Thunnosauria

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Thunnosaurians
Temporal range: Early Jurassic-Late Cretaceous, 199.6–93.5 Ma
Ichthyosaurus breviceps 2.jpg
Ichthyosaurus breviceps fossil
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Order: Ichthyosauria
Node: Neoichthyosauria
Node: Thunnosauria
Motani, 1999
Subgroups

Thunnosauria (Greek for "tuna lizard" – thunnos meaning "tuna" and sauros meaning "lizard") is an extinct clade of parvipelvian ichthyosaurs from the Early Jurassic to the early Late Cretaceous (HettangianCenomanian) of Asia, Australia, Europe, North America, and South America. Named by Ryosuke Motani in 1999, it contains the basal taxa Ichthyosaurus and Stenopterygius and the family Ophthalmosauridae. In thunnosaurs, the fore fin is at least twice as long as the hind fin.[1][2]

Phylogeny[]

Thunnosauria is a node-based taxon defined in 1999 as "the last common ancestor of Ichthyosaurus communis and Stenopterygius quadriscissus and all of its descendants".[1] The cladogram below follows the topology from a 2010 analysis by Patrick S. Druckenmiller and Erin E. Maxwell.[3]

Thunnosauria 

Ichthyosaurus Ichthyosaurus BW.jpg

Stenopterygius Stenopterygius BW.jpg

"Ophthalmosaurus" natans

 Ophthalmosauridae 

Aegirosaurus

Ophthalmosaurus Ophthalmosaurus BW.jpg

Mollesaurus

Athabascasaurus

Brachypterygius

Arthropterygius

Caypullisaurus

"Platypterygius" hercynicus

"Platypterygius" australis

Platypterygius

Maiaspondylus

"Platypterygius" americanus

References[]

  1. ^ a b Ryosuke Motani (1999). "Phylogeny of the Ichthyopterygia" (PDF). Journal of Vertebrate Paleontology. 19 (3): 472–495. doi:10.1080/02724634.1999.10011160.
  2. ^ Michael W. Maisch & Andreas T. Matzke (2000). "The Ichthyosauria". Stuttgarter Beiträge zur Naturkunde. Serie B. 298: 1–159.
  3. ^ Patrick S. Druckenmiller & Erin E. Maxwell (2010). "A new Lower Cretaceous (lower Albian) ichthyosaur genus from the Clearwater Formation, Alberta, Canada". Canadian Journal of Earth Sciences. 47 (8): 1037–1053. Bibcode:2010CaJES..47.1037D. doi:10.1139/E10-028.


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