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The ability of the nitrogen-fixing bacterial endophyte Acetobacter diazotrophicus strain PAl5 to enhance the growth of sugarcane SP70-1143 was evaluated in the growth chamber, greenhouse, and field by comparing plants inoculated with wild-type and Nif mutant MAd3A in two independent experiments. The wild-type and Nif mutant strains colonized sugarcane plants equally and persisted in mature plants. In N-deficient conditions, sugarcane plants inoculated with A. diazotrophicus PAl5 generally grew better and had a higher total N content 60 days after planting than did plants inoculated with mutant MAd3A or uninoculated plants. These results indicate that the transfer of fixed N from A. diazotrophicus to sugarcane might be a significant mechanism for plant growth promotion in this association. When N was not limiting, growth enhancement was observed in plants inoculated with either wild-type or Nif- mutants, suggesting the additional effect of a plant growth promoting factor provided by A. diazotrophicus. A 15N2 incorporation experiment demonstrated that A. diazotrophicus wild-type strains actively fixed N2 inside sugarcane plants, whereas the Nif- mutants did not.

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ÐIn a sustainable agriculture farming systems experiment, soils managed under organic farming practices had greater microbial abundance and activity, and higher numbers of bacterial-feeding nematodes during crop growth, than those managed under conventional farming practices. We tested rates of organic matter decomposition in the two soils and monitored the abundance and activity of soil biota during the decomposition process. Dierences in soil biology between soils from organic and conventional farming systems did not persist when soils were amended with organic matter and maintained under similar conditions. Microbial communities in soil from the conventional system were sucient and active enough to respond to organic inputs. There were minimal dierences in the ability of the microbial communities of the two soils to decompose organic residues. However, when soils were removed from the ®eld at dierent times, cover crop decomposition rates were more consistent in the organic soils, suggesting a greater abundance and diversity of the microbial community in those soils. Microbial activity was most suppressed when ®eld soils were dry but responded to organic matter amendment very rapidly when favorable moisture contents were restored. The pattern of microbial activity in both organic and conventional soils following organic matter incorporation consisted of a 100 h activity phase and then a gradual decline to a relatively constant stasis phase.