Abstract
Key message
For long-term environmental investigations, tree-ring δ 15 N values are inappropriate proxies for foliar δ 15 N for both Fagus sylvatica and Picea abies under moderate N loads.
Abstract
Currently it is unclear whether stable nitrogen isotope signals of tree-rings are related to those in foliage, and whether they can be used to infer tree responses to environmental changes. We studied foliar and tree-ring nitrogen (δ15N) and carbon (δ13C) isotope ratios in European beech (Fagus sylvatica L.) and Norway spruce (Picea abies L.) from six long-term forest monitoring sites in Switzerland together with data on N deposition and soil N availability, as well as a drought response index over the last two decades. For both species, tree-ring δ15N and δ13C values were less negative compared to foliar δ15N and δ13C values, most likely due to recycling and reallocation of N within the tree and fractionation processes associated with the transport of sucrose and the formation of tree-rings, respectively. Temporal trends recorded in foliar δ15N were not reflected in tree-ring δ15N, with much higher variations in tree-rings compared to foliage. Soil N availability and N deposition were partially able to explain changes in foliar δ13C, while there were no significant correlations between environmental variables and either tree-ring or foliar δ15N. Our results suggest an uncoupling between the N isotopic composition of tree-rings and foliage. Consequently, tree-ring δ15N values are inappropriate proxies of foliar δ15N values under low-to-moderate N deposition loads. Furthermore, at such low levels of deposition, tree-ring δ15N values are not recommended as archives of tree responses to soil C/N or bulk N deposition.
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Acknowledgments
We are thankful to O. Schramm, N. Hajjar, Y–Y. Cheung-Tang and A. Brechbühl for the sample collections and respective analyses; P. Jakob and F. Sutter for providing site information; G. Schneiter and M. Rebetez for providing the meteorological measurements; L. Walthert for providing soil measurements; P. Sutter and M. Gysin for their assistance in the foliage sampling; local site collaborators for bi-weekly sample collections; D. Pezzotta and the WSL central laboratory for chemical and isotope analyses. We would also like to acknowledge K. Steiner, B. Fritschi and the WSL Forest Hydrology group for the Alptal measurements. We are grateful to the Dendroecology group at the WSL institute and C. Lötscher and M. Saurer of the Ecosystem Fluxes group at the Paul Scherrer Institute for their assistance during sample measurements. This study was funded by the Swiss State Secretariat for Education, Research and Innovation (SERI) as part of a project (Grant No. C10.0128) within COST Action ES0806 (Stable Isotopes in Biosphere–Atmosphere-Earth System Research SIBAE), and by the Swiss Federal Office for the Environment (FOEN).
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Tomlinson, G., Buchmann, N., Siegwolf, R. et al. Can tree-ring δ15N be used as a proxy for foliar δ15N in European beech and Norway spruce?. Trees 30, 627–638 (2016). https://doi.org/10.1007/s00468-015-1305-1
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DOI: https://doi.org/10.1007/s00468-015-1305-1