G. Scholle et al., HEXOSAMINES IN THE ORGANIC LAYER OF 2 BEECH FOREST SOILS - EFFECTS OFMESOFAUNA EXCLUSION, Biology and fertility of soils, 15(4), 1993, pp. 301-307
In December 1988, litter bags (mesh size: 45 and 1000 mum) were expose
d in the organic layer of unlimed and limed moder soil under beech for
est in the Solling area of Germany. Bags were retrieved on three sampl
ing dates (May, September, and November 1989) and amounts (g m-2) of g
lucosamine and galactosamine were determined. Horizon-specific differe
nces generally explained by far the largest part of the treatment vari
ance. In the substrate sampled in December 1988 from the unlimed area
glucosamine increased by a factor of 11.8 from the L1 layer to the H l
ayer and galactosamine by a factor of 15.9. With the exception of the
F2 layer, the hexosamine amounts found in the limed substrate sampled
in December 1988 were higher in all horizons than in the corresponding
horizons sampled from the unlimed area. Exclusion of mesofauna from t
he 45-mum litter bags generally reduced the level of amino sugars at b
oth sites. The difference between the two mesh sizes was most pronounc
ed in the lowermost horizons (F2 and H) and quite small in the upper h
orizons. The exclusion of mesofauna significantly increased the glucos
amine:galactosamine ratio in the two L layers of the unlimed soil on a
ll sampling dates. Seasonal fluctuations suggested that the actual ami
no sugar content of the organic layer was essentially the function of
two components, the first reflecting long-term accumulation of microbi
al metabolites, and the second reflecting short term fluctuations in t
he microbial colonization of various C sources together with spatial a
nd temporal differences in the ability of the microflora to produce an
d to decompose hexosamines. The results of this study show that the me
sofauna in the beech forest soils investigated significantly affected
both the amino sugar components measured, and thus stimulated the accu
mulation of one of the most important N pools in forest soils.