11 research outputs found
Foliar ÎŽ15N values characterize soil N cycling and reflect nitrate or ammonium preference of plants along a temperate grassland gradient
The natural abundance of stable 15N isotopes in soils and plants is potentially a simple tool to assess ecosystem N dynamics. Several open questions remain, however, in particular regarding the mechanisms driving the variability of foliar ÎŽ15N values of non-N2 fixing plants within and across ecosystems. The goal of the work presented here was therefore to: (1) characterize the relationship between soil net mineralization and variability of foliar ÎÎŽ15N (ÎŽ15Nleaf â Ύ15Nsoil) values from 20 different plant species within and across 18 grassland sites; (2) to determine in situ if a plantâs preference for NO3â or NH4+ uptake explains variability in foliar ÎÎŽ15N among different plant species within an ecosystem; and (3) test if variability in foliar ÎÎŽ15N among species or functional group is consistent across 18 grassland sites. ÎÎŽ15N values of the 20 different plant species were positively related to soil net mineralization rates across the 18 sites. We found that within a site, foliar ÎÎŽ15N values increased with the speciesâ NO3â to NH4+ uptake ratios. Interestingly, the slope of this relationship differed in direction from previously published studies. Finally, the variability in foliar ÎÎŽ15N values among species was not consistent across 18 grassland sites but was significantly influenced by N mineralization rates and the abundance of a particular species in a site. Our findings improve the mechanistic understanding of the commonly observed variability in foliar ÎÎŽ15N among different plant species. In particular we were able to show that within a site, foliar ÎŽ15N values nicely reflect a plantâs N source but that the direction of the relationship between NO3â to NH4+ uptake and foliar ÎÎŽ15N values is not universal. Using a large set of data, our study highlights that foliar ÎÎŽ15N values are valuable tools to assess plant N uptake patterns and to characterize the soil N cycle across different ecosystems