Rajasaurus
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Rajasaurus ( ) is a genus of carnivorous abelisaurid theropod dinosaur from the Late Cretaceous of India, containing one species: Rajasaurus narmadensis. The bones were excavated from the Lameta Formation in the Gujarat state of Western India, probably inhabiting what is now the Narmada River Valley. It was formally described by palaeontologist Jeffrey A. Wilson and colleagues in 2003 based on a partial skeleton comprising the braincase, spine, hip bone, legs, and tail–a first for an Indian theropod. The dinosaur likely measured , and had a single horn on the forehead which was probably used for display and head-butting. Like other abelisaurids, Rajasaurus was probably an ambush predator. India at this time was an island, due to the break-up of the supercontinent Gondwana, though it is possible animals still were able to migrate to and from nearby continents. The creation of the subfamily Majungasaurinae, and its inclusion of abelisaurids from India, Madagascar, and Europe–including Rajasaurus–further reiterates this. The Lameta Formation has yielded several other dinosaur species, including abelisaurids and titanosaurian sauropods, similar to other Gondwanan landmasses. The area during the Cretaceous was probably forested, and served as nesting grounds for several creatures.
Rajasaurus ( ) is a genus of carnivorous abelisaurid theropod dinosaur from the Late Cretaceous of India, containing one species: Rajasaurus narmadensis. The bones were excavated from the Lameta Formation in the Gujarat state of Western India, probably inhabiting what is now the Narmada River Valley. It was formally described by palaeontologist Jeffrey A. Wilson and colleagues in 2003 based on a partial skeleton comprising the braincase, spine, hip bone, legs, and tail–a first for an Indian theropod. The dinosaur likely measured , and had a single horn on the forehead which was probably used for display and head-butting. Like other abelisaurids, Rajasaurus was probably an ambush predator. India at this time was an island, due to the break-up of the supercontinent Gondwana, though it is possible animals still were able to migrate to and from nearby continents. The creation of the subfamily Majungasaurinae, and its inclusion of abelisaurids from India, Madagascar, and Europe–including Rajasaurus–further reiterates this. The Lameta Formation has yielded several other dinosaur species, including abelisaurids and titanosaurian sauropods, similar to other Gondwanan landmasses. The area during the Cretaceous was probably forested, and served as nesting grounds for several creatures.
Discovery and naming
The Lameta Formation was first discovered in 1981 by geologists working for the Geological Survey of India (GSI), G. N. Dwivedi and Dhananjay Mahendrakumar Mohabey, after being given limestone structures–later recognised as dinosaur eggs–by workers of the ACC Cement Quarry in the village of Rahioli near the city Balasinor in the Gujarat state of western India. The remains of Rajasaurus were found in this fossil-rich limestone bed to which GSI geologist Suresh Srivastava was assigned to excavate on two separate trips from 1982–1983 and 1983–1984. In 2001, teams from the American Institute of Indian Studies and the National Geographic Society, with the support of the Panjab University, joined the study in order to reconstruct the excavated remains. Fragments of Rajasaurus were also found near Jabalpur in Madhya Pradesh in the northern part of the Lameta Formation, namely a piece of the upper jaw. Rajasaurus was then formally described in 2003 by geologist Jeffrey A. Wilson and colleagues. The holotype specimen of Rajasaurus comprises a partial skeleton, GSI Type No. 21141/1-33, which includes the maxillae, premaxillae, braincase, and quadrate bone on the skull; and spine, hip bone, legs, and tail in post-cranial remains. It is the first Indian theropod to have preserved these post-cranial remains. It is possible Rajasaurus, Lametasaurus, and Indosaurus are synonymous, though this cannot be confirmed due to fragmentary remains, and the Lametasaurus specimen has been lost. The generic name Rajasaurus derives from the Sanskrit rāja, meaning 'king, sovereign, chief, or best of its kind' and Ancient Greek sauros, meaning 'lizard'; and its specific name narmadensis refers to the Narmada River in central India near where it was discovered.
Description
In 2010, palaeontologist Gregory S. Paul estimated the body length of Rajasaurus at and weight at . In 2016, its length was estimated to be , with the known vertebrae significantly smaller in size than those of Pycnonemosaurus, Carnotaurus and Ekrixinatosaurus. Rajasaurus closely resembled the Madagascan abelisaurid Majungasaurus. Rajasaurus typically had four fingers, short arms, and, to compensate, a heavily-constructed head which was the primary tool for hunting; however, the skull was short, they probably had modest jaw musculature, and the teeth were short. Rajasaurus probably had a bite force similar to Allosaurus at around . The pelvis and hindlimb bones of the contemporaneous Lametasaurus have been suggested to belong to Rajasaurus, based on shared features in the . It also appears to be from a larger specimen than the holotype.
Classification
Wilson, in 2003, assigned Rajasaurus to the subfamily Carnotaurinae, being more closely related to abelisaurids like Majungasaurus and the South American Carnotaurus than to African abelisaurids–as Africa, he believed, had separated from Gondwana first, and South America, India, and Madagascar were connected via Antarctica–on the basis of several similarities such as the presence of a sagittal crest, neck vertebrae with two air pockets, the configuration of the nasal bones, a fleshy growth ("excrescence") on the frontal bone, and a thick skull roof. However, if this were the case, then African abelisaurids would display endemism and not Rajasaurus. In 2008, palaeontologist Matthew Carrano created the subfamily Brachyrostra for South American abelisaurids as a sister taxon to Carnotaurinae, with the abelisaurids migrating through the Gondwanan continents via small land connections as they broke apart until they were completely separated in the Middle Cretaceous. In 2014, the subfamily Majungasaurinae was erected by palaeontologist Thierry Tortosa to separate the newly discovered European Arcovenator, Majungasaurus, Indosaurus, Rahiolisaurus, and Rajasaurus from South American abelisaurids based on physical characteristics such as elongated antorbital fenestrae in front of the eye sockets, and a sagittal crest that widens into a triangular surface towards the front of the head. Despite large oceanic barriers, it has been suggested that a migration of abelisaurids took place in the Late Cretaceous between Africa, Europe, Madagascar, and India which ultimately isolated South American abelisaurids; it is possible that migration occurred between Europe and India across Africa given its proximity to both, and the volcanic Dras-Kohistan island arc may have allowed island hopping and an indirect path to Asia, though these are still questionable explanations. The following cladogram was recovered by Tortosa (2014): Rajasaurus is distinguished from other genera by its single forehead horn (though Majungasaurus also only has one), the elongated supratemporal fenestrae (holes in the upper rear of the skull), and the ilia bones on the hip which feature a ridge separating the brevis shelf from the hip joint.
Palaeobiology
The horn of Rajasaurus could have been used for display or head-butting with other Rajasaurus individuals. Head-butting, inferred from the lack of shock-absorbing cancellous bone in the skull, could have been both or either low-motion shoving matches like modern day marine iguanas (Amblyrhynchus cristatus), or focused on the neck and the flank like giraffes (Giraffa spp.). The neck muscles, though, in abelisaurids were adapted for withstanding high stress. The horn could have been used for defending territory or for mating matches. Abelisaurids may have been ambush predators, using a bite-and-hold tactic to hunt large prey. The leg bones of Majungasaurus are comparatively short to other similarly-sized theropods, suggesting the dinosaur was comparatively slower–this same condition is seen in Rajasaurus. However, ceratosaurs may have been able to rapidly accelerate.
Palaeoecology
]] Rajasaurus has been found in the Lameta Formation, a rock unit radiometrically dated to the Maastrichtian age of the latest Cretaceous representing an arid or semi-arid landscape with a river flowing through it–probably providing shrub cover near the water–which formed between episodes of volcanism in the Deccan Traps. Rajasaurus likely inhabited what is now the Narmada River Valley. The formation is known for being a sauropod nesting site, yielding several dinosaur eggs, and sauropod herds likely chose sandy soil for nesting; though eggs belonging to large theropods have been found, it is unknown if they belong to Rajasaurus. Sauropod coprolite remains indicate they lived in a forested landscape, consuming plants such as Podocarpus, Araucaria, and Cheirolepidiaceae conifers; cycads; palm trees; early grass; and Caryophyllaceae, Sapindaceae, and Acanthaceae flowering plants. Ferns were also common in India with Osmundaceae, Schizaeales, Dicksoniaceae, Gleicheniaceae and Salviniales being found. The prehistoric snake Sanajeh mainly raided the nests of sauropods for eggs, though it is possible it also targeted smaller theropod eggs. ]] India, by the Late Cretaceous, had separated from Madagascar and South America during the break-up of Gondwana, and Rajasaurus lived on an isolated island, likely causing endemism and unique characteristics not seen in other abelisaurids. However, despite being an island, there is no evidence of endemic animals with unique traits from Late Cretaceous India, perhaps indicating a continued connection to other parts of the world, likely Africa due to its proximity. The similarity between European and Indian sauropod egg taxa suggests an inter-continental migration of animals between India, Europe, and South America during the Cretaceous, despite water barriers. Several dinosaurs have been described from the Lameta Formation, such as the noasaurid Laevisuchus; abelisaurids Indosaurus, Indosuchus, Lametasaurus, and Rahiolisaurus; and the titanosaurian sauropods Jainosaurus, Titanosaurus, and Isisaurus. The diversity of abelisauroid and titanosaurian dinosaurs in Cretaceous India indicates they shared close affinities to the dinosaur life of the other Gondwanan continents, which had similar inhabitants. The dinosaurs in India probably all went extinct due to volcanic activity around 350,000 years before the Cretaceous–Paleogene boundary. Dinosaurs probably avoided areas with volcanic fissure vents and lava flows.
Cultural significance
The Gujarat state has declared the fossil site in Balasinor a "dinosaur park," sometimes called the "Jurassic Park of India" in reference to the 1993 film, in response to the massive rush of tourism, with the crowning attraction being Rajasaurus. In Rahioli, a life-sized statue was erected in honour of its discovery. The Indian theme park Adlabs Imagica features the Rajasaurus River Adventure, a water ride following the fictional "Dr. Roy" through prehistoric times. Rajasaurus also appeared in the "Badlands" episode of Prehistoric Planet, where at least two individuals are shown hunting down Isisaurus hatchlings as they pass through the volcanic fields of the Deccan Traps.
See also
Timeline of ceratosaur research Dryptosauroides Compsosuchus Jubbulpuria Ornithomimoides Orthogoniosaurus
References
External links
"Rajasaurus stalked the banks of Narmada" The Hindu, 2003
Text derived from https://en.wikipedia.org/w/index.php?oldid=1373395422 under CC BY-SA 4.0; modifications have been made.