“…By contrast, in the higher diversity soils, the effect of inorganic nutrient amendments was negative compared to untreated soils, despite the fact that the fertilizer‐treated soils had initially more bioavailable P and N. This inconsistent effect from inorganic fertilizer addition could be ascribed to the rapid nutrient metabolization that occurred in the higher diverse soil, in which the pool of added nutrients was rapidly depleted and thus possibly made unavailable to the pyrene‐degrading microbial subcommunity in the critical first few weeks of exposure to pyrene. Conversely, in less diverse soils, inorganic amendments took longer to be metabolized, increasing nutrient availability for pyrene degraders (Sarkar et al ., 2005; Kalantary et al ., 2014; Lukić et al ., 2016), which in turn had a boosting effect on the biodegradation rate (Leff et al ., 2015; Zhu et al ., 2016; Xue et al ., 2018; Sivaram et al ., 2019). Consistent with these findings, inorganic nutrient addition in the low diversity soil supported a unique assemblage of bacterial indicator taxa with known bioremediation abilities, such as members of Proteobacteria and Firmicutes (Venail and Vives, 2013; Ren et al ., 2016; Zada et al ., 2021), while the differentiation of the indicator community in nutrient‐amended samples was relatively weaker in the high diversity soil.…”