Journal of the Royal Society of New Zealand abstracts
Comparison of soil microbial properties and fauna under tussock-grassland
and pine plantation
G. W. Yeates, S. Saggar*
To investigate responses of selected soil characteristics to vegetation changes
in high-country soils, samples were collected from under unburned
Chionochloa rigida grassland, burned
C. rigida,
12-year-old
Pinus radiata trees and from glades within pine forest where
trees had failed to grow. Under
P. radiata there were lower soil pH and
exchangeable Ca, Mg, K and Fe, while lower microbial C, N and P in the
plantation confirmed other findings that
P. radiata reduces C, N and P
pools in mineral soil. Relatively small differences in microbial biomass C and
P between tussock >25 and <14 years since burning suggest that burning
has a lesser effect than
P. radiata on these properties. Burning,
however, affected biomass N. Numerical abundance of megascolecid earthworms was
greatest in tussock-grassland and in glades; they were least abundant under
P. radiata. However, the heaviest individual earthworms occurred under
P. radiata and in glades. Indices suggest a less stable or more rapidly
reproducing nematode fauna under
P. radiata; nematode generic diversity
was lowest under
P. radiata. Although the four vegetation types affected
soil properties in various ways, most properties under the
P. radiata
plantation were most different. The decline in microbial biomass C, N and P and
the microbial C: organic C ratio under
P. radiata suggest lower organic
matter inputs into the soil, and as such could be regarded as a decline in
ecological sustainability. The associated shift in the structure of the biotic
community observed in this study emphasizes the rôle of biotic factors as
independent variables for monitoring soil organic matter dynamics under
different land-uses.
Keywords: soil microbial biomass; soil organic matter; earthworms; nematodes;
tussock-grassland; land use; sustainability
(c) Journal of The Royal Society of New Zealand,
Volume 28, Number 3, September 1998, pp 523-535
PDF file of entire paper: medium quality (918K); (scanned from paper original: notes about this process)
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