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128<br />

Galdino Andrade<br />

decrease in the viable vegetative or spore form Bacillus units in the soil. Reddy<br />

and Rhae (1989) reported that a strain of B. subtilis introduced into an onion<br />

rhizosphere at a concentration of 7.2¥10 5 seed –1 could be recovered at only<br />

7¥10 3 <strong>plant</strong> –1 after 30 days, despite the decrease in numbers, the B. subtilis was<br />

effective in suppressing indigenous soil microbiota in the rhizosphere. Young<br />

et al. (1995) also observed that B. cereus survival was not influenced by developing<br />

wheat roots and the absence of a rhizosphere effect may be due to the<br />

fact that B. cereus was isolated originally from non-rhizosphere soil. The<br />

Bacillus spp. are often reported to be present in low numbers in the rhizosphere<br />

compared with other bacteria, such as fluorescent pseudomonas (Elliot<br />

Juhnke et al. 1987).<br />

Populations of C, P-cycling microorganisms and formed nodules changed<br />

during the <strong>plant</strong> growth period and were influenced by B. thuringiensis inoculation<br />

in soybean <strong>plant</strong>s. No differences were found on assemblages of bacteria<br />

and fungi in soil inoculated with B. thuringiensis, but time influenced the<br />

populations. The time corresponded to <strong>plant</strong> growth, AM root colonisation<br />

and nodule formation. Some physiological changes during <strong>plant</strong> growth,<br />

including C compounds released to the medium, influenced bacteria growth<br />

(Amora-Lazcano and Azcón 1997). AM colonisation and Bradyrhizobium<br />

japonicum nodulation normally decreased the amount of <strong>plant</strong> root-derived<br />

and organic matter available for heterotrophic bacteria and other soil<br />

microorganism growth by altering the root cell permeability, thus affecting<br />

exudation (Schwab et al. 1983). The carbon cycling microbiota populations<br />

also decreased their number of cells, possibly because of changes in C concentration<br />

in the rhizosphere. Negative correlation between symbiotic and<br />

cellulolytic, amylolytic and proteolytic microorganisms shows that carbon<br />

compounds from the root are important factors for their proliferation. Deleterious<br />

effects of AM roots on soil bacteria have also been observed, suggesting<br />

C competition (Marschner and Crowley 1996), although AM fungi and<br />

rhizobia do not consume C from the rhizosphere due to their symbiotic condition<br />

(Secilia and Bagyaraj 1987; Paulitz and Linderman 1989). Cellulolytic<br />

and amylolytic microorganisms decreased their cell number during the<br />

experiment, whereas proteolytic microorganisms increased their population<br />

the first time. This result suggested that this group had an extra supply of<br />

nutrients from inoculated crystal protein. The faster decrease in the proteolytic<br />

cell number after day 15 could be explained by the small amount of ICP<br />

free in the soil. Saxena et al. (1999) suggested that ICP binds rapidly and<br />

tightly to clays and humic acids and is protected against microbial degradation<br />

by being bound to soil particles. AM infection and nodule number<br />

increased in the time following the <strong>plant</strong> growth. The saprophyte fungi population<br />

decreased when the soil was inoculated with Cry- strain, and the same<br />

effect was observed in AM infection. In another experiment carried out under<br />

axenic conditions in Petri dishes, Cry– and Cry+ strains showed an inhibitory<br />

effect against the growth of some saprophytes fungi. This fungistasis effect

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