Long-Term Trends in Nitrogen Isotope Composition and Nitrogen Concentration in Brazilian Rainforest Trees Suggest Changes in Nitrogen Cycle

Direct or indirect anthropogenic effects on ecosystem nitrogen cycles are important components of global change. Recent research has shown that N isotopes in tree rings reflect changes in ecosystem nitrogen sources or cycles and can be used to study past changes. We analyzed trends in two tree species from a remote and pristine tropical rainforest in Brazil, using trees of different ages to distinguish between the effect of tree age and long-term trends. Because sapwood differed from heartwood in δ¹⁵N and N concentration and N can be translocated between living sapwood cells, long-term trends are best seen in dead heartwood. Heartwood δ¹⁵N in Spanish cedar (<i>Cedrela odorata</i>) and big-leaf mahogany (<i>Swietenia macrophylla</i>) increased with tree age, and N concentrations increased with age in <i>Cedrela</i>. Controlling for tree age, δ¹⁵N increased significantly during the past century even when analyzing only heartwood and after removing labile N compounds. In contrast to northern temperate and boreal forests where wood δ¹⁵N often decreased, the δ¹⁵N increase in a remote rainforest is unlikely to be a direct signal of changed N deposition. More plausibly, the change in N isotopic composition indicates a more open N cycle, i.e., higher N losses relative to internal N cycling in the forest, which could be the result of changed forest dynamics