Elevation-dependent variations of tree growth and intrinsic water-use efficiency in Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China

被引:60
作者
Wu, Guoju [1 ,2 ]
Liu, Xiaohong [1 ]
Chen, Tuo [1 ]
Xu, Guobao [1 ]
Wang, Wenzhi [1 ,2 ]
Zeng, Xiaomin [1 ,2 ]
Zhang, Xuanwen [1 ,2 ]
机构
[1] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China
来源
FRONTIERS IN PLANT SCIENCE | 2015年 / 6卷
关键词
tree rings; basal area increment; carbon isotope; SPEI; elevation gradient; physiological response; Northwestern China; CARBON-ISOTOPE DISCRIMINATION; ATMOSPHERIC CO2; CLIMATE-CHANGE; FAGUS-SYLVATICA; RING DELTA-C-13; STABLE-ISOTOPES; NORWAY SPRUCE; FOREST; DROUGHT; DECLINE;
D O I
10.3389/fpls.2015.00309
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Rising atmospheric CO2 concentration (C-a) is expected to accelerate tree growth by enhancing photosynthesis and increasing intrinsic water-use efficiency (iWUE). However, the extent of this effect on long-term iWUE and its interactions with climate remains unclear in trees along an elevation gradient. Therefore, we investigated the variation in the radial growth and iWUE of mature Picea schrenkiana trees located in the upper tree-line (A1 : 2700 m a.s.l.), middle elevation (A2 : 2400 m a.s.l.), and lower forest limit (A3 : 2200 m a.s.l.), in relation to the rising Ca and changing climate in the Wusun Mountains of northwestern China, based on the basal area increment (BAI) and tree-ring delta C-13 chronologies from 1960 to 2010. We used the CRU TS3.22 dataset to analyze the general response of tree growth to interannual variability of regional climate, and found that BAI and delta C-13 are less sensitive to climate at A1 than at A2 and A3. The temporal trends of iWUE were calculated under three theoretical scenarios, as a baseline for interpreting the observed gas exchange at increasing Ca. We found that iWUE increased by 12-32% from A1 to A3 over the last 50 years, and showed an elevation-dependent variation in physiological response. The significant negative relationship between BAI and iWUE at A2 and A3 showed that tree growth has been decreasing despite long-term increases in iWUE. However, BAI remained largely stable throughout the study period despite the strongest iWUE increase [at constant intercellular CO2 concentration (C-i) before 1980] at Al. Our results indicate a drought-induced limitation of tree growth response to rising CO2 at lower elevations, and no apparent change in tree growth and diminished iWUE improvement since 1980 in the upper tree-line. This study may contradict the expectation that combined effects of elevated Ca and rising temperatures have increased forest productivity, especially in high-elevation forests.
引用
收藏
页码:1 / 12
页数:12
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