Global decadal variability of plant carbon isotope discrimination and its link to gross primary production

被引:13
|
作者
Lavergne, Alienor [1 ]
Hemming, Deborah [2 ,3 ]
Prentice, Iain Colin [4 ,5 ,6 ,7 ]
Guerrieri, Rossella [8 ]
Oliver, Rebecca J. [9 ]
Graven, Heather [1 ,5 ]
机构
[1] Imperial Coll London, Dept Phys, Exhibit Rd, London SW7 2AZ, England
[2] Met Off Hadley Ctr, Exeter, Devon, England
[3] Birmingham Inst Forest Res, Birmingham, W Midlands, England
[4] Imperial Coll London, Georgina Mace Ctr Living Planet, Dept Life Sci, Ascot, Berks, England
[5] Imperial Coll London, Grantham Inst Climate Change & Environm, London, England
[6] Macquarie Univ, Dept Biol Sci, N Ryde, NSW, Australia
[7] Tsinghua Univ, Dept Earth Syst Sci, Beijing, Peoples R China
[8] Univ Bologna, Dept Agr & Food Sci, Bologna, Italy
[9] UK Ctr Ecol & Hydrol, Wallingford, Oxon, England
基金
欧盟地平线“2020”;
关键词
carbon isotope discrimination; forest ecosystems; gross primary production; JULES model; land carbon uptake; tree rings; WATER-USE EFFICIENCY; ENVIRONMENT SIMULATOR JULES; TEMPERATURE RESPONSE FUNCTIONS; ATMOSPHERIC CO2 CONCENTRATION; MESOPHYLL CONDUCTANCE; C-13; DISCRIMINATION; MODEL DESCRIPTION; EUROPEAN FORESTS; RADIAL GROWTH; TREE GROWTH;
D O I
10.1111/gcb.15924
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Carbon isotope discrimination (Delta C-13) in C-3 woody plants is a key variable for the study of photosynthesis. Yet how Delta C-13 varies at decadal scales, and across regions, and how it is related to gross primary production (GPP), are still incompletely understood. Here we address these questions by implementing a new Delta C-13 modelling capability in the land-surface model JULES incorporating both photorespiratory and mesophyll-conductance fractionations. We test the ability of four leaf-internal CO2 concentration models embedded in JULES to reproduce leaf and tree-ring (TR) carbon isotopic data. We show that all the tested models tend to overestimate average Delta C-13 values, and to underestimate interannual variability in Delta C-13. This is likely because they ignore the effects of soil water stress on stomatal behavior. Variations in post-photosynthetic isotopic fractionations across species, sites and years, may also partly explain the discrepancies between predicted and TR-derived Delta C-13 values. Nonetheless, the "least-cost" (Prentice) model shows the lowest biases with the isotopic measurements, and lead to improved predictions of canopy-level carbon and water fluxes. Overall, modelled Delta C-13 trends vary strongly between regions during the recent (1979-2016) historical period but stay nearly constant when averaged over the globe. Photorespiratory and mesophyll effects modulate the simulated global Delta C-13 trend by 0.0015 +/- 0.005 parts per thousand and -0.0006 +/- 0.001 parts per thousand ppm(-1), respectively. These predictions contrast with previous findings based on atmospheric carbon isotope measurements. Predicted Delta C-13 and GPP tend to be negatively correlated in wet-humid and cold regions, and in tropical African forests, but positively related elsewhere. The negative correlation between Delta C-13 and GPP is partly due to the strong dominant influences of temperature on GPP and vapor pressure deficit on Delta C-13 in those forests. Our results demonstrate that the combined analysis of Delta C-13 and GPP can help understand the drivers of photosynthesis changes in different climatic regions.
引用
收藏
页码:524 / 541
页数:18
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