Effects of 14-year continuous nitrogen addition on soil arylsulfatase and phosphodiesterase activities in a mature tropical forest

We investigated the impacts of 14-year continuous N addition on activities of arylsulfatase (AS) and phosphodiesterase (PDE), which catalyze soil organic sulfur (S) and phosphorus (P), respectively. The response of AS to N addition was compared with that of C- and N-acquiring enzymes, i.e., β-1,4-glucosidase (BG), β-D-cellobiohydrolase (CBH), β-1,4-Xylosidase (BX), β-1,4-N-acetyl-glucosaminnidase (NAG), and leucine amino peptidase (LAP). We also compared the impact of N addition on PDE activity with that on phosphomonoesterase (PME) activity. The results showed that N addition clearly decreased soil AS activity, whereas activities of C- and N-acquiring enzymes did not exhibit similar changes. The inconsistent response of AS activity with the enzymes was attributed to soil acidification induced by long-term N addition, which shifts the pH condition to a more optimal condition for AS activity and accelerates the accumulation of S in soils. The ratio of PME to PDE were significantly elevated by N addition, implying that the microbial and plant resource allocation to PME relative to PDE increased after N addition at our study site. The shift in resource allocation may have occurred because (i) the types of phosphatases secreted by biota shifted toward phosphatases that require one-step reaction to obtain P (such as PME) in the more-severely P-depleted condition, or (ii) soil acidification provided a more optimal condition for PDE than PME, which resulted in lower PDE production appearing as lower enzyme activity at the same pH condition in the laboratory. Overall, our results indicated different responses of exoenzyme activities to external N input. This highlights the importance of atmospheric N deposition on microbial activity and collateral C and nutrient dynamics in tropical natural forests.