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changes. That allows to identify soil eutrophication already in its initial stages. The<br />

most important quantitative indicators reflecting these processes are increase of the<br />

total earthworm population, and formation of a stable Lumbricus rubellus population.<br />

Further stages of eutrophication processes feature changes of the earthworm<br />

communitie dominance structure- Dendrobaena octaedra, as the dominant species in<br />

natural forests, is replaced by Lumbricus rubellus. Greatly eutrophicated biotypes are<br />

characterized with formation of 3 to 4 species communities and diversification of the<br />

earthworm ecological groups. Very essential is formation of the endogeic<br />

populations, especially Aporrectodea caliginosa, what may occur only in a particular<br />

stage of the organic matter decomposition (Стриганова, 1980). Aporrectodea<br />

caliginosa is one of the most important soil animal representatives, which as a key<br />

species may significantly influence and quicken both processes in the soil and<br />

processes of the ecosystem. Formation of a stable population of Aporrectodea<br />

caliginosa may indicate on irreversible changes in the soil. However, pine forest<br />

eutrophication final stages may be easily identified by fitocenotic changes.<br />

Earthworms, as a bioindicator of these processes, have greater significance in the<br />

indication of the initial stages.<br />

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