Insular India

Insular India was an isolated landmass which became the Indian subcontinent. Across the latter stages of the Cretaceous and most of the Paleocene, following the breakup of Gondwana, the Indian subcontinent remained an isolated landmass as the Indian Plate drifted across the Tethys Ocean, forming the Indian Ocean. The process of India's separation from Madagascar first began 88 million years ago, but complete isolation only occurred towards the end of the Maastrichtian, a process that has been suggested to be the creation of the Deccan Traps. Soon after, the land mass moved northward rather quickly, until contact with Asia was established 55 million years ago. Even then, both landmasses did not become fully united until around 35 million years ago,[1][2] and periods of isolation occurred as recently as 24 million years ago.[3]

Plate tectonic reconstruction of the Tethys realm at 100 Mya; at the start of the Late Cretaceous. During the Late Jurassic, Gondwana began breaking up, eventually pushing Africa and India north across the Tethys and opening up the Indian Ocean

Thus, for a period of 53 million years India retained a degree of isolation, 11 of which it was a complete island continent. This allowed its local biota to follow the typical patterns seen in islands and diversify in unique ways, much as in modern Madagascar, its sister landmass. Faunal interchanges with other landmasses, like Africa and Europe (then an archipelago of islands across the Tethys) occurred during this period, and a considerable Asian influence can already been seen long before contact was made. This rendered India rather peculiar as not just an isolated continent but also a "stepping stone" in the dispersal of many animal and plant clades across Africa, Europe, Madagascar, Asia and possibly even Oceania. Still, several "archaic" clades managed to survive. The vast majority of India's terrestrial vertebrate life was wiped out in the Cretaceous-Paleogene extinction event; only 3 extant tetrapod lineages can trace their ancestry to Cretaceous India. Most of India's few other surviving Gondwanan lineages were outcompeted during the Paleogene by newly-arriving lineages. However, plants and invertebrate fauna were less affected.[4][5]

During the Paleogene, dispersing tetrapod lineages from Asia repopulated India, with some, such as lagomorphs, evolving on the continent.[6] By the time full contact was established, a large percentage of India's old and new indigenous fauna had been outcompeted by Eurasian species. However, several groups like lagomorphs[6] have become widespread across the world, as have floral groups such as dipterocarps, which went on to become dominant tree species throughout much of tropical Asia.[5] A significant portion of Asian mantises also originated on Insular India.[7] The islands of the Seychelles still retain an indigenous herpetofauna, presumably an echo of the amphibian and reptile species seen in India as an island.

  1. ^ Scotese, Christopher R. (January 2001). "The collision of India and Asia (90 mya — present)". Paleomap Project. Retrieved 28 December 2004.
  2. ^ Aitchison, Jonathan C.; Ali, Jason R.; Davis, Aileen M. (2007). "When and where did India and Asia collide?". Journal of Geophysical Research. 112 (B5). Bibcode:2007JGRB..11205423A.
  3. ^ Biotic interchange between the Indian subcontinent and mainland Asia through time. Nat Commun. 2016 Jul 4;7:12132. doi: 10.1038/ncomms12132.
  4. ^ Karanth, K. Praveen (2021). "Dispersal vs. vicariance: the origin of India's extant tetrapod fauna". Frontiers of Biogeography. 13 (1). doi:10.21425/F5FBG48678. S2CID 231519470.
  5. ^ a b Bansal, Mahi; Morley, Robert J.; Nagaraju, Shivaprakash K.; Dutta, Suryendu; Mishra, Ashish Kumar; Selveraj, Jeyakumar; Kumar, Sumit; Niyolia, Deepti; Harish, Sachin Medigeshi; Abdelrahim, Omer Babiker; Hasan, Shaa eldin; Ramesh, Bramasamdura Rangana; Dayanandan, Selvadurai; Morley, Harsanti P.; Ashton, Peter S. (2022-01-28). "Southeast Asian Dipterocarp origin and diversification driven by Africa-India floristic interchange". Science. 375 (6579): 455–460. Bibcode:2022Sci...375..455B. doi:10.1126/science.abk2177. ISSN 0036-8075. PMID 35084986. S2CID 246360938.
  6. ^ a b Rose K.D., Deleon V.B., Mmissian P., Rana R.S., Sahni A., Singh L. & Smith T. (2008). – Early Eocene lagomorph (Mammalia) from western India and the early diversification of Lagomorpha. – Proc. Royal Society B, RSPB 2007.1661.R1
  7. ^ Svenson, Gavin J.; Whiting, Michael F. (October 2009). "Reconstructing the origins of praying mantises (Dictyoptera, Mantodea): the roles of Gondwanan vicariance and morphological convergence". Cladistics. 25 (5): 468–514. doi:10.1111/j.1096-0031.2009.00263.x. PMID 34879623. S2CID 86659271.

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