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

Fig. 1.

Fig. 1

Cumulative SOM-derived respiration of 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 (added at levels corresponding to approximately 1% of soil organic C), or left unamended as controls. Points represent means ± standard errors of four replicates. Significant differences between amended samples and controls at the end of the incubation are indicated (*, p < 0.05; **, p < 0.01; ***, p < 0.001).