期刊
FRONTIERS IN PLANT SCIENCE
卷 8, 期 -, 页码 -出版社
FRONTIERS MEDIA SA
DOI: 10.3389/fpls.2017.01996
关键词
dark respiration; photosynthetic C-13 discrimination; post-photosynthetic isotope fractionation; C-3 species; C-4 species; water stress
资金
- National Key Basic Research Program of China [2015CB150800]
- State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences [G2014-02-01]
- National Natural Science Foundation of China [31270445, 31570470, 41671207]
- National Key Technology Support Program [2013BACO9B03]
- Fundamental Research Funds for the Central Universities [2412016KJ008]
- Program of Introducing Talents of Discipline to Universities [B16011]
- Main Service Project of Characteristic Institute of Chinese Academy of Sciences [TSS-2015-014-FW-5-1]
- 9th Thousand Talents Program of China
Whether photosynthetic pathway differences exist in the amplitude of nighttime variations in the carbon isotope composition of leaf dark-respired CO2 (delta C-13(l)) and respiratory apparent isotope fractionation relative to biomass (Delta(R),(biomass)) in response to drought stress is unclear. These differences, if present, would be important for the partitioning of C-3-C-4 mixed ecosystem C fluxes. We measured delta C-13(l), the delta C-13 of biomass and of potential respiratory substrates and leaf gas exchange in one C-3 (Leymus chinensis) and two C-4 (Chloris virgata and Hemarthria altissima) grasses during a manipulated drought period. For all studied grasses, delta C-13(l) decreased from 21:00 to 03:00 h. The magnitude of the nighttime shift in delta C-13(l) decreased with increasing drought stress. The delta C-13(l) values were correlated with the delta C-13(l) of respiratory substrates, whereas the magnitude of the nighttime shift in delta C-13(l) strongly depended on the daytime carbon assimilation rate and the range of nighttime variations in the respiratory substrate content. The Delta(R),(biomass) in the C-3 and C-4 grasses varied in opposite directions with the intensification of the drought stress. The contribution of C-4 plant-associated carbon flux is likely to be overestimated if carbon isotope signatures are used for the partitioning of ecosystem carbon exchange and the delta C-13(l) of biomass is used as a substitute for leaf dark-respired CO2. The detected drought sensitivities in delta C-13(l) and differences in respiratory apparent isotope fractionation between C-3 and C-4 grasses have marked implications for isotope partitioning studies at the ecosystem level.
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