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. 2014 Aug;75(100):143–151. doi: 10.1016/j.soilbio.2014.04.014

Fig. 3.

Fig. 3

Phospholipid fatty acid (PLFA) patterns in topsoil, cryoturbated, and mineral subsoil horizons from a tundra ecosystem in the central Siberian Arctic. Samples were amended with glucose, amino acids, cellulose or protein, or left unamended as controls. Patterns are displayed by non-metric multidimensional scaling (NMDS) of PLFA abundances (% of total C in PLFAs). Points represent means ± standard errors of five replicates; significant differences to the respective controls are indicated (*, p < 0.05; **, p < 0.01; ***, p < 0.001). Data of PLFA abundances are presented in Supplementary Table 3.