The Brigalow Belt is a wide band of acacia wooded grassland that runs between tropical rainforest of the coast and the semi-arid interior of Queensland, Australia. The Northern and Southern Brigalow Belts are two of the 85 bioregions across Australia and the 15 bioregions (see Interim Biogeographic Regionalisation for Australia) in Queensland. Together they form most of the Brigalow tropical savanna ecoregion.
Location and description
The Northern Brigalow Belt covers just over 13.5 million hectares and reaches down from just north of Townsville, to Emerald and Rockhampton on the tropic, while the Southern Brigalow Belt runs from there down to the Queensland/New South Wales border and a little beyond until the habitat becomes the eucalyptus dominated Eastern Australian temperate forests.
This large, complex strip of countryside covers an area of undulating to rugged slopes, consisting of ranges as well as plains of ancient sand and clay deposits, basalt and alluvium. The Northern Brigalow Belt includes the coal producing Bowen Basin with the nearby Drummond Basin and the fertile Peak Downs areas while the southern belt runs into the huge Great Artesian Basin with the sandstone gorges of the Carnarvon Range of the Great Dividing Range separating the two areas. The south-west side includes the farming area of Darling Downs.
A number of important rivers drain the Brigalow Belt mostly running eastwards towards the coast, including the large Fitzroy River system and the Belyando and Burdekin rivers near the tropic. The south-western areas drain westwards into the Murray-Darling basin via the Maranoa, Warrego and Condamine Rivers.
The northern belt has tropical summer rains and warm weather all year round, while south of the tropic the winter is slightly cooler and there is more year-round rainfall as well as the summer. All along the belt the interior with less than 500 mm of rainfall per year is drier than the coast which may have 750 mm and more.
The characteristic plant communities are woodlands of highly water stress tolerant brigalow, a slender acacia tree which thrives on the clay soil and once covered much of the area especially the fertile lowlands. However most of the brigalow has been cleared to make agricultural land and eucalypt woodlands of silver-leaved and narrow-leaved ironbarks, poplar box and other boxes, blackbutt and coolibah are now more intact especially on the higher slopes.
Dichanthium grasslands are another typical habitat of the area while pockets of thicker woodland of brigalow mixed with Casuarina cristata and Ooline occur in moister valleys and vine thickets, wetlands and softwood scrubs are sometimes found although in their undeveloped state, these specialised micro-habitats are rare today. There is a particularly rich variety of habitats in areas such as Isla Gorge and Blackdown Tableland in the sandstone belt of the Carnarvon Range. The Northern Brigalow Belt is one of fifteen national biodiversity hotspots in Australia.
The region is home to the Unadorned Rock-wallaby and the Black-striped Wallaby, which lives in the areas of vine thicket along with a wingless dung beetle (Onthophagus apterus). Two endangered mammals are found in the Brigalow Belt; the Bridled Nail-tail Wallaby in Taunton and Idalia National Parks, and the burrowing Northern Hairy-nosed Wombat in the grassland and eucalyptus of Epping Forest National Park. Birds found here include Black-throated Finch and Russet-tailed Thrush, while endemic reptiles include the Fitzroy River Turtle.
Threats and preservation
Much of the brigalow woodland has been cleared or radically reduced to the extent that some wildlife, failing to thrive in the altered environment, has become extinct here with a number of the remaining communities threatened or endangered. The clearance of brigalow and poplar box is ongoing as there are a number of nature reserves of which do protect the various types of habitat found in the Belt including brigalow and eucalyptus woodland, grassland, vine thicket, high peaks, sandstone gorges and wetlands however these tend to be located on the sandstone uplands rather than the fertile lowlands, where the brigalow woodlands are still vulnerable to clearance and are often limited to small areas of parkland.[clarification needed] The grasslands of the region are also under threat from introduced pasture grasses such as buffelgrass and weeds such as Congress weed. One particular threat comes from dams and weirs on the Dawson River.
A little more than two per cent of the Brigalow Belt lies within national parks and other protected areas. The largest national parks in the Brigalow Belt are: Taunton (the largest at 115 km2); Epping Forest, Dipperu, Bowling Green Bay, Goodedulla National Park, Chesterton Range National Park, Homevale National Park, Blackdown Tableland National Park, Expedition National Park, and Carnarvon National Park.
Subregions of the Brigalow Belt include Townsville Plains, Bogie River Hills, Cape River Hills, Beucazon Hills, Wyarra Hills, Northern Bowen Basin, Belyando Downs, Upper Belyando Floodout, Anakie Inlier, Basalt Downs, Isaac - Comet Downs, Nebo - Connors Ranges, South Drummond Basin and Marlborough Plains.
- Fensham, R.J.; McCosker, J.C.; Cox, M.J. (1998). "Estimating clearance of Acacia-dominated ecosystems in central Queensland using land-system mapping data". Australian Journal of Botany 46: 305–319. doi:10.1071/bt96129.
- Young, P.A.R., B.A. Wilson, J.C. McCosker, R.J. Fensham, G. Morgan, and P. M. Taylor. 1999. Brigalow Belt. Pages 11/1-11/81 in P. Sattler and R. Williams, editors. The Conservation Status of Queensland's Bioregional Ecosystems. Environmental Protection Agency, Brisbane, Australia
- Thackway, R., and I.D. Creswell. 1995. An Interim Biogeographic Regionalisation for Australia: A framework for establishing a national system of reserves, Version 4. Australian Nature Conservation Agency, Canberra, Australia.
- Arnold, S.; Thornton, C.; Baumgartl, T. (2012). "Ecohydrological feedback as a land restoration tool in the semi-arid Brigalow Belt, QLD, Australia". Agriculture, Ecosystems and Environment 163: 61–71. doi:10.1016/j.agee.2012.05.020.
- Arnold, S., P. Audet, D. Doley, and T. Baumgartl. 2013. Hydropedology and ecohydrology of the Brigalow Belt, Australia: opportunities for ecosystem rehabilitation in semi-arid environments. Vadose Zone Journal, https://www.soils.org/publications/vzj/articles/12/4/vzj2013.03.0052?highlight=&search-result=1)
- Arnold, S., Y. Kailichova, and T. Baumgartl. 2014. Germination of Acacia harpophylla (Brigalow) seeds in relation to soil water potential: implications for rehabilitation of a threatened ecosystem. PeerJ, https://peerj.com/articles/268/
- "Brigalow tropical savanna". Terrestrial Ecoregions. World Wildlife Fund.
- "Expedition National Park: Nature, culture and history". Department of National Parks, Recreation, Sport and Racing. Retrieved 9 July 2013.
- "Australia's Biogeographical Regions". Department of the Environment, Water, Heritage and the Arts, Australian Government. Retrieved 2009-01-13.
- "Australian Natural Resource Atlas". Department of the Environment, Water, Heritage and the Arts, Australian Government.
- Sattler, P. S. and R. D. Williams (1999) (eds)The Conservation Status of Queensland’s Bioregional ecosystems. Environmental Protection Agency, Brisbane
- IBRA Version 6.1 data. (Search in "Title" for "IBRA").