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4 Microorganisms on the Rhizosphere Microcosm 65<br />

<strong>plant</strong>s (k strategists) to establish in the area and to form a forest in equilibrium.<br />

The pioneer <strong>plant</strong>s can survive under adverse conditions due to the presence<br />

in the rhizosphere of microorganisms which supply nutrients for their<br />

metabolism, and in turn, their exudates maintain these rhizosphere microorganisms.<br />

The k strategist mycorrhizae are sufficiently stable to maintain the<br />

required nutrient levels for this <strong>plant</strong> group. In this sense, groups of r strategist<br />

microorganisms succeed each other, maintaining the dynamic of the system<br />

and the reconstitution of other biogeochemical cycles until the system<br />

equilibrium is reached with the establishment of late secondary and climax<br />

<strong>plant</strong> groups.<br />

10 Dynamics Among the Functional Microrganism Groups<br />

of the Carbon, Nitrogen, Phosphorus and Sulphur Cycles<br />

There are several stages in each biogeochemical cycle, and many microorganisms<br />

can take part in one or more cycles depending on the diversity of their<br />

metabolic path (Fig. 10). Microbiota metabolic versatility makes a single bacteria<br />

species able to use various carbohydrates, such as glucose, fructose and<br />

saccharose, as a carbon and energy source, and in their absence they can use<br />

amino acids or other compounds.<br />

The biosphere is composed of all living organisms which depend on matter<br />

transformation for their maintenance. The functional microorganism groups<br />

are inserted in this system which transforms matter and maintains the levels<br />

of nutrients available on Earth. Due to their functional importance, they can<br />

be used as biological indicators to determine any natural or artificial impact<br />

which may occur in the soil. It is obvious that the complexity of the biological<br />

interactions occurring on the soil–<strong>plant</strong> interface must be simplified to allow<br />

quick and accurate assessment of these microorganism populations. Thus,<br />

only those stages of the biogeochemical cycles which directly influence <strong>plant</strong><br />

growth should be chosen. However, different stages can be selected according<br />

to the experimental objective.<br />

Autotrophic organisms have the important function of matter de-mineralisation<br />

and transform it into organic molecules. In this group are <strong>plant</strong>s that<br />

de-mineralise carbon, i.e. transform carbon dioxide (CO 2) into glucose, which<br />

is then polymerised mainly into starch, cellulose, hemicellulose and lignin.<br />

Plants are also responsible for transforming NO 3 – ,NH3 + ,and SO4 2– into amino<br />

acids, PO 4 2– into nucleic acids while ATP, NADP, and SO4 2– can be transformed<br />

into glutathione.<br />

In a simplified way, <strong>plant</strong>s can be considered as nutrients from the soil<br />

solution plus solar energy accumulated in chemical form. Plants generally<br />

release organic molecules into the soil in two ways: (1) by depositing dead<br />

<strong>plant</strong> material to form the litter; and, (2) by exuding excretion and lysates into

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