Post‐disturbance conifer tree‐ring δ 15 N reflects openness of the nitrogen cycle across temperate coastal rainforests
Author:
Affiliation:
1. British Columbia Ministry of Forests, Lands, Natural Resource Operations and Rural Development Victoria BC Canada
2. Centre for Forest Biology University of Victoria Victoria BC Canada
Publisher
Wiley
Subject
Plant Science,Ecology,Ecology, Evolution, Behavior and Systematics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/1365-2745.13482
Reference88 articles.
1. Soil C:N stoichiometry controls carbon sink partitioning between above-ground tree biomass and soil organic matter in high fertility forests
2. Tree-ring growth and stable isotopes (13C and 15N) detect effects of wildfires on tree physiological processes in Pinus sylvestris L.
3. Temperature effects on nitrogen form uptake by seedling roots of three contrasting conifers
4. Response of the Nitrogen Isotopic Composition of Tree-Rings Following Tree-Clearing and Land-Use Change
5. 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
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