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. 2013 Mar 19;8(3):e57127. doi: 10.1371/journal.pone.0057127

Table 1. Summary of SMA regressions of log10-transformed C, N, and P contents in soil and microbial pools, along with predictors of soil C mineralization (CO2) and microbial metabolism (qCO2).

Analysis x y n r2 Int. Slope x∶y ratio x∶y mean CV
Soil allometry *C N 280 0.86 −0.77 0.88 C∶N 18.8 ± 0.8 0.7
*C P 261 0.18 0.23 0.29 C∶P 445 ± 43 1.6
*N P 261 0.24 0.27 0.42 N∶P 21.4 ± 1.7 1.3
Microbial allometry MBC MBN 237 0.84 −1.11 1.08 mC∶N 10.7 ± 0.6 0.8
*MBC MBP 298 0.70 −2.07 1.18 mC∶P 87.2 ± 13.2 2.6
MBN MBP 267 0.71 −0.79 1.04 mN∶P 9 ± 1.2 2.2
Microbial biomass C MBC 289 0.75 −1.34 0.88 MBC∶C 2.01% ± 0.08 0.6
N MBC 266 0.73 −0.52 0.99
*P MBC 247 0.132 0.08 1.37
Respiration and metabolism MBC CO2 92 0.7 −4.17 1.57
**mC∶P qCO2 92 0.21 1.97 −1.15
**Pi qCO2 38 0.44 0.51 0.65

Bivariate relationships were significant (P<0.001) for all relationships shown. Slopes significantly different from one (P>0.05) are shown in boldface font. Slopes not different from one (not bold) indicate an isometric (linear) relationship among parameters. The geometric mean and standard errors (SE) of stoichiometric ratios (x∶y ratio, x∶y mean) are given for reference, but are not representative where allometric slopes are different than 1. The coefficient of variation (CV) of these stoichiometric ratios is provided as a dimensionless index of dispersion about the mean. Single asterisks (*) indicate where different slopes are observed by considering only forest and pasture soils (Table S1), and ** indicates relationships fit for all soils excluding litter and humus.