Regional ecosystem details for 10.3.15
| Regional ecosystem | 10.3.15 |
|---|---|
| Vegetation Management Act class | Least concern |
| Wetlands | Palustrine |
| Biodiversity status | Of concern |
| Subregion | 1, 2, (3), (4) |
| Estimated extent1 | Pre-clearing 30000 ha; Remnant 2021 29000 ha |
| Short description | Eucalyptus camaldulensis and/or E. coolabah woodland in closed depressions |
| Structure code | Woodland |
| Description | Eucalyptus camaldulensis and/or E. coolabah or E. brownii or E. cambageana or Casuarina cristata or Acacia cambagei open woodlands to woodlands or grasslands and/or seasonal lagoons vegetation. Includes ephemeral grasslands, herblands and clay pans. Includes some partially open depressions such as Webb Lake and Lake Moocha. Occurs on grey clay soils in closed depressions on sandplain or ferricrete. Palustrine. (BVG1M: 34b). Vegetation communities in this regional ecosystem include: 10.3.15a: [RE not in use]²: This vegetation community is now mapped as 10.3.15ax1. Open grassland of Brachyachne spp. Brachyachne convergens or B. tenella dominate the sparse ground layer. RE is defunct. Palustrine. (BVG1M: 34b). 10.3.15ax1: Mixed tussock grassland of Astrebla squarrosa, Dactyloctenium radulans, Aristida latifolia, Bothriochloa ewartiana and Iseilema vaginiflorum in closed depressions. Occurs on flat terrain with clayey soil. Contains Palustrine. (BVG1M: 34b). 10.3.15b: [RE not in use]²: This vegetation community is now mapped as 10.3.15c. Ephemeral herbland, grassland or bare ground. Variable ecosystem with dominant graminoids including Eriachne armitii and Fimbristylis dichotoma. Aristida jerichoensis, Chloris pectinata and Eragrostis spp. Are commonly present. Occurs in closed depressions on Tertiary sandplain or ferricrete with grey clay soils. Palustrine. (BVG1M: 34b). 10.3.15c: Closed depressions usually with Eleocharis equisetina swamp. Variable ecosystem with dominants including Eleocharis equisetina, Pseudoraphis spinescens or Eriachne benthamii. Occurs in closed depressions on Tertiary sandplain or ferricrete with grey clay soils. Palustrine. (BVG1M: 34b). 10.3.15d: [RE not in use]²: This vegetation community is now mapped as 10.3.15dx1. Acacia cambagei dominates the very sparse canopy. Brachyachne convergens dominates the very sparse ground layer. Occurs in closed depressions on Tertiary sandplain or ferricrete with grey clay soils. Palustrine. (BVG1M: 26a). 10.3.15dx1: Acacia cambagei low woodland with seasonal ground layer of tussock grasses and forbs. Occurs on clay lenses in sand sheets. Not a Wetland. (BVG1M: 26a). 10.3.15e: Eucalyptus camaldulensis woodland, occasionally with Corymbia dallachiana and Corymbia plena. A second tree layer commonly occurs and may include Acacia stenophylla, Acacia salicina and Melaleuca nervosa. The mixed ground layer includes Diplachne fusca, Cyperus spp., Eleocharis pallens, Aristida jerichoensis and Eragrostis speciosa. Occurs in closed depressions on sandy plains. Palustrine. (BVG1M: 34b). 10.3.15ex1: [RE not in use]²: This vegetation community is now mapped as 10.3.15e. Eucalyptus camaldulensis open woodland dominates the very sparse canopy. The ground layer is dominated by tussock grasses including Eragrostis speciosa, Schizachyrium fragile and Elionurus citreus. Occurs on sand over hard pan on alluvial plain. Contains Palustrine. (BVG1M: 34b). 10.3.15f: Eucalyptus coolabah woodland, commonly with Acacia cambagei. Duma florulenta shrub layer may be present. The ground layer is typically tussock grasses and sedges including Diplachne fusca, Eulalia aurea, Paspalidium jubiflorum and Cyperus spp. Occurs on closed to partially open depressions. Palustrine. (BVG1M: 34b). 10.3.15g: Eucalyptus brownii woodland with tussock grass ground layer dominated by Eulalia aurea. Occurs in closed depressions. Palustrine. (BVG1M: 34b). 10.3.15h: [RE not in use]²: This vegetation community is now mapped as 10.3.15hx1. Eucalyptus coolabah dominates the very sparse canopy. Eremophila bignoniiflora dominates the very sparse shrub layer. Brachyachne convergens and Eragrostis setifolia dominate the very sparse ground layer. Chloris pectinata, Cyperus scariosus, Desmodium campylocaulon, Iseilema vaginiflorum, Neptunia gracilis and Sida trichopoda are commonly occurring forbs and grasses. Occurs in closed depressions on Tertiary sandplain or ferricrete with grey clay soils in the west. Palustrine. (BVG1M: 34b). 10.3.15hx1: Eucalyptus coolabah low woodland to woodland with tussock grass ground layer. Occurs in closed depressions in sand plains. Palustrine. (BVG1M: 34b). 10.3.15i: [RE not in use]²: This vegetation community is now mapped as 10.3.15hx1. Eucalyptus coolabah dominates the very sparse canopy. The very sparse ground layer is frequently dominated by Pseudoraphis spinescens. Occurs in closed depressions on Tertiary sandplain in the east. Palustrine. (BVG1M: 34b). 10.3.15j: [RE not in use]²: This vegetation community is now mapped as 10.3.15c. The very sparse to sparse ground layer is dominated by Eleocharis spp. Usually with Pseudoraphis spinescens. In wet times there will be open water which gives way as the country dries out to an annual forbland which may have a mix of native and exotic species. During drier periods most of this community will be completely bare. RE is defunct. Not a Wetland. (BVG1M: 34b). 10.3.15k: [RE not in use]²: This vegetation community is now mapped as 10.3.15g. Eucalyptus brownii dominates the very sparse canopy. E. brownii also occurs as scattered trees or forms a low tree layer. The ground layer is dominated Eulalia aurea. RE is defunct. Palustrine. (BVG1M: 17a). 10.3.15l: [RE not in use]²: This vegetation community is now mapped as 10.3.30. Casuarina cristata dominates the very sparse canopy as well as the low tree layer. Eucalyptus coolabah is occasionally present in the canopy. Paspalidium jubiflorum, P. caespitosum and Neptunia gracilis in a weakly developed very sparse ground layer. RE is defunct. Palustrine. (BVG1M: 25a). 10.3.15m: Eucalyptus coolabah and/or Eucalyptus cambageana woodland with tussock grass ground layer. Occurs on the perimeter of Lake Galilee on the margins of lunettes. Not a Wetland. (BVG1M: 16c). 10.3.15n: [RE not in use]²: This vegetation community is now mapped as 10.3.15c. Diplachne fusca dominates the very sparse to mid-dense ground layer. RE is defunct. Palustrine. (BVG1M: 34b). 10.3.15o: [RE not in use]²: This vegetation community is now mapped as 10.3.15f. Eucalyptus coolabah dominates the very sparse to sparse canopy. Sporobolus mitchellii and Cyperus spp. dominate the very sparse ground layer. Occurs on the inside edge of the lake adjacent to old sand dunes. Palustrine. (BVG1M: 34a). |
| Supplementary description | Gunn et al. (1967), Rn; Lorimer (1998), Ql1, Ql3; Perry et al. (1964), E, Br; Thompson and Turpin (in prep), E73, E73a, E73b, G9, Wa, Da; Turner et al. (1993), E3, E6, L1 |
| Protected areas | White Mountains NP |
| Special values | 10.3.15: Seasonal wetland values for water bird nesting and feeding. Habitat for newly discovered species Goodenia sp. (Torrens Creek E.J.Thompson+ HUG754). The only recorded locations of Calostemma luteum and Hypoxis hygrometrica in the DEU occur in 10.3.15. The seasonal wetlands are in this ecosystem are important for water bird nesting and feeding, and aquatic species and potential habitat for the endangered species, Eriocaulon aloefolium, Eriocaulon giganticum, and Ammannia robertsii. As for other riparian zones, this ecosystem has important values for stabilising top soils, providing corridors for wildlife, and for trapping soil and maintaining water quality. 10.3.15d: Potential habitat for vulnerable species Acacia crombiei. |
| Fire management guidelines | SEASON: Wet to mid-dry season while soil retains moisture. INTENSITY: Low to occasional moderate. INTERVAL: Approximately 5-10 years. Do not burn during drought years. Concentrate burning during wet years. INTERVAL_MIN: 5. INTERVAL_MAX: 10. STRATEGY: Most of the vegetation communities will be difficult to burn. Mosaic 50-80% of area targeted. ISSUES: Grazing can impact heavily and combined with low rainfall fuel loads will be low making burning difficult. Can be advantageous to burn in year following good rains to manage currant bush and false sandalwood. Eucalypts such as E. dallachiana and E. coolabah germinate and recruit following rainfall; do not burn to thin as attrition will reduce density in drought years. |
| Comments | 10.3.15: Subject to soil and pasture degradation. Potential for invasion by weed species including *Cryptostegia grandiflora (rubber vine) and Parkinsonia aculeata, and degradation by high total grazing pressure. Pigs are attracted to these areas causing major soil disturbance, fouling of water holes, and destroying wildlife and habitat. 10.3.15b: Relatively uncommon ecosystem only found in the driest parts of the bioregion in subregion 1 represented by small sandy closed depressions and edges of some larger lakes. 10.3.15c: Widespread but does not occupy extensive areas. 10.3.15d: Uncommon ecosystem only known from subregion 1 near Ludgate Hill. 10.3.15e: An uncommon ecosystem occurring in northern parts of subregion 2. It has been recorded at Lake Moocha, Webb Lake, The Dry Swamp and Thirlestone. 10.3.15f: Occurs mostly on the perimeter of Lake Galilee and also at Lake Barcoorah. 10.3.15g: Uncommon ecosystem occurring mostly in northern parts of subregion 2. 10.3.15h: Uncommon ecosystem only known from subregion 1. 10.3.15i: A rare ecosystem occurring mostly near Barcaldine. 10.3.15j: Uncommon ecosystem known from near Webb Lake, Lake Moocha and the Dry Swamp. Further survey required for comprehensive floristic composition. 10.3.15l: Very rare ecosystem only known from the perimeter of Lake Galilee. *Vachellia farnesiana is present as scattered shrubs. 10.3.15m: Very rare ecosystem only known from Lake Galilee. Naturalised species associated with this regional ecosystem include *Echinochloa colona, *Cenchrus ciliaris and *Chloris virgata, which may dominate the ground layer. 10.3.15n: Very rare ecosystem only known from near Lake Buchanan. 10.3.15o: Very rare ecosystem only known from Lake Galilee. |
1 Estimated extent is from version 13.1 pre-clearing and 2021 remnant regional ecosystem mapping. Figures are rounded for simplicity. For more precise estimates, including breakdowns by tenure and other themes see remnant vegetation in Queensland.
2 Superseded: Revision of the regional ecosystem classification removed this regional ecosystem code from use. It is included in the regional ecosystem description database because the RE code may appear in older versions of RE mapping and the Vegetation Management regulation.
