Australian Natural Resources Atlas

Natural Resource Topics

Australian Native Vegetation Assessment 2001

Maria Cofinas, Colin Creighton
National Land and Water Resources Audit, 2001
ISBN 0 642 37128 8

Major vegetation groups and their status in each State & Territory
Northern Territory

Mulga distribution patterns south of Alice Springs, NT

Mulga distribution patterns south of Alice Springs, NT

Photo: Murray Fagg

Key features

The Northern Territory has a diversity of vegetation that is maintained by its variety of climate and soils (Parks and Wildlife Commission, no date):

In the north, the vegetation is typically tropical savanna (eucalypt woodland and eucalypt open woodland with a grassy understorey). This landscape experiences dramatic seasonal changes with intense growth in the wet season (summer) and widespread fires in the dry season (winter). Famous worldwide for the tropical wetlands and rugged sandstone escarpments of Kakadu National Park the wetlands are of importance for conservation, providing breeding areas, habitat and refuge for important wildlife populations (Parks and Wildlife Commission, no date) (Figure 24, Table 19).

From the north a transition area moves from eucalypt woodlands into areas of melaleuca and acacia forests and woodlands and south into the spinifex (hummock grasslands), Mitchell grass (tussock grasslands) and acacia woodlands and shrublands. The vegetation increases in diversity around Alice Springs with areas of mulga, mallee, chenopods, hummock grasslands, small pockets of eucalypt woodlands and salt lakes.

The Northern Territory is the only area in Australia that does not have conspicuous temperate flora.

Bioregions in Northern Territory

Tiwi-Cobourg

This bioregion has gently sloping terrain and includes the mainland Cobourg Peninsula and the Tiwi Islands. It is within the tropical monsoonal north of Australia, with a distinct wet dry season and high temperatures throughout the year.

Major land uses are traditional Indigenous uses and nature conservation.

Arnhem Coast

This bioregion has gently undulating plains and low plateaus and is within the tropical monsoonal north of Australia, with distinct wet and dry seasons, and high temperatures throughout the year. It includes the northern Arnhem coast and Groote Eylandt.

The major land use is traditional Indigenous use.

Darwin Coastal

This bioregion has gently undulating plains and is within the tropical monsoonal north of Australia, with a distinct wet dry season and high temperatures throughout the year. It includes the city of Darwin.

Major land uses are traditional Indigenous uses, nature conservation (including parts of Kakadu National Park and World Heritage Area and Litchfield National Park), urban and other intensive uses and grazing. Approximately 85,000 hectares have been cleared.

Pine Creek

This bioregion consists of hilly to rugged terrain and is within the tropical monsoonal belt of northern Australia.

The region has undergone some localised clearing and the major land uses are grazing, nature conservation (including parts of Kakadu National Park and World Heritage Area and Litchfield National Park), traditional Indigenous uses and other intensive uses including horticulture.

Arnhem Plateau

This bioregion consists of rugged dissected terrain and plateaus and is within the tropical monsoonal belt of northern Australia.

Major land uses are traditional Indigenous uses and nature conservation (including parts of Kakadu National Park and World Heritage Area).

Central Arnhem

This bioregion consists of gently sloping terrain and low hills and is within the tropical monsoonal belt of northern Australia.

The major land use is traditional Indigenous use.

Near Adelaide River, NT

Near Adelaide River, NT

Photo: Murray Fagg

Daly Basin

This bioregion consists of gently undulating plains and scattered low plateau remnants and has a tropical monsoonal climate with distinct wet and dry seasons and high temperatures throughout the year.

The major land use is grazing on native pastures and traditional Indigenous uses with some horticulture, grazing on modified pastures and nature conservation. The region has undergone some clearing (approximately 167,000 ha) for these developments.

Victoria Bonaparte

This region extends into Western Australia and consists of a number of basins and the interior is dominated by the Victoria River Plateau, a large highly dissected plateau up to about 350 m above sea level. It has a dry winter, warm monsoon climate.

The major land use is grazing on native pastures, traditional Indigenous uses and nature conservation.

Ord-Victoria Plains

This bioregion extends into Western Australia and consists of level to gently undulating plains with scattered hills and a climate that is dry, hot and tropical with summer rainfall.

Major land uses are cattle grazing and some nature conservation (e.g. Gregory National Park).

Sturt Plateau

This bioregion consists of gently undulating plains with a hot, summer rainfall climate.

Major land uses are traditional Indigenous uses and cattle grazing.

Gulf Fall Uplands

This bioregion falls mainly in the Northern Territory with a very small part in Queensland. It consists of undulating terrain with scattered low steep hills and a dry, hot, summer rainfall climate.

Major land uses are cattle grazing and traditional Indigenous uses.

Mitchell Grass Downs

This bioregion extends into Queensland and consists of undulating plains with deep heavy clay soils and a hot arid climate.

Major land uses are cattle grazing (with much of the region dependent on the underlying Great Artesian Basin for water) and some nature conservation.

Davenport Murchison Ranges

The bioregion is characterised by a chain of rocky ranges and a hot and dry climate.

Major land uses are grazing, traditional Indigenous uses, minimal use (vacant crown land) and some nature conservation.

Tanami Desert

This bioregion extends into Western Australia and consists of hills and ranges with sand plains and a hot arid climate with summer rain.

Major land uses are traditional Indigenous uses, grazing and some minimal use and nature conservation (Puurta Co-Management Area).

Great Sandy Desert

This bioregion extends into Western Australia and includes extensive sand plains, dune fields, lakes and remnant rocky outcrops with a hot, arid climate. The monoliths Uluru and Kata Tjuta are in the very south-east of the bioregion.

Major land uses are traditional Indigenous uses, grazing and nature conservation (including the Uluru-Kata Tjuta National Park and World Heritage Area).

Burt Plain

This bioregion consists of plains and low rocky ranges with an arid climate.

The major land use is cattle grazing with some traditional Indigenous uses.

Channel Country

This bioregion extends largely into Queensland and South Australia with a small area in New South Wales. It is characterised by low hills and braided river systems with an arid climate that has very dry, hot summers and short, dry winters.

The major land use is cattle grazing.

Simpson-Strzelecki Desert

This bioregion extends into South Australia with small areas in Queensland and New South Wales. It consists of arid dune fields and sand plains.

Major land uses are grazing, minimal use (vacant crown land) and traditional Indigenous uses.

Finke

This bioregion extends into South Australia and consists of arid sand plains, dissected uplands and valleys with a hot arid climate.

The major land use is cattle grazing.

MacDonnell Ranges

This bioregion consists of high relief and foothills with an arid climate modified by the presence of the mountain ranges.

Major land uses are traditional Indigenous uses, nature conservation (including the Finke Gorge and West MacDonnell National Parks) and cattle grazing.

Central Ranges

This bioregion extends into Western Australia and South Australia and consists of ranges and sand plains and has an arid climate.

The major land use is traditional Indigenous uses.

Figure 24: Present  major vegetation groups in the Northern Territory.
Table 19: Area (km²) of pre-European and native vegetation in the Northern Territory*.
Major vegetation group Present Pre-European
Hummock grasslands 490,232 490,363
Eucalypt open woodlands 175,775 175,842
Eucalypt woodlands 123,078 123,992
Tropical eucalypt woodlands/grasslands 107,254 109,430
Acacia shrublands 86,035 86,272
Tussock grasslands 83,613 83,678
Eucalypt open forests 58,471 59,346
Acacia open woodlands 48,703 48,814
Mallee woodlands and shrublands 35,450 35,450
Chenopod shrubs, samphire shrubs and forblands 33,753 33,757
Acacia forests and woodlands 29,866 30,442
Other forests and woodlands 29,497 29,508
Melaleuca forests and woodlands 19,244 19,402
Other grasslands, herblands, sedgelands and rushlands 7,633 7,666
Mangroves, tidal mudflats, samphires and bare areas, claypans, sand, rock, salt lakes, lagoons, lakes 5,410 5,551
Other shrublands 5,294 5,473
Rainforest and vine thickets 977 978
Eucalypt low open forests 70 70
Note: * in order of greatest to smallest area.

Vegetation change

The Northern Territory has the most intact native vegetation of all States and Territories. It has not been significantly affected by intense land use pressure. Approximately 0.60 million hectares of native vegetation has been removed, but this is limited to a few areas, mainly associated with the Daly Basin, Darwin Coastal, Pine Creek and Sturt Plateau bioregions in the north and the MacDonnell Ranges bioregion in the south. Major vegetation groups affected are the tropical eucalypt woodlands/grasslands, eucalypt open forests and other eucalypt woodlands and acacia forests and woodlands.

Agricultural expansion is proposed or underway in some regions and a large proportion of the Territory is grazed. Careful land use planning will ensure that many values of the existing vegetation are conserved and that land uses are sustainable.

An assessment of landscape health in the Northern Territory including factors of clearing, grazing, feral animals and weeds provides a summary on a subregional basis of the landscape stresses (NLWRA 2001c).

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