Last updated:
18 Oct 2022
Distribution of the species within this region
The Spike-Rush is known or predicted to occur in the following sub-regions of the
Cobar Peneplain Interim Biogeographic Regionalisation of Australia Region.
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Vegetation formations, classes and types
In this region the Spike-Rush - Cobar Peneplain is known to
be associated with the following vegetation formations and classes. Click on a name to get background information
about it.
- Forested wetlands
- Inland Riverine Forests
- 10 River Red Gum - Black Box woodland wetland of the semi-arid (warm) climatic zone (mainly Riverina Bioregion and Murray Darling Depression Bioregion)
- 11 River Red Gum - Lignum very tall open forest or woodland wetland on floodplains of semi-arid (warm) climate zone (mainly Riverina Bioregion and Murray Darling Depression Bioregion)
- 36 River Red Gum tall to very tall open forest / woodland wetland on rivers on floodplains mainly in the Darling Riverine Plains Bioregion
- Freshwater wetlands
- Inland Floodplain Shrublands
- 24 Canegrass swamp tall grassland wetland of drainage depressions, lakes and pans of the inland plains
- 17 Lignum shrubland wetland of the semi-arid (warm) plains (mainly Riverina Bioregion and Murray Darling Depression Bioregion)
- 160 Nitre Goosefoot shrubland wetland on clays of the inland floodplains
- 240 River Coobah tall shrubland wetland of the floodplains in the Riverina Bioregion and Murray Darling Depression Bioregion
- Inland Floodplain Swamps
- 181 Common Reed - Bushy Groundsel aquatic tall reedland grassland wetland of inland river systems
- 182 Cumbungi rushland wetland of shallow semi-permanent water bodies and inland watercourses
- 226 Cyperus - Typha sedgeland wetland of the arid zone climate zone
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- Grassy woodlands
- Floodplain Transition Woodlands
- 251 Mixed Eucalypt woodlands of floodplains in the southern-eastern Cobar Peneplain Bioregion
- 56 Poplar Box - Belah woodland on clay-loam soils on alluvial plains of north-central NSW
- 244 Poplar Box grassy woodland on alluvial clay-loam soils mainly in the temperate (hot summer) climate zone of central NSW (wheatbelt).
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