文摘
Moss N isotope (未15Nbulk) has been used to monitor N deposition, but it remains questionable whether inhibition of nitrate reductase activity (NRA) by reduced dissolved N (RDN) engenders overestimation of RDN in deposition when using moss 未15Nbulk. We tested this question by investigation of 未15Nbulk and 未15NO3鈥?/sup> in mosses under the dominance of RDN in N depositions of Guiyang, SW China. The 未15Nbulk of mosses on bare rock (鈭?.9鈥? was unable to integrate total dissolved N (TDN) (未15N = 鈭?.3鈥?, but it reflected 未15N-RDN (鈭?.5鈥? exactly. Moreover, 未15N-NO3鈥?/sup> in mosses (鈭?.7鈥? resembled that of wet deposition (鈭?.9鈥?. These isotopic approximations, together with low isotopic enrichment with moss [NO3鈥?/sup>] variations, suggest the inhibition of moss NRA by RDN. Moreover, isotopic mixing modeling indicated a negligible contribution from NO3鈥?/sup> to moss 未15Nbulk when the RDN/NO3鈥?/sup> reaches 3.8, at which maximum overestimation (21%) of RDN in N deposition can be generated using moss 未15Nbulk as 未15N-TDN. Moss 未15N-NO3鈥?/sup> can indicate atmospheric NO3鈥?/sup> under distinctly high RDN/NO3鈥?/sup> in deposition, although moss 未15Nbulk can reflect only the RDN therein. These results reveal pitfalls and new mechanisms associated with moss isotope monitoring of N deposition and underscore the importance of biotic N dynamics in biomonitoring studies.