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Abstract
Nitrogen deposition in the northeastern US changed N availability in the latter part of the twentieth century, with potential legacy effects. However, long-term N cycle measurements are scarce. N isotopes in tree rings have been used as an indicator of N availability through time, but there is little verification of whether species differ in the strength of this signal. Using long-term records at the Fernow Experimental Forest in West Virginia, we examined the relationship between soil conditions, including net nitrification rates, and wood δ
15N in 2014, and tested the strength of correlation between tree ring δ
15N of four species and stream water NO
3− loss from 1971 to 2000. Higher soil NO
3− was weakly associated with higher wood δ
15N across species, and higher soil net nitrification rates were associated with higher δ
15N for
Quercus rubra only. The δ
15N of
Liriodendron tulipifera and
Q. rubra, but neither
Fagus grandifolia nor
Prunus serotina, was correlated with stream water NO
3−.
L. tulipifera tree ring δ
15N had a stronger association with stream water NO
3− than
Q. rubra. Overall, we found only limited evidence of a relationship between soil N cycling and tree ring δ
15N, with a strong correlation between the wood δ
15N and NO
3− leaching loss through time for one of four species. Tree species differ in their ability to preserve legacies of N cycling in tree ring δ
15N, and given the weak relationships between contemporary wood δ
15N and soil N cycle measurements, caution is warranted when using wood δ
15N to infer changes in the N cycle.
Citation
Burnham, Mark B.; Adams, Mary Beth; Peterjohn, William T. 2019. Assessing tree ring δ15N of four temperate deciduous species as an indicator of N availability using independent long-term records at the Fernow Experimental Forest, WV. Oecologia. 191(4): 971-981. https://doi.org/10.1007/s00442-019-04528-4.