Abstract
The phosphorus (P) requirements of Australian plants are reviewed. Many
Australian plants have highly developed abilities for acquiring and
conservatively using P. This is seen as an evolutionary response to the
combined environmental pressures of fire, soil P levels that are in the lower
part of the range for world soils, and low and eratic rainfall. In natural
Australian ecosystems, more than 50% of the P in the A horizon is in
organic combination. Organic matter is the main source for the growth of
perennial plants, so the only successful assessments of
‘available’ P measure labile organic P and microbial P. However,
the inorganic P of ashbeds is essential to the rapid establishment of fire
ephemerals and tree seedlings in natural ecosystems. Almost all Australian
plants develop associations with mycorrhizal fungi, or produce hairy roots, as
ways of increasing P uptake. Highly developed abilities to redistribute P from
ageing to young tissues enable Australian plants to have a low P requirement
per unit of biomass production. This also results in low P losses in sawlogs
from natural forests, but not necessarily from short-rotation plantations. The
special role of P in the ecology and conservation of heathlands is reviewed.
Finally, an overview is given of the P requirements of Australian plants being
grown in soil-less media in nurseries.
Subject
Earth-Surface Processes,Soil Science,Environmental Science (miscellaneous)
Cited by
117 articles.
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