植物生态学报 ›› 2011, Vol. 35 ›› Issue (2): 119-124.DOI: 10.3724/SP.J.1258.2011.00119
所属专题: 稳定同位素生态学; 生态学研究的方法和技术
• 研究论文 • 下一篇
收稿日期:
2010-03-03
接受日期:
2010-05-17
出版日期:
2011-03-03
发布日期:
2011-01-21
通讯作者:
于贵瑞
作者简介:
**E-mail: yugr@igsnrr.ac.cn
REN Shu-Jie*(), YU Gui-Rui**(
)
Received:
2010-03-03
Accepted:
2010-05-17
Online:
2011-03-03
Published:
2011-01-21
Contact:
YU Gui-Rui
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。
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. 植物生态学报, 2011, 35(2): 119-124. DOI: 10.3724/SP.J.1258.2011.00119
REN Shu-Jie, YU Gui-Rui. Carbon isotope composition (δ13C) of C3 plants and water use efficiency in China. Chinese Journal of Plant Ecology, 2011, 35(2): 119-124. DOI: 10.3724/SP.J.1258.2011.00119
生活型 Life form | 均值 Mean (‰) | 差异 Difference | 物种数 No. of species |
---|---|---|---|
草本 Grass | -(26.81 ± 1.53) | A | 341 |
灌木 Shrub | -(27.50 ± 1.91) | B | 86 |
乔木 Tree | -(28.30 ± 1.75) | C | 51 |
表1 不同生活型植物叶片碳稳定性同位素组成(δ13C)的比较
Table 1 Comparison of leaf carbon isotope composition (δ13C) between different life-form plants
生活型 Life form | 均值 Mean (‰) | 差异 Difference | 物种数 No. of species |
---|---|---|---|
草本 Grass | -(26.81 ± 1.53) | A | 341 |
灌木 Shrub | -(27.50 ± 1.91) | B | 86 |
乔木 Tree | -(28.30 ± 1.75) | C | 51 |
系统发育类型 Phylogenic type | 均值 Mean (‰) | 差异 Difference | 物种数 No. of species |
---|---|---|---|
种子植物 Seed plant | - (27.07 ± 1.68) | A | 473 |
蕨类植物 Fern | -(29.99 ± 1.41) | B | 5 |
裸子植物 Gymnosperm | (-26.39 ± 2.41) | a | 10 |
被子植物 Angiosperm | (-27.08 ± 1.66) | a | 463 |
单子叶植物 Monocotyledon | (-26.37 ± 1.70) | A | 86 |
双子叶植物 Dicotyledon | (-27.24 ± 1.61) | B | 377 |
表2 不同系统发育植物叶片碳稳定性同位素组成(δ13C)的比较
Table 2 Comparison of leaf carbon isotope composition (δ13C) between different phylogenic plants
系统发育类型 Phylogenic type | 均值 Mean (‰) | 差异 Difference | 物种数 No. of species |
---|---|---|---|
种子植物 Seed plant | - (27.07 ± 1.68) | A | 473 |
蕨类植物 Fern | -(29.99 ± 1.41) | B | 5 |
裸子植物 Gymnosperm | (-26.39 ± 2.41) | a | 10 |
被子植物 Angiosperm | (-27.08 ± 1.66) | a | 463 |
单子叶植物 Monocotyledon | (-26.37 ± 1.70) | A | 86 |
双子叶植物 Dicotyledon | (-27.24 ± 1.61) | B | 377 |
图3 中国区域C3植物叶片碳稳定性同位素组成(δ13C)的空间分布格局。经度, y = 0.0036x - 27.273 (R2 = 0.000 5, n = 791); 纬度, y = 0.0965x - 30.562 (R2 = 0.123 5, n =791); 年平均温度, y = -0.0812x - 26.561 (R2 = 0.104 5, n = 791); 年平均降雨量, y = -0.002x - 25.977 (R2 = 0.173, n = 791)。
Fig. 3 Spatial pattern of leaf carbon isotope composition (δ13C) of C3 species in China. MAT, mean annual air temperature; MAP, mean annual precipitation. Longitude, y = 0.003 6x - 27.273 (R2 = 0.000 5, n = 791); latitude, y = 0.096 5x - 30.562 (R2 = 0.123 5, n = 791); MAT, y = -0.081 2x - 26.561 (R2 = 0.104 5, n = 791); MAP, y = -0.002x - 25.977 (R2 = 0.173, n = 791).
生活型 Life form | 纬度 Latitude | 年均温 MAT | 年均降雨量 MAP | 物种数 No. of species |
---|---|---|---|---|
乔木 Tree | 32.62C | 9.89A | 780.15A | 117 |
灌木 Shrub | 35.42B | 8.93A | 549.88B | 228 |
草本 Grass | 38.92A | 2.06B | 389.99C | 603 |
表3 不同生活型植物样点分布情况比较
Table 3 Comparison of sample sites distribution about different life-form plants
生活型 Life form | 纬度 Latitude | 年均温 MAT | 年均降雨量 MAP | 物种数 No. of species |
---|---|---|---|---|
乔木 Tree | 32.62C | 9.89A | 780.15A | 117 |
灌木 Shrub | 35.42B | 8.93A | 549.88B | 228 |
草本 Grass | 38.92A | 2.06B | 389.99C | 603 |
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