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Piatnitzkysauridae

From Wikipedia, the free encyclopedia

Piatnitzkysaurids
Temporal range: Early - Late Jurassic, 179–152 Ma
Piatnitzkysaurus, type genus of the Piatnitzkysauridae
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Infraorder: Carnosauria (?)
Family: Piatnitzkysauridae
Carrano, Benson & Sampson, 2012
Type species
Piatnitzkysaurus floresi
Bonaparte, 1979
Genera

Piatnitzkysauridae is an extinct family of megalosauroid or basal allosauroid dinosaurs. It only consists of three to four known dinosaur genera: Condorraptor, Marshosaurus, Piatnitzkysaurus and possibly Xuanhanosaurus. The most complete and well known member of this family is Piatnitzkysaurus, which also gives the family its name.[1]

Description

A skull of Marshosaurus showing the maxilla

So far all known piatnitzkysaurids have only been found in Jurassic deposits of the western hemisphere/New world (however, if Xuanhanosaurus is included than this may expand their range).[2] Piatnitzkysaurus and Condorraptor hail from the Cañadón Asfalto Formation of Argentina, which has been dated from the Toarcian epoch of the Early Jurassic to the Bathonian epoch of the Middle Jurassic (approximately 179 to 168 million years ago). Marshosaurus was found in the Morrison Formation of the United States, which was dated to the Kimmeridgian epoch of the Late Jurassic.

Piatnitzkysaurids were among the first large theropods present in South America, and are evidence for a radiation of basal tetanurans in the middle Jurassic.[1] Although there is support for basal megalosauroid affinities, piatnitzkysaurids also share some traits with allosaurids, such as a 'sigmoidal' humerus. It has been proposed that they are basal Allosaurs or Non Megalosaurian Megalosauroids.

If Piatnitzkysaurids are Megalosauroids, they can be distinguished from other megalosauroids and placed into their own category due to the following synapomorphies (distinguishing features):[1]

In addition, this family shows several reversals to basal Tetanuran traits. These include:[1]

Classification

Life restoration of Piatnitzkysaurus

Piatnitzkysauridae is defined as all members of Megalosauroidea more closely related to Piatnitzkysaurus than to either Spinosaurus or Megalosaurus. Condorraptor, Marshosaurus, and Piatnitzkysaurus were all placed in a clade by Benson in 2010 during a redescription of Megalosaurus.[3] This clade was defined as a family by Carrano et al in 2012. Piatnitzkysauridae has been recovered as the sister taxa to Megalosauria, a clade containing the megalosaurids (such as Megalosaurus and Torvosaurus) and the spinosaurids (such as Spinosaurus and Baryonyx).[1]

Condorraptor and Piatnitzkysaurus are generally grouped together within this family in a clade excluding Marshosaurus. This is not only due to Condorraptor and Piatnitzkysaurus being from the same locality and time period, but also due to them having flat anterior faces of presacral vertebrae as well as a pronounced ventral keel on the anterior dorsal vertebrae.[1][3] Due to the strong resemblance to Piatnitzkysaurus, it has been suggested that the sister taxa Condorraptor could be better interpreted as the result of individual variation within the species, and not as separate taxa. The main noted differences between the two dinosaurs include both a less well developed enemial crest and a first sacral vertebra with a shallower fossa in Condorraptor.[4]

Xuanhanosaurus, a problematic tetanuran with uncertain affinities, was placed as the sister taxon of these three genera when their relation was first observed in 2010.[3] However, due to the incompleteness of Xuanhanosaurus's remains, this placement is considered uncertain. Other studies have considered Xuanhanosaurus a basal tetanuran.[1] Xuanhanosaurus is still sometimes found as a Piatnitzkysauridae.[5]

In 2019, Rauhut and Pol described Asfaltovenator vialidadi, a basal allosauroid displaying a mosaic of primitive and derived features seen within Tetanurae. Their phylogenetic analysis found traditional Megalosauroidea to represent a basal grade of carnosaurs, paraphyletic with respect to Allosauroidea. Because the authors amended the definition of Allosauroidea to include all theropods that are closer to Allosaurus fragilis than to either Megalosaurus bucklandii or Neornithes, the Piatnitzkysauridae was found to fall within Allosauroidea. A cladogram displaying the relationships they recovered is shown below:[6]

Carnosauria

Monolophosaurus

Spinosauridae

Megalosauridae

Allosauroidea

Xuanhanosaurus

Piatnitzkysauridae

Asfaltovenator

Metriacanthosauridae

Allosaurus

Carcharodontosauria

References

  1. ^ a b c d e f g Carrano, M. T.; Benson, R. B. J.; Sampson, S. D. (2012). "The phylogeny of Tetanurae (Dinosauria: Theropoda)". Journal of Systematic Palaeontology. 10 (2): 211–300. doi:10.1080/14772019.2011.630927. S2CID 85354215.
  2. ^ "Piatnitzkysauridae". Paleobiology Database. Retrieved 20 June 2013.
  3. ^ a b c d BENSON, ROGER B. J. (2010-04-01). "A description ofMegalosaurus bucklandii(Dinosauria: Theropoda) from the Bathonian of the UK and the relationships of Middle Jurassic theropods". Zoological Journal of the Linnean Society. 158 (4): 882–935. doi:10.1111/j.1096-3642.2009.00569.x. ISSN 0024-4082.
  4. ^ Novas, Fernando (2009). The Age of Dinosaurs in South America. Indiana University Press. p. 118. ISBN 0253352894.
  5. ^ Rauhut, Oliver (2016). "A new megalosaurid theropod dinosaur from the late Middle Jurassic (Callovian) of north-western Germany: Implications for theropod evolution and faunal turnover in the Jurassic". Palaeontologia Electronica. 19 (2). doi:10.26879/654.
  6. ^ Rauhut, Oliver W. M.; Pol, Diego (2019-12-11). "Probable basal allosauroid from the early Middle Jurassic Cañadón Asfalto Formation of Argentina highlights phylogenetic uncertainty in tetanuran theropod dinosaurs". Scientific Reports. 9 (1): 18826. doi:10.1038/s41598-019-53672-7. ISSN 2045-2322. PMC 6906444. PMID 31827108.
This page was last edited on 10 September 2023, at 18:32
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