植物生态学报 ›› 2026, Vol. 50 ›› Issue (2): 352-361.DOI: 10.17521/cjpe.2025.0179 cstr: 32100.14.cjpe.2025.0179
冯哲1,3, 许格希1,3, 刘顺1,3, 陈健1,3, 李非凡1,3, 巩闪闪1,3, 贾磊1,3, 孙镇1,3, 余美霓1,3, 史作民1,2,3,*(
), 周庆宏4, 蒋冬梅4
收稿日期:2025-05-16
接受日期:2025-08-25
出版日期:2026-02-28
发布日期:2026-04-01
通讯作者:
*史作民(shizm@caf.ac.cn)基金资助:
FENG Zhe1,3, XU Ge-Xi1,3, LIU Shun1,3, CHEN Jian1,3, LI Fei-Fan1,3, GONG Shan-Shan1,3, JIA Lei1,3, SUN Zhen1,3, YU Mei-Ni1,3, SHI Zuo-Min1,2,3,*(
), ZHOU Qing-Hong4, JIANG Dong-Mei4
Received:2025-05-16
Accepted:2025-08-25
Online:2026-02-28
Published:2026-04-01
Contact:
*SHI Zuo-Min (shizm@caf.ac.cn)Supported by:摘要:
植物元素组成及其化学计量特征对于理解植物养分策略与生态系统生物地球化学循环至关重要。尽管“生物地球化学生态位假说”和“化学计量可塑性假说”已在宏观尺度得到验证, 但在极端胁迫环境中, 特别是在考虑系统发育保守性时, 其适用性仍不确定。该研究采集了金沙江干热河谷区5个地点13种共240个灌木和草本植物叶片样本, 测定了其碳(C)、氮(N)、磷(P)化学计量特征及对应土壤理化性质。通过贝叶斯系统发育线性混合模型等方法, 定量评估了生境因子与系统发育对叶片化学计量特征变异的相对贡献, 并探讨了主要生境因子对叶片养分利用策略的调控机制。结果表明, 生境因子对叶片化学计量特征变异的解释度较低, 其中海拔是叶片C、P含量及C:P、N:P的主要驱动因子, 土壤pH则主导叶片N含量和C:N的变化。系统发育分析显示, 叶片N、P含量及C:N、C:P表现出显著的系统发育信号, 贝叶斯模型结果进一步支持系统发育对叶片化学计量特征的主要影响。除系统发育保守性外, 叶片C含量的差异与植物生活型有关, 而N:P则表现出较高的种内可塑性。总之, 该区域叶片化学计量格局主要受系统发育保守性控制, 并由表型可塑性加以补充。该研究有助于深化对环境胁迫条件下植物多样性维持机制的理解, 同时拓展了区域尺度上植物养分利用策略的相关认识。
冯哲, 许格希, 刘顺, 陈健, 李非凡, 巩闪闪, 贾磊, 孙镇, 余美霓, 史作民, 周庆宏, 蒋冬梅. 生境因子和系统发育协同驱动云南金沙江干热河谷植物叶片化学计量特征. 植物生态学报, 2026, 50(2): 352-361. DOI: 10.17521/cjpe.2025.0179
FENG Zhe, XU Ge-Xi, LIU Shun, CHEN Jian, LI Fei-Fan, GONG Shan-Shan, JIA Lei, SUN Zhen, YU Mei-Ni, SHI Zuo-Min, ZHOU Qing-Hong, JIANG Dong-Mei. Habitat factors and phylogeny jointly drive leaf stoichiometry in dry-hot valley region of Jinsha River, Yunnan, China. Chinese Journal of Plant Ecology, 2026, 50(2): 352-361. DOI: 10.17521/cjpe.2025.0179
图1 金沙江干热河谷采样点。HP, 华坪; LQ, 禄劝; YM, 元谋; YR, 永仁; YS, 永胜。
Fig. 1 Study sites in dry-hot valley of Jinsha River. HP, Huaping; LQ, Luquan; YM, Yuanmou; YR, Yongren; YS, Yongsheng.
| 采样地点 Study site | 纬度 Latitude (° N) | 经度 Longitude (° E) | 海拔 Altitude (m) | 年平均气温 Mean annual temperature (℃) | 年降水量 Mean annual precipitation (mm) | 胸高断面积 Basal area (cm2·m-2) | 草本盖度 Herb cover (%) |
|---|---|---|---|---|---|---|---|
| 永胜 Yongsheng | 26.20 | 100.62 | 1 297 | 18.3 | 825.0 | 5.85 | 90 |
| 华坪 Huaping | 26.37 | 101.23 | 1 307 | 20.5 | 857.8 | 20.42 | 88 |
| 永仁 Yongren | 26.40 | 101.46 | 1 496 | 18.5 | 925.6 | 34.51 | 93 |
| 元谋 Yuanmou | 25.72 | 101.78 | 1 217 | 20.2 | 827.9 | 2.70 | 92 |
| 禄劝 Luquan | 26.30 | 102.64 | 1 023 | 21.3 | 879.6 | 3.42 | 95 |
表1 金沙江干热河谷采样点基本信息
Table 1 Basic information on the study sites in dry-hot valley of Jinsha River
| 采样地点 Study site | 纬度 Latitude (° N) | 经度 Longitude (° E) | 海拔 Altitude (m) | 年平均气温 Mean annual temperature (℃) | 年降水量 Mean annual precipitation (mm) | 胸高断面积 Basal area (cm2·m-2) | 草本盖度 Herb cover (%) |
|---|---|---|---|---|---|---|---|
| 永胜 Yongsheng | 26.20 | 100.62 | 1 297 | 18.3 | 825.0 | 5.85 | 90 |
| 华坪 Huaping | 26.37 | 101.23 | 1 307 | 20.5 | 857.8 | 20.42 | 88 |
| 永仁 Yongren | 26.40 | 101.46 | 1 496 | 18.5 | 925.6 | 34.51 | 93 |
| 元谋 Yuanmou | 25.72 | 101.78 | 1 217 | 20.2 | 827.9 | 2.70 | 92 |
| 禄劝 Luquan | 26.30 | 102.64 | 1 023 | 21.3 | 879.6 | 3.42 | 95 |
图2 用基于随机森林模型和五折交叉验证的递归特征消除法筛选与植物叶片化学计量特征相关的生境变量。变量的最终选择情况由浅色条目表示。深色条目表示其他次重要的预测变量, 但未用于后续分析。C, 碳; N, 氮; P, 磷。AP, 土壤有效磷含量; ELE, 海拔; MAP, 年降水量; MAT, 年平均气温; NH+ 4-N, 土壤铵态氮含量; NO- 3-N, 土壤硝态氮含量; pH, 土壤pH; SBD, 土壤容重; STC, 土壤总碳含量; STN, 土壤总氮含量; STP, 土壤总磷含量; TK, 土壤总钾含量; WC, 土壤含水量; MSE, 均方误差。
Fig. 2 Recursive Feature Elimination based on random forest and 5-fold cross-validation was used to select habitat variables associated with plant leaf stoichiometry. The final selection of variables is indicated by the light bars. Dark bars indicate additional, next most important predictors, but not used for subsequent analyses. C, carbon; N, nitrogen; P, phosphorus. AP, soil effective phosphorus content; ELE, elevation above sea level; MAP, mean annual precipitation; MAT, mean annual air temperature; NH+ 4-N, soil ammonium nitrogen content; NO- 3-N, soil nitrate nitrogen content; pH, soil pH; SBD, soil bulk density; STC, soil total carbon content; STN, soil total nitrogen content; STP, soil total phosphorus content; TK, soil total potassium content; WC, soil water content; MSE, mean squared error.
图3 使用线性混合效应模型分析叶片化学计量特征与入选变量的关系。效应强度以标准化固定效应系数表示。C, 碳; N, 氮; P, 磷。ELE, 海拔; MAP, 年降水量; MAT, 年平均气温; pH, 土壤pH; STN, 土壤总氮含量; STP, 土壤总磷含量; TK, 土壤总钾含量; WC, 土壤含水量; LMM, 线性混合效应模型。
Fig. 3 Relationships between leaf stoichiometric and the selected variables were analyzed using linear mixed effect models. Effect magnitudes are expressed as normalized fixed effect coefficients. See Fig. 2 for variable abbreviations. C, carbon; N, nitrogen; P, phosphorus. ELE, elevation above sea level; MAP, mean annual precipitation; MAT, mean annual air temperature; pH, soil pH; STN, soil total nitrogen content; STP, soil total phosphorus content; TK, soil total potassium content; WC, soil water content; LMM, linear mixed-effect model.
图4 贝叶斯系统发育线性混合模型(A)和物种变异分解结果(B)。A中“生境因子”代表固定效应(通过递归特征消除法从生境因素中选取的一部分子集)。C, 碳; N, 氮; P, 磷。
Fig. 4 Results of the Bayesian phylogenetic mixture model (A) and variance partitioning of species-level variation (B). In panel A, “Environments” represents the fixed effects (a subset of habitat factors selected through recursive feature elimination). C, carbon; N, nitrogen; P, phosphorus.
| Blomberg’s K | p | Pagel’s λ | p | |
|---|---|---|---|---|
| C | 0.155 | 0.135 | 0.507 | 0.297 |
| N | 0.479** | 0.003 | 0.915* | 0.017 |
| P | 0.385* | 0.016 | 0.736* | 0.014 |
| C:N | 0.583** | 0.004 | 0.951* | 0.011 |
| C:P | 0.354* | 0.025 | 0.746* | 0.021 |
| N:P | 0.290 | 0.526 | 0.868 | 0.190 |
表2 植物叶片化学计量特征的系统发育信号
Table 2 Phylogenetic signals of plant leaf stoichiometric traits
| Blomberg’s K | p | Pagel’s λ | p | |
|---|---|---|---|---|
| C | 0.155 | 0.135 | 0.507 | 0.297 |
| N | 0.479** | 0.003 | 0.915* | 0.017 |
| P | 0.385* | 0.016 | 0.736* | 0.014 |
| C:N | 0.583** | 0.004 | 0.951* | 0.011 |
| C:P | 0.354* | 0.025 | 0.746* | 0.021 |
| N:P | 0.290 | 0.526 | 0.868 | 0.190 |
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