| Tratayenia | |
|---|---|
 | |
| Life restoration | |
Scientific classification | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | Theropoda |
| Clade: | †Megaraptora |
| Family: | †Megaraptoridae |
| Genus: | †Tratayenia Porfiriet al., 2018 |
| Type species | |
| †Tratayenia rosalesi Porfiriet al., 2018 | |
Tratayenia is an extinctgenus ofmegaraptorantheropoddinosaurs known from remains found in theSantonian-ageBajo de la Carpa Formation ofArgentina.[1] The type and only species,Tratayenia rosalesi, was described in March 2018.[2]
Tratayenia can be distinguished from other megaraptorans on the basis of threeautapomorphies (unique derived features) of the front portion of each dorsal vertebra, as well as a single autapomorphy of the sacrum.Tratayenia is one of the youngest known genera of megaraptorans, having lived only about 83 million years ago.
The holotype consists of a well-preserved partial skeleton, MUCPv 1162, which includes several articulated portions of thebackbone. One portion of the skeleton is a string of five dorsalvertebrae, likely the seventh to eleventh dorsals. The largest articulated portion of the skeleton is a string of vertebrae including the last two dorsals as well as the fivesacrals and much of the rightilium. Other preserved bones include two partial dorsalribs and fragments of thepubis andischium.[1]
This skeleton was first discovered in 2006 at aBajo de la Carpa Formation fossil site byUniversidad Nacional del Comahue technician Diego Rosales. Shortly thereafter it was excavated by UNC paleontologist Juan D. Porfifi. Porfiri and his colleagues published a preliminary report on the new dinosaur in a 2008 abstract, and suggested that it may have been a relative ofCarcharodontosauridae.[3] In 2018, the new taxon was described with thegeneric nameTratayenia, named after Tratayén, the fossil site at which it was excavated. Thespecific nameTratayenia rosalesi honors Diego Rosales.[1]
Tratayenia was a medium-sized megaraptoran, growing up to 8 metres (26 ft) long. It was closely related to genera such asMegaraptor,Australovenator, andMurusraptor. Like most othermegaraptorans, it probably had large claws on its hands for use in hunting prey. Analysis of the Baja de la Carpa indicates thatTratayenia may have been geologically one of the youngest megaraptorans yet discovered.Tratayenia is also the largest-bodied carnivorous animal named from the Bajo de la Carpa Formation, reinforcing the hypothesis that megaraptorids were apex predators in southern South America from theTuronian through theSantonian or earlyCampanian, following the extinction ofcarcharodontosaurids.[1][2]
The dorsalvertebrae were tall and narrow, with large pits known as pleurocoels on the side of their centra (spool-shaped main portion). These features are common in the vertebrae of large carnivorous theropods. Some of the vertebrae had fragments of bone in the pleurocoels, which were likely remnants of thin bony walls known as septa which divided the pits. Septa are also known in other megaraptorans and carcharodontosaurids. The neural arches of the vertebrae are taller and narrower inTratayenia than in most other theropods. The tubular transverse processes (rib facets) project upwards and to the side. A large and deep excavation is located directly below each transverse process, bounded from the front and rear by thin laminae (ridges). The front edge is formed by the paradiapophyseal lamina and the rear edge is formed by the posterior centrodiapophyseal lamina. These features are also known in the megaraptoranMurusraptor.[1]
Theprezygapophyses (front vertebral joint plates) are rectangular when see from the side, with the front and lower edges converging at nearly a right angle. This is anautapomorphy (unique adaptation) ofTratayenia. A ridge known as a prezygodiapophyseal lamina connects the prezygapophyses to the transverse processes. Another autapomorphy ofTratayenia is that the prezygodiapophyseal lamina is parallel to the paradiapophyseal lamina. Other theropods either have a weakly developed (or absent) paradiapophyseal lamina, or one which is angled relative to the prezygodiapophyseal lamina. The front edge of each vertebra has a third autapomorphy, related to two pairs of laminae (four total) connecting the prezygapophyses to the neural spines. At the base of the neural spines, the two laminae comprising each pair are very close together. But as the laminae get closer to the prezygapophyses, they diverge into a shape akin to an inverted Y. There are two of these inverted Y-like structures visible from the front, for both the left and right sides of a vertebra.[1]
The postzygapophyses (rear vertebral joint plates) are more typical in shape, and the rear edge of each vertebra has a small, blade-likehyposphene which splits into three ridges from below. The neural spines are tall and rectangular when seen from the side, and uniformly thin when seen from the front. Most are completely vertically, but one of the dorsal vertebrae preserved near the hip slightly inclines forward as in variousallosauroids. Preserved rib fragments are curved and hollow. They connected to the vertebrae by means of two distinctcondyles, separated by a large opening which may have been continuous with the inner cavity.[1]
Tratayenia has fivesacral (hip) vertebrae, as is the norm for theropods. They are very similar to the dorsal vertebrae in various aspects, such as the presence of large pleurocoels, tall and narrow centra, and laminae-bound excavations below the transverse processes. However, they only have a single autapomorphy: the anteroposterior (front-to-back) width of the neural spine increases drastically in the second to fifth sacral vertebrae compared to the first vertebra. In fact, the fifth sacral's neural spine is twice as long anteroposteriorly than that of the first. This trait has also been observed inTyrannosaurus and an unnamed megaraptoran sacrum (SNMS 58023) from theRomualdo Member of theSantana Formation inBrazil,[4] so its status as an autapomorphy ofTratayenia is not concrete. Some of the sacral vertebrae have neural spines which are fused together, and the last three curve backwards. The fourth sacral has a shape similar to those of the Santana Formation sacrum.[1]
Theilium (upper blade of the hip) was heavilypneumatized, meaning that it was filled with air pockets. Pneumatization of the ilium is most common in megaraptorans among theropods, as seen in taxa such asAerosteon andMurusraptor. The outer surface of the ilium is perforated by several pneumatic pores, similar to that ofAerosteon, but the upper edge of the bone is straight, in contrast with the curved ilium ofAerosteon. A bone identified as the pubic boot (expanded tip of thepubis) has been found in the holotype, as well as fragments of theischium, which has the form of a long, thin shaft covered in grooves.[1]
Megaraptorans have very controversial relations to other theropods. The first mainstream hypothesis is that they arecarnosaurs, distantly related toAllosaurus and more closely related toNeovenator andcarcharodontosaurids. The second popular hypothesis considers them to be basaltyrannosauroids, part of thecoelurosaur lineage which includes the crestedproceratosaurids as well as the famoustyrannosaurids such asTyrannosaurus.[5] A third hypothesis also considers them to be coelurosaurs, but outside Tyrannosauroidea and basal to practically all other groups of Coelurosauria. Porfiriet al.'s description ofTratayenia prefers this third hypothesis.[1]
Thecladogram below follows the strict consensus (average result) of the 12 mostparsimonious trees (the simplest evolutionary paths, in terms of the total amount of sampled features evolved or lost between sampledtaxa) found by Porfiriet al. (2018)'s phylogenetic analysis.[1] Although the results are different, the methodology analysis was practically identical to that of Apesteguiaet al. (2016), only differing in the fact that it incorporatedTratayenia andMurusraptor, two megaraptorans not sampled in the analysis of Apesteguiaet al.[5]
Tratayenia lived in theBajo de la Carpa Formation alongside manylizards andturtles, thesnake speciesDinilysia patagonica, manybirds such asPatagopteryx deferrariisi, a diverse amount ofcrocodylomorphs and manydinosaurs such asViavenator exxoni andTraukutitan eocaudata.
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