摘要：
This paper is on the biological impact of arsenic and antimony on the flora and microflora on a former Sbmining
site in Schlaining (Stadtschlaining, Burgenland, Austria). Several habitats were investigated with respect to biodiversity
and metalloid contamination in soil. Although the overburden of the mining activity had been remediated less than
ten years ago, metalloid concentrations occurred in soil up to 1.4 As and 3.6% Sb, respectively, in some microhabitats,
as determined by Instrumental Neutron Activation Analysis. These metalloids were embedded into a nonuniform mineralogical
background. Metalloid mobility could not be explained by common models, indicating that predictions on the mobility
of geogenic metalloids require additional mineralogical data. The biological effects of this contamination were variable.
We observed that metalloid resistant strands of microorganisms appeared in the contaminated soil. In cultivation experiments,
Sb was found to be more toxic than As. Sulphur oxidising strand were more resistant than organotrophic ones
and grew even better on cultivation media spiked with 10 ppm As than on the unspiked control. The flora was only partially
influenced: the lowest biodiversity was found in metalloid richest soils, but moderate contamination resulted in enhanced
species numbers. Only in one case, where the pH-buffering capacity of the soil was exceeded by consumption of
the entire carbonate, no embryophytes occurred. This was probably due to extreme pH conditions as well as to metalloid
concentrations. Our data support the hypothesis that higher plants are rather affected by extreme soil conditions, which often
coincide with As contaminations, than by the contamination itself. A small rivulet in this area contained 26 μg/l and
thus exceeded the WHO guideline value for As in drinking water by a factor of 2.6. Indeed we observed a diminished biodiversity
in this rivulet.
