Temporal range: Triassic
(Anisian to Ladinian, about 247-242 Mya)
|Dorsal view of fossil showing top of skull|
The genus was named in 1887 by George H. Baur. The name means "Mixed Lizard", and was chosen because it appears to have been a transitional form between the eel-shaped ichthyosaurs such as Cymbospondylus and the later dolphin-shaped ichthyosaurs, such as Ichthyosaurus. Baur named Mixosaurus as a new genus because its forefin was sufficiently different from that of Ichthyosaurus.
Mixosaurus includes 3 species. Previously this number was bigger, and Mixosaurus was considered as the most common genus of Triassic ichthyosaurs, whose fossils have been found all over the world, including China, Timor, Indonesia, Italy, Spitsbergen, Svalbard, Canada, as well as Alaska and Nevada in the US.
Mixosaurus was a small to medium-sized ichthyosaur, not growing more than 2 meters in total length with small species not growing more than 1 meter. It possessed a long tail with a low fin, suggesting it could have been a slow swimmer, but also possessed a dorsal fin for stability in the water. The paddle-like limbs were made up of five toes each, unlike the three toes found in later Ichthyosaurs. Noteworthy, however, is that each toe had more individual bones than is usual in reptiles, and the front limbs were longer than the back limbs, both adaptations typical of later ichthyosaurs. The jaws were narrow, with several sharp teeth, that would have been ideal for catching fish. They had relatively large skulls compared to their bodies, unlike the basal ichthyosaurs, but resembled fish-shaped ichthyosaurs that appeared later. They had around 50 vertebrae in front of the pelvic girdle, around twice as many as terrestrial diapsids. Recent studies suggest that genus Mixosaurus may have lived near shore or in a shelf-like habitat as it possesses more compact spongy bone within its long bones than other Ichthyosaurs.
There are 3 species of Mixosaurus currently recognised, Mixosaurus cornalianus, Mixosaurus panxianesis and Mixosaurus kuhnschnyderi. They share many similar characteristics throughout the cranial and post cranial with the main differences morphology occurring in the dental region. Examples of the dental variation are the extent of the dental groove in the upper jaw, the shape and size of the teeth and the number of rows of teeth 
Previous authors assigned to the genus other species, including M. atavus (Quenstedt, 1852), M. callawayi Schmitz et al., 2004, M. xindianensis Chen & Cheng, 2010 and M. yangjuanensis Liu & Yin, 2008.
Mixosaurus cornalianus is the only Triassic ichthyosaur for which completely articulated skeletons have been found. Many specimens have been collected but Mixosaurus cornalianus is not well studied, this is because all of the known specimens have been compressed during the preservation process.
Mixosaurus panxianensis was discovered in the Middle Triassic of the Guizhou Province, China. The specimens have been found in the Guanling Formation, which consists of thinly bedded bituminous limestones and marls.
The specimens found have important Mixosaurid characteristics such as a long sagittal crest along the top of the skull but is seen as a different species because there is no external contact between the jugal and the quadratojugal.
Articulated skeletons have been found and the centra of the vertebrae are higher than they are long. This is evidence for its transitional position between basal early Triassic ichthyosaurs and more derived Jurassic and Cretaceous species; who have disc shaped circular centra of the vertebrae.
In recent years the taxonomy and phylogeny of mixosaurid ichthyosaurs has been a controversial topic. Most recently, Mixosauridae has been separated into Mixosaurinae and the sister group Phalarondontinae. Mixosaurus containing M. cornalianus, M. kuhnschnyderi and M. panxianensis, Phalarodon contains P. fraasi, P. callawayi and P. atavus.
Mixosaurids are characterised by a relatively short and wide humerus and Phalarodon are characterised by the lack of a dental groove in the upper jaw. Phalarodon fossils are found in every major Mixosaur locality.
Mixosaurid species declared as nomen dubium, meaning the description was insufficient to fully classify them as a species, are M. maotaiensis, M. helveticus, M. timorensis, M. major, M. timorensis, M. nordenskioeldii.
It was suggested that Tholodus schmidi should be included in Mixosauridae but only dental material has been found so it is difficult to assign it to a genus.
- Cheng Ji, Da-Yong Jiang, Ryosuke Motani, Olivier Rieppel, Wei-Cheng Hao, and Zuo-Yu Sun (2016). "Phylogeny of the Ichthyopterygia Incorporating Recent Discoveries from South China". Journal of Vertebrate Paleontology. 36 (1): e1025956. doi:10.1080/02724634.2015.1025956.
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- Jun Liu, Ryosuke Motani, Da-Yong Jiang; et al. (2013). "The first specimen of the Middle Triassic Phalarodon atavus (Ichthyosauria: Mixosauridae) from South China, showing postcranial anatomy and peri-Tethyan distribution". Palaeontology. 56 (4): 849–866. doi:10.1111/pala.12021.
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- Houssaye, Alexandra; Scheyer, Torsten M.; Kolb, Christian; Fisher, Valentin; Sander, P. Martin (April 2014). "A New Look at Ichthyosaur Long Bone Microanatomy and Histology: Implications for Their Adaption to an Aquatic Life". PLOS ONE. 9 (4): 1–10. doi:10.1371/journal.pone.0095637.
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- Schmitz.; et al. (2010). "The taxonomic status of Mixosaurus nordenskioeldii". Journal of Vertebrate Paleontology. 25 (4): 983–985. doi:10.1671/0272-4634(2005)025[0983:ttsomn]2.0.co;2.
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