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In geology, Australia (also called Australia-New Guinea, Sahul, Meganesia, Greater Australia, Australasia, or Australinea) is a continent comprising (in order of size) the Australian mainland, New Guinea, Tasmania, and intervening islands, all of which sit on the same continental shelf. These landmasses are separated by seas overlying the continental shelf — the Arafura Sea and Torres Strait between Australia and New Guinea, and Bass Strait between mainland Australia and Tasmania.

When sea levels were lower during the Pleistocene ice age, including the last glacial maximum about 18,000 years ago, the lands formed a single, continuous landmass. During the past ten thousand years, rising sea levels overflowed the lowlands and separated the continent into today's low-lying semi-arid mainland and the two mountainous islands of New Guinea and Tasmania.

Geologically, the continent extends to the edge of the continental shelf, so the now-separate lands can still be considered a continent.^[1] Due to the spread of flora and fauna across the single Pleistocene landmass, the separate lands have a related biota.

New Zealand is not on the same continental shelf and so is not part of the continent of Australia but is part of the submerged continent Zealandia and the wider region known as Oceania.

Australia is classified by the Australian Government Department of Foreign Affairs and Trade as the world's largest island and the world's smallest continent.^[2]

Mainland Australia, with an area of 7.69 million square kilometres, is alternately regarded as either the Earth’s largest island or smallest continent. It stretches about 3700 kilometres from north to south and about 4000 kilometres from east to west.

Geography and nomenclature

The Australian continent is the smallest and lowest-lying human-inhabited continent on Earth, having a total land area of some 8,560,000 square kilometres. Though the Commonwealth of Australia occupies much of the continent and is often mistaken for being the entire continent, Australia and adjacent islands are connected by a shallow continental shelf covering some 2,500,000 square kilometres including the Sahul Shelf^[3][4] and Bass Strait and half of which is less than 50 metres deep.

As Australia the country is largely comprised of a single island, and comprises most of Australia the continent, it is sometimes informally referred to as "the island continent".

Prior to the 1970s, archaeologists called the single Pleistocene landmass by the name Australasia,^[5] although this word is most often used for a wider region that includes lands like New Zealand that are not on the same continental shelf. In the early 1970s they introduced the term Greater Australia for the Pleistocene continent.^[5] Then at a 1975 conference and consequent publication,^[6] they extended the name Sahul from its previous use for just the Sahul Shelf to cover the continent.^[5] A biologist, unaware of the terms used by archaeologists, suggested in 1984 the name Meganesia, meaning "great island" or "great island-group", applying it to both the Pleistocene continent and the present-day lands,^[7] and this name has been taken up by biologists.^[8] However, others have used Meganesia with different meanings: travel writer Paul Theroux included New Zealand in his definition^[9] and others have used it for Australia, New Zealand and Hawaii.^[10] Another biologist, Richard Dawkins, unimpressed with Sahul and Meganesia, coined the name Australinea in 2004.^[11]

Geology

The continent primarily sits on the Indo-Australian Plate. The lands were joined with Antarctica as part of the southern supercontinent Gondwana until the plate began to drift north about 96 million years ago (mya). For most of the time since then, Australia-New Guinea has remained a single, continuous landmass.

When the last ice age ended about 10,000 years ago, rising sea levels formed Bass Strait, separating Tasmania from the mainland. Then about 8,000 to 6,500 years ago, the lowlands in the north were flooded by the sea, separating New Guinea and Australia.

Biology

As the continent drifted north from Antarctica, 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.

Animal groups such as macropods, monotremes, and cassowaries are endemic to Australia. There were three main reasons for the enormous diversity that developed in both plant and animal life.

• While much of the rest of the world underwent significant cooling and thus loss of species diversity, Australia-New Guinea was drifting north at such a pace that the overall global cooling effect was roughly equalled by its gradual movement toward the equator. Temperatures in Australia-New Guinea, in other words, remained reasonably constant for a very long time, and a vast number of different plant and animal species were able to evolve to fit particular ecological niches.
• Because the continent was more isolated than any other, very few outside species arrived to colonise, and unique native forms developed unimpeded.
• Finally, despite the fact that the continent was already very old and thus relatively infertile, there are dispersed areas of high fertility. Where other continents had volcanic activity and/or massive glaciation events to turn over fresh, unleached rocks rich in minerals, the rocks and soils of Australia-New Guinea were left largely untouched except by gradual erosion and deep weathering. In general, fertile soils produce a profusion of life, and a relatively large number of species/level of biodiversity. This is because where nutrients are plentiful, competition is largely a matter of outcompeting rival species, leaving great scope for innovative co-evolution as is witnessed in tropical, fertile ecosystems. In contrast, infertile soils tend to induce competition on an abiotic basis meaning individuals all face constant environmental pressures, leaving less scope for divergent evolution, a process instrumental in creating new species.

For about 40 million years Australia-New Guinea was almost 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 mya.

Eventually, the Australia-New Guinea tectonic plate collided with the Eurasian plate to the north. The collision caused the northern part of the continent to buckle upwards, forming the high and rugged mountains of New Guinea and, by reverse (downwards) buckling, the Torres Strait that now separates the two main landmasses. The collision also pushed up the islands of Wallacea, which served as island 'stepping-stones' that allowed plants from Southeast Asia's rainforests to colonise New Guinea, and some plants from Australia-New Guinea to move into Southeast Asia. The ocean straits between the islands were narrow enough to allow plant dispersal, but served as an effective barrier to exchange of land mammals between Australia-New Guinea and Asia.

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

• Australia
• Australasia
• Oceania
• Plate tectonics
• Paleoclimatology
• Biogeography

References

•  • [ e] Continents of the world

Africa-Eurasia America Eurasia Oceania Africa Antarctica Asia Australia Europe N. America S. America Geological supercontinents Gondwana Laurasia Pangaea Pannotia Proto-Gondwana Proto-Laurasia Rodinia Columbia Kenorland Ur Vaalbara Historical continents Arctica Asiamerica Atlantica Avalonia Baltica Cimmeria Congo craton Euramerica Kalahari Desert Kazakhstania Laurentia Siberia South China Ur Submerged continents Kerguelen Plateau Zealandia     Mythical and theorised continents     Atlantis Lemuria Mu Terra Australis Possible future continents Pangaea Ultima Amasia

•  • [ e] Regions of the world
Africa Central Eastern Northern Southern Western Americas Anglo Caribbean Central Latin Middle North Northern South Asia Central Eastern Northern Southern Southeastern Southwestern / Western Europe Central Eastern Northern Southern Western	Oceania Australasia Melanesia Micronesia Polynesia Other   Asia Pacific Caucasus Far East Indian subcontinent Middle East   Polar Arctic Antarctic Oceans World Arctic Atlantic Indian Pacific Southern
See also