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Review of Grassland Management in south-eastern ... - Parks Victoria

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<strong>Parks</strong> <strong>Victoria</strong> Technical Series No. 39<br />

<strong>Grassland</strong> <strong>Management</strong> <strong>in</strong> SE Australia<br />

INDEX OF TABLES AND FIGURES<br />

TABLES<br />

Table 1. F<strong>in</strong>d<strong>in</strong>gs from recent reviews <strong>of</strong> graz<strong>in</strong>g impacts on biodiversity outcomes……..…..7<br />

Table 2. State box show<strong>in</strong>g example <strong>of</strong> what can be recorded to simply <strong>in</strong>form management<br />

and describe particular states........................................................................................................... 17<br />

Table 3. Basic state-and-transition diagram show<strong>in</strong>g example <strong>of</strong> how these may be used to<br />

describe management outcomes or hypothesis. ........................................................................... 18<br />

Table 4. Impacts <strong>of</strong> <strong>Management</strong> Options – What do we know?................................................ 21<br />

Table 5. Recommended template for Northern Pla<strong>in</strong>s semi arid grasslands <strong>in</strong> Glassons<br />

<strong>Grassland</strong> Reserve management plan............................................................................................ 25<br />

FIGURES<br />

Figure 1. Estimated extent <strong>of</strong> lowland grassy ecosystems at the time <strong>of</strong> European settlement (black).<br />

The current distribution <strong>of</strong> ‘natural’ lowland grassy ecosystems is estimated to be less than 0.5% <strong>of</strong><br />

this area. Mapp<strong>in</strong>g <strong>in</strong>formation was obta<strong>in</strong>ed from Geosciences Australia’s database us<strong>in</strong>g tree, shrub<br />

and grass cover to estimate distribution <strong>of</strong> vegetation types. ................................................................. 1<br />

Figure 2. Estimated extent <strong>of</strong> lowland grassy ecosystems at the time <strong>of</strong> European settlement<br />

separated <strong>in</strong>to ra<strong>in</strong>fall zones. Dark areas are those with annual ra<strong>in</strong>fall more than 450 mm, hatched<br />

areas will have annual ra<strong>in</strong>fall below 450 mm <strong>in</strong> some years, and gray areas have average annual<br />

ra<strong>in</strong>fall below 450 mm <strong>in</strong> all years. Mapp<strong>in</strong>g <strong>in</strong>formation from Geoscience Australia’s database. ......... 2<br />

Figure 3. Basalt Pla<strong>in</strong>s grassland structure, reproduced from Patton (1935). Themeda triandra<br />

tussocks (T) with associated grassland species <strong>in</strong> the <strong>in</strong>tertussock spaces. The spac<strong>in</strong>g and variation<br />

<strong>in</strong> the size and structure <strong>of</strong> the Kangaroo grass tussocks with<strong>in</strong> this diagram is the ma<strong>in</strong> po<strong>in</strong>t to<br />

observe. The use <strong>of</strong> graz<strong>in</strong>g is believed to reduce the variability <strong>of</strong> tussock size and thus reduce the<br />

variability <strong>in</strong> the size and shape <strong>of</strong> <strong>in</strong>ter-tussock spaces. If, as many authors and managers assume,<br />

the variability <strong>in</strong> structure is vital for plant recruitment <strong>in</strong> these systems, as well as faunal habitat, then<br />

manag<strong>in</strong>g grasslands to achieve variable tussock structure and “mak<strong>in</strong>g the environment right” to<br />

allow natural ecological process to occur should be the aim <strong>of</strong> management........................................ 3<br />

Figure 4. Hypothesized structure <strong>of</strong> pre-European settlement Northern Pla<strong>in</strong>s <strong>Grassland</strong>. Reproduced<br />

from Foreman (1996). The large perennial shrubs depicted above are now miss<strong>in</strong>g from many<br />

Northern Pla<strong>in</strong>s grasslands. Tussock spac<strong>in</strong>g <strong>in</strong> these systems is believed to have been ma<strong>in</strong>ta<strong>in</strong>ed by<br />

<strong>in</strong>ter-specific <strong>in</strong>teractions between w<strong>in</strong>ter and summer active perennial forbs and grasses (although<br />

the dynamics <strong>of</strong> this system are not understood, graz<strong>in</strong>g exclusion plots have shown this trend with an<br />

<strong>in</strong>itial dramatic <strong>in</strong>crease <strong>in</strong> the density <strong>of</strong> w<strong>in</strong>ter active species such a wallaby grass and their<br />

subsequent decl<strong>in</strong>e and an <strong>in</strong>crease <strong>in</strong> spac<strong>in</strong>g between tussocks and summer active species<br />

dom<strong>in</strong>ance). The patterns shown above are assumed to be driven by an <strong>in</strong>crease <strong>in</strong> the variability <strong>of</strong><br />

VI

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