Variation of Oriental Oak (Quercus variabilis) Leaf δ13C across Temperate and Subtropical China: Spatial Patterns and Sensitivity to Precipitation

Forests

Baoming Du¹  Hongzhang Kang¹  Yanhua Zhu¹  Xuan Zhou¹  Shan Yin¹  Paul J. Burgess²  Chunjiang Liu¹ 

[1] School of Agriculture and Biology and Research Centre for Low-Carbon Agriculture, Shanghai Jiao Tong University, Shanghai 200240, China; E-Mails:;School of Energy, Environment and Agrifood, Cranfield University, Cranfield MK43 0AL, UK; E-Mail:

关键词: carbon isotope;    oak;    precipitation;    latitude;    Quercus variabilis;   

DOI  :  10.3390/f6072296

来源: mdpi

【 摘 要 】

The concentration of the carbon-13 isotope (leaf δ¹³C) in leaves is negatively correlated with the mean annual precipitation (MAP) atlarge geographical scales. In this paper, we explain the spatial pattern of leaf δ¹³C variation for deciduous oriental oak (Quercus variabilis Bl.) across temperate and subtropical biomes and its sensitivity to climate factors such as MAP. There was a 6‰ variation in the leaf δ¹³C values of oak with a significant positive correlation with latitude and negative correlations with the mean annual temperature (MAT) and MAP. There was no correlation between leaf δ¹³C and altitude or longitude. Stepwise multiple regression analyses showed that leaf δ¹³C decreased 0.3‰ per 100 mm increase in MAP. MAP alone could account for 68% of the observed variation in leaf δ¹³C. These results can be used to improve predictions for plant responses to climate change and particularly lower rainfall.

【 授权许可】

CC BY   
© 2015 by the authors; licensee MDPI, Basel, Switzerland.