1.1.7.1 Ecological systems


The Macquarie, Castlereagh and Bogan river basins covers an area of approximately 85,000 km2 and is home to approximately 185,000 people. It contains a large variety of vegetation, landforms and communities, including 82 broad vegetation types that provide habitat for over 550 vertebrates (Central West CMA, 2011a). Many species and communities are listed as threatened or endangered (Central West CMA, 2011b). Land use in the Macquarie-Bogan river basin is dominated by extensive agriculture with over 80% of the river basin being used for grazing, 9% for dryland cropping and 5% for forestry, conservation and other native landscapes (Green et al., 2011). More information on land use is provided in Section 1.1.2.2.3 .

Broadly speaking, the Macquarie, Castlereagh and Bogan river basins can be subdivided into three areas in an east to west direction: the central west tablelands, the central west slopes and the central west plains. This broad gradation depicts regional scale changes in landforms and climates. The central west tablelands, which are mostly upstream from the subregion, generally have an elevation of between 450 and 1000 m. The topography through this area is mostly undulating to hilly and there can be significant variation in soils over very short distances. Soils are mostly derived from sandstone granite shale/slate and basalt parent materials (Central West CMA, 2008c).

The slopes area lies west of the tablelands area at lower altitudes of between 250 and 700 m above sea level. The topography ranges from steep hills to gently undulating landscapes and alluvial river plains. The geology is based on a series of faults and folds of sedimentary parent material in the southern part of the area, interspersed with granite intrusions and basalts from old volcano and overland flows. The northern part of the slopes region is made up of the southernmost edge of the Great Artesian Basin. Soils range from highly fertile alluvium and basalts to deep sands of the Pilliga Sandstone. Soil salinity is a major issue, particularly in the Talbragar and Little river basins (Central West CMA, 2008b).

The plains area lies to the west of the slopes area. This area consists of broad flat plains with occasional rocky outcrops, and occurs between 150 and 300 m above sea level. The plains are dominated by lower rainfall semi-arid rangelands, and the western portion is characterised by braided channels and associated floodplains (Central West CMA, 2008d).

Prior to European settlement the subregion supported a complex mosaic of forests, temperate and semi-arid woodlands, wetlands and grasslands (Green et al., 2011). Subsequently much of the natural vegetation has been cleared for livestock production and intensive agriculture (Central West CMA, 2009). The Central West subregion is comprised of five Interim Biogeographic Regionalisation of Australia (IBRA) bioregions (NSW Government, 2011, Figure 35). The Darling Riverine Plains and Brigalow Belt South IBRA bioregions dominate the Central West subregion, primarily associated with the Gunnedah Lowlands and Mitchell Slopes, respectively (Figure 6). Smaller areas of the Sydney Basin IBRA bioregion (on the Merriwa Plateau) and the NSW South Western Slopes IBRA bioregion and Cobar Peneplain IBRA bioregion (associated with the Gunnedah Lowlands) also occur in the south of the subregion. Brief descriptions of the characteristics of these IBRA bioregions are shown in Table 17.

The Central West subregion contains several areas of national and international significance. These include:

  • Macquarie Marshes – listed on the Ramsar List of Wetlands of International Importance, the National Heritage Register and the National Trust Register
  • Pilliga Scrub – the largest native forest area in NSW dominated by mixed cypress pine (Callitris sp.) and eucalypt woodlands
  • Goobang National Park – the largest remnant forest woodland in the Central West
  • Warrumbungle Ranges – a dormant volcanic landscape and national park popular for hiking and climbing (Central West CMA, 2008a).

In addition to these, there are 23 national parks estate sites listed within the Macquarie, Castlereagh and Bogan river basins with approximately 1300 km2 of reserved habitat in the Macquarie-Bogan river basin alone. With the exception of the Macquarie Marshes, most of these reserves are in the tablelands and slopes areas (Green et al., 2011).

Table 17 Brief description of the Interim Biogeographic Regionalisation of Australia (IBRA) bioregions in the Central West subregion


IBRA bioregion

Landform

Biodiversity values

Brigalow Belt South

Landscapes derived from extensive basalt flow and quartz sandstones, variable soils and vegetation types.

Supports a variety of forests and woodlands including a number of endangered ecological communities, plant and animal species.

Cobar Peneplain

Prominent topographical landscape of rolling downs and flat plains punctuated by stony ridges and ranges and formed on the Lachlan Fold Belt.

Vegetation is mainly open woodlands of bimble or poplar box, red box and white cypress. This IBRA bioregion supports 19 plant species listed in NSW’s Threatened Species Conservation Act 1995 (TSC Act).

Darling Riverine Plains

Occupies most of the upper catchment of the Darling and Barwon rivers in northern NSW and southern Queensland and includes the channels and floodplains of the lower reaches of these river basins.

River channels support red gum communities, with coolibah and black box communities on floodplains. The region contains 19 plant species and 63 animal species listed in the TSC Act.

NSW South Western Slopes

A large area of foothills and ranges comprising the western fall of the Great Dividing Range, and comprised of a wide variety of rock and soil types across the region.

Higher rainfall regions to the east are characterised by woodlands dominated by white box, grading to communities dominated by grey box and white cypress pine in the west. The TSC Act lists 36 threatened plant species and 67 animal species.

Sydney Basin

Geological basin filled with horizontal sandstones and shales of Permian to Triassic age that overlie older rocks of the Lachlan Fold Belt.

Diverse range of vegetations types as a result of high diversity in soil and landform types. The IBRA bioregion contains 152 plant species and 116 animal species listed in the TSC Act.

Source data: NSW Government (2011)

The South Eastern Highlands IBRA bioregion is upstream from the Central West subregion.

Figure 35

Figure 35 Interim Biogeographic Regionalisation of Australia (IBRA) bioregions and wetlands in the Central West subregion

Source data: IBRA version 7 (2012) ©Commonwealth of Australia 2012

Last updated:
5 January 2018