Plants and animals related to Asian species are found to the north-west. Australasian species are found mainly to the south-east, with some Asian species. The line is named after Alfred Russel Wallace, who noticed this clear dividing line during his travels through the East Indies in the 19th century.
The distance between Bali and Lombok is only about 35 kilometers. Surprisingly, the distributions of many bird species observe the line, because many birds do not cross even the smallest stretches of open ocean water. Some bats have distributions that cross the Wallace Line, but other mammals are generally limited to one side or the other; an exception is the Crab-eating Macaque. Other groups of plants and animals show differing patterns, but the overall pattern is striking and reasonably consistent.
The term 'Wallace's Line' was first used by Huxley in 1868.
The root cause of Wallace's line is that the ancient supercontinent Gondwana was separated entirely from other parts of the world after Pangaea broke up. Australasia and its smaller islands were part of Gondwana, and that is why their fauna is so different from that of south-east Asia. Wallace's line marks where part of the old Gondwana plate touches part of the old Laurasia plate.
During Quaternary ice age cold periods, when the ocean levels were up to 120 m lower, both Asia and Australia were joined with their respective islands. The deep water between those two large continental shelf areas was — for over 50 million years — a barrier that kept the flora and fauna of Australia separated from that of Asia. Wallacea consists of islands that were never recently connected by dry land to either of the continental land masses, and thus was populated by organisms capable of crossing the straits between islands. 'Weber's Line' runs through this area (rather to the east of centre), at the tipping point between dominance by species of Asian vs. species of Australian origin.
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Wallace's Line delineates Australian and Southeast Asian fauna. The probable extent of land at the time of the last glacial maximum, when the sea level was more than 110 m lower than today, is shown in grey. The deep water of the Lombok Strait between Bali and Lombok formed a water barrier even when lower sea levels linked the now-separated islands and landmasses on either side.
Wallace Line Facts for Kids. Kiddle Encyclopedia.