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Australia-New Guinea

Although the area known as Australia-New Guinea today includes two very different nations and part of a third, and although the two main landmasses are currently separated by Torres Strait, from the biological and geological points of view, it is a single unit.

The continent of Australia and the large island of New Guinea both sit on top of a single tectonic plate. Both were joined onto Antarctica as part of the southern supercontinent Gondwana until the plate began to drift north about 96 million years ago, and for most of the time since then Australia-New Guinea has remained a single landmass.

As the continent drifted north, a unique flora and fauna developed. Marsupials and monotremes also existed on other continents, but only in Australia-New Guinea did they out-compete the placental mammals and come to dominate. Bird life also flourished, in particular the ancestors of the great passerine order that would eventually spread to all parts of the globe and account for more than half of all living avian species.

There were three main reasons for the enormous diversity that developed in both plant and animal life.

For about 40 million years Australia-New Guinea was completely isolated. During this time, the continent experienced numerous changes in climate, but the overall trend was towards greater aridity. When South America eventually separated from Antarctica, the development of the cold Antarctic Circumpolar Current changed weather patterns across the world. For Australia-New Guinea, it brought a marked intensification of the drying trend. The great inland seas and lakes dried out. Much of the long-established broad-leaf deciduous forest began to give way to the distinctive hard-leaved sclerophyllous plants that characterise the modern Australian landscape.

For many species, the primary refuge was the relatively cool and well-watered Great Dividing Range. Even today, pockets of remnant vegetation remain in the cool uplands, some species not much changed from the Gondwanan forms of 60 or 90 million years ago.

Eventually, the Australia-New Guinea tectonic plate collided with the Indonesian plate to the north. As a result of the collision, the northern part of the continent was buckled upwards, forming the high and rugged mountains of New Guinea and, by reverse (downwards) buckling, the strait that now separates the two main landmasses.

Although New Guinea is the most northerly part of the continent, and could be expected to be the most tropical in climate, the altitude of the New Guinea highlands is such that a great many animals and plants that were once common across Australia-New Guinea now survive only in the tropical highlands (where they are severely threatened by overpopulation pressures).

''See also Plate tectonics, Paleoclimatology, Biogeography