Tree water-use efficiency and growth dynamics in response to climatic and environmental changes in a temperate forest in Beijing, China

Li Fu; Yan Xu; Zhihong Xu; Bingfang Wu; Dan Zhao

doi:10.1016/j.envint.2019.105209

Tree water-use efficiency and growth dynamics in response to climatic and environmental changes in a temperate forest in Beijing, China

Environ Int. 2020 Jan:134:105209. doi: 10.1016/j.envint.2019.105209. Epub 2019 Oct 31.

Authors

Li Fu¹, Yan Xu², Zhihong Xu³, Bingfang Wu⁴, Dan Zhao⁵

Affiliations

¹ Environmental Futures Research Institute and School of Environment and Science, Griffith University, Nathan, QLD 4111, Australia; State Key Laboratory of Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China.
² Environmental Futures Research Institute and School of Environment and Science, Griffith University, Nathan, QLD 4111, Australia.
³ Environmental Futures Research Institute and School of Environment and Science, Griffith University, Nathan, QLD 4111, Australia. Electronic address: zhihong.xu@griffith.edu.au.
⁴ State Key Laboratory of Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China. Electronic address: wubf@radi.ac.cn.
⁵ State Key Laboratory of Remote Sensing, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China.

PMID: 31677597
DOI: 10.1016/j.envint.2019.105209

Abstract

Understanding the responses of local forests to the gradually rising atmospheric CO₂ concentrations (c_a) and changing environment is critical for appropriate management activities. This work used tree ring width measures (i.e. basal areal increment, BAI) and carbon (C) and nitrogen (N) signals to explore the intrinsic water use efficiency (iWUE) and tree growth dynamics of three major tree species (Pinus massoniana, P.tabuliformis and Larix gmelinii) in the Miyun Reservae Basin (MRB) of Beijing. The results indicate that c_a was a primary contributor to tree growths, especially at the remote site where rising c_a accounted for 92% and 74% of BAI changes for P. tabuliformis and L. gmelinii, respectively. N deposition was found to have a positive effect on BAI at this site. The controlling effect of c_a on tree growth at the close-to-city site was smaller (52% and 44% of the contributions for P. tabuliformis and P. massoniana, respectively), while the negative influences of N deposition on BAI tends to be intensified. iWUE showed consistent increase during the entire growth period at all sites. Quadratic relationships between iWUE and BAI were observed, which indicated that the rising c_a stimulated photosynthesis, contributing to the initial BAI and iWUE increase. However, the intensified water stress resulting from reduced precipitation and increased temperature led to a reduction in tree stomatal conductance causing the subsequent increase in iWUE but decrease in BAI. Of the site- and species-related responses of tree growth to c_a, climatic and environmental changes in the MRB, the site-related variation dominated. The non-linear relationship between BAI and c_a combined with the quadratic relationship between BAI and iWUE indicate a decreased ability of forests to capture atmospheric CO₂ once the CO₂ tipping point has passed.

Keywords: Carbon and nitrogen isotope; Climate change; Nitrogen deposition; Tree ring; Water use efficiency.

Publication types

Research Support, Non-U.S. Gov't

MeSH terms

Beijing
Carbon Dioxide
China
Climate Change
Forests*
Trees*
Water

Substances

Water
Carbon Dioxide