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. 2010 Jan 8;76(5):1471–1479. doi: 10.1128/AEM.02072-09

TABLE 1.

Mean contribution of T-RFs that constituted a significantly greater proportion of the T-RFLP profiles from the H2-treated microcosms

RE Result fora:
GES soil
QRS soil
H2-specific T-RF length (nt) % Go (n = 4) % Ga (n = 10) % Gh (n = 10) P value (Ga vs Gh) H2-specific T-RF length (nt) % Qo (n = 3) % Qa (n = 8) % Qh (n = 9) P value (Qa vs Qh)
BstUI 223 3.7 4.1 12.0 0.0011 220 2.5 3.5 16.7 0.0014
HaeIII 65 3.6 4.1 8.5 0.0091 223b 0.6 0.3 14.7 0.0009
HhaI 358 2.6 6.6 14.6 0.0112 177 0.03 0.02 9.2 0.0002
HinfI 323 17.8 16.6 26.8 0.0169 166 0.1 0.08 5.5 0.0010
MspI 140 2.1 3.0 6.0 0.0538 158 2.3 2.0 10.7 0.0044
Sau96I 64 2.1 3.0 6.1 0.0428 314 0 0 13.1 0.0017
a

The contributions are shown by soil type (where G represents GES soil microcosms and Q represents QRS soil microcosms) and treatment (where o represents original soil, a represents air-treated soil, and h represents H2-treated soil). The results of two-tailed t tests between the T-RFs' contributions to the treated samples from each soil are presented. n indicates the number of T-RFLP profiles analyzed for each soil and treatment for all six REs. In each case, the percentage shown represents the mean contribution of the T-RF to the total area of the T-RFLP profiles.

b

Comparisons of the HaeIII T-RFLP profiles generated from QRS soil are shown in Fig. 4.