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Population 1<br />

Population 2<br />

Population 3<br />

Population 4<br />

Population 5<br />

cycles (Fig. 2). An example is the cellulolytic functional group; if the soil suspension<br />

is inoculated in Petri dishes with selective culture media for cellulolytic<br />

microorganisms, where cellulose is the only carbon source, and the<br />

culture is incubated at 28 °C for 3 days, some colonies will form halos around<br />

the colonies after staining with Congo red. If we count the different organisms<br />

by decreasing order of numbers, we can observe colonies forming units<br />

of fungi, actinomycetes and then bacteria. Many species will be observed<br />

within the fungi group, as will also occur with actinomycetes and bacteria<br />

populations.<br />

The number of colony forming units (CFU) and the ratio between colony<br />

size and degradation halo diameter should be considered in an evaluation<br />

study, while assessing the cellulolytic activity. These parameters determine<br />

the community size and/or the activity of the individuals that compose it. The<br />

biodiversity of the fungi, actinomycetes and bacteria that form this functional<br />

group are secondary parameters when assessing the functionality of the biogeochemical<br />

cycle under study.<br />

3 Carbon Cycle Functional Groups<br />

4 Microorganisms on the Rhizosphere Microcosm 53<br />

Celulase<br />

producers<br />

Protease<br />

producers<br />

Functional<br />

group of<br />

celulolytic<br />

Functional<br />

group of<br />

Proteolytic<br />

Fig. 2. Many populations of microorganisms may participate in one or more<br />

biogeochemical cycling<br />

C cycle<br />

N cycle<br />

The largest carbon reservoir is present in the sediments and rocks of the<br />

Earth, but the turnover time is so long that flow from this compartment is relatively<br />

insignificant on a human scale. From the viewpoint of living organisms,<br />

a large amount of organic carbon is found in land <strong>plant</strong>s. This represents<br />

the carbon of forests and grasslands and constitutes the major site of photosynthetic<br />

CO 2 fixation. However, more carbon is present in dead organic<br />

material, called humus, than in living organisms (Madigan et al. 2000)<br />

Plant residues are the largest fraction of all organic carbon entering the<br />

soil. Plants contain 15–60 % cellulose, 10–30 % hemicellulose, 2–30 % lignin,

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