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5 - The edaphic theory II. Soil types, drainage, and fertility

Published online by Cambridge University Press:  23 November 2009

D. M. J. S. Bowman
Affiliation:
Northern Territory University, Darwin
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Summary

Andrews (1916) eloquently expressed the idea that soil fertility was critical in delimiting rainforest when he wrote that around Sydney:

there are sheltered areas or pockets of volcanic soil or shales, on which dense luxuriant plant growths abound forming canopies of dark and glossy green, which exclude a great proportion of the sun's rays. Surrounding these patches are the hungry sandstones forming so much of the large Sydney and Blue Mountains district, whose vegetation is in striking contrast with that of the rich soils. Here is to be seen no luxuriant foliage, no twining nor towering canopy to the jungle, but instead merely an array of Eucalyptus, phyllodineous acacias, banksias of sombre hue and casuarinas.

Subsequently, a number of ecologists have also advocated the idea that soil fertility is critical in determining the distribution of rainforest vegetation (McLuckie and Petrie 1927; Davis 1936; Fraser and Vickery 1938, Pidgeon 1940; Herbert 1960; Florence 1964, 1965; Webb 1968). The object of this chapter is to show that Australian rainforests are not consistently limited by soil texture, drainage, or soil fertility.

Geology and soil types

While it is true that the largest tracts of rainforest in Australia are, and were before being cleared, associated with fertile basaltic soils, the importance of soil parent material in controlling rainforest has been over-emphasised.

Type
Chapter
Information
Australian Rainforests
Islands of Green in a Land of Fire
, pp. 84 - 98
Publisher: Cambridge University Press
Print publication year: 2000

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