Variation in the δ¹³C of foliage of Pinus sylvestris L. in relation to climate and additions of nitrogen: analysis of a 32‐year chronology

Abstract

We report an analysis of both the long-and short-term drivers of the carbon (C) isotope composition (d 13 C) values of current year needles of Pinus sylvestris L. linked to changing atmospheric carbon dioxide (CO 2 ) concentrations (c a ) and climate using data from a uniquely long-term nitrogen (N) fertilization experiment in the north of Sweden (consisting of three N dosage levels and a control treatment) from 1970 until 2002. N loading produced trees with less negative d 13 C of foliage, by around 0.45% on average, with the difference in d 13 C between control and N treatments not dependant upon N dosage. The average d 13 C values decreased at a rate of around 0.03% yr À1 , even after accounting for the Suess effect (the decrease in the atmospheric CO 2 d 13 C due to anthropogenic emissions of isotopically light CO 2 ). This decrease is large enough to cause a significant, progressive change in the d 13 C down through a soil profile. Modelled values of plant intrinsic water use efficiency (WUE i ) and the ratio of leaf internal to external [CO 2 ] (c i /c a ) showed that this was the result of c i increasing in parallel with c a (while c i /c a increased), thus causing little change in WUE i over the 32 years of study. The residuals from the relationships between year and d 13 C were used to examine the impact of climate on the interannual variation of C isotope composition of needles. This included the use of a fire hazard index (FHI) model, which integrates climatic factors known to influence plant stomatal conductance and hence d 13 C. The FHI produced the best fit with d 13 C values when climate data were averaged over the whole growth season (for control plots) and for July for all the N treatments, explaining ca. 60% of the total interannual variation in d 13 C. Further, trees from the N treatments appeared more susceptible to air-humidity-based climate parameters, as seen from higher correlation coefficients, than were control trees. Thus, our data suggest the possibility of increased susceptibility to drought conditions in ecosystems with moderate to high N deposition rates. Also, there is the possibility that, because there was no apparent change in WUE i of P. sylvestris in this ecosystem over the last 32 years, the rate of sequestration of C into boreal ecosystems may not increase with c a , as has been predicted.

Long-term variation of tree growth and intrinsic water-use efficiency in Schrenk spruce with increasing CO2 concentration and climate warming in the western Tianshan Mountains, China

“…These results suggest that other factors, especially drought, may have influenced tree response to increasing C a Xu et al 2013). Such phenomenon was not taken into consideration in the current models, which predict a continuing rise in terrestrial carbon storage as a result of the combined effects of CO 2 fertilization and climate change with the rising C a (Betson et al 2007;Leuzinger and Körner 2007). Therefore, if a long-term reduction in sensitivity to atmospheric CO 2 exists among large proportion of trees in the temperate regions, the degree of future terrestrial carbon storage would have been overestimated (Peñuelas et al 2008).…”

Increased intrinsic water-use efficiency during a period with persistent decreased tree radial growth in northwestern China: Causes and implications

“…Nevertheless, some studies are not found this trend (e.g. Marshall and Monserud, 1996;Beston et al, 2007).…”

Physiological responses to fertilization recorded in tree rings: isotopic lessons from a long‐term fertilization trial

“…They noted that while leaf area significantly increased in response to fertilization, fine root area necessary for water uptake did not, causing the root area : leaf area ratio in fertilized trees to be half that of control trees. Betson et al (2007) found that the variation in needle d 13 C over time in fertilized trees was more sensitive to climatic variation than control trees, implying that this sensitivity was an increased susceptibility to drought in fertilized trees. No significant differences between treatments were found for earlywood.…”