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56<br />

Galdino Andrade<br />

organic nitrogen in the soil such as free-living ammonifiers and protozoans,<br />

which also have an important function of mobilisation and mineralisation of<br />

nitrogen compounds (Fig. 4). The choice of these groups within the nitrogen<br />

cycle was based on their ability to produce ammonia as an end product. Both<br />

the nitrogen fixers and the ammonifiers such as the protozoa release ammonia<br />

into the rhizosphere. However, the pathway production is different: (1) the<br />

first group uses atmospheric nitrogen that by biological fixation produces<br />

ammonia, (2) the second group takes part in the mineralisation process of<br />

nitrogen organic compounds and, (3) the third group, such as microorganism<br />

predators, obtain proteins from their prey and excrete ammonia, among other<br />

substances.<br />

Atmospheric nitrogen fixation is a fundamental process for the maintenance<br />

of the biosphere, as all organisms require proteins. Nitrogenase is an<br />

enzyme complex which is responsible for nitrogen fixation and requires great<br />

quantities of energy for its activity. Non-symbiotic biological fixation of<br />

nitrogen is carried out by some free-living bacteria genera which are associ-<br />

Protozoans<br />

Feeding<br />

Bacteria<br />

Excretion<br />

Microbiota<br />

Proteins<br />

Aminoacids<br />

Excretion<br />

Celular death<br />

Proteases<br />

Peptidases<br />

Microbial<br />

Mineralization<br />

NH4 + N2<br />

Nitrogen<br />

fixation<br />

Fig. 4. The activity of some functional groups of microorganisms in the nitrogen cycle

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