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. 2020 Jun 23;10(14):7509–7524. doi: 10.1002/ece3.6477

TABLE 1.

Soil effects on OTU Shannon diversity by marker

Marker Soil layer Variable Mean SD 0.025 0.5 0.975
18S Litter Intercept 3.871 11.000 −19.413 4.034 25.957
pH 0.067 0.061 −0.054 0.067 0.187
Carbon −0.057 0.077 −0.209 −0.056 0.089
Chemical 0.109 0.090 −0.069 0.109 0.278
Physical 0.017 0.043 −0.070 0.018 0.100
Soil Intercept 3.393 0.703 1.804 3.456 4.653
pH −0.019 0.045 −0.108 −0.019 0.070
Carbon −0.287 0.048 −0.384 −0.287 −0.194
Chemical 0.049 0.034 −0.011 0.048 0.122
Physical 0.029 0.031 −0.033 0.030 0.089
COI Litter Intercept 3.871 11.000 −19.413 4.034 25.957
pH 0.067 0.061 −0.054 0.067 0.187
Carbon −0.057 0.077 −0.209 −0.056 0.089
Chemical 0.109 0.090 −0.069 0.109 0.278
Physical 0.017 0.043 −0.070 0.018 0.100
Soil Intercept −1.670 12.588 −26.767 −1.834 24.665
pH 0.085 0.055 −0.022 0.085 0.192
Carbon 0.109 0.074 −0.037 0.109 0.253
Chemical 0.620 0.082 0.460 0.619 0.782
Physical −0.019 0.035 −0.087 −0.019 0.050
ITS Litter Intercept 3.871 11.000 −19.413 4.034 25.957
pH 0.067 0.061 −0.054 0.067 0.187
Carbon −0.057 0.077 −0.209 −0.056 0.089
Chemical 0.109 0.090 −0.069 0.109 0.278
Physical 0.017 0.043 −0.070 0.018 0.100
Soil Intercept −1.400 10.548 −22.631 −1.470 20.545
pH −0.114 0.058 −0.229 −0.114 0.000
Carbon −0.389 0.085 −0.557 −0.388 −0.224
Chemical 0.319 0.081 0.161 0.319 0.480
Physical −0.046 0.037 −0.119 −0.046 0.027

The table shows the coefficients of each predictor in four Bayesian general multivariate regression models using stochastic partial differential equations (SPDE) that explicitly consider spatial correlation, modeling OTU diversity dependent on soil properties for Amazonian fungi in litter and soil. Since the organic carbon content and pH are considered important variables for soil biota, we use them as independent variables. Bold indicates important predictor variables (credible intervals not crossing zero). The importance of soil properties differed between markers and were significant only for the soil diversity. Carbon content was important for 18S and ITS soil, and chemical PC1 was important for COI and ITS.