Fig. 6
From: Divergent accumulation of microbial necromass and plant lignin components in grassland soils
Variations of amino sugar concentrations in different soils. Pearson correlation with clay contents (a) and aridity index (b) in the Mongolian (n = 38) and non-Mongolian grassland soils (n = 38). SOC, soil organic carbon. Error bars represent s.e.m. for three site replicates in the Mongolian grasslands. Data for non-Mongolian soils are derived from the literature14,20,24,25, which uses a different clay measurement method from the Mongolian soils
