Gm. Lodge, THE ROLE AND FUTURE USE OF PERENNIAL NATIVE GRASSES FOR TEMPERATE PASTURES IN AUSTRALIA, New Zealand Journal of Agricultural Research, 37(3), 1994, pp. 419-426
Increasingly in Australia there is evidence of pasture decline; acidif
ication, salinisation, and land degradation are all indications that p
astoral and landform ecosystems are not in equilibrium. With declining
terms of trade for farmers, rapidly increasing costs of pasture estab
lishment and maintenance, and an increased environmental awareness in
the community, it is timely to consider the future and role of perenni
al native grasses in temperate pastures. Undoubtedly the sowing of per
sistent, well-adapted, deep-rooted native or introduced grasses can re
duce the rate of acidification or salinisation. Native grasses evolved
under conditions of a mostly dry and fluctuating climate, low nitroge
n and phosphorus soils, low grazing pressure by soft-footed marsupial
herbivores, low trampling pressure, high summer fire frequency, and lo
w densities of legumes such as Swainsona, Lotus, and Glycine. While in
troduced temperate perennial grasses often require a companion legume
and fertiliser input for productivity and persistence, the adaptive ch
aracteristics of some native grasses may be useful, particularly in ma
rginal environments where sown perennial grasses have poor persistence
. In many districts, all native grasses were thought to have similar a
daptive characters and so a philosophy evolved among many agricultural
ists to replace indigenous plants with fertilised legume-based pasture
s. This assumed that the level of land capability could be permanently
increased by adding introduced species to the pasture ecosystem, but
there is increasing evidence that this may not be so. Where useful nat
ive grasses predominate, they have a continuing role as a major pastur
e resource on most properties. Some farmers on the Tablelands of New S
outh Wales have developed stable and productive native grass-based pas
tures, carrying 8-15 dry sheep equivalents/ha, by manipulating grazing
pressure, fertiliser use, and legume growth. In winter rainfall and c
ropping zones, such as the Riverina of New South Wales and the Mallee
districts of Victoria, where native pastures occupy less than 25% of t
he agricultural land, native grasses are under test, because it is tho
ught they are more likely than introduced species to have a restorativ
e role in acidified, salinised, or degraded cropping lands. The availa
bility of seed of the better native grasses by domestication and seed
harvesting is seen as an adjunct to these roles, and not as providing
replacements for other persistent, productive perennial grasses.