Allosauroidea

Allosauroids Temporal range: Ma PreꞒ Ꞓ O S D C P T J K Pg N (Possible Late Toarcian and Late Maastrichtian records)
Allosaurus fragilis skull, San Diego Natural History Museum
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Clade:	Dinosauria
Clade:	Saurischia
Clade:	Theropoda
Clade:	†Carnosauria
Superfamily:	†Allosauroidea Marsh, 1878
Type species
† Allosaurus fragilis Marsh, 1877
Subgroups[3]
†Asfaltovenator[1] †Xuanhanosaurus †Erectopus †Unquillosaurus? †Scipionyx? †Metriacanthosauridae †Piatnitzkysauridae?[1] †Allosauria †Allosauridae †Carcharodontosauria †Datanglong? †Lusovenator †Siamraptor[2] †Ulughbegsaurus? †Carcharodontosauridae †Neovenatoridae †Megaraptora?

Allosauroidea is a superfamily or

Allosauroids share certain distinctive features, one of which is a triangular-shaped

Allosauroids maintained a similar center of mass across all sizes, which is found to be between 37% and 58% of the femoral length anterior to the hip. Other similarities across all allosauroids include the structure of their hind limb and pelvis. The pelvis in particular is thought to be designed to reduce stress regardless of body size. In particular, the way the femur is inclined reduces the bending and torsion stress. Furthermore, like other animals with tails, allosauroids possess a caudofemoralis longus (CFL) muscle that allowed them to flex theirs. Larger allosauroids are found to have a lower CFL muscle-to-body-mass proportion that smaller allosauroids.^[12]

In addition to body similarities, allosauroids are also united by certain skull features. Some of the defining ones include a smaller mandibular fenestra, a short quadrate bone, and a short connection between the braincase and the palate.^[20] Allosauroid skulls are about 2.5 to 3 times longer as they are tall.^[19] Their narrow skull along with their serrated teeth allow allosauroids to better slice flesh off of their prey. Allosauroid teeth are flat and have equally-sized denticles on both edges. The flat side of the tooth face the sides of the skull, while the edges align on the same plane as the skull.^[21] From analyzing the skull of different allosauroids, the volume of the cranial vault ranges between 95 milliliters in Sinraptor to 250 milliliters in Giganotosaurus.^[22]

Allosaurus and Concavenator preserve skin impressions showing their integument. In Allosaurus, skin impressions showing small scales measuring 1-3 mm are known from the side of the torso and the mandible. Another skin impression from the ventral side of the neck preserves scutes. An impression from the base of the tail preserves larger scales around 2 cm in diameter. However, it has been noted that these may be sauropod scales due to their similarity and the fact that non-theropod remains were discovered associated with the tail of this particular Allosaurus specimen.^[23] Concavenator preserves scutes on the underside of the tail, as well as scutes on the feet along with small scales. A series of knobs on the ulna of Concavenator have been interpreted by some authors as quill knobs theorized to have supported primitive quills;^[24] however this interpretation has been questioned, and they have been suggested to represent traces of ligaments instead.^[25]

Classification

The

The cladogram presented here is simplified after the 2012 analysis by Carrano, Benson and Sampson after the exclusion of three "wildcard" taxa Poekilopleuron, Xuanhanosaurus and Streptospondylus.^[3]

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:^[1]

Carnosauria	Monolophosaurus Spinosauridae Megalosauridae Allosauroidea Xuanhanosaurus Piatnitzkysauridae Asfaltovenator Metriacanthosauridae Allosaurus Carcharodontosauria

Paleobiology and behavior

Multiple severe injuries have been found on allosauroid remains, which implies that allosauroids were frequently in dangerous situations and supports the hypothesis of an active, predatory lifestyle. Despite the multitude of injuries, only a few of those injuries show signs of infection. For those injuries that did become infected, the infections were usually local to the site of the injury, implying that the allosauroid immune response was able to quickly stop any infection from spreading to the rest of the body. This type of immune response is similar to modern reptilian immune responses; reptiles secrete fibrin near infected areas and localize the infection before it can spread via the bloodstream.^[13]

The injuries were also found to be mostly healed. This healing may indicate that allosauroids had an intermediate metabolic rate, similar to non-avian reptiles, which means they require fewer nutrients in order to survive. A lower nutrient requirement means allosauroids do not need to undertake frequent hunts, which lowers their risk of sustaining traumatic injuries.^[13]

Although the remains of other large theropods like tyrannosaurids bear evidence of fighting within their species and with other predators, the remains of allosauroids do not bear much evidence of injuries from theropod combat. Most notably, despite a good fossil record, allosauroid skulls lack the distinctive face-biting wounds that are common in tyrannosaurid skulls, leaving open the question of if allosauroids engaged in interspecies and intraspecies fighting.^[27] Allosauroid remains are also often found in groups, which implies social behavior. While there are alternative explanations for the groupings, like predator traps or habitat reduction due to drought, the frequency of finding allosauroid remains in groups supports the social animal theory. As social animals, allosauroids would share the burden of hunting, allowing injured members of the pack to recover faster.^[13]

Paleobiogeography

The paleobiogeographical history of allosauroids closely follows the order that Pangaea separated into the modern continents.^[28] By the Middle Jurassic period, tetanurans had spread to every continent and diverged into the allosauroids and the coelurosaurs.^[18] Allosauroids first appeared in the Middle Jurassic period and were the first giant taxa (weighing more than 2 tons) in theropod history. Along with members of the superfamily Megalosauroidea, allosauroids were the apex predators that occupied the Middle Jurassic to the early Late Cretaceous periods.^[4] Allosauroids have been found in North America, South America, Europe, Africa, and Asia.^[28] Specifically, a world-wide dispersal of carcharodontosaurids likely happened in the Early Cretaceous. It has been hypothesized that the dispersal involved Italy's Apulia region (the “heel” of the Italian peninsula), which was connected to Africa by a land bridge during the Early Cretaceous period; various dinosaur footprints found in Apulia support this theory.^[26]

Allosauroids were present in both the northern and southern continents during the Jurassic and Early Cretaceous, but they were later displaced by the tyrannosauroids in North America and Asia during the Late Cretaceous. This is likely due to regional extinction events, which, along with increased species isolation through the severing of land connections between the continents, differentiated many dinosaurs in the Late Cretaceous.^[18]

References

Further reading

• Currie, P. J.; Zhao, X. (1993). "A new carnosaur (Dinosauria, Theropoda) from the Upper Jurassic of Xinjiang, People's Republic of China" (PDF). Canadian Journal of Earth Sciences. 30 (10): 2037–2081.
  doi:10.1139/e93-179
  .
• Holtz, T. R., Jr. and Osmólska H. 2004. Saurischia; pp. 21–24 in D. B. Weishampel, P. Dodson, and H. Osmólska (eds.), The Dinosauria (2nd ed.), University of California Press, Berkeley.
• Sereno, P. C. (1997). "The origin and evolution of dinosaurs" (PDF). Annual Review of Earth and Planetary Sciences. 25: 435–489.
  doi:10.1146/annurev.earth.25.1.435
  .
• Sereno, P. C. (1998). "A rationale for phylogenetic definitions, with application to the higher-level taxonomy of Dinosauria". Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 210: 41–83.
  doi:10.1127/njgpa/210/1998/41
  .
• Fernandes De Azevedo, Rodrigo P.; Simbras, Felipe Medeiros; Furtado, Miguel Rodrigues; Candeiro, Carlos Roberto A.; Bergqvist, Lílian Paglarelli (2013). "First Brazilian carcharodontosaurid and other new theropod dinosaur fossils from the Campanian–Maastrichtian Presidente Prudente Formation, São Paulo State, southeastern Brazil". Cretaceous Research. 40: 131–142.
  doi:10.1016/j.cretres.2012.06.004
  .

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