Parvinatator

Parvinatator, from Latin, “parvus” little and “natator” swimmer, is an extinct genus of small ichthyopterygian marine reptile that lived during the Early to Middle Triassic. Its fossils have been found in British Columbia, Canada.[1]

Parvinatator
Temporal range:
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Ichthyopterygia
Family: Parvinatatoridae
McGowan and Motani, 2003
Genus: Parvinatator
Nicholls and Brinkman, 1995
Type species
Parvinatator wapitiensis
Nicholls and Brinkman, 1995

Geological information

The only known Parvinatator fossil was located in an unknown horizon from the Sulfur Mountain Formation in a talus deposit, so its exact geological age is unknown. Best estimates place the fossil somewhere between the Olenekian and Ladinian age around 251-235 mya.[2] Other small ichthyosaurs have been found nearby including Grippia, Utatsusaurus, and Phalarodon.

Historical information / discovery

Parvinatator wapitiensis was discovered in the Sulfur Mountain Formation in British Columbia, Canada, by Elisabeth Nicholls and Don Brinkman in 1995. The only fossil recovered of this genus is a partial skull and two forefins.[1] The skull has been tectonically deformed, partially dis-articulated and broken with the posterior section rotated forward into the orbit. The left forefin is well preserved with only minor overlapping and breakage, while the right forefin is heavily overlapped and broken.[3]

Description and paleobiology

Based on analysis of tooth size relative to the skull width, Parvinatator is estimated to be less than 1 meter long,[2] approximately the same size and general shape of other basal ichthyosaurs, although it is unknown if Parvinatator lacked a dorsal fin like Utatsusaurus and Grippia. Also like other early ichthyosaurs, Parvinatator most likely used an eel-like lateral body movement for propulsion,[4] known as anguilliform. Based on jaw size and tooth shape, Parvinatator is thought to have feed on small fish and cephalopods similarly to other basal ichthyosaurs, as opposed to hard shelled organisms such as mollusks and clams.[3] Ichthyosaurs typically had large eyes suggesting they would hunt in the dark, either at night or in deep water.[5] After the skull's dis-articulated orbit was reconstructed, it matched the approximate shape and typical size of other ichthyosaurs eyes.[3]

Grippia longirostris from the early Triassic is a close relative.

Skull

The fossil of the skull is small, measuring approximately 15 cm in width by 10 cm in height. The skull had been dis-articulated, broken and tectonically deformed, but was reconstructed by Ryosuke Motani, leading to several differences from Nicholls and Brinkman's original description, including; the presence of the squamosal, quadratojugal, and a reduced supratemporal, a lack of contact between the prefrontal and postfrontal, as well as between the jugal and quadratojugal (which was previously identified as the squamosal).[3] Other diagnostic characteristics of the Parvinatator skull are as follows:

Forefin

Utatsusaurus, another close relative.

Unlike some basal ichthyosaurs, Parvinatator's forefin appears well adapted for aquatic life, although it was probably used for controlling pitch rather than locomotion.[9] On the well preserved left forefin of Parvinatator the ulna is reduced in both length and width and smaller than the radius. Several bones of digits 4 and 5 are fused together as well.[1][3]

Phylogeny

There is some disagreement about the exact location of Parvinatator among its relatives. The following phylogeny by Motani places Parvinatator with Utatsusaurus as basal ichthyopterygians but not true ichthyosaurs.[2]

Ichthyopterygia

Utatsusaurus

Parvinatator

Eoichthyosauria
Grippidia

Chaohusaurus

Grippia

Ichthyosauria

Cymbospondylus

Mixosauria

Merriamosauria

Shastasauria

Euichthyosauria

Toretocnemus

Californosaurus

Parvipelvia

Macgowania

Hudsonelpidia

Suevoleviathan

Eurhinosauria

Temnodontosaurus

Thunnosauria

Stenopterygius

Ichthyosaurus

Ophthalmosauria

However, according to Maisch and Matzke in 2000, Parvinatator is a true ichthyosaur and more derived than Utatsusaurus and Grippia.[10]

Ichthyosauria 

Thaisaurus

Utatsusaurus

 Grippidia 

Chaohusaurus

Grippia

Parvinatator

Quasianosteosaurus

 Hueneosauria 

Mixosauria

 Longipinnati 

Toretocnemidae

Cymbospondylidae

Merriamosauria

See also

References

  1. Nicholls, E. & Brinkman, D. (1995). A new ichthyosaur from the Triassic Sulphur Mountain formation of British Columbia. Sarjeant WAS (ed.): Vertebrate fossils and the evolution of scientific concepts: 521–535 London (Gordon & Breach).
  2. Motani, R. (1999). Phylogeny of the Ichthyopterygia. Journal of Vertebrate Paleontology, 19:3, 473-496.
  3. Motani, R. (1997). Phylogeny of the Ichthyosauria (Amniota: Reptilia) with special reference to Triassic forms. Ph.D. dissertation, University of Toronto, Toronto, Ontario, Canada.
  4. Motani, R., You, H., & Mcgowan, C. (1996). Eel-like swimming in the earliest ichthyosaurs. Nature, 382, 347-348.
  5. Motani, R.; Rothschild, B.M.; Wahl, W. (1999). "Large eyes in deep diving ichthyosaurs". Nature. 402: 747.
  6. Maisch, M. (2010). Phylogeny, systematics, and origin of the Ichthyosauria – the state of the art. Palaeodiversity, 3, 151–214.
  7. Maisch, M.W. & Matzke, A.T. (2002). The skull of a large Lower Triassic ichthyosaur from Spitzbergen and its implications for the origin of the Ichthyosauria. Lethaia, 35, 250–256.
  8. Cuthbertson, R. S., Russell, A. P., & Anderson, J. S. (2013). Cranial morphology and relationships of a new grippidian (Ichthyopterygia) from the Vega-Phroso Siltstone Member (Lower Triassic) of British Columbia, Canada. Journal of Vertebrate Paleontology, 33, 831-847.
  9. McGowan, C. (1973). "Differential growth in three ichthyosaurs: Ichthyosaurus communis, I. breviceps, and Stenopterygius quadriscissus (Reptilia, Ichthyosauria)". Life Sciences Contributions Royal Ontario Museum. 93: 1–21.
  10. Maisch, M.W.; Matzke, A.T. (2000). "The Ichthyosauria". Stuttgarter Beitrage zur Naturkunde, Serie B (Geologie und Palaontologie). 298: 1–159.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.