植物生态学报 ›› 2024, Vol. 48 ›› Issue (8): 955-966.DOI: 10.17521/cjpe.2023.0390 cstr: 32100.14.cjpe.2023.0390
• 综述 • 下一篇
陈炫铮1, 朱耀军2,3, 高居娟4, 刘一凡1, 王荣5, 方涛1, 罗芳丽1,6,*(), 薛伟7,*(
), 于飞海7
收稿日期:
2023-12-26
接受日期:
2024-05-06
出版日期:
2024-08-20
发布日期:
2024-05-16
通讯作者:
*罗芳丽(ecoluofangli@163.com);薛伟(x_wei1988@163.com)
基金资助:
CHEN Xuan-Zheng1, ZHU Yao-Jun2,3, GAO Ju-Juan4, LIU Yi-Fan1, WANG Rong5, FANG Tao1, LUO Fang-Li1,6,*(), XUE Wei7,*(
), YU Fei-Hai7
Received:
2023-12-26
Accepted:
2024-05-06
Online:
2024-08-20
Published:
2024-05-16
Contact:
LUO Fang-Li(ecoluofangli@163.com), XUE Wei(x_wei1988@163.com)
Supported by:
摘要:
植物-土壤反馈作为植物分布、群落组成和演替的重要驱动力, 近年来受到广泛关注。时空变异是驱动植物-土壤反馈效应的重要因素, 但目前缺乏对其研究进展的梳理。该文综述了植物-土壤反馈时空变异的研究进展, 并提出了未来可以继续深入的研究方向。在植物-土壤反馈时间尺度上, 重点论述了植物不同发育阶段、实验周期与反馈效应的关系。在植物-土壤反馈的空间尺度上, 重点讨论了植物空间分布及空间转移、土壤微生物类群及理化因子空间位置差异以及地上与地下系统对反馈系统的影响。基于研究进展, 该文提出在反馈时间尺度上, 需关注长期的、多点的动态反馈过程, 提高反馈过程时间尺度上的分辨率; 应充分考虑微生物类群与驯化和测试植物作用的缓冲时间, 设置合理的驯化和反馈周期, 让研究结果更为客观; 在空间尺度上, 需关注植物空间分布、土壤因子空间异质性以及地上和地下系统对反馈效应的影响, 尽量做到接种土壤在物理结构上的相似性, 以期获得更真实的反馈效应。
陈炫铮, 朱耀军, 高居娟, 刘一凡, 王荣, 方涛, 罗芳丽, 薛伟, 于飞海. 植物-土壤反馈时空变异研究进展. 植物生态学报, 2024, 48(8): 955-966. DOI: 10.17521/cjpe.2023.0390
CHEN Xuan-Zheng, ZHU Yao-Jun, GAO Ju-Juan, LIU Yi-Fan, WANG Rong, FANG Tao, LUO Fang-Li, XUE Wei, YU Fei-Hai. Research progress on spatial-temporal variation of plant-soil feedback. Chinese Journal of Plant Ecology, 2024, 48(8): 955-966. DOI: 10.17521/cjpe.2023.0390
图1 植物-土壤反馈的时空格局(A)及调控机制(B)。A中绿色和棕色箭头代表原物种继续生长, 黑色箭头代表新物种在原物种驯化后的土壤中生长; 不同颜色深浅的斑块代表物种对土壤的影响程度; 在时间尺度上, 植物生长时间越长, 微生物对土壤影响越大; 在空间尺度上, 随着空间向外扩展, 微生物对土壤的影响逐渐减弱。时间尺度(如驯化与反馈时间的长短等)对土壤中养分与微生物组成产生影响, 空间尺度(如纬度、海拔差异等)对土壤属性产生影响, 二者共同调控植物生长。所涉及的参考文献详见附录。
Fig. 1 Spatial-temporal pattern (A) and regulatory mechanism (B) of plant-soil feedback. In A, green and brown arrows indicate continued growth of the original species, and black arrows indicate growth of new species in the domesticated soil of original species. Patches with different shades of color represent the degree of soil influenced by new species. At the temporal scale, the longer time the plant grow, the greater the effect of microorganisms on soil. At the spatial scale, with the outward expansion of root space, the influence of microorganisms on soil gradually weakens. The time scale (e.g., domestication and feedback time) affects soil nutrient and microbial composition, and the spatial scale (e.g., latitude and altitude differences) affects soil properties, both of which jointly regulate plant growth. References to trend charts are listed in Supplement.
内容 Content | 参考文献 Reference |
---|---|
调控时间长度 Duration of conditioning | Dudenhöffer et al., |
反馈时间长度 Duration of feedback | Speek et al., |
原产地距离 Distance from the origin | Janzen, |
盐度梯度 Salinity gradient | Jiang et al., |
斑块异质性 Pactch hererogeneity | Huang et al., |
附录 图1B中趋势图数据来源
Supplement Data sources for trend plots in Fig. 1B
内容 Content | 参考文献 Reference |
---|---|
调控时间长度 Duration of conditioning | Dudenhöffer et al., |
反馈时间长度 Duration of feedback | Speek et al., |
原产地距离 Distance from the origin | Janzen, |
盐度梯度 Salinity gradient | Jiang et al., |
斑块异质性 Pactch hererogeneity | Huang et al., |
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