Rahiolisaurus
Rahiolisaurus is a genus of abelisaurid theropod dinosaur which existed in India during the Late Cretaceous period. It was described in 2010, based on fossils recovered from the Lameta Formation in the Indian state of Gujarat. These fossils include elements from at least seven different individuals and are believed to have been from the Maastrichtian stage, sometime between 72.1 and 66 million years ago, making it one of the last non-avian dinosaurs known in the fossil record. Despite representing a variety of different growth stages, all recovered fossils from the locality indicate a single species, the type species Rahiolisaurus gujaratensis.
| Rahiolisaurus Temporal range: Late Cretaceous, | |
|---|---|
| Life restoration of Rahiolisaurus gujaratensis | |
| Scientific classification | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | Theropoda |
| Family: | †Abelisauridae |
| Subfamily: | †Majungasaurinae |
| Genus: | †Rahiolisaurus Novas et al., 2010 |
| Species: | †R. gujaratensis |
| Binomial name | |
| †Rahiolisaurus gujaratensis Novas et al., 2010 | |
Discovery and naming edit
During two expeditions, one in 1995 and the other in 1997, numerous remains of abelisaurids were recovered from a single quarry 50 square metres in area. The collected remains included cervical, dorsal, sacral, and caudal vertebrae, portions of pectoral and pelvic girdles, and several hind limb bones. Because of the unearthing of seven differently sized right tibiae, it was suggested that the assemblage was formed by at least seven individuals of different ontogenetic stages. Within the collection were several duplicate bones, such as the ilia, pubes, femora and tibiae, that exhibited similar morphological features of typical abelisauroid traits. However, despite these remains being of different size gradation and representing growth series, hardly any taxonomic variation was discovered. It was interpreted by Novas et al. that the entire theropod collection from this quarry may be referred to the single species Rahiolisaurus.[1]
Individual bones of the newly discovered abelisaurid was given separate catalogue numbers. The holotype of Rahiolisaurus is represented by a partial association of pelvic elements and a femur that were found in the field. It consists of a right ilium (ISIR 550), a right pubis (ISIR 554), and a right femur (ISIR 557). In addition, an axis (ISIR 658) was found in articulation with cervicals 3 (ISIR 659) and 4 (ISIR 660) and are attributed to the species. These bones are currently housed at the collection of the Geology Museum, Indian Statistical Institute, Kolkata.[1]
Rahiolisaurus was named after the village of Rahioli, located near the fossil site where the dinosaurs remains were discovered. The specific name, gujaratensis, means "from Gujarat" in Latin.[1]
Description edit
Rahiolisaurus was initially described as a large-sized abelisaurid and around 8 metres (26 ft) long and weighing 2 metric tons (2.2 short tons),[1][2] but the allometry-based estimate for different specimens suggest a shorter body length of 6.22–6.75 metres (20.4–22.1 ft).[3] It shares many similarities with another Indian abelisaurid, Rajasaurus, but includes differences such as an overall more gracile and slender-limbed form.[1] Abelisaurids 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.[2] Abelisaurids likely had a bite force similar to Allosaurus at around 3,500 newtons (790 lbf).[4]
Classification edit
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.[5][6]
The following cladogram was recovered by Tortosa (2014):[5]
Palaeoecology edit
Rahiolisaurus 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.[7][8] Rahiolisaurus 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;[9] though eggs belonging to large theropods have been found, it is unknown if they belong to Rahiolisaurus.[10] 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.[11]
Several dinosaurs have been described from the Lameta Formation, such as the noasaurid Laevisuchus; abelisaurids Indosaurus, Indosuchus, Lametasaurus, and Rajasaurus; 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.[12] Dinosaurs in India probably went extinct due to volcanic activity around 350,000 years before the Cretaceous–Paleogene boundary. They likely avoided areas with volcanic fissure vents and lava flows.[13]
See also edit
References edit
- ^ a b c d e Novas, Fernando E., Chatterjee, Sankar, Rudra, Dhiraj K., Datta, P.M. (2010). "Rahiolisaurus gujaratensis, n. gen. n. sp., A New Abelisaurid Theropod from the Late Cretaceous of India" in: Saswati Bandyopadhyay (ed.): New Aspects of Mesozoic Biodiversity. Springer Berlin / Heidelberg. pp. 45–62. doi:10.1007/978-3-642-10311-7. ISBN 978-3-642-10310-0.
- ^ a b Paul, G. S. (2010). The Princeton Field Guide to Dinosaurs. Princeton University Press. pp. 84–86. ISBN 978-0-691-13720-9.
- ^ Grillo, O. N.; Delcourt, R. (2016). "Allometry and body length of abelisauroid theropods: Pycnonemosaurus nevesi is the new king". Cretaceous Research. 69: 71–89. doi:10.1016/j.cretres.2016.09.001.
- ^ Delcourt, R. (2018). "Ceratosaur Palaeobiology: New Insights on Evolution and Ecology of the Southern Rulers". Scientific Reports. 8 (9730): 9730. doi:10.1038/s41598-018-28154-x. PMC 6021374. PMID 29950661.
- ^ a b Tortosa, T.; Buffetaut, E.; Vialle, N.; Dutour, Y.; Turini, E.; Cheylan, G. (2014). "A new abelisaurid dinosaur from the Late Cretaceous of southern France: Palaeobiogeographical implications". Annales de Paléontologie. 100: 63–86. doi:10.1016/j.annpal.2013.10.003.
- ^ Kapur, V. V.; Khosla, A. (2016). "Late Cretaceous terrestrial biota from India with special reference to vertebrates and their implications for biogeographic connections". Cretaceous Period: Biotic Diversity and Biogeography. 71: 161–172.
- ^ Brookfield, M. E.; Sanhi, A. (1987). "Palaeoenvironments of the Lameta beds (late Cretaceous) at Jabalpur, Madhya Pradesh, India: Soils and biotas of a semi-arid alluvial plain". Cretaceous Research. 8 (1): 1–14. doi:10.1016/0195-6671(87)90008-5.
- ^ Mohabey, D. M. (1996). "Depositional environment of Lameta Formation (late Cretaceous) of Nand-Dongargaon inland basin, Maharashtra: the fossil and lithological evidences". Memoirs of the Geological Survey of India. 37: 1–36.
- ^ Tandon, S. K.; Sood, A.; Andrews, J. E.; Dennis, P. F. (1995). "Palaeoenvironments of the dinosaur-bearing Lameta Beds (Maastrichtian), Narmada Valley, Central India" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 117 (3–4): 153–184. doi:10.1016/0031-0182(94)00128-U.
- ^ Lovgren, S. (13 August 2003). . National Geographic News. Archived from the original on December 11, 2003. Retrieved 8 April 2009.
- ^ Sonkusare, H.; Samant, B.; Mohabey, D. M. (2017). "Microflora from Sauropod Coprolites and Associated Sedimentsof Late Cretaceous (Maastrichtian) Lameta Formation of Nand-Dongargaon Basin, Maharashtra". Geological Society of India. 89 (4): 391–397. doi:10.1007/s12594-017-0620-0. S2CID 135418472.
- ^ Weishampel, D. B.; Barrett, P. M.; Coria, R.; Le Loeuff, J.; Xijin, Z.; Xing, X.; Sahni, A.; Gomani, E. M. P.; Noto, C. R. (2004). "Dinosaur Distribution". In Weishampel, D. B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria (2nd ed.). Berkeley: University of California Press. p. 595. ISBN 978-0-520-24209-8.
- ^ Mohabey, D. M.; Samant, B. (2013). "Deccan continental flood basalt eruption terminated Indian dinosaurs before the Cretaceous–Paleogene boundary". Geological Society of India Special Publication (1): 260–267.