Extinct and Fossil Forms
During the early Tertiary period, the Indian tableland, what is today peninsular India, was a large island. Prior to becoming an island it was connected to the African region. During the tertiary period this island was separated from the Asian mainland by a shallow sea. The Himalayan region and the greater part of Tibet lay under this sea. The movement of the Indian subcontinent into the Asian landmass created the great Himalayan ranges and raised the sea bed into what is today the plains of northern India.
Once connected to the Asian mainland, many species moved into India. The Himalayas were created in several upheavals. The Siwaliks were formed in the last and the largest number of fossils of the Tertiary period are found in these ranges.
The Siwalik fossils include Mastodons, hippopotamus, rhinoceros, Sivatherium, a large four-horned ruminant, giraffe, horses, camels, bison, deer, antelope, gorillas, pigs, chimpanzees, orangutans, baboons, langurs, macaques, cheetahs, sabre-toothed cats, lions, tigers, sloth bear, Aurochs, leopards, wolves, dholes, porcupines, rabbits and a host of other mammals.
Many fossil tree species have been found in the intertrappean beds including Grewioxylon from the Eocene and Heritieroxylon keralensis from the middle Miocene in Kerala and Heritieroxylon arunachalensis from the Mio-Pliocene of Arunachal Pradesh and at many other places. The discovery of Glossopteris fern fossils from India and Antarctica led to the discovery of Gondwanaland and led to the greater understanding of continental drift. Fossil Cycads are known from India while seven Cycad species continue to survive in India.
Titanosaurus indicus was perhaps the first dinosaur discovered in India by Richard Lydekker in 1877 in the Narmada valley. This area has been one of the most important areas for paleontology in India. Another dinosaur known from India is Rajasaurus narmadensis, a heavy-bodied and stout carnivorous abelisaurid (theropod) dinosaur that inhabited the area near present-day Narmada river. It was 9 m in length and 3 m in height and somewhat horizontal in posture with a double-crested crown on the skull.
Some fossil snakes from the Cenozoic era are also known.
Some scientists have suggested that the Deccan lava flows and the gases produced were responsible for the global extinction of dinosaurs however these have been disputed.
Himalayacetus subathuensis the oldest-known whale fossil of the family Protocetidae (Eocene), about 53.5 million years old was found in the Simla hills in the foothills of the Himalayas. This area was underwater (in the Tethys sea) during the Tertiary period (when India was an island off Asia). This whale may have been capable of living partly on land. Other fossil whales from India include Remingtonocetus approximately 43-46 million years old.
Several small mammal fossils have been recorded in the intertrappean beds, however larger mammals are mostly unknown. The only major primate fossils have been from the nearby region of Myanmar.
- See also Geology of India
Read more about this topic: Fauna Of India
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