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Plagiosauridae

Description

Plagiosauridae is a clade of temnospondyl amphibians of the Middle to Late Triassic. Deposits of the group are most commonly found in non-marine aquatic depositional environments from central Europe and Greenland, but other remains have been found in Russia, Scandinavia, and possibly Thailand.


Source Data
SourceIDLink
Global Biodiversity Information Facility ID (GBIF)3241136https://www.gbif.org/species/3241136
Rankfamily
Taxonomy (GBIF)Life : Animalia : Chordata : Amphibia : Plagiosauridae
Taxonomic Status (GBIF)accepted
Classification
(GBIF)
RankNameAuthor
familyPlagiosauridae
Scientific NamePlagiosauridae
Wikipediahttps://en.wikipedia.org/wiki/Plagiosauridae

Subtaxa

NameStatusCommon Name(s)Fossil OccurrencesOldestYoungest
Aranetsia
genus
accepted (GBIF)No associated record in PBDB
Gerrothorax
genus
accepted (GBIF)No associated record in PBDB
Megalophthalma
genus
accepted (GBIF)No associated record in PBDB
Melanopelta
genus
accepted (GBIF)No associated record in PBDB
Plagiobatrachus
genus
accepted (GBIF)No associated record in PBDB
Plagiorophus
genus
accepted (GBIF)No associated record in PBDB
Plagiosaurus ✝
genus
accepted (GBIF)
listed (PBDB)
4216 Ma
Late/Upper Triassic
209 Ma
Late/Upper Triassic
Plagioscutum
genus
accepted (GBIF)No associated record in PBDB
Plagiosternum
genus
accepted (GBIF)No associated record in PBDB
Plagiosuchus
genus
accepted (GBIF)No associated record in PBDB

References

Benton, M.J. (ed). (1993). The Fossil Record 2. Chapman & Hall, London, 845 pp. - via The Interim Register of Marine and Nonmarine Genera
SN2000: Brands, S. J. (compiler) 1989-2005. Systema Naturae 2000. Amsterdam, The Netherlands (2006 version). Available online at http://sn2000.taxonomy.nl/. - via The Interim Register of Marine and Nonmarine Genera
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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