This is a list of non-avian dinosaurs whose remains have been recovered from the India n subcontinent or Madagascar . Though widely separated today, the Indian subcontinent and Madagascar were connected throughout much of the Mesozoic and shared similar dinosaur faunas, distinct from what has been found on other modern African and Asian landmasses.
The Indian fossil record of dinosaurs is good, with fossils coming from the entire Mesozoic era – starting with the Triassic period (a geological period that started 251.9 million years ago and continued till 201.3 million years ago), to the Jurassic period (201 million years ago to 145 million years ago) and Cretaceous period (from 145 million years ago to 66 million years ago), when globally all non-avian dinosaurs and 65 per cent of all life became extinct. Madagascar also preserves various unique dinosaurs from the Jurassic and Cretaceous.
Name | Year | Formation | Location | Notes | Images |
---|---|---|---|---|---|
Alwalkeria | 1994 | Lower Maleri Formation (Late Triassic, Carnian) | India | Possessed different types of teeth in its upper jaw | |
Archaeodontosaurus | 2005 | Isalo III Formation (Middle Jurassic, Bajocian to Bathonian) | Madagascar | Retained "prosauropod"-like teeth despite its late age | |
Barapasaurus | 1975 | Kota Formation (Early Jurassic, Sinemurian to Pliensbachian) | India | Several individuals have been found associated with tree trunks, which may represent the aftermath of a flood [1] | |
Brachypodosaurus | 1934 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Has been suggested to be a thyreophoran, but such an identification is unlikely | |
Bruhathkayosaurus | 1987 | Kallamedu Formation (Late Cretaceous, Maastrichtian) | India | Reportedly exceptionally large but its fossils have been lost. [2] Its bones have been informally speculated to be misidentified tree trunks [3] [4] [5] but later research suggests at least the tibia is real [6] | |
Coeluroides | 1933 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Potentially synonymous with Ornithomimoides [7] | |
Compsosuchus | 1933 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Has been suggested to be both an abelisaurid [8] and a noasaurid [9] | |
Dahalokely | 2013 | Ambolafotsy Formation (Late Cretaceous, Turonian) | Madagascar | Shares features of both abelisaurids and noasaurids | |
Dandakosaurus | 1982 | Kota Formation (Early Jurassic, Pliensbachian to Toarcian) | India | Poorly known but large for an early theropod | |
Dryptosauroides | 1932 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Only known from six caudal vertebrae | |
Indosaurus | 1933 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Had a characteristically thickened skull | |
Indosuchus | 1933 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Its skull was flattened and topped by a short crest | |
Isisaurus | 2003 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Unusually proportioned with a short, robust neck and long limbs | |
Jainosaurus | 1995 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Originally named as a species of Antarctosaurus | |
Jaklapallisaurus | 2011 | Upper Maleri Formation (Late Triassic, Norian to Rhaetian) | India | May have been closely related to South American sauropodomorphs [10] | |
Kotasaurus | 1988 | Kota Formation (Early Jurassic, Sinemurian to Pliensbachian) | India | The neural spines of its vertebrae were massively constructed, which is a basal trait | |
Laevisuchus | 1933 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Only known from three vertebrae but can confidently be assigned to the Noasauridae [11] | |
Lametasaurus | 1923 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Described based on now lost remains, it is currently seen as a possible chimera including theropod material and osteoderms of uncertain origin | |
Lamplughsaura | 2007 | Upper Dharmaram Formation (Early Jurassic, Sinemurian) | India | Large and robustly built | |
Lapparentosaurus | 1986 | Isalo III Formation (Middle Jurassic, Bathonian) | Madagascar | Relatively fast-growing as evidenced by the preservation of a large amount of fibrolamellar bone [12] | |
Majungasaurus | 1955 | Maevarano Formation (Late Cretaceous, Maastrichtian) | Madagascar | Bite marks on several specimens have been found to perfectly match the teeth of this genus, suggesting cannibalistic tendencies [13] | |
Masiakasaurus | 2001 | Maevarano Formation (Late Cretaceous, Maastrichtian) | Madagascar | Possessed procumbent teeth at the tips of its jaws which may indicate a feeding specialization | |
Nambalia | 2011 | Upper Maleri Formation (Late Triassic, Norian to Rhaetian) | India | Known from the remains of two individuals | |
Narindasaurus | 2020 | Isalo III Formation (Middle Jurassic, Bathonian to Callovian) | Madagascar | The oldest known turiasaur | |
Ornithomimoides | 1932 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Two species have been named, both from isolated vertebrae | |
Orthogoniosaurus | 1931 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Only known from a single, fragmentary tooth | |
Pradhania | 2007 | Upper Dharmaram Formation (Early Jurassic, Sinemurian) | India | Closely related to Massospondylus [14] | |
Rahiolisaurus | 2010 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Remains of multiple growth stages are known | |
Rajasaurus | 2003 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Possessed a single, short horn on its forehead that may have been used for display and head-butting [15] | |
Rapetosaurus | 2001 | Maevarano Formation (Late Cretaceous, Maastrichtian) | Madagascar | Known from almost the entire skeleton, including the skull | |
Tharosaurus | 2023 | Jaisalmer Formation (Middle Jurassic, Bathonian) | India | The oldest dicraeosaurid, diplodocoid and neosauropod currently known | |
Titanosaurus | 1877 | Lameta Formation (Late Cretaceous, Maastrichtian) | India | Although only known from a few bones, this genus is the namesake of the Titanosauria and the Titanosauriformes | |
Vahiny | 2014 | Maevarano Formation (Late Cretaceous, Maastrichtian) | Madagascar | May have been a rare component of its habitat due to the paucity of its remains |
This is a timeline of selected dinosaurs from the list above. Time is measured in Ma, megaannum, along the x-axis.
The Mesozoic Era is the era of Earth's geological history, lasting from about 252 to 66 million years ago, comprising the Triassic, Jurassic and Cretaceous Periods. It is characterized by the dominance of gymnosperms such as cycads, ginkgoaceae and araucarian conifers, and of archosaurian reptiles such as the dinosaurs; a hot greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic.
Theropoda, whose members are known as theropods, is an extant dinosaur clade that is characterized by hollow bones and three toes and claws on each limb. Theropods are generally classed as a group of saurischian dinosaurs. They were ancestrally carnivorous, although a number of theropod groups evolved to become herbivores and omnivores. Theropods first appeared during the Carnian age of the late Triassic period 231.4 million years ago (Ma) and included the majority of large terrestrial carnivores from the Early Jurassic until at least the close of the Cretaceous, about 66 Ma. In the Jurassic, birds evolved from small specialized coelurosaurian theropods, and are today represented by about 11,000 living species.
Megalosaurus is an extinct genus of large carnivorous theropod dinosaurs of the Middle Jurassic Epoch of southern England. Although fossils from other areas have been assigned to the genus, the only certain remains of Megalosaurus come from Oxfordshire and date to the late Middle Jurassic.
Coelurosauria is the clade containing all theropod dinosaurs more closely related to birds than to carnosaurs.
Ceratosaurs are members of the clade Ceratosauria, a group of dinosaurs defined as all theropods sharing a more recent common ancestor with Ceratosaurus than with birds. The oldest known ceratosaur, Saltriovenator, dates to the earliest part of the Jurassic, around 199 million years ago. Ceratosauria includes three major clades: Ceratosauridae, Noasauridae, and Abelisauridae, found primarily in the Southern Hemisphere. Originally, Ceratosauria included the above dinosaurs plus the Late Triassic to Early Jurassic Coelophysoidea and Dilophosauridae, implying a much earlier divergence of ceratosaurs from other theropods. However, most recent studies have shown that coelophysoids and dilophosaurids do not form a natural group with other ceratosaurs, and are excluded from this group.
Tetanurae is a clade that includes most theropod dinosaurs, including megalosauroids, allosauroids, and coelurosaurs. Tetanurans are defined as all theropods more closely related to modern birds than to Ceratosaurus and contain the majority of predatory dinosaur diversity. Tetanurae likely diverged from its sister group, Ceratosauria, during the late Triassic. Tetanurae first appeared in the fossil record by the Early Jurassic about 190 mya and by the Middle Jurassic had become globally distributed.
Masiakasaurus is a genus of small predatory noasaurid theropod dinosaurs from the Late Cretaceous of Madagascar. In Malagasy, masiaka means "vicious"; thus, the genus name means "vicious lizard". The type species, Masiakasaurus knopfleri, was named after the musician Mark Knopfler, whose music inspired the expedition crew. It was named in 2001 by Scott D. Sampson, Matthew Carrano, and Catherine A. Forster. Unlike most theropods, the front teeth of M. knopfleri projected forward instead of straight down. This unique dentition suggests that they had a specialized diet, perhaps including fish and other small prey. Other bones of the skeleton indicate that Masiakasaurus were bipedal, with much shorter forelimbs than hindlimbs. M. knopfleri was a small theropod, reaching 1.8–2.1 m (5.9–6.9 ft) long and weighing 20 kg (44 lb).
Abelisauridae is a family of ceratosaurian theropod dinosaurs. Abelisaurids thrived during the Cretaceous period, on the ancient southern supercontinent of Gondwana, and today their fossil remains are found on the modern continents of Africa and South America, as well as on the Indian subcontinent and the island of Madagascar. Isolated teeth were found in the Late Jurassic of Portugal, and the Late Cretaceous genera Tarascosaurus, Arcovenator and Caletodraco have been described in France. Abelisaurids possibly first appeared during the Jurassic period based on fossil records, and some genera survived until the end of the Mesozoic era, around 66 million years ago.
Rahonavis is a genus of bird-like theropod from the Late Cretaceous of what is now northwestern Madagascar. It is known from a partial skeleton found by Catherine Forster and colleagues in Maevarano Formation rocks at a quarry near Berivotra, Mahajanga Province. Rahonavis was a small predator, at about 70 centimetres (2.3 ft) long and 0.45-2.27 kg, with the typical dromaesaurid-like raised sickle claw on the second toe. It was originally the first African coelurosaur until the discovery of Nqwebasaurus in 2000.
Dravidosaurus is a controversial taxon of Late Cretaceous reptiles, variously interpreted as either a ornithischian dinosaur or a plesiosaur. The genus contains a single species, D. blanfordi, known from mostly poorly preserved fossils from the Coniacian of southern India.
Megalosauridae is a monophyletic family of carnivorous theropod dinosaurs within the group Megalosauroidea. Appearing in the Middle Jurassic, megalosaurids were among the first major radiation of large theropod dinosaurs. They were a relatively primitive group of basal tetanurans containing two main subfamilies, Megalosaurinae and Afrovenatorinae, along with the basal genus Eustreptospondylus, an unresolved taxon which differs from both subfamilies.
Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 2001.
Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 2006.
The Balabansai Formation is a geological formation in Kazakhstan, Kyrgyzstan and Uzbekistan whose strata date back to the Bathonian and Callovian stages of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation. The lithology primarily consists of variegated sandstones, siltstones, claystones, and rare gravels and marls. Many taxa have been found in the formation, including amphibians and mammals.
Deltapodus is an ichnogenus of footprint produced by a stegosaurian dinosaur According to the main Stegosauria article:
The Jurassic Museum of Asturias is located in the area of Rasa de San Telmo near the parish of Llastres in the municipality of Colunga, Asturias, Spain. Though the municipality of Ribadesella was initially proposed, Colunga was chosen for the building site in the late 1990s. Several landmarks are visible from the museum including the Bay of Biscay, the Sierra del Sueve, and the Picos de Europa. Strategically located over a mount on the Rasa de San Temo, the museum is in the midst the Jurassic Asturias.
Megapnosaurus is an extinct genus of coelophysid theropod dinosaur that lived approximately 188 million years ago during the early part of the Jurassic Period in what is now Africa. The species was a small to medium-sized, lightly built, ground-dwelling, bipedal carnivore, that could grow up to 2.2 m (7.2 ft) long and weigh up to 13 kg (29 lb).