Soil microbial stoichiometry and community structure responses to long-term natural forest conversion to plantations in a subtropical region

Soil microbial stoichiometry reflects carbon (C) and nutrient (e.g., nitrogen (N) and phosphorus (P)) elemental balances under land-use change (LUC). However, how soil microbial community (SMC) structure and stoichiometry respond to long-term LUC in forests is still unclear. Here, we investigated three 36-year-old typical plantations, Cryptomeria fortunei , Metasequoia glyptostroboides , and Cunninghamia lanceolata , and the natural forest to assess their soil microbial stoichiometry and SMC structure. Three plots (30×30 m 2 ) were randomly set in each forest site. In each plot of every forest site, soil samples of three depths (0–10, 10–30, and 30–60 cm) were collected. Dissolved organic C, N, and P (abbreviated as DOC, DON, and DOP, respectively) and environmental factors were measured. We also detected microbial biomass C, N, and P as well as SMC structure. The results showed that the soil microbial C:N:P stoichiometry had a strong or strict homeostasis regardless of soil depth and exhibited decoupling from the SMC structure at each depth. The SMC structure across forest types was mainly driven by mean annual soil temperature (MAST) and DOC at 0–10 cm depth, by soil water content and MAST at 10–30 cm depth, and by DOC to DOP ratio at 30–60 cm depth. Thus, SMC structure could be jointly regulated by available resources and environment. These results suggest that the C dynamics in forests tend to gain resilience or re-equilibrium over more than three decades after forest conversion. These findings highlight the importance of reforested plantations forest management for sustaining soil C over a long term.