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The Asian elephant became a siege engine, a mount in war, a status symbol, a beast of burden, and an elevated platform for hunting during historical times in South Asia. [137] Ganesha on his vahana mūṣaka the rat, c. 1820. Asian elephants have been captured from the wild and tamed for use by humans.
Articles related to the Asian elephant (Elephas maximus), a species of elephant distributed throughout the Indian subcontinent and Southeast Asia, from India in the west to Borneo in the east, and Nepal in the north to Sumatra in the south. Three subspecies are recognised—E. m. maximus, E. m. indicus and E. m. sumatranus.
Asian elephants once ranged from Western to East Asia and south to Sumatra. [150] and Java. It is now extinct in these areas, [149] and the current range of Asian elephants is highly fragmented. [150] The total population of Asian elephants is estimated to be around 40,000–50,000, although this may be a loose estimate.
African elephant heads are completely rounded and large, while Asian elephant heads form two hills or humps on the top, with a line down the center of their face. African Elephant vs. Asian ...
The pre-eminent threats to the Asian elephant today are habitat loss, degradation, and fragmentation, which are driven by an expanding human population, and lead in turn to increasing conflicts between humans and elephants when elephants eat or trample crops. Hundreds of people and elephants are killed annually as a result of such conflicts.
The earliest members of the modern genera of Elephantidae appeared during the latest Miocene–early Pliocene around 5 million years ago. The elephantid genera Elephas (which includes the living Asian elephant) and Mammuthus (mammoths) migrated out of Africa during the late Pliocene, around 3.6 to 3.2 million years ago. [16]
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Elephas is a genus of elephants and one of two surviving genera in the family Elephantidae, comprising one extant species, the Asian elephant (E. maximus). [1] Several extinct species have been identified as belonging to the genus, extending back to the Pliocene or possibly the late Miocene .