Soil pH and Organic Carbon Properties Drive Soil Bacterial Communities in Surface and Deep Layers Along an Elevational Gradient.

Results Vegetation and Soil Properties Along the Elevational Gradient The sum of basal area of trees followed a decreasing trend with elevation ( r = −0.579, p = 0.024, Table 1 and Supplementary Table 2 ).

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In the surface layer, SOC, TN, C:N ratio POC%, and RP% showed an increasing trend with elevation; and M o :SOC ratio and LPI% showed an opposite trend ( Supplementary Table 2 ).

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