Summary
Summary
Summary
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changes dominance structure, Dendrobaena octaedra is replaced by Lumbricus<br />
rubellus. Populations of endogeic Aporrectodea caliginosa form in greatly<br />
eutrophicated biocommunities.<br />
7. Formation of humus horizon in the eutrophicated soils create additional<br />
living-space for earthworms, both with appropriate feeding conditions and possibility<br />
to migrate into deeper layers in case of unfavorable meteorological conditions.<br />
8. Earthwrom activities in the eutrophicated forest soils become an essential<br />
inner factor of the biocenosis, and initiate further soil transformation process.<br />
Earthworms improve physical soil properties, activate breakdown of the organic<br />
matter and their spread into the soil profile, thus promoting formation of thicker<br />
humus horizon. Close to the populated areas establishment of new earthworm<br />
populations occur faster than in isolated forest areas, therefore, in such areas quicken<br />
the forest eutrophication processes.<br />
9. Earthworms are considered as great indicatiors of the oligotrophic pine<br />
forest eutrophication processes. The most important bioindicative indicators in the<br />
initial stages of the eutrophication processes are the total earthworm population<br />
density increase, 3 to 4 species earthworm communities, formation of a stable<br />
Lumbricus rubellus population, and expansion of the ecological group spectrum.<br />
10. Changes in earthworm communities are being detected before visual<br />
changes in the forest phytocenosis. That allows to identify soil eutrophication in its<br />
initial stages.<br />
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