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Phosphorus dynamics in a tropical forest soil restored after strip mining
Background and aims We hypothesized that successful early ecosystem and soil development in these P-deficient soil materials will initially depend on effective re-establishment of P storage and cycling through organic matter. This hypothesis was tested in a 26-year chronosequence of seven lightly fertilized, oxidic soil materials restored to eucalypt forest communities after bauxite mining.
Methods Total P (Pt) status, Hedley P fractions and partial chemical speciation (NaOH-EDTA extraction and analysed using solution 31P NMR spectroscopy) were determined in the restored soils.
Results Concentrations of Pt and most Hedley fractions changed with restoration period, declined with depth and were strongly positively correlated with C and N concentrations. Biological P dominated the Labile and Intermediate P fractions while Long-term P was dominantly inorganic.
Organic P concentrations in NaOH-EDTA extracts and their chemical natures were similar in restored and unburned native forest sites. Phosphomonoesters were the dominant class of organic P.
Conclusions Surprisingly rapid P accretion and fractional changes occurred over 26 years, largely in the surface soils and closely associated with organic matter status. Alkaline hydrolysis products of phosphodiesters and pyrophosphate indicated the importance of microbial P cycling. The important consequences for long-term ecosystem development and biological diversity require further study
Ectomycorrhizal fungal spores in the mounds of tropical Australian termites (isoptera)
The spores of ectomycorrhizal (ECM) fungi are shown to occur regularly within the mounds of grass-, litter- and\ud
wood-feeding termites in Australian savannah and forest environments, except in closed-forest environments lacking putative ECM host species. The spore population densities in mound materials are substantially greater and the communities more diverse at the generic level than those of soils adjacent to putative hosts. Many genera are common to both locations. Some implications of the presence of these fungi for nutrient flow and local diversity are considered