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中国区域478种C3植物叶片碳稳定性同位素组成与水分利用效率
引用本文:任书杰,于贵瑞.中国区域478种C3植物叶片碳稳定性同位素组成与水分利用效率[J].植物生态学报,2011,35(2):119-124.
作者姓名:任书杰  于贵瑞
作者单位:中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室, CERN综合研究中心, 北京 100101
基金项目:国家自然科学基金重大项目(30590381); 中国科学院知识创新工程重要方向资助项目(KZCX2-YW-432); 国家重点基础研究发展计划(2010CB833504)资助
摘    要:目前, 在中国区域关于植物碳稳定性同位素组成(δ13C)已经有了很多的研究, 同时, δ 13C作为植物水分利用效率(WUE)的替代指标, 得到了越来越广泛的应用。而这些研究多集中在站点或小的区域尺度, 那么在整个中国区域尺度上, δ13C能否作为植物WUE的替代指标值得探讨。该文通过对文献资料的收集整理, 研究了中国区域187个采样点478种C3植物叶片的δ13C, 统计分析结果表明δ13C的变化范围为-33.50‰- -22.00‰, 均值为-(27.10 ± 1.70)‰。在乔木、灌木和草本3种不同的生活型间, 叶片δ13C的差异达到极显著水平, 其中以草本的δ13C最高, 乔木最低, 这与在站点或小的区域尺度上的研究结果不同。对不同系统发育类型的植物而言, 种子植物的δ13C极显著地大于蕨类植物; 祼子植物与被子植物间的差异未达到显著水平; 单子叶植物极显著地大于双子叶植物。叶片δ13C值随经度的变化没有明显的规律, 但是随纬度的增加, δ 13C极显著地升高。随年均温度和年均降雨量的降低, 叶片δ13C值极显著升高。年均降雨量与δ13C间的这种极显著的负相关关系, 与WUE和降水量间的关系一致, 这表明在大的区域尺度上, δ13C可以作为植物WUE的指示指标。

关 键 词:C3植物" target="_blank">3植物')">C3植物    生活型    降雨量    稳定性同位素    水分利用效率
收稿时间:2010-03-03

Carbon isotope composition (δ13C) of C3 plants and water use efficiency in China
REN Shu-Jie,YU Gui-Rui.Carbon isotope composition (δ13C) of C3 plants and water use efficiency in China[J].Acta Phytoecologica Sinica,2011,35(2):119-124.
Authors:REN Shu-Jie  YU Gui-Rui
Institution:Synthesis Research Center of Chinese Ecosystem Research Network, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
Abstract:Aims There were many studies about carbon isotope compositions (δ13C) of C3 plant in China, and δ13C have been widely used as the index of water use efficiency (WUE). But most of the studies focused on sites or small-scale regions, so the spatial pattern of δ13C, the relationships between δ13C and climate factors, and if δ13C can represent water use efficiency (WUE) in large-scale regions should be further studied. Methods Based on the collection of references, we studied leaf δ13C of 478 C3 species from 187 sites in China. Important findings The results showed that the range of δ13C was from -33.50‰ ~ -22.00‰, and the mean was - (27.10±1.70) ‰. There were significant difference between δ13C of grass, shrub and tree. δ13C of grass was highest, and that of tree was lowest. The result was different from other studies in sites and small-scale regions. For different phylogenic plants, δ13C of seed plant was significantly higher than fern, the difference between gymnosperm and angiosperm wasn’t significant, but monocotyledon was significantly higher than dicotyledon. Leaf δ13C had irregular variation with longitude increasing, but significantly increased with latitude increasing. Leaf δ13C significantly increased with mean annual temperature and mean annual precipitation decreasing. The relationship between δ13C and precipitation was similar to that of WUE and precipitation, so we can conclude that δ13C of C3 plant can be used as the index of WUE in large-scale regions as well as in sites or small-scale regions.
Keywords:C3 plant  life-form  precipitation  stable isotope  water use efficiency  
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