Western Sydney Dry Rainforest
Geography
It is a dry, scrubby, vegetation community that is disjointed and is limited to the covered slopes and gully bottoms of the Cumberland Plain, where it is found in small parts in the natural areas of Picton, Camden, Grose Vale, Cattai, Campbelltown, Razorback, Abbotsbury (near Calmsley Hill City Farm), and as well to the north in Richmond, Parramatta, Ryde, Baulkham Hills, where it grades from a dry rainforest with a closed non-eucalypt canopy into moist woodland with an open canopy dominated by eucalypts.
It is found in relatively higher rainfall areas compared to the areas on the western Sydney plain in precipitous and more rugged terrain. Only about 950 hectares remain, almost all of which occurring as highly disunited patches under 10 ha in size.
Ecology
The dry rainforest is a low, closed forest that mostly features non-eucalypts, such as Melaleuca styphelioides, Acacia implexa, Alectryon subcinereus and Melicope micrococca with an understory of various shrubs, and a mostly sparse cover of grasses, vine thickets, ferns and other herbs such as Alchornea ilicifolia. Plants that generally occur in other types of rainforest/moist woodland in New South Wales are usually nonexistent in this community, such as palms and mosses.
Shrubs include Notelaea longifolia, Spartothamnella juncea, Marsdenia viridiflora, Clerodendrum tomentosum and Pittosporum revolutum, with vines such as Aphanopetalum resinosum, Pandorea pandorana and Causonis clematidea.
Fauna
Fauna species include Mixophyes iteratus, Alectura lathami, Stagonopleura guttata, Acanthorhynchus tenuirostris and Anthochaera phrygia.
References
- ^ Western Sydney Dry Rainforest and Moist Woodland on Shale: a nationally-protected ecological communityDepartment of Environment. Retrieved 14 September 2022. Text was copied from this source, which is available under a Creative Commons Attribution 4.0 International License.
- ^ Western Sydney Dry Rainforest in the Sydney Basin Bioregion - profile Office of Environment & Heritage. Retrieved 14 September 2022.