prevailed. The evolutionary precursors to mammals dominated the country until a mass extinction event ended their reign.

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References

  1. Denton Jr., Robert K. & Robert C. O'Neill (1998). "Parrisia neocesariensis, a new batrachosauroidid salamander and other amphibians from the Campanian of eastern North America". Journal of Vertebrate Paleontology. 18 (3): 484–494. Bibcode:1998JVPal..18..484D. doi:10.1080/02724634.1998.10011076. JSTOR   4523920.
  2. S. E. Evans and G. J. McGowan. 2002. An amphibian assemblage from the Purbeck Limestone Group. Special Papers in Palaeontology68:103-119
  3. "†family Batrachosauroididae Auffenberg 1958". Paleobiology Database. Fossilworks. Retrieved 17 December 2021.