Main
Isisaurus (Indian Statistical Institute (ISI) Lizard) is a genus of titanosaurian sauropod dinosaur that lived in the Lameta Formation, India, as well as the Pab Formation, Balochistan, west Pakistan, 70 - 66 million years ago, during the Maastrichtian stage of the Late Cretaceous Period.
Paleobiology[]
Size and Physique[]

Isisaurus is a medium-sized sauropod, 18 meters (60 feet) long, and weighing 15 metric tons (17 short tons),[1] with a humerus length of 1.5 meters (5 feet).[2] It is known from well-preserved postcranial materials, better remains compared to other titanosaurs at the time of its description. It is said to have a robust, compact skull, made to feed from several types of tree leaves, evidence supported by coprolites (fossilized dung) believed to belong to Isisaurus containing at least four types of parasitic fungi known to infect tree leaves.[3]
Prehistoric Planet's Portrayal[]
Main: Isisaurus on Prehistoric Planet
Main: Isisaurus on Prehistoric Planet
As is the case for Rajasaurus, an abelisaur that lived alongside this titanosaur, Prehistoric Planet depicts Isisaurus with red skin covered in black splotches, a color scheme that, in tandem with its rugged appearance, helps it blend in with the rocky volcanic environment it is found in. Its mouth and horizontal stripes on the underside of its black neck are colored grayish-white, and it also has a row of spines running from the back of its head to the tail, much like Austroposeidon. These features and color scheme give Isisaurus an overall iguana-esque appearance, fitting given how the practice of the Isisauruses climbing up to the summits of volcanoes to bury their eggs in the warm soil is very much like what land iguanas of the Galapagos Islands do today.[4]
The juveniles, aside from having larger eyes, smaller back spines, and overall different proportions from the adults as expected, also have a protrusion poking from the center of their upper lip. This projection, known as an "egg tooth", is a temporary tool that birds, reptiles, and monotremes grow as hatchlings to help them break out of their eggs, with this tooth eventually falling off or getting reabsorbed by the bill or mouth as they grow older.

Isisaurus was featured twice in Badlands. The episode's first segment is about the dangerous journey of the females through the fields of The Deccan to lay their eggs in the warm soil of a caldera, and the fifth, final segment of the episode shows the eggs hatching months later, with the newborn sauropods rushing back through The Deccan to rejoin their mothers' herds in the forests, encountering dangers from boiling mud pits to opportunistic Rajasauruses along the way. The Uncovered segment "Were Dinosaurs Good Parents?" discusses the several strategies dinosaurs had to protect or raise their eggs and young, with direct evidence of dinosaur eggs in The Deccan being brought up to show that dinosaurs have been relying on the geothermal heat of volcanic regions to incubate their eggs much like some animals do today. Isisaurus, along with the other sauropods that appeared in the first two seasons of Prehistoric Planet (except for the Nemegt Forest Titanosaur), is also featured on the Uncovered segment "How Did Dinosaurs Get So Big?"
Paleoecology[]
Paleoenvironment[]
Main: Lameta Formation
Main: Lameta Formation

― David Attenborough, Badlands
Isisaurus lived 70 - 66 million years ago in the Lameta Formation in the Gujarat State of India as well as the Pab Formation in Balochistan, west Pakistan. The Lameta Formation is associated with the Deccan Traps, one of the largest volcanic features on Earth.

― David Attenborough, Badlands
The Lameta Formation is interpreted as a semi-arid landscape, though later, more recent studies suggest that it is more of a tropical humid region with rivers, lakes,[5][6] and, as shown on Prehistoric Planet, forests past the jagged terrain of the central Indian badlands. The intense volcanic activity of the Deccan Traps by that time, combined with the tropical climate of the area, subjected Late Cretaceous central India to rainfall of around 1,760 - 1,860 millimeters (69.3 - 73.3 inches) per year, higher than the annual precipitation of modern-day India during a monsoon, around 1,200 millimeters (47.2 inches).[7] These conditions would have maintained a tropical or subtropical biome, an idea supported by four leaf-infecting parasitic fungi found within coprolites attributed to Isisaurus.[3]
Paleofauna[]

The Lameta Formation is known as the nesting grounds of titanosaurs like Isisaurus, Jainosaurus, and the dubious Titanosaurus, with evidence showing that the animals used the geothermally-heated volcanic sand of the region to incubate their eggs.[8][PhP 1] These sauropods serve as prey for abelisaurs like Rajasaurus, Indosaurus, Indosuchus, the potentially-dubious Lametasaurus, and Rahiolisaurus gujaratensis. Other animals in the region include noasaurids like Laevisuchus and the dubious Compsosuchus, possible ornithischians (including one mistaken for a late-surviving stegosaur), snakes like Madtsoia and its relative Sanajeh, and the side-necked turtle Jainemys.

― David Attenborough, Badlands
Isisaurus and its contemporaries were among the last non-avian dinosaurs on Earth prior to the Cretaceous-Paleogene Extinction Event, a catastrophe that wiped out three-quarters of life on Earth. However, at least one study theorizes that all Indian dinosaurs may have actually been killed off by a massive eruption in the Deccan Traps 350,000 years before the arrival of the asteroid that wiped out the non-avian dinosaurs.[9]
Nesting Preferences and Parental Habits[]
― David Attenborough, Badlands
The Isisaurus females are shown to be dedicated to making a journey through the treacherous region of The Deccan every spring, braving the dangers and the struggles up steep slopes to higher ground just to lay eggs in the nesting site made ideal by geothermal heating that would keep their eggs warm. The newly-born hatchlings also make this same journey, though given how there is almost nothing for them to eat (except their mothers' dung and the small amount of plants that grow from them) in the desolate volcanic wasteland, where the traps and predators can easily kill hundreds of them in an instant, they do not have much of a choice.
― Dr. Darren Naish, Lead Scientific Consultant
Based on evidence of nesting sites found in different parts of the world,[10] titanosaurs in general seem to be good parents, laying their eggs in warm soil that provides desirable incubation. Lands kept warm by geothermal heating seem to be preferred, and such volcanic areas can also provide secondary benefits, like forming a hostile environment that wards off predators.
― David Attenborough, Badlands
Even so, Isisaurus is depicted as being an r-strategist. Species that follow the r-selection strategy spawn many offspring, and thus do not provide extensive parental care, since most of the juveniles are not expected to reach adulthood, with many dying while many more survive to bring forth the next generation. Once a female has laid her eggs, her young are no longer her concern. Once these babies hatch, they are left to survive the dangers of the world independently, with the only other help given to them coming in the form of unintentional aid, rations such as food, healthy bacteria, and guiding pheromones in the excrement left by their mothers.
Feeding Preferences and Coprophagy[]
― David Attenborough, Badlands
Similar to some modern-day animals, Isisauruses (at least, the juveniles) are shown to be coprophagous, dung-eating. Many creatures, from rodents, rabbits, and pigs, to gorillas, hippos, and elephants, would consume their excrement for various reasons, be it to break down seeds or other undigested food matter for a second time and gain all the possible nutrition from them, to gain the vitamins produced by gut bacteria, or to help their own digestive systems. When such animals are born, their stomach is devoid of the gut bacteria necessary to obtain any nutrition from plants, so it is best for them to get such bacteria from the feces of adults as early as possible.
Gallery[]
References[]
General[]
- ↑ 1.0 1.1 1.2 The Princeton Field Guide to Dinosaurs
- ↑ 2.0 2.1 New titanosaurid (Dinosauria: Sauropoda) from the Late Cretaceous of central India
- ↑ 3.0 3.1 Fungi in dinosaurian (Isisaurus) coprolites from the Lameta Formation (Maastrichtian) and its reflection on food habit and environment
- ↑ Iguanas of the volcanic Galapagos islands
- ↑ Lithofacies architecture and depositional environment of Late Cretaceous Lameta Formation, central India
- ↑ Palaeosols and palaeoclimate reconstruction of the Maastrichtian Lameta Formation, Central India
- ↑ Triple oxygen isotopes in intertrappean fossil woods: Evidence of higher tropical rainfall during Deccan volcanism
- ↑ Palaeoenvironments of the dinosaur-bearing Lameta Beds (Maastrichtian), Narmada Valley, Central India
- ↑ Deccan Continental Flood Basalt Eruption Terminated Indian Dinosaurs before the Cretaceous-Paleogene Boundary
- ↑ What do giant titanosaur dinosaurs and modern Australasian megapodes have in common?
Prehistoric Planet[]
Fauna by Area | |
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Africa | |
Madagascar | |
Morocco | |
America, North | |
Alberta, Canada |
Horseshoe Canyon Formation |
Scollard Formation | |
United States |
Hell Creek and Lance Formations |
Javelina Formation | |
Prince Creek Formation | |
Western Interior Seaway |
|
America, South | |
Argentina | |
Brazil | |
Others | |
Antarctica | |
López de Bertodano Formation |
|
Snow Hill Island Formation |
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Asia | |
China | Nanxiong Formation |
Songliao Basin | |
India |
|
Japan | |
Mongolia | Barun Goyot Formation |
Nemegt Formation | |
Russia | |
Europe | |
Hațeg Island |
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Tethys Ocean |
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Others | |
Oceania | |
New Zealand |
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