80 0 000 7 88 0 011 161 49 0 000 4 51 0 02 4 92 0 03 476 9 0 000

80 0.000 7.88 0.011 161.49 0.000 4.51 0.02 4.92 0.03 476.9 0.000 17.41 0.000 Tarafdar

et al. [41] reported significantly higher actinomycetes population in non-Bt planted soil (5.25 X 106 CFU g-1) compared to Bt brinjal planted soil (4.3 × 106 CFUg-1). 26s Proteasome structure No significant changes were found in the studies conducted with transgenic cotton [42], corn [3], cabbage [43], and tomato [36]. Differences in the total actinomycetes population between the non-Bt and Bt crops might attributed to the release of root exudates from the transgenic brinjal into the soil that could have changed the available organic carbon and in turn, influenced the carbon turnover [38]. Tarafdar et al. [41] suggested that reductions in the actinomycetes population under Bt cotton cultivation were due to changes in the root exudates. However, other studies [3, 36, 44] supported that genetic modification of the plant had no role in changing the microbial population. Significant differences in the actinomycetes population were observed between the crop growth stages (Table 2). Variation among the stages could be due to the changes in the soil nutrients e.g., available organic carbon, mineral-N, K2O, Zn, Fe, Mn and soil pH. The correlation analysis shows positive significant correlation of organic carbon content and click here mineral-N with population load of actinomycetes (r = 0.82, and r = 0.85 (Table 3), respectively).

These results are consistent www.selleckchem.com/products/pha-848125.html with those of others [45,

46]. Table 3 Pearson’s correlation (r) matrix for soil pH, nutrients and actinomycetes population Properties Year Crop Stages pH Organic C K2O S Zn Fe Mn Mineral- N Actinomycetes population Year 1                       Crop 0.00 1   Liothyronine Sodium                   Stages 0.00 0.00 1                   pH -0.01 0.25 0.64** 1                 Organic C 0.58 0.24 0.52** 0.71** 1               K2O -0.21 0.21 0.02 0.62** 0.32 1             S -0.09 0.13 0.09 0.11 0.30 0.09 1           Zn -0.02 0.34 0.37 0.66** 0.93** 0.45** 0.40 1         Fe -0.98 0.24 0.35 0.52* 0.73** 0.11 0.25 0.67 1       Mn -0.00 0.14 0.54* 0.79** 0.71** 0.15 0.37 0.63** 0.81** 1     Mineral-N -0.00 -0.03 0.30 0.81** 0.92** 0.27 0.24 0.85** 0.74** 0.81** 1   Actinomycetes population -0.06 0.11 0.82 0.54** 0.82** 0.45** 0.04 0.84** 0.64** 0.56** 0.85** 1 ** Correlation is significant at the 0.01 level (n = 20); * Correlation is significant at the 0.05 level (n = 20). Phylogenetic analysis of 16S rRNA gene sequences from non-Bt and Bt brinjal rhizospheric soils Thirty eight OTUs were generated from 282 positive clones for non-Bt brinjal soils. In case of Bt soils, a total of 278 positive clones clustered into 29 OTUs for pre-vegetation, branching, flowering, maturation and post-harvest stages. Different OTUs when evaluated after RFLP finger-printing analysis, showed affiliation with 14 and 11 actinomycetal groups from the respective non-Bt and Bt brinjal soils (Figure 2 and Figure 3).

Comments are closed.