Accounting for the effect of temperature in clarifying the response of foliar nitrogen isotope ratios to atmospheric nitrogen deposition

Atmospheric nitrogen deposition affects nitrogen isotope composition (δ¹⁵N) in plants. However, both negative effect and positive effect have been reported. The effects of climate on plant δ¹⁵N have not been corrected for in previous studies, this has impeded discovery of a true effect of atmospheric N deposition on plant δ¹⁵N. To obtain a more reliable result, it is necessary to correct for the effects of climatic factors. Here, we measured δ¹⁵N and N contents of plants and soils in Baiwangshan and Mount Dongling, north China. Atmospheric N deposition in Baiwangshan was much higher than Mount Dongling. Generally, however, foliar N contents showed no difference between the two regions and foliar δ¹⁵N was significantly lower in Baiwangshan than Mount Dongling. The corrected foliar δ¹⁵N after accounting for a predicted value assumed to vary with temperature was obviously more negative in Baiwangshan than Mount Dongling. Thus, this suggested the necessity of temperature correction in revealing the effect of N deposition on foliar δ¹⁵N. Temperature, soil N sources and mycorrhizal fungi could not explain the difference in foliar δ¹⁵N between the two regions, this indicated that atmospheric N deposition had a negative effect on plant δ¹⁵N. Additionally, this study also showed that the corrected foliar δ¹⁵N of bulk data set increased with altitude above 1300m in Mount Dongling, this provided an another evidence for the conclusion that atmospheric N deposition could cause ¹⁵N-depletion in plants.