ABSTRACT

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The vast majority of nutrient cycling processes in soil are carried out by

microorganisms. Organic nutrients and some inorganic compounds are supplied

through animal excreta, death of plants and animals, and exudation by plant roots

of plant-derived photosynthetic material. In agricultural ecosystems, nutrient

input is also provided by fertilizer application. This material must be recycled.

Some nutrients are returned to plants through uptake by roots, while others are

released to groundwaters, to runoff or to atmospheric gases. Although soil

macrofauna (nematodes, worms, enchytraeids) play a role in these recycling

processes, most of them are carried out by soil bacteria, archaea, fungi and

protozoa, for the purpose of this chapter collectively called soil microorganisms.