Thecodontia
Thecodontia, now considered an obsolete taxonomic grouping, was formerly used to describe a diverse "order" of early archosaurian reptiles that first appeared in the latest Permian period and flourished until the end of the Triassic period. All of them were built somewhat like crocodiles but with shorter skulls, more erect pose and usually somewhat lighter. The group includes the ancestors of dinosaurs, pterosaurs, and crocodilians, as well as a number of extinct forms that did not give rise to any descendants. The term thecodont is still used as an anatomical description of the tooth morphology seen in these species and others.

Dmitry Bogdanov · CC BY-SA 3.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.
On record
Recorded, not inferred- Sits inside
- ArchosauriaPBDB
- Diet
- carnivorePBDB
- Motility
- actively mobilePBDB, for Osteichthyes
- Environment
- terrestrialPBDB, for Diapsida
Time the record covers
At least 45 million years on record.
The record covers at least 247 Mya to 201.4 Mya. No occurrence read is dated outside 251.902 Mya to 174.7 Mya.
25 occurrences of Thecodontia on record, most of them in the Middle Triassic. The Paleobiology Database records this as a living group, and the chart stops with its fossils rather than at the present. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.
When
25 occurrencesThese are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.
Found in
10 formations
- Ermaying Formation8
- Donguz Formation2
- Röt Formation · Upper Buntsandstein Group2
- Zhenzhuchong Formation1
- Lossiemouth Sandstone Formation1
- Elliot Formation · Stormberg Group1
Loading coastlines…
The named rock units Thecodontia has been recovered from, largest first. Drawn where the rock is now, not where it formed. 6 occurrences have no formation on record, which is common for older literature.
Thecodontia and its relatives
Middle TriassicWhere Thecodontia and its relatives were recorded in the Middle Triassic.
Found in the same rock
76 taxa- Shansisuchus shansisuchus6 sites
- Clevosaurus4 sites
- Planocephalosaurus4 sites
- Sigmala4 sites
- Kuehneosaurus3 sites
- Pseudosuchia3 sites
- Archosauria2 sites
- Archosauriformes2 sites
- Capitosauroidea2 sites
- Ceratodus recticristatus2 sites
- Dongusuchus efremovi2 sites
- Kannemeyeriidae2 sites
- Parakannemeyeria2 sites
- Plagioscutum ochevi2 sites
- Proterosuchia2 sites
- Rabidosaurus cristatus2 sites
- Rhadiodromus klimovi2 sites
- Shansiodon wuhsiangensis2 sites
- Sphenodontia2 sites
- Uralosaurus magnus2 sites
- Actinopterygii1 site
- Aetosauria1 site
- Amotosaurus rotfeldensis1 site
- Anomoiodon krejcii1 site
The Paleobiology Database records 25 sites for Thecodontia, and this reads all of them. The number is how many of those sites it was catalogued from too. The 24 sharing the most are listed.
This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.
Entered from
14 references- The pseudosuchians in China8
- The ecology of a Late Triassic reptile assemblage from Gloucestershire, England4
- Tetrapod localities from the Triassic of the SE of European Russia2
- Otuminisaurus limensis Rusconi, 1948: a problematic temnospondyl amphibian from the Triassic of Argentina1
- Dinozavri severnoi Yevrazii: Novye dannye o sostave kompleksov, ekologii i paleobiogeografii [Dinosaurs of northern Eurasia: new data about assemblages, ecology, and paleobiogeography]1
- Dinosaurian Faunas of China1
- Geology and paleontology of the Dockum Formation (Upper Triassic), west Texas and eastern New Mexico1
- Palaeoecology, taphonomy, and dating of Permo-Triassic reptiles from Elgin, north-east Scotland1
- New reptiles from the Middle Triassic in the southern Ural forelands1
- Fossils from the Elliot and Clarens Formations (Karoo Sequence) of the northeastern Cape, Orange Free State and Lesotho, and a suggested biozonation based on tetrapods1
- Suborder Proterosuchia Broom 1906b1
- Les niveaux paléontologiques de première apparition des mammifères primoridaux en Afrique du Sud et leur ichnologie. Establissement de zones stratigraphiques detaillees dans le Stormberg du Lesotho (Afrique du Sud) (Trias Supérieur à Jurassique) [The paleontological levels of the first appearance of primordial mammals in southern Africa and their ichnology. Establishment of detailed stratigraphic zones in the Stormberg of Lesotho (southern Africa) (Upper Triassic to Jurassic).1
Each of the 25 occurrences read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. 2 further references are not listed. Entries link to doi.org where the Paleobiology Database holds an identifier, and to its own record where it does not. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.
Media and terms
Media content1
Picture of Thecodontia
- Source
- Wikipedia/Commons
- Credit
- Dmitry Bogdanov
- Licence
- CC BY-SA 3.0
- Commercial use
- the licence allows it
No 3D scan was found. Smithsonian Open Access, MorphoSource and Sketchfab were all searched.
The description on this site
- Source
- Wikipedia, “Thecodontia”
- Licence
- CC BY-SA 4.0
This is what the site found, which is not the same as what exists.
Keep going
What may have been alongside itArchosauria through timeFormations of the Middle TriassicThe world it lived on
Occurrence data from the Paleobiology Database, CC BY 4.0. (Owen 1859)