Biogeography

The geographic distribution of organisms on the planet follows patterns that are best explained by evolution in conjunction with the movement of tectonic plates over geological time. Broad groups that evolved before the breakup of the supercontinent Pangaea (about 200 million years ago) are distributed worldwide. Groups that evolved since the breakup appear uniquely in regions of the planet, such as the unique flora and fauna of northern continents that formed from the supercontinent Laurasia, and of the southern continents that formed from the supercontinent Gondwana. The presence of members of the plant family Proteaceae in Australia, Southern Africa, and South America is best explained by their presence on Gondwana prior to the southern supercontinent breaking up.

Two depictions of land masses on Earth with marsupial distribution highlighted. On left, depiction of land masses on Earth during Jurassic Period 160 million years ago. South America, Antarctica and Australia are highlighted and all attached. On right, depiction of land masses on modern day Earth with highlighted areas including parts of USA and Mexico, South America and Australia. "Modern and Jurassic Marsupial Distribution"

Figure 1. Southern supercontinent break-up

The great diversification of marsupials in Australia and the absence of other mammals reflect Australia’s long isolation. Australia has an abundance of endemic species (species found nowhere else) which is typical of islands whose isolation by expanses of water prevents species from migrating. Over time, these species diverge evolutionarily into new species that look very different from their ancestors that existed on the mainland. The marsupials of Australia, the finches of the Galápagos, and many species on the Hawaiian Islands are all unique to their one point of origin, yet they display distant relationships to ancestral species on the mainlands.