Australian Natural Resources Atlas

Natural Resource Topics

Rangelands — tracking changes 2001

Australian Collaborative Rangeland Information System
National Land and Water Resources Audit, 2001
ISBN: 0 642 37114 8

Brigalow (Acacia harpophylla): often cleared for grazing in Queensland. Photo: Eric Anderson

Change in biophysical resources

Biophysical resources are soil, nutrients, water, plants and animals. Information on these resources can be used to assess how well landscapes conserve soil and recycle plant nutrients and how landscape condition is changing.

Change in biophysical resources influences:

Information products under this component are summarised in Table 1.

Change in biophysical resources
Table 1. Information products for change in biophysical resources.
Key attributes Description and current status Rationale for inclusion
Product 1. Water availability and sustainability

Definition of surface and groundwater resources; their availability and quality

Assessment of surface and groundwater sustainable yield

Water resource characterisation and assessments of use against sustainability criteria are undertaken at irregular intervals, with the last assessment being Australian Water Resources Assessment 2000 (National Land and Water Resources Audit 2001a). Water resources are a key limiting factor to development, including agricultural enterprise, urban and mining activities. Water use needs to be managed in the context of sustainability-flow regimes for surface water and yield for groundwater.
Product 2. Change in landscape function
Change in vegetation cover from Landsat satellite data

Change in landscape function from monitoring site data

Changes in landscape function using NOAA satellite data, including continued refinement of methods (product in development)
The Tropical Savannas project and a companion project in South Australia have defined, applied and demonstrated methods for applying Landsat data at an operational level.

Data variables include vegetation patchiness, woody plant density, frequency of perennial grasses and soil surface condition.

Change in minimum cover of perennial vegetation and change in rainfall use efficiency (as assessed by NOAA) are roughly related to change in landscape function. These products are readily available at continental and regional scales, but are yet to be proven.
This product will provide information at various scales. Data archiving will allow for time sequences and tracking change. Ground monitoring data provide direct estimates of factors affecting landscape processes and are used to validate remotely sensed methods.
Product 3. Change in biological diversity
Change in composition of perennial plant species and abundance of specified invasive, fire sensitive, threatened and grazing-sensitive species

Changes in the composition of ant communities

Change in distribution and abundance of threatened vertebrates (mammals and birds) from repeat surveys of wildlife
Biodiversity monitoring activities are ready to implement and could use existing ground-based sites for vegetation monitoring.

Additional sites will be needed to collect information on non-pastoral areas.

Ant monitoring is done through projects such as WEST 2000 and the Great Artesian Bore Recapping project.

There is little institutional vertebrate monitoring at regional scales. The only Australia-wide vertebrate collection is the Bird Atlas.
This product provides direct estimates of biodiversity and assists validation of the links between remotely sensed and ground-based assessments.

Changes in the composition of ant communities are used to reflect local changes in biodiversity integrity.

Periodic re-sampling of a set of benchmark wildlife surveys will provide spatial context to the site-based information.
Product 4. Supporting information
Long-term photographic records of landscape change

Regional resource condition assessments and other regional/local information collection
Long-term photographic sequences of representative sites and landscapes around Australia provide rangeland condition context information within defined land systems (e.g. see Cunningham 2000a, b).

Resource inventory surveys, pastoral lease inspections and other activities provide further context and issue specific information.
This product provides context to help interpret changes in biophysical resources.

Product 1. Water availability and sustainability

Most rivers in Australia's rangelands are ephemeral and so water used is mainly derived from local run-off or groundwater. Pastoral rangelands use natural and artificial watering points that are typically less than 10 km apart. These provide water for not only domesticated stock but also for native and feral grazing animals. This can lead to intensive grazing near watering points and potential threats to biodiversity (Landsberg et al. 1997).

Capping of leaking bores: an imperative for groundwater management. Photo: MDBC

Definition of surface and groundwater resources available and their quality

Australian Water Resources Assessment 2000 (National Land and Water Resources Audit 2001a) assessed the quantity, quality, use, allocation and management of surface water and groundwater resources. There were 325 surface water management areas and 535 groundwater management units defined as a basis for management and reporting. For the first time, Australia has a spatially defined set of groundwater management units, an important basis for improved groundwater management. Sixty-one broadly defined groundwater provinces (defined by the former Australian Water Resources Council) have been used as an aggregation unit for map representations of groundwater management data because groundwater management units can overlie each other and therefore cannot be easily represented as a single map.

Groundwater resources

Substantially increased effort by Australia's water resource managers is required to precisely define sustainable yield and improve management of Australia's groundwater management units. Priority must continue to be given to the highly- and over-committed groundwater management units.

Water resource development

Development opportunities vary across Australia: in tropical Australia opportunities based on water capture (e.g. dams, bore fields, harvesting of overland flows) are still to be fully assessed and realised; in southern Australia development is approaching its extraction limits and caps on further allocation are being introduced.

Understanding water use

The greatest increases by volume in water use are in New South Wales (3600 GL) and Queensland (2300 GL)-accounting for 25% of total annual water use. Water use and delivery efficiency, recycling, trading and pricing are increasingly becoming priorities and provide opportunities for development.

The results of the assessment of surface and groundwater are available in the Atlas at national, State, groundwater management unit and surface water management area levels.

Information available in the Atlas for each groundwater management unit

Water availability
  • Developed yield (average annual volume that can be abstracted for use by existing infrastructure measured in megalitres per year [ML/yr])
  • Abstraction (average annual volume currently extracted for use measured in megalitres per year [ML/yr])
Aquifer characteristics
  • Depth (average depth to aquifer)
  • Thickness (thickness of strata)
  • Salinity (salt concentration as measured by electrical conductivity in microSiemens per centimetre [µS/cm)
  • Bore levels (monthly hydrographs)

Assessment of sustainable groundwater yield

Sustainable groundwater yield is the level of extraction that should not be exceeded over a specified planning time frame to protect the higher value-social, environmental and economic-uses associated with the aquifer.

Key considerations are:

Assessment of groundwater systems against sustainable yield is difficult. Assessment must consider use, allocation and environmental water requirements in the context of resource characterisation. Not much is known about groundwater-dependent ecosystems. A precise assessment cannot be made for many of the groundwater systems in Australia as characterisation data for groundwater management units are either partially or completely lacking.

The Great Artesian Basin

The Great Artesian Basin is one of the world's largest aquifer systems. It covers an estimated 1.7 million km² and stores 8 700 000 GL. Each year the Great Artesian Basin supplies 570 GL of water for a variety of uses-mainly grazing and mining.

Management of the groundwater resource of the Great Artesian Basin is shared between Queensland, New South Wales, South Australia and the Northern Territory. The Strategic Management Plan (Great Artesian Basin Consultative Committee 2000) provides for its management as a single resource, including continued bore rehabilitation and piping of bore drains (costed at approximately $220 m) to minimise waste from previously free-flowing bores in the Great Artesian Basin. Further work required includes:

  • recovering artesian pressure to achieve pastoral and biodiversity outcomes;
  • making water available for new users; and
  • reducing adverse impacts of water distribution on natural resources and biodiversity.

Water use in the Great Artesian Basin exceeds State and Territory sustainable estimates (Figure 3).

Estimates of sustainability - Great Artesian Basin use profile-indicating priority areas for investment in bore rehabilitation and piping of bore drains.
Category Number of groundwater management units in category
1 4
2 0
3 6
4 24

Estimates of sustainability

A four-class classification system was developed to provide a simple method to communicate the status of the use and allocation of Australia's water resources.

Category Extraction* % Development status
1 <30 Low development
2 30-70 Moderate development
3 70-100 Highly developed
4 >100 Overdeveloped

* Water extraction as a percentage of sustainable yield

Category 1 systems have zero to low levels of resource use: direct management intervention and information requirement are low.

Category 2 systems are moderately developed: management intervention and resource information requirement is moderate.

Category 3 systems are close to, or at, their extraction limit and require a high level of management inputs. Resource information and monitoring are vital for these systems.

Category 4 systems are over-committed in water allocation and/or use: insufficient provision has been made for environmental and non-consumptive uses, management intervention and information requirements are substantial.

Figure 3. Groundwater management units in each abstraction development category (2000).
Figure 3. Groundwater management units in each abstraction development category (2000).

Excerpt from Australian Water Resources Assessment 2000 (National Land and Water Resources Audit 2001a)

Great Artesian Basin groundwater province summary data
Groundwater management unit Sustainable yeild (ML) Groundwater use Groundwater allocation Sustainable yield assessment reliability
Total abstraction (ML) Development category Total allocation (ML) Development category
New South Wales
Great Artesian Basin - Central - New South Wales 5,750 6,580 4 6,580 4 D
Great Artesian Basin - Southern Recharge 10,100 11,580 4 36,490 4 D
Great Artesian Basin - Surat 53,640 70,780 4 70,780 4 D
Great Artesian Basin - Warrego 38,770 44,390 4 44,390 4 D
Lower Gwydir alluvium 35,000 40,762 4 99,032 4 C
Lower Namoi alluvium 95,000 43,849 3 213,264 4 A
Queensland
Condamine - Condamine Groundwater Management Unit Sub-area 1 1,440 2,157 4 3,560 4 A
Condamine - Condamine Groundwater Management Unit Sub-area 2 2,490 4,252 4 10,723 4 A
Condamine - Condamine Groundwater Management Unit Sub-Area 3 14,810 19,179 4 49,562 4 A
Condamine - Condamine Groundwater Management Area Sub-area 5 1,500 154 1 1,126 3 A
Condamine River (down-river of Condamine Groundwater Management Area) 3,500 1,800 3 1,898 2 C
Great Artesian Basin - Barcaldine - Queensland 36,310 44,170 4 44,170 4 D
Great Artesian Basin - Central - Queensland 16,680 28,000 4 28,000 4 D
Great Artesian Basin - Eastern Recharge A - Queensland 1,400 1,600 4 1,600 4 D
Great Artesian Basin - Eastern Recharge B - Queensland 32,450 37,140 4 37,140 4 D
Great Artesian Basin - Eastern Recharge C - Queensland 15,690 17,950 4 17,950 4 D
Great Artesian Basin - Flinders - Queensland 39,270 48,710 4 48,710 4 D
Great Artesian Basin - Gulf - Queensland 18,570 21,260 4 21,260 4 D
Great Artesian Basin - Mimosa - Queensland 13,970 15,990 4 15,990 4 D
Great Artesian Basin - Northwest - Queensland 10,680 12,230 4 12,230 4 D
Great Artesian Basin - Surat - Queensland 71,960 96,720 4 96,720 4 D
Great Artesian Basin - Warrego - Queensland 48,960 59,400 4 59,400 4 D
Great Artesian Basin - Western - Queensland 80 90 4 90 4 D
Great Artesian Basin - Western Recharge - Queensland 80 90 4 90 4 D
St George alluvium 18,000 2,000 1 6,340 2 C
Weipa 64,000 63,000 3 210 1 D
Winton/Mackunda Formations 24,000 n/a 4 n/a 1 D
South Australia
Curdimurka (Wellfield A) n/a 2,000 3 15,000 3 n/a
Total Great Artesian Basin -South Australia 60,000 54,800 3 63,800 3 D
Muloorina (Wellfield B) n/a 5,500 3 - 3 n/a
Unincorporated area - Hamilton n/a n/a 1 n/a n/a D
Unincorporated area - Peake Denison n/a n/a 1 n/a n/a n/a
NorthernTerritory
Great Artesian Basin - Western - Northern Territory 490 570 4 570 4 D
Great Artesian Basin - Western Recharge - Northern Territory 330 380 4 380 4 D

Estimates of data reliability

Class Groundwater quantity*
A Based on reliable recorded and surveyed data that have required little or no extrapolation or interpolation. Estimated accuracy: ±10%.
B Based on approximate analysis and limited surveys. Some measured data and some interpolation/extrapolation to derive the dataset. Estimated accuracy: ±10% to 25%.
C Little measured data, based on reconnaissance data. Estimated accuracy: ±25% to 50%.
D Derived without investigation data. Figures estimated from data in nearby catchments, or extrapolated/interpolated from any available data. Estimated accuracy: ±50%.

Product 2. Change in landscape function

The landscape function framework focuses on understanding how well a landscape is working as a system by studying the regulation of nutrients and water across the landscape (Ludwig et al. 1997). It is a spatial and dynamic concept focusing on landscape processes (e.g. nutrient cycling) rather than outputs (e.g. the particular species composition of vegetation). It is free of value judgements, and its information can be used and interpreted within a range of value systems. Broad indicators of landscape function include condition and trend of perennial vegetation, and a range of soil surface attributes.

Abundance of perennial grasses endemic to an area is an indication that the landscape is functioning well.

Monitoring for landscape function analysis is more cost-effective than for other types of analysis as less emphasis is placed on a complete inventory of species at a site. The key attributes for assessing landscape function are change in vegetation cover and species monitored through a combination of methods from remote-sensed imagery and ground-based data collection.

Landscape function versus condition

Landscape function and land condition are separate measures.

  • Landscape function is characterised by the interrelationships of landscape components in relation to changes in energy and materials in space and time. Assessment of landscape function is a necessary precursor to a judgement of condition.
  • Condition of a landscape is a value judgement and is related to its worth for a particular land use. It can be influenced by preconceptions, and cultural and social views (Figure 4).
Figure 4. Continuum of landscape function. Adopted from: Ludwig at al. 1997.
Figure 4. Continuum of landscape function. Adopted from: Ludwig at al. 1997

Rangeland vegetation

Most rangeland vegetation is dominated by native species.

In northern and eastern Australia the dominant vegetation types are eucalypt woodland with a grassy understorey, eucalypt forest and acacia woodland with a grassy understorey, and open grasslands. The distribution of forest and woodland is determined by rainfall effectiveness and soil type-little water, higher evaporation rates and low fertility limit the height and density of trees.

Hummock grassland of hard spinifex (Triodia basedowii) on sandy plains in the Great Victoria Desert. Photo: Eric Anderson

In central and central-western Australia the dominant vegetation type is shrubland where acacias, eucalypts and casuarina species make up the tree layer with a grassy or shrubby understorey. Common plants are the mallee (multi-stemmed eucalypts) and mulga (e.g. Acacia aneura).

Chenopod species (including bluebush and saltbush) are widespread, particularly across the southern half of the rangelands. The chenopods form communities that are drought- and salt-tolerant and of reasonable palatability to stock. Grasslands are also widely distributed with tussock grasses such as Mitchell grass (common in the central east). Hummock or spinifex grasslands cover large areas of inland Australia and are a dominant understorey layer across vast areas of north-western Australia where acacias and eucalypts form the dominant overstorey.

The National Vegetation Information System is being developed as part of the Audit's Australian Native Vegetation Assessment 2001. It contains information on the type and extent of Australia's native vegetation both now and before European settlement. It provides a classification framework that is comparable across administrative boundaries. The scale, spatial coverage and level of classification of the information varies depending on mapping activities and data that has been collated into the National Vegetation Information System (Figures 5, 6 & 7). Estimates of pre-European vegetation give us a benchmark to assess vegetation change relative to European disturbance, and an indication of change in composition, that can be used for conservation planning and revegetation strategies.

Figure 5. Major vegetation groups: Australia.

Figure 5. Major vegetation groups: Australia.

Figure 6. Major vegetation groups: Queensland.
Figure 6. Major vegetation groups: Queensland
Figure 7. Major vegetation groups: Desert Uplands bioregion.

Figure 7. Major vegetation groups: Desert Uplands bioregion.

Change in vegetation cover from Landsat satellite data

Landsat satellite imagery provides information on vegetation response to rainfall and allows an assessment of landscape function. Australia-wide coverage and regular updating and archiving mean that images can be chosen by season and climate history. The images can be used to provide a measure of vegetation cover and change over time. Field verification and the collection of data at permanent monitoring sites refine satellite-based interpretations and improve understanding of complex landscape processes.

Remote sensing is a good monitoring tool because:

  • image databases are made up of objective, consistently processed data;
  • it allows monitoring at a range of scales and across environments;
  • it can be integrated with ground data to detect change and identify function in rangelands (Figures 8, 9 & 10); and
  • it is cost-effective, providing an ability to regularly monitor large areas and store a large amount of information on Australian landscapes.

Relationships between ground monitoring and remote sensing techniques are important. They enable an understanding of how landscapes respond to disturbance and variable seasons over a long period, and allow comparison between functional and dysfunctional landscapes.

Shrubland: the dominant vegetation type in central Australia. Photo: Department of Agriculture WA
Figure 8. Landsat-derived vegetation cover map at the paddock scale in the Stony Plains bioregion (March 1988).
Figure 8. Landsat-derived vegetation cover map at the paddock scale in the Stony Plains bioregion (March 1988). Location map of Stony Plains The cover index is calculated from the visible reflectance bands of the Landsat image. Vegetation levels are represented by red (lowest cover) through to orange, yellow, green, light blue and dark blue (highest cover).

The location of the photograph is marked by the white square on the image.

A uniform cover of bladder saltbush (Atriplex vesicaria) and scattered dead finish (Acacia tetragonophylla) occurs on the Gibber plain on the left hand side of the fence, with barley Mitchell grass (Atrebla pectinata), feathertop wiregrass (Aristida latifolia) and common bottlewashers (Enneapogon avenaceus) on the more heavily grazed right hand side of the fence. Grazing by cattle only occurs in this area for short periods when surface water is available.

To the right side of the fence, the bladder saltbush has been substantially reduced by intense grazing from sheep and cattle over several decades. The image indicates cover differences. Interpretation of causes and effects on plant communities is provided by integrating remote-sourced data with ground data.

Source: Brook et al. 2001.

Figure 9. Integrated ground- and satellite-based monitoring system.

Landsat sequences (1983 to 1997) from the Victoria Bonaparte and Ord Victoria Plains bioregions have been processed and combined with landscape function data from ground sites and ancillary data to provide summaries and interpretation of changes in the region.

Summaries of the intensity and trend of Landsat cover indices (mean and slope) are displayed as map products over discrete image sequences (A).

By examining the brightness and variation in cover indices over time, in relation to distance from water and the location of fences, roads and land resources, a first indication of vegetation composition and landscape function can be interpreted. On the image, light blue and green represent high cover indices over a 1 ha monitoring site (2VRD24) represented by a solid red square and surrounds (hollowed square) from 1994-97. Within this 20 km² image, landscapes with low cover indices (red and dark blue) and decreasing trend (yellow) are also identified; riparian and rugged landscapes are masked and fence lines are represented as white lines.

Ground monitoring data provide information on a site's functionality (B) with which to evaluate variations over time from 1983 to 1997 (C).

Based on the four years of Landscape Function Analysis data, using only 'number of plant patches' in this example, it is apparent that this site is functioning well and able to recover from disturbance (i.e. heavy grazing in 1996). From the time-trace (C), we can interpret that the vegetative cover documented at the site (D) was generally higher than in the poor to average seasons from 1988 to 1992. However in these poorer years, cover at the site was still significantly higher compared with the regional average.

Source: Karfs et al. 2000.

D
1995 1996
1997 1998
A
Figure 9a. Summaries of the intensity and trend of Landsat cover indices.
B
Figure 9b. Ground monitoring data provide information on a site's functionality.
C
Figure 9c. Variations over time from 1983 to 1997.
Figure 10. Regional trend for the Ord Victoria Plains bioregion in north-west Australia.

Figure 10. Regional trend for the Ord Victoria Plains bioregion in north-west Australia.

Location map of Ord Victoria Plains Analysing three land types separately and then combining them into a contiguous coverage creates a regional trend product from 1992 to 1997. The area analysed covers 66 550 km² within four mosaic Landsat scenes .

Light green represents areas where cover increased; dark green represents areas with stable cover; red represents areas where cover decreased. In this example, fire scars have not been removed and much of the red is attributed to burnt country. Fire history maps overlain on this image would aid in interpreting landscape condition.

These data show that cover has increased over much of the region. This trend can be attributed to a run of good seasons from 1993 to 1997. This is also consistent with the interpretation of ground data collected at monitoring sites over the same period.

Source: Karfs et al. 2000

The location of watering points often determines the distribution of stock in areas of low or variable rainfall. The reducing intensity of grazing on the landscape at increasing distance from water is called a 'grazing gradient'. If vegetation cover close to water is fully restored after significant rainfall then the grazing gradient is temporary, showing that grazing has not had a long-term effect. If the gradient persists after significant rainfall, then grazing has had a long-term impact on pasture productivity (Figure 11). Grazing effects can be separated from seasonal effects by using remote sensing imagery over a range of time periods. Grazing gradients: careful management of watering points is essential. Photo: MDBC
Figure 11. Grazing gradient, Stony Plains bioregion in South Australia.

The graph shows how grazing effects can be separated from seasonal variation.

  • 1988 was a dry period
  • 1989 and 1997 were wet periods
  • The difference between the top lines and the bottom line reflects the seasonal variation in vegetation cover.
  • The difference between the top lines shows a reduction in landscape function up to 9 km from water because the vegetation cover in 1997 has not recovered to the 1989 levels.

Source: Brook et al. 2001

Figure 11. Grazing gradient, Stony Plains bioregion in South Australia.

Change in landscape function from monitoring site data

At the site scale, landscape function can be directly assessed using the Landscape Function Analysis approach. A range of attributes can be used to provide an indication of landscape function. One example is that the frequency and change in frequency of perennial species can be used to provide a broad estimate of the ability of the landscape to regulate nutrients and water (Table 2); soil or vegetation cover could also be used in this example (Figure 12). The specific attribute used will depend on the objective of the analysis.

Spinifex: grasslands are an important part of rangeland ecosystems. Photo: Allan Fox
Table 2. Changes in Kimberley grasslands, Western Australia.

Average change in perennial grass frequency and average crown cover estimates (%) for all woody species taller than 1 m, by vegetation group. Data came from monitoring sites assessed between 1994 and 1996 and reassessed between 1997 and 1999. The frequency of perennial grasses can be used as a broad indicator of landscape function.

Vegetation group No. of sites Mean frequency Significant change
1994-1996 1997-1999
Average change in perennial grass frequency (%)
Black soil plains 113 74.4 80.7 *
Curly spinifex 69 83.7 85.7
Coastal vegetation 12 86.2 89.2
Frontage grass 13 70.0 75.4
Limestone grass 14 39.9 47.1
Northern ribbon grass 32 88.5 85.7
Southern ribbon grass 64 75.0 76.6
Soft spinifex 23 84.9 86.5
Average crown cover (%)
Black soil plains 113 1.8 1.4 *
Curly spinifex 69 13.2 13.8
Coastal vegetation 12 1.0 0.5
Frontage grass 13 7.9 9.3
Limestone grass 14 6.7 4.8
Northern ribbon grass 32 12.5 12.5
Southern ribbon grass 64 6.1 5.6
Soft spinifex 23 5.0 7.7

Significance was tested using the two-tailed paired t-test. Not significant = P>0.05

Figure 12. Soil surface vegetative cover from 1989 to 2000 for selected bioregions in western New South Wales.

Soil surface vegetative cover levels for all bioregions except the Riverina remained between 30% and 70%. The Broken Hill Complex bioregion experienced significant decrease in vegetative cover in 1999. The number of sites in each bioregion varies (see Table A1). At each site, data is collected within 4 x 300 m transects and 4 x14 quadrats.

Figure 12. Soil surface vegetative cover from 1989 to 2000 for selected bioregions in western New South Wales.

Product 3. Change in biological diversity

During the years since you last saw it, there have been many changes in this country. The rabbits have supplanted the marsupials and the indigenous plants are gradually giving way to inferior kinds of herbage.

P.M. Byrne describing Charlotte Waters 1921, (quoted in Calaby 1996)

Native vegetation

The benefits of tracking changes in Australia's native vegetation are far from well documented. However the link between vegetation and animal biodiversity is well recognised (e.g. in the southern arid zone there is a direct link between vegetation and animal biodiversity):

... the lack of effective regeneration of perennial shrubs and trees ... is like a time bomb quietly ticking away; as this aging generation of chenopods, mulga, western myall and native pines thins and dies out, we will witness unprecedented changes in bird community composition ...

Reid & Fleming 1992

The major threats to native vegetation are grazing by stock and feral animals, and change in fire frequency (Figure 13).

Acacia peuce: a rare tree restricted to three locations in Queensland and the Northern Territory. Photo: Eric Anderson
Figure 13. Known and predicted occurrence of threatened plants by subregion. Species are considered threatened if they are listed under the Environment Protection and Biodiversity Conservation Act 1999 (Commonwealth).

Threatened species may be listed as extinct, endangered, vulnerable or conservation dependent.

Figure 13. Known and predicted occurrence of threatened plants by subregion. Species are considered threatened if they are listed under the Environment Protection and Biodiversity Conservation Act 1999 (Commonwealth).

Native fauna

Major threats to vertebrate fauna are grazing by domestic stock and feral animals, habitat change, and predation by feral animals such as cats and foxes (Figure 14 & 15). Native mammals lost from the rangelands over the last 200 years form one of the largest known extinction records in the world (Childs et al. 2001) (Figure 16). Bird populations have also been declining rapidly since European settlement. Although the extent of change in bird populations has not yet matched that of mammals, this may be due to a time lag and extinctions may become increasingly evident over the next few decades.

Figure 14. Known and predicted occurrence of threatened vertebrate fauna by subregion. Continued management is essential to minimise further extinctions.
Figure 14. Known and predicted occurrence of threatened vertebrate fauna by subregion. Continued management is essential to minimise further extinctions.
Figure 15. Distribution of greater bilby in Australia.

The greater bilby (Macrotis lagotis) is a ground-dwelling marsupial that was once common in many parts of the dry interior and temperate coastal regions. Loss of habitat and competition with introduced animals mean that it now occurs only in fragmented populations in mulga shrublands and spinifex grasslands. Wild populations are being monitored and captive breeding programs aim to retain their genetic diversity.

Figure 15. Distribution of greater bilby in Australia.
Figure 16. Loss of terrestrial mammal species across Australia's rangelands (calculated as the number of species assumed to be present in 1788 minus the current number).

The figure probably under-represents the loss of species across tropical savannas. Figure 16. Loss of terrestrial mammal species across Australia's rangelands (calculated as the number of species assumed to be present in 1788 minus the current number). The figure probably under-represents the loss of species across tropical savannas.

Location map of Flinders Lofty BlockFLINDERS LOFTY BLOCK

Changing biodiversity and threatening processes within a bioregion

Major land uses

Extensive grazing by sheep is the dominant land use and has been since the 1840s. Agriculture (mainly wheat) and mining (including coal and copper) have historically been important. Tourism is now a major industry.

Conservation areas

Although 10% of the bioregion is protected in conservation areas, these include only 14 of the 49 recognised environmental subregions.

Yellow-footed rock wallaby (Petrogale xanthopus): winning the conservation battle. Photo: Earth Sanctuaries Condition and threats

Overgrazing by sheep, rabbits and goats has led to degradation, including lack of regeneration for a range of woody plant species.

Eight exotic animal species (rabbit, fox, cat, goat, black rat, house mouse, donkey and brown hare) are established in the bioregion. Rabbits (arriving in approximately 1880) and foxes (1900) have been extremely common until release of the calicivirus.

The understorey of many vegetation associations (e.g. white cypress pine Callitris glaucophylla woodland and tussock grasslands) is now mostly made up of exotic plant species, especially where stock have grazed heavily. One hundred and twenty-three exotic plants have been recorded in the greater Flinders Ranges area including rosy dock (Acetosa vesicaria), Salvation Jane or Patterson's curse (Echium plantagineum), red brome (Bromus rubens), ward's weed (Carrichtera annua), Maltese cockspur Centaurea melitensis, common storksbill (Erodium cicutarium), spiked malvastrum (Malvastrum americanum), Schismus barbatus, smooth mustard (Sisymbrium erysimoides), common sow thistle (Sonchus oleraceus), onion weed (Asphodelus fistulosus), horehound (Marrubium vulgare) and woolly burr-medic (Medicago minima).

Changes in biodiversity

Mammal fauna has suffered major losses, mainly in the regional extinction of 24 out of the 50 mammal species. These include small macropods, bandicoots, dasyurids, bats and rodents. Until recent control of rabbits, foxes and goats, the yellow-footed rock wallaby (Petrogale xanthopus) was continuing to decline.

Three plant species are believed to have become extinct in the Flinders Ranges: reed bent-grass (Deyeuxia quadriseta), blunt pondweed (Potamogeton ochreatus), and Pilularia novae-hollandia.

Location map of Gulf PlainsGULF PLAINS

Changing biodiversity and threatening processes within a bioregion

Major land uses

The dominant land use is cattle grazing on native pastures, dating back to the 1860s. Mining continues to be a significant industry.

Conservation areas

Two point five percent of the Queensland part of the bioregion is in conservation reserves. None of the Northern Territory portion is reserved.

Golden-shouldered parrots (Psephotus chrysopterygius) are confined to Cape York Peninsular where just a few thousand remain. Photo: Daryl AlbertsonCondition and threats

Of the 83 regional ecosystems defined for the Queensland part of this bioregion, three are considered endangered and 26 are considered of concern. Most (72%) of those that are endangered and of concern are associated with watercourses and flood plains.

... the three major processes that pose a threat to biodiversity in the Gulf Plains are unsustainable grazing pressures, weed infestation and the development of ponded pastures. High total grazing pressure is causing increasing land degradation through changes in the density of ground cover and in species composition ... This is having a particular effect on riverine areas and on wetlands. Changes in stock and pasture management are leading to a reduction in seasonal burning, and a consequent increase in the density of the woody stratum ... The major weed threatening biodiversity is rubber vine (Cryptostegia grandiflora), that now infests most major river systems ... Potential or local problem weed species include parkinsonia (Parkinsonia aculeata) and prickly acacia (Acacia nilotica). Salvinia (Salvinia molesta), water hyacinth (Eichhornia crassipes), calotrope (Calotropis procera), and noogoora burr (Xanthium pungens) are also locally significant ... Ponded pastures pose a threat ... to wetlands ... [through] the introduction of ponded pasture species to natural wetlands, where they displace most native wetland plants and animals. A secondary concern is the impact of retaining walls on floodplain hydrology ... Clearing of gidgee (Acacia cambagei) communities is occurring.

Sattler & Williams 1999

Changes in biodiversity

Major declines and local extinctions of the golden-shouldered parrot (Psephotus chrysopterygius) have occurred across the Gulf of Carpentaria part of its range. This decline has been attributed to habitat change (principally invasion of grassland areas by melaleucas) caused by altered fire regimes over the last century. No plant species are known to have become extinct in this bioregion.

Location map of Great Victoria DesertGREAT VICTORIA DESERT

Changing biodiversity and threatening processes within a bioregion

Major land uses

The Great Victoria Desert is sparsely inhabited. Most of the area is Indigenous land-in some cases tenured as conservation reserve. A network of exploration lines was surveyed and cleared across large areas during the late 1960s and early 1970s. Mineral exploration continues. Parts of the bioregion were used as restricted area for the Woomera Rocket Range, for nuclear testing and as storage for spent atomic fuels. Pastoral leases exist in the less arid margins.

Conservation areas

The 'Unnamed Conservation Park' in the South Australian portion of the bioregion is one of Australia's largest (21 327 km²) conservation reserves. More than 10% of the South Australian and 5-10% of the Western Australian parts of the bioregion are in conservation reserves.

Desert Death Adder (Acanthophis pyrrhus): one of the deadliest snakes of central Australia. Photo: Brian BushCondition and threats

The impacts of rabbits and pastoralism on land condition resulted in fewer perennial species and lower plant density especially for the most susceptible vegetation type-chenopod shrublands.

... the introduction of several exotic mammals, most notably the rabbit, has undoubtedly been responsible for the decline in some mammals but for reptiles the full impact is possibly yet to come. Rabbits are present throughout much of the eastern Great Victoria Desert and continue to severely modify the environment. By eating all young seedlings, rabbits have for the past 100 years effectively prevented regeneration of many of the palatable, slow-growing, perennial tree and shrub species over much of the area. As this process continues, the whole character of the eastern Great Victoria Desert is likely to change dramatically as species like mulga die out over large areas. With them will go the characteristic assemblages of species they support ... Fires which have killed most mature mulgas over large areas of far eastern sections of the Great Victoria Desert are hastening this process.'

Greenslade et al. 1986

Changes in biodiversity

Reptiles are a feature of this bioregion with relatively intact populations. Two snake species (the desert death adder [Acanthophis pyrrhus] and western black-naped snake [Neelaps bimaculatus]) have not been observed in the South Australian part of the bioregion for about 60 years-a possible decline that may be of concern.

One-third of mammal species have become extinct in this bioregion during the last 40 years including the numbat (Myrmecobius fasciatus), bilby (Macrotis lagotis), burrowing bettong (Bettongia lesueur) and stick-nest rats (Leporillus spp.).

Some bird species are declining, including mallee fowl (Leipoa ocellata) and scarlet-chested parrot (Neophema splendida). Comparison of recent bird records with those reported between 1873 and 1945 suggest that Australian bustard (Ardeotis australis), bush stone-curlew (Burhinus grallarius) and spinifex pigeon (Geophaps plumifera) have declined.

The decline in species is occurring in both non-pastoral and conservation areas. This highlights the need to reduce feral animal populations as part of protective management activities across all tenures.

Product 4. Supporting information

Long-term photographic records

Photo sequences provide a local record of change and are particularly useful as tools for raising awareness (Figure 17). They show types and extent of change that have occurred over time and provide context and assist in interpreting broader-scale changes collated through remote sensing and plot monitoring.

The Audit in cooperation with State and Northern Territory agencies has compiled sets of photographic sequences for some bioregions. These can be accessed on the Rangelands Monitoring part of the Atlas.

Figure 17. Photo sequence at one point (1928 to 2000) Koonamore Vegetation Reserve, South Australia.
Figure 17. Koonamore Vegetation Reserve, December 1928. Figure 17. Koonamore Vegetation Reserve, December 1970. Figure 17. Koonamore Vegetation Reserve, December 2000.
Figure 17. Koonamore Vegetation Reserve, December 1929. Figure 17. Koonamore Vegetation Reserve, December 1976. Source: University of Adelaide
Figure 17. Koonamore Vegetation Reserve, December 1968. Figure 17. Koonamore Vegetation Reserve, December 1989.

Regional resource assessments

Much of Australia's rangelands has been mapped into land systems or land units using consistent resource inventory techniques. Many of these surveys and accompanying pastoral lease inspections include estimates of resource condition based on field traverse by combining estimates of soil erosion and vegetation state. Although the surveys were not designed to be repeated, they provide baselines with which to compare recent change, and highlight areas where condition is poor (Figure 18).

Figure 18. Resource condition summaries for regional rangeland surveys within Western Australia (Van Vreeswyk et al., [in prep.]) given by region and year survey commenced.
Figure 18. Resource condition summaries for regional rangeland surveys within Western Australia (Van Vreeswyk et al., [in prep.]) given by region and year survey commenced. .