Commonwealth of Australia

 

Amendment to the list of threatened ecological communities under section 181 of the Environment Protection and Biodiversity Conservation Act 1999

 

 

I, PETER ROBERT GARRETT, Minister for the Environment, Heritage and the Arts, pursuant to paragraphs 184(1)(a) and (b) of the Environment Protection and Biodiversity Conservation Act 1999, hereby amend the list referred to in section 181 of that Act by:

 

deleting from the list in the endangered category

Cumberland Plain Woodlands; and

including in the list in the critically endangered category

Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest

as described in the Schedule to this instrument.

 

 

 

 

 

Dated this…......Seventeenth..............day of….............November.................2009

 

 

 

 

 

 

 

Peter Robert Garrett

 

Minister for the Environment, Heritage and the Arts

 


SCHEDULE

Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest

 

The Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest is an ecological community that is endemic to New South Wales, with occurrences in and around the Cumberland Plain, west of Sydney. Its distribution is limited to the Sydney Basin Bioregion.

The ecological community mostly occurs on flat to undulating or hilly terrain, generally at elevations up to 350 metres above sea level with some occurrences extending onto locally steep sites and at slightly higher elevations. The ecological community is predominantly associated with clay soils derived from Wianamatta Shale geology with minor occurrences present on other soil groups, which occur on the plains and in the vicinity of shale outcrops. Part of the ecological community also is associated with shale soils with high concentrations of iron-indurated gravel or overlain by Tertiary Alluvium and those sites are marked by the shale-gravel transition forest component of the ecological community.

The Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest is a type of eucalypt woodland to forest with an understorey (i.e. the ground plus shrub layers) that varies from predominately grassy to predominately shrubby.

The upper tree layer is typically dominated by Eucalyptus moluccana (Coastal Grey Box) and E. tereticornis (Forest Red Gum). A range of other tree species commonly occur in association with Coastal Grey Box and Forest Red Gum and may be locally dominant, including: E. crebra (Narrow-leaved Ironbark), E. eugenioides (Thin-leaved Stringybark) and Corymbia maculata (Spotted Gum). In the shale-gravel transition forest component of the ecological community, the tree layer may be locally dominated by E. fibrosa (Red Ironbark), with Coastal Grey Box and Forest Red Gum occurring less frequently.

The lower tree layer is absent to sparse, when present. This layer may include younger individuals of the upper tree layer species. Other small trees typically present in this layer include: Acacia implexa (Hickory Wattle), A. parramattensis (Parramatta Wattle), A. decurrens (Black Wattle, Green Wattle), Exocarpos cupressiformis (Native Cherry) and Melaleuca decora (Paperbark). Paperbark frequently occurs in the shale-gravel transition forest component of the ecological community.

The understorey may include shrub and ground layers of variable development and composition. The understorey is typically dominated by the ground layer. However, the ground layer may be reduced where a well developed shrub layer is present. The shrub layer is often dominated by Bursaria spinosa (Blackthorn) but other shrub species may also be present. The ground layer is typically dominated by a range of native grasses and other herbs and shows considerable variation in floristic composition across remnant patches.

The key diagnostic attributes for the Cumberland Plain Shale Woodlands and Shale-Gravel Transition Forest ecological community are as follows: