Recovery plan for the brush-tailed rock-wallaby - Department of ...
Recovery plan for the brush-tailed rock-wallaby - Department of ...
Recovery plan for the brush-tailed rock-wallaby - Department of ...
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Approved NSW <strong>Recovery</strong> Plan Brush-<strong>tailed</strong> <strong>rock</strong>-<strong>wallaby</strong><br />
Valley (NPWS 1999), and could potentially have adversely affected <strong>the</strong> BTRW colony in <strong>the</strong><br />
area by preventing <strong>the</strong>ir escape. Bugg (1995) speculates <strong>the</strong> Kangaroo River colony has persisted<br />
because much <strong>of</strong> its habitat remains unburnt. Major fires erupt in <strong>the</strong> area on a 10–15 year cycle<br />
and remain a constant threat to BTRW colonies. DECC and local bushfire services conduct<br />
hazard reduction works in strategic locations in <strong>the</strong> area to minimise <strong>the</strong> risk <strong>of</strong> major fires, but<br />
acknowledge <strong>the</strong> potential <strong>of</strong> worst case situations (NPWS 1999).<br />
There is anecdotal evidence <strong>of</strong> easterly movement <strong>of</strong> <strong>the</strong> Kangaroo River colony after <strong>the</strong> 1983<br />
fire. Lobert and Waters (1988) and Pearson (1992) consider that fire may reduce food<br />
availability <strong>for</strong> <strong>the</strong> BTRW, but Capararo and Beynon (1996) consider fires adjacent to <strong>rock</strong><strong>wallaby</strong><br />
colonies may favour grass growth <strong>for</strong> feeding.<br />
Over many years, fires may change <strong>the</strong> vegetation structure and floristics. For example, frequent<br />
burning is likely to be responsible <strong>for</strong> <strong>the</strong> loss or contraction <strong>of</strong> rain<strong>for</strong>est. Bugg (1995) believes<br />
that vegetation change may partially explain <strong>the</strong> local decrease in BTRW abundance at<br />
Kangaroo Valley. The impact <strong>of</strong> fire regimes on this species requires research.<br />
The ultimate impact <strong>of</strong> fire is probably determined by <strong>the</strong> combination <strong>of</strong> fire intensity and<br />
regime, which are determined by land management practices, topography and climatic factors.<br />
Fur<strong>the</strong>r research in this area is required. In assessing <strong>the</strong> appropriate management response to<br />
fire, both <strong>the</strong> effects on vegetation structure (e.g. promotion <strong>of</strong> grasses, opening <strong>of</strong> canopy, loss<br />
<strong>of</strong> mesic vegetation), and o<strong>the</strong>r factors (e.g. fox and goat invasions), will need to be considered.<br />
9.1.7 Bioclimatic factors<br />
The influence <strong>of</strong> bioclimatic changes on BTRW distribution remains unknown. Some argue that<br />
bioclimatic changes, resulting in lower rainfall and a decline in rain<strong>for</strong>est vegetation, have<br />
contributed to <strong>the</strong> contraction in BTRW distribution (Bugg 1994). In contrast, Short and<br />
Milkovits (1990) consider climatic variables relatively unimportant compared to micro-habitat<br />
variables. The great habitat flexibility demonstrated by BTRWs suggests that, given a slow<br />
transition in climate that alters ra<strong>the</strong>r than changes habitat, <strong>the</strong> species may be able to adapt<br />
locally to future climate changes.<br />
Preliminary research indicates that some climatic variables correlate with extinction patterns in<br />
<strong>the</strong> species across its range. However, it is likely that <strong>the</strong>se correlations are not causative, but<br />
ra<strong>the</strong>r reflect <strong>the</strong> patterns <strong>of</strong> o<strong>the</strong>r extinction factors, <strong>for</strong> example, land clearing and fox numbers<br />
(Cavanagh unpub.).<br />
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