Field and Greenhouse Trials Performed with Phosphate Solubilizing Bacteria and Fungi

Hani Antoun

Departement of Soil and Agrifood Engineering, Faculty of Agriculture and Food Science, Laval University, Quebec, CANADA

E-mail: Antoun@rsvs.ulaval.ca

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Soils microorganisms are involved in a range of processes that affect P transformation and thus influence the subsequent availability of phosphate to plant roots (Richardson, 2001).

Free-living phosphate solubilizing microorganisms (PSM) are always present in soils. The populations of inorganic P-solubilizing microorganisms are sometimes very low, less than 102 cfu g-1 of soil as observed in a soil in Northern Spain (Peix et al., 2001). In four Quebec soils the number of root free PSM ranged from 2.5-to 3 x 106 cfu g-1 of soil and they represented from 26-to 46% of the total soil microflora (Chabot et al., 1993). As observed with other soil microbes the number of PSM is more important in the rhizosphere than in non-rhizosphere soil (Kucey et al., 1989), and the number of phosphate solubilizing bacteria is more important than that of fungi (Kucey, 1983). However, inoculation studies aimed are improving P nutrition in plants involved bacteria and fungi, and commercially in Western Canada the phosphate inoculant JumpStart (PhilomBios, Saskatoon, Sask.) sold for wheat, canola, mustard and other legumes contain an isolate of Penicillium bilaii  (http://www.philombios.ca/).

Rhizobacteria, are bacteria that aggressively colonize plant roots. Plant growth promoting rhizobacteria (PGPR) are a very small portion of rhizobacteria (2-5%) that promote plant growth (Antoun and Kloepper, 2001).  PGPR use one or more of direct or indirect mechanisms of action to improve plant growth and health. These mechanisms can probably be active simultaneously or sequentially at different stages of plant growth. P-solubilization, biological nitrogen fixation, improvement of other plant nutrients uptake and phytohormone production like indole-3-acetic acid are some examples of mechanisms that directly influence plant growth. Some PGPR have the enzyme 1-aminocyclopropane-1-carboxylate (ACC) deaminase, which hydrolyses ACC, the immediate precursor of ethylene in plants (Glick et al., 1995). By lowering ethylene concentration in seedlings and thus its inhibitory effect, these PGPR stimulate seedlings root length (Glick et al., 1999).  Biological control of plant pathogens and deleterious microbes, through the production of antibiotics, lytic enzymes, hydrogen cyanide, and siderophores or through competition for nutrients and space can improve significantly plant health and promote growth as evidenced by increases in seedling emergence, vigor and yield (Antoun and Kloepper, 2001). Induction of the systemic resistance against many pathogens, insect and nematodes (Ramamoorthy et al., 2001; Zehnder et al., 2001) is also a recent indirect mechanism of action of PGPR. All these traits that can be present in PGPR, illustrate how it is complex and difficult to associate the promotion of plant growth with P solubilization, and they explain in part the reason of obtaining better responses from plant inoculated with a mixture of PGPR.  Furthermore, approximately two-thirds of all land plants form the arbuscular mycorrhizal (AM) type of association (Hodge, 2000). PGPR can promote mycorrhizal functioning. Recently for example, Villegas and Fortin (2001) showed an interesting specific synergistic interaction between the P solubilizing bacterium Pseudomonas aeruginosa and the AM fungus Glomus intraradices. Transformed mycorrhizal carrot roots or G. intraradices external mycelium and Pseudomonas aeruginosa solubilized more P from the sparingly soluble tricalcium phosphate when combined than when each alone. No synergistic effect was observed with the other two P-solubilizing bacteria tested (Pseudomonas putida and Serratia plymuthica) showing the specificity of this interaction.

With the aim of developing a phosphate inoculant that will allow the use of the different sparingly soluble P inorganic forms present in many Quebec soils, and reduce the amounts of P fertilizers used with corn and lettuce, 69 bacteria and 23 fungi able to solubilize tricalcium phosphate were first isolated from four different soils. Many organisms lost their P-solubilizing ability after subculturing on media containing sparingly soluble P, and finally 31 bacteria and 14 fungi were retained. Among them, 10 bacteria and 3 fungi produced large clarification halo zones on media containing Ca-P and exhibited good growth on media containing Al-P or Fe-P as sole P sources.  A maize inoculation trial with these PSM was performed under greenhouse conditions in a silty clay loam soil (pH 6.00; organic matter 4.60%; available P and K 198 and 663 Kg ha-1). After 3 weeks of growth, inoculation with the PSM tested did not produce any significant effect at the P<0.05 level on maize shoots dry matter yield or on shoots total P content. However, a 5 and 6% increases in dry matter yields were observed with strains 22c of Enterobacter sp. and 24 of Pseudomonas sp. (significant at P<0.11 and P<0.15 levels). The total P content of maize inoculated with strains 22a and 22c of Enterobacter sp. and Pseudomonas sp.  24 was 8 to 11% higher than that of the inoculated control (significant at the P<0.13 and P<0.10 levels). The highest non-significant increases in maize shoots dry matter yield and total P content (4%) were observed with the fungus Rhizopus sp. 68.  Field inoculation trials of maize were performed with bacteria 22a, 22c and 24 and the fungus isolate 68 in a silty clay loam soil (pH 5.47; organic matter 4.99%; available P and K 222 and 347 Kg ha-1). After 60 days of growth the height of maize plant inoculated with all bacteria tested (22a, 22c or 24) was significantly (P<0.01) higher as compared to the uninoculated control.  After 108 days growth, inoculation with bacteria causes 14 to 23 % increases of maize shoot dry matter yield. However, only the 23 % increase observed with strain 22c was significant at the P<0.01 level. Although maize plants inoculated with the bacteria contained 7 to 20 % more total P these value were not statistically significant. Under the field conditions used the fungus 68 did not show any significant effect.

The results obtained in these two assays suggest that a 3 weeks inoculation trial under greenhouse conditions in non-sterile soils is probably a short period. With inoculated maize grown in the field the absence of significant effects on P concentration or plant total P suggest that traits other than P-solubilization might be involved. In fact all the bacterial strains tested are IAA producers and like fungus 68 they also produce siderophores. Under similar field conditions lettuce inoculated with bacteria 22a and 24 and with fungus 68 produced more fresh matter yields (18%, P<0.01; 14%, P<0.01 and 11%, P<0.03 respectively) as compared to uninoculated controls after 48 days of growth.

Strains from the genera Pseudomonas, Bacillus and Rhizobium are among the most powerful P solubilizers (Rodriguez and Fraga, 1999).  We focused our interest on rhizobia, because these bacteria well known for their beneficial symbiotic atmospheric nitrogen fixing symbiosis with legumes, have an excellent potential to be used as PGPR with non legumes   (Antoun et al., 1998). In a test performed with 266 strains belonging to different genera and species, 54% of the strains were able to solubilize dicalcium phosphate. The highest P solubization activity was obtained with two strains P31 and R1 of Rhizobium leguminosarum bv. phaseoli. The two selected rhizobia were superior root colonizers of maize and lettuce as compared to other P-solubilizing bacteria (Chabot et al., 1996 b).  These rhizobia were included in maize and lettuce field inoculation trials performed in 3 sites varying in their available P content from poorly to very fertile soils (Chabot et al., 1996a). The P-solubilization effect seems to be the most important mechanism of plant growth promotion in moderately to fertile soils, and was less effective in poor soils. Mutants altered in their P-solubilization activities (solubilizing significantly less P than the wild type) were used to determine the importance of this trait in strain R1 (Chabot et al., 1998). The results obtained confirmed that growth promotion by P-solubilization is less effective in poor soils as observed under field conditions.

In order to study the mechanisms of actions involved in the mineral phosphate solubilizing (Mps) activity by a tropical Penicillium rugulosum  (Mps+) isolated from a Venezuelan soil, two unique UV induced mutants were produced (Reyes et al. 1999 b): a mutant with altered (Mps-) or amplified (Mps++) activity. The use of these mutants allowed the identification of three possible P solubilization mechanisms in P. rugulosum: production of gluconic acid, of citric acid and the H+ pump (Reyes et al., 1999a). These mechanisms are influenced by the N, P and C sources present in the culture media. These mutants were also used to study the solubilization of phosphate rocks and minerals (Reyes et al. 2001) and in maize inoculation assays (Reyes et al. 2002). All P. rugulosum strains were able to stimulate the growth of maize plants as indicated by 3.6 to 28.6% increases in dry matter yields. In the presence of rock phosphate, P-uptake by maize plants inoculated with the two mutants Mps++ and Mps- was not always in agreement with their P-solubilizing phenotypes. 

Results on plant inoculation with PSM found in the literature will also be presented and discussed.

REFERENCES

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