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20 Mycorrhizal Fungi and Plant Growth Promoting<br />

Rhizobacteria<br />

José-Miguel Barea, Rosario Azcón<br />

and Concepción Azcón-Aguilar<br />

1 Introduction<br />

Soil microbial communities are crucial in maintaining a biological balance in<br />

soil, a key issue for the sustainability of either natural ecosystems or agroecosystems<br />

(Kennedy and Smith 1995). When provided with available carbon<br />

substrates, soil microorganisms are able to develop a range of activities in the<br />

microhabitats where they flourish and some of these activities are of great relevance<br />

for <strong>plant</strong> growth and health and for soil quality (Bowen and Rovira<br />

1999). Soil-borne microbes are found bound to the <strong>surface</strong> of soil particles or<br />

in the soil aggregates, while others interact specifically with <strong>plant</strong> roots (Glick<br />

1995). Particularly important from the point of view of <strong>plant</strong> <strong>surface</strong> <strong>microbiology</strong><br />

are the interactions at the root – soil interface where microorganisms,<br />

<strong>plant</strong> roots and soil constituents interact (Lynch 1990; Azcón-Aguilar and<br />

Barea 1992; Linderman 1992; Kennedy 1998; Bowen and Rovira 1999; Barea<br />

2000; Gryndler 2000) to develop a dynamic environment what is known as the<br />

rhizosphere (Hiltner 1904). The rhizosphere, therefore, is the zone of influence<br />

of <strong>plant</strong> roots on the soil microbiota; a microcosm with physical, chemical<br />

and biological properties different from those of the root-free bulk soil<br />

(Bowen and Rovira 1999; Gryndler 2000; Barea 2000). A characteristic of the<br />

rhizosphere is that microbial diversity is altered and that the activity and<br />

number of microorganisms is increased (Kennedy 1998).<br />

The supply of photosynthates and decaying <strong>plant</strong> material to the root-associated<br />

microbiota is a key issue for rhizosphere formation and functioning.<br />

The release of organic material is known to occur mainly as root exudates,<br />

acting as either signals or growth substrates (Werner 1998). However, once<br />

the microbial population is established, rhizosphere developments are<br />

affected by microbially induced changes on rooting patterns and by the supply<br />

of available nutrients to <strong>plant</strong>s, which in turn modify the quality and<br />

quantity of root exudates (Bowen and Rovira 1999; Barea 2000; Gryndler<br />

2000). Microbial interactions in the rhizosphere are known to markedly influence<br />

<strong>plant</strong> fitness and soil quality (Lynch 1990; Bethlenfalvay and Schüepp<br />

Plant Surface Microbiology<br />

A.Varma, L. Abbott, D. Werner, R. Hampp (Eds.)<br />

© Springer-Verlag Berlin Heidelberg 2004

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