Megafauna are large animals that roamed the Earth during the Pleistocene Epoch, 1.6 million - 10,000 years ago.

In Australia, Megafauna included the huge wombat-shaped Diprotodon and giant goanna Megalania. European Megafauna included Woolly Rhinoceroses, Mammoths, Cave Lions and Cave Bears. In North American, Megafauna included Giant Ground Sloths and Sabre-toothed Tigers, and African Megafauna included elephants, giraffes, rhinoceroses and hippopotamuses. Africa's Megafauna is all that remains around today.

Extinction theories

The extinction of megafauna around the world was probably due to environmental and ecological factors. It was almost completed by the end of the last ice age. It is believed that megafauna initially came into existence in response to glacial conditions and became extinct with the onset of warmer climates.

In temperate Eurasia and North America, megafauna extinction concluded simultaneously with the replacement of the vast periglacial tundra by an immense area of forest. Glacial species, such as mammoths and woolly rhinocerous, were replaced by animals better adapted to forests, such as elk, deer and pigs. Reindeers (caribou) retreated north, while horses moved south to the central Asian steppe. This all happened about 10 000 years ago, despite the fact that humans colonised North America less than 15 000 years ago and non-tropical Eurasia nearly 1 million years ago.

Tropical and subtropical areas have experienced less radical climatic change. The most dramatic of these changes was the transformation of a vast area of north Africa into the world's largest desert. Significantly, Africa escaped major faunal extinction as did tropical and sub-tropical Asia. The Asian elephant survives until the present day, while the Asian rhinoceros survives even on the relatively small island of Java, Indonesia.