Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate
Abstract Variation across climate gradients in the isotopic composition of nitrogen (N) and carbon (C) in foliar tissues has the potential to reveal ecological processes related to N and water availability. However, it has been a challenge to separate spatial patterns related to direct effects of cl...
Guardado en:
Autores principales: | , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/d893d3768fbb49539e029bc4a2b58aed |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:d893d3768fbb49539e029bc4a2b58aed |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:d893d3768fbb49539e029bc4a2b58aed2021-12-02T11:52:36ZContinental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate10.1038/s41598-017-08156-x2045-2322https://doaj.org/article/d893d3768fbb49539e029bc4a2b58aed2017-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-017-08156-xhttps://doaj.org/toc/2045-2322Abstract Variation across climate gradients in the isotopic composition of nitrogen (N) and carbon (C) in foliar tissues has the potential to reveal ecological processes related to N and water availability. However, it has been a challenge to separate spatial patterns related to direct effects of climate from effects that manifest indirectly through species turnover across climate gradients. Here we compare variation along environmental gradients in foliar N isotope (δ15N) and C isotopic discrimination (Δ13C) measured in 755 specimens of a single widely distributed tree species, Populus balsamifera, with variation represented in global databases of foliar isotopes. After accounting for mycorrhizal association, sample size, and climatic range, foliar δ15N in P. balsamifera was more weakly related to mean annual precipitation and foliar N concentration than when measured across species, yet exhibited a stronger negative effect of mean annual temperature. Similarly, the effect of precipitation and elevation on Δ13C were stronger in a global data base of foliar Δ13C samples than observed in P. balsamifera. These results suggest that processes influencing foliar δ15N and Δ13C in P. balsamifera are partially normalized across its climatic range by the habitat it occupies or by the physiology of the species itself.Andrew J. ElmoreJoseph M. CraineDavid M. NelsonSteven M. GuinnNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 7, Iss 1, Pp 1-9 (2017) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Medicine R Science Q |
spellingShingle |
Medicine R Science Q Andrew J. Elmore Joseph M. Craine David M. Nelson Steven M. Guinn Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
description |
Abstract Variation across climate gradients in the isotopic composition of nitrogen (N) and carbon (C) in foliar tissues has the potential to reveal ecological processes related to N and water availability. However, it has been a challenge to separate spatial patterns related to direct effects of climate from effects that manifest indirectly through species turnover across climate gradients. Here we compare variation along environmental gradients in foliar N isotope (δ15N) and C isotopic discrimination (Δ13C) measured in 755 specimens of a single widely distributed tree species, Populus balsamifera, with variation represented in global databases of foliar isotopes. After accounting for mycorrhizal association, sample size, and climatic range, foliar δ15N in P. balsamifera was more weakly related to mean annual precipitation and foliar N concentration than when measured across species, yet exhibited a stronger negative effect of mean annual temperature. Similarly, the effect of precipitation and elevation on Δ13C were stronger in a global data base of foliar Δ13C samples than observed in P. balsamifera. These results suggest that processes influencing foliar δ15N and Δ13C in P. balsamifera are partially normalized across its climatic range by the habitat it occupies or by the physiology of the species itself. |
format |
article |
author |
Andrew J. Elmore Joseph M. Craine David M. Nelson Steven M. Guinn |
author_facet |
Andrew J. Elmore Joseph M. Craine David M. Nelson Steven M. Guinn |
author_sort |
Andrew J. Elmore |
title |
Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
title_short |
Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
title_full |
Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
title_fullStr |
Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
title_full_unstemmed |
Continental scale variability of foliar nitrogen and carbon isotopes in Populus balsamifera and their relationships with climate |
title_sort |
continental scale variability of foliar nitrogen and carbon isotopes in populus balsamifera and their relationships with climate |
publisher |
Nature Portfolio |
publishDate |
2017 |
url |
https://doaj.org/article/d893d3768fbb49539e029bc4a2b58aed |
work_keys_str_mv |
AT andrewjelmore continentalscalevariabilityoffoliarnitrogenandcarbonisotopesinpopulusbalsamiferaandtheirrelationshipswithclimate AT josephmcraine continentalscalevariabilityoffoliarnitrogenandcarbonisotopesinpopulusbalsamiferaandtheirrelationshipswithclimate AT davidmnelson continentalscalevariabilityoffoliarnitrogenandcarbonisotopesinpopulusbalsamiferaandtheirrelationshipswithclimate AT stevenmguinn continentalscalevariabilityoffoliarnitrogenandcarbonisotopesinpopulusbalsamiferaandtheirrelationshipswithclimate |
_version_ |
1718395014538592256 |