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Radial growth response of two oaks to climate at their disparate distribution limits in semiarid areas, Beijing, China

Impending climate warming is expected to influence plant growth and distribution, and the distribution range limit of tree species is extremely sensitive to climate change. However, synchronous comparisons of responses of different tree species with overlapping ecological niches to climate at their...

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Bibliographic Details
Published in:Ecosphere (Washington, D.C) D.C), 2020-02, Vol.11 (2), p.n/a
Main Authors: Gao, Wen‐Qiang, Lei, Xiang‐Dong, Fu, Li‐Yong, Duan, Guang‐Shuang, Zhou, Meng‐Li, Cao, Jian
Format: Article
Language:English
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Summary:Impending climate warming is expected to influence plant growth and distribution, and the distribution range limit of tree species is extremely sensitive to climate change. However, synchronous comparisons of responses of different tree species with overlapping ecological niches to climate at their distribution range limit in the same region have received little attention. In the present study, we assessed the discrepancy in radial growth responses of two dominant oak species to climate at their distribution range limit (southern range limit for Quercus mongolica, northern range limit for Quercus variabilis) in Beijing, China. Furthermore, growth–climate relationships were examined using linear mixed‐effects models, and growth trends up to the year 2100 were forecast based on future climate scenarios (RCP2.6 and RCP8.5). Our results indicated that there were no significant differences in the growth response to climate between Q. variabilis at its northern limit and Q. mongolica at its southern limit, and the growth of the two tree species was positively correlated with the minimum temperature and negatively correlated with the climatic moisture deficit of autumn. However, the growth response to climate variables varied at different sites. Additionally, the model forecast showed an increase in radial growth of Q. variabilis at its northern limit and Q. mongolica at its southern limit up to the end of the present century.
ISSN:2150-8925
2150-8925
DOI:10.1002/ecs2.3062