MVG 13 - OPEN WOODLANDS

Gidgee woodlands () near Coopers Creek, Innamincka, SA (Photo: M. Fagg)

Overview  Many Acacia woodlands are dominated by a single Acacia species, which may co-occur with other members of the genus, either in the understorey or in transitional segments of environmental gradients.  Species composition and the identity of the dominant species vary along rainfall gradients, with substrate and to a lesser extent rainfall seasonality (Beadle 1981; Johnson and Burrows 1994).  MVG 13 comprises several subgroups including: “gidgee” and “myall” woodlands that occur as mean annual rainfall declines below 550 mm and “mulga” which dominate woodlands on stony or sandy landscapes across the arid zone and across the northeast semi-arid landscapes adjoining savanna.  Mulga vegetation takes on a variety of structural expressions and is consequently classified partly within MVG 6, in accordance with the Kyoto Protocol definition of forest cover in ( > 2 m tall and crown cover > 20%, foliage projective cover > 10%); and partly within MVG 13 where the canopy layer is sparser or MVG 16 where the woody dominants are not predominantly single-stemmed

Facts and figures

Major Vegetation Group MVG 13 - Acacia Open Woodlands Major Vegetation Subgroups xx. Gidgee woodlands NSW, QLD, SA, NT (number of NVIS descriptions) 22. Semi-arid myall woodlands NSW, QLD 24. Arid myall woodlands NSW, SA, WA 20. Stony mulga woodlands and shrublands NSW, QLD, NT, SA, WA 23. Sandplain Acacia woodlands and shrublands NSW, QLD, NT, SA, WA Typical NVIS structural formations Woodland (low) Open woodland (mid, low)

Number of IBRA regions 36 Most extensive in IBRA region Est. pre-1750 and present: Mulga Lands (Qld and NSW) Estimated pre-1750 extent (km2) 320 981 Present extent (km2) 314 040 Area protected (km2) 23 815

Acacia aneura (Mulga) woodland western NSW (Photo: B. Pellow)

Structure and physiognomy  Woodland structure varies from 5 – 20 m tall with canopy cover 10 -30% along the regional rainfall gradient and with local soil moisture gradients between rises and depressions (Johnson and Burrows 1994; Neldner et al. 2013).  Open woodlands are distinguished from shrublands (MVG 16) by the predominantly single- stemmed growth form of the woody dominants.  Typically the structure of this MVG comprises a canopy dominated by Acacia species, a smaller shrub layer and a ground layer of perennial grasses and forbs and ephemeral species.  Canopy emergents, where present, include scattered eucalypts and casuarinas.  of the dominate layer vary from microphyll phyllodes or leaves (2.5 – 20 cm2) to nanophyll phyllodinous needles (0.25 – 2.5 cm2), (Johnson & Burrows 1994).  Understories may include open layers of shrubs with typically sparse ground layers of tussock grasses and forbs that vary depending on canopy cover, rainfall and substrate.  In myall woodlands an open layer of chenopod shrubs and other woody species and an open to continuous groundcover of grasses and herbs may occur (Keith 2004; NSW Scientific Committee 2005).

Indicative flora  A single species of Acacia typically dominates, but may co-occur with other members of the genus as sub-dominants or occasionally co-dominants.  Five Major Vegetation Subgroups are recognised, of which two also occur in MVG 6 and in MVG 16. Three of the subgroups are dominated by Acacia in the ‘Microneurae’ group within section Plurinerves of the genus, with chenopods and/or tussock grasses primarily of tribes Chlorideae and Sporoboleae on fine-textured alkaline soils. Two other subgroups are dominated by Acacia species from section Juliflorae of the genus, with tussock grasses primarily of tribes Aristideae and Andropogoneae on coarse-textured acid soils (Johnson & Burrows 1994). o Gidgee woodlands (also represented in MVG 6) - Acacia cambagei is the primary dominant, and there may be scattered emergent eucalypts (section Adnataria). Co- occurring shrubs are sparse but may include species of Alectryon, Atriplex, Carissa, Enchylaena, Eremophila, Senna and Terminalia. In the swales of red desert dunefields, Acacia georginae becomes the sole dominant tree, while in the higher rainfall areas Acacia argyrodendron is the sole dominant. The groundlayer comprises a sparse cover of tussock grasses including species of Astrebla, Enteropogon, Paspalidium and Sporobolus (Johnson and Burrows 1994; Keith 2004; Neldner et al. 2013). o Semi-arid myall woodlands - Acacia pendula is the sole dominant species, often populated with the mistletoe , although eucalypts (section Adnatria), Alectryon, Casuarina and other species of Acacia may be present as subordinates or scattered emergents, especially in the north. The more extensive southern occurrences have understories dominated by chenopod genera including Atriplex, Chenopodium, Enchylaena, Maireana, Rhagodia and Sclerolaena, although many of these may be eliminated by heavy grazing leaving a grassy groundlayer assemblage of Austrostipa, Chloris, Eragrostis and Sporobolus with forbs of the Asteraceae and Brassicaceae (Keith 2004). Chenopods are less common in the northern part of the distribution, where Eremophila maculata becomes a more conspicuous shrub and Astrebla and Dichanthium become more prominent grass genera (Johnson and Burrows 1994). o Arid myall woodlands - Acacia papyrocarpa dominates to the west of the Flinders Ranges, while the related Acacia loderi dominates to the east. These may co-occur with Casuarina pauper, Myoporum platycarpum, Pittosporum angustifolium and . Shrubs include species of Senna, Eremophila and Grevillea on deeper soils or, where calcrete is close to the surface, Maireana sedifolia, other Maireana species, Atriplex vesicaria and numerous Sclerolaena species. Widespread grasses include species of Austrostipa, Austrodanthonia and Enneapogon (Beadle 1981; Johnson and Burrows 1994; Beard et al. 2013). o Stony mulga woodlands and shrublands (also represented in MVGs 6 and 16) - Acacia aneura (mulga) is the primary dominant, often present in monospecific stands, but unlike most other Acacia assemblages, commonly co-occurs with other Acacia species or with scattered Eucalyptus or Casuarina. Widespread congeners include Acacia victoriae and Acacia tetragonophylla, while Acacia estrophiolata Acacia grasbyi, Acacia quadrimarginea, and Acacia xiphophylla may be regionally abundant in parts of central and The sparse shrub layer includes species of Atalaya, Eremophila, Senna, Dodonaea and Maireana. The ground cover varies inversely with overstorey cover and responds to rain. It is dominated by tussock grasses including species of Aristida, Enneapogon and Eragrostis, with Austrostipa in the south (Johnson and Burrows 1994; Neldner et al. 2013). o Sandplain Acacia woodlands and shrublands (also represented in MVG 16) - include Acacia aneura with Acacia calcicola, Acacia ligulata, Acacia murrayana, Acacia ramulosa and Acacia tetragonophylla in various combinations across the distribution of this subgroup, along with species of Dodonaea, Eremophila, Grevillea, Hakea and Senna, with Acacia ancistrocarpa in the north. The ground layer includes a diversity of ephemeral Asteraceae, hummock grasses (Triodia species), and/or tussock grasses such as Aristida, Enneapogon, Eragrostis and Austrostipa (Johnson and Burrows 1994; Keith 2004).

Environment  Occurs largely within the 150 mm to 550 mm annual rainfall range across arid and semi-arid areas of Australia.  The climatic conditions are generally dry, hot summers, with cool to warm winters. Rainfall is variable although maximum falls are either in summer (northern) or in winter (southern).  In southern Australia rainfall occurs in winter while in northern Australia rainfall is linked to the monsoons of summer ((Hodgkinson 2002).  Different subgroups occur on contrasting substrates: o Gidgee woodlands occur on deep fine texted soils in landscape depressions, replacing Brigalow woodlands as mean annual rainfall declines below 550 mm in central and western Queensland, and adjoining areas of the , South Australia and northern NSW (Johnson and Burrows 1994; Keith 2004) o Semi-arid myall woodlands are distributed on mostly grey clay soil plains, often of ancient alluvial origin, within a belt defined by the 375 mm and 550 mm isohyets to the east of Australia’s arid zone stretching from the Riverina district in the south to Clermont in central Queensland (Johnson and Burrows 1994; Keith 2004). o Arid myall woodlands occur within the 150 to 280 mm annual rainfall belt across the southern arid zone from the north-western fringe of the Nullarbor Plain to far western New South Wales on calcareous loams and clay loams, usually with a shallow calcrete subsoil (Beadle 1981; Johnson and Burrows 1994). o Stony mulga woodlands and shrublands occur on open peneplains with light-textured loams and hard subsoils, high levels of iron and low phosphorus where mean annual rainfall is between 200 and 500 mm from central Queensland to the west Australian coast (Johnson and Burrows 1994; Keith 2004). o Sandplain Acacia woodlands and shrublands occur on siliceous red sandplains, mainly on the crests and slopes of dunes, across the central and western deserts (Johnson and Burrows 1994; Keith 2004).

Geography  Dominates large areas of semi-arid and arid Australia particularly Western Australia, the Northern Territory, South Australia, Queensland and New South Wales.  Largely occur on extensive undulating plains and downs, low hills and valleys of the rangelands.  Largest areas occur in the Queensland (91 014 km2), South Australia (73 939 km2) and Western Australia (61 309 km2).

Change  Approximately 2% of the estimated pre-1750 extent cleared accounting for 0.7% of total clearing in Australia mainly as a result of pastoral activities in Queensland and New South Wales.  Approximately 7 000 km2 cleared since European settlement.  Modified by clearing for pastoral activities, change in local drainage systems, increased local grazing pressure by providing stock watering, an overall increase in grazing through the introduction and spread of feral animals.  High levels of grazing in Myall woodland has led to the replacement of chenopod shrubs and tall perennial tussock grasses with short perennial grasses and unpalatable annual herbs (Beadle 1948), as well as introduction of exotic herbs and grasses such as Bromus spp., Erodium spp., Lepidium africanum, Medicago spp., Sisymbrium spp. and Trifolium spp. Introduced shrubs, notably Lycium ferocissimum (African boxthorn) have also invaded some areas occupied by this community (NSW Scientific Committee 2005).  Extensive invasion of Buffel grass (Cenchrus ciliatus) across arid and semi-arid parts of Queensland and Northern Territory is making Acacia woodlands more regularly prone to fires, threatening the persistence of trees and shrubs.

 Less than 30% of Myall woodland remains in New South Wales (NSW Scientific Committee 2005) with much of the clearing taking place during droughts to provide emergency stock food (Keith 2004)  Overgrazing by cattle and feral vertebrates has degraded extensive areas of Gidgee and Mulga woodlands, resulting in a lack of regeneration, soil compaction and erosion, reduction of woody debris, as well as disruption of grove-intergrove patterns critical to water movement, resource capture and landscape function (Tongway and Ludwig 1990).  Foremost threats are over-grazing (including cattle, sheep and feral animals) and changes to fire regimes (NLWRA 2001b).

Tenure Acacia Open Woodlands occur largely on leasehold land.

New South Wales: leasehold, protected areas and very small areas on freehold land

Northern Territory: leasehold land,protected areas, some freehold land, little other crown land

Queensland: leasehold land, protected areas, isolated areas on freehold land

South Australia: leasehold land, protected areas, little on freehold land

Western Australia: leasehold land, protected areas, some other crown land

Key values  Biodiversity, several endangered ecological communities and species are known from temperate regions of this MVG.  Maintenance of landscape function and soil productivity.  Remnant populations of a wide range of vertebrate and invertebrate species.  Pastoral production.

List of key management issues  Grazing pressure from both domestic stock and feral animals. Trampling and grazing by large herbivores has a number of impacts.  Interactions between stocking rates and drought cycles, implementing pastoral management systems that avoid cumulative legacies of soil degradation caused by sustained overgrazing into successive drought episodes.  Location and access to artificial watering points, which are associated with intensification of herbivore activity and associated impacts.  Control of introduced grasses on pastoral lands to limit their influence on fire regimes and native groundcover.  Fire regimes, recognising that some introduced grasses such as Cenchrus ciliaris (buffel grass) burn with greater intensity than native pasture grasses, thereby altering regeneration responses of trees and shrubs.  Indirect effects of climate change.  Feral animals including pigs, goats, cats and foxes.  Long term monitoring to inform future management strategies.

References Australian Surveying and Land Information Group (1990) Atlas of Australian Resources. Volume 6 Vegetation. AUSMAP, Department of Administrative Services, Canberra, 64pp. & 2 maps. Beadle NCW (1948) Vegetation and pastures of western New South Wales. Soil Conservation Service, Sydney.

Beadle N.C.W. (1981) The Vegetation of Australia. Cambridge Univ. Press, Cambridge, 690pp. Beard J.S., Beetson, G.R, Harvey J.M. Hopkins A.J.M and Shepherd D.P. (2013) The Vegetation of Western Australia at 1:3,000,000 Scale. Explanatory Memoir. Second Edition. Science Division, Department of Parks and Wildlife, Western Australia. Hodgkinson K.C. (2002). Fire regimes in Acacia woodland landscapes: effects on functional processes and biological diversity . In Flammable Australia. The fire regimes and biodiversity of a continent. (ed Bradstock R.A., Williams J.E and Gill A.M.) pp. 259 - 280. Cambridge University Pres, Cambridge Johnson R.W. and Burrows W.H. (1994) Acacia open forests, woodlands and shrublands. In: Australian Vegetation (ed. R.H. Groves) pp. 257-290. Cambridge Univ. Press, Cambridge. Keith D. (2004) Ocean Shores to Desert Dunes. The native vegetation of New South Wales and the ACT. Department of Environment and Conservation (NSW), Hurstville National Land and Water Resources Audit (2001) Australian Native Vegetation Assessment 2001. National Land and Water Resources Audit, Canberra, 332pp. Neldner, V.J., Niehus, R.E., Wilson, B.A., McDonald, W.J.F. and Ford, A.J. (2014). The Vegetation of Queensland. Descriptions of Broad Vegetation Groups. Version 1.1. Queensland Herbarium, Department of Science, Information Technology, Innovation and the Arts. NSW Scientific Committee (2005). Final Determination Myall Woodland in the Darling Riverine Plains, Brigalow Belt South, Cobar Peneplain, Murray-Darling Depression, Riverina and NSW South Western Slopes bioregions - endangered ecological community listing. New South Wales Scientific Committee, Hurstville. National Land and Water Resources Audit (2001b) Rangelands—Tracking Changes, National Land and Water Resources Audit, Canberra. Tongway D. J. and Ludwig, J. A. (1990) Vegetation and soil patterning in semi-arid mulga lands of Eastern Australia. Australian Journal of Ecology 15, 23–34.

Data sources Interim Biogeographic Regionalisation for Australia (IBRA), Version 6.1. Land Tenure in Australia's Rangelands (1955 to 2000), National Land and Water Resources Audit. National Vegetation Information System, Version 4.1. 1996/97 Land Use of Australia, Version 2. Collaborative Australian Protected Areas Database – CAPAD 2004 – Terrestrial.

Notes  Additional large areas identified in NVIS 3 from improved data for Western Australia, South Australia, Queensland and the Northern Territory; also gap-filling (non-NVIS) data in South Australia.  See the Introduction to the MVG fact sheets for further background on this series.

Semi-arid myall woodlands (Acacia pendula), western NSW (Photo: B. Pellow)