植物生态学报 ›› 2026, Vol. 50 ›› Issue (3): 674-684.DOI: 10.17521/cjpe.2025.0083 cstr: 32100.14.cjpe.2025.0083
何堂庆1, 王变变2, 曹鑫鑫1, 张康成1, 汪晓东1, 王浩1, 白彤硕1, 赵叶新1, 张艺1, 王益3, 仇云鹏4,*(
), 胡水金4
收稿日期:2025-03-05
接受日期:2025-05-27
出版日期:2026-03-20
发布日期:2026-04-03
通讯作者:
*仇云鹏(yunpeng_qiu@njau.edu.cn)基金资助:
HE Tang-Qing1, WANG Bian-Bian2, CAO Xin-Xin1, ZHANG Kang-Cheng1, WANG Xiao-Dong1, WANG Hao1, BAI Tong-Shuo1, ZHAO Ye-Xin1, ZHANG Yi1, WANG Yi3, QIU Yun-Peng4,*(
), HU Shui-Jin4
Received:2025-03-05
Accepted:2025-05-27
Online:2026-03-20
Published:2026-04-03
Contact:
*QIU Yun-Peng(yunpeng_qiu@njau.edu.cn)
Supported by:摘要:
植物-丛枝菌根真菌(AMF)共生体系构成了陆地生态系统关键的养分传递网络, 在维持生态系统功能方面发挥着重要作用。然而, 目前对于AMF群落组成及其生态功能如何响应全球气候变化仍知之甚少。该研究依托黄土高原半干旱草地的全球变化长期控制实验平台, 利用野外原位样方调查和高通量测序技术, 探讨了降水增加背景下植物水分和养分获取策略及AMF群落组成的响应特征及其潜在关联。研究结果表明, 降水增加提高了半灌木和杂类草的生物量, 降低了禾草的生物量。相较于禾草, 半灌木和杂类草通常具有更加粗短的根系, 这可能增强了AMF的定殖潜力。高通量测序结果显示, 降水增加显著改变了AMF群落组成: 提高了巨孢囊霉科和类球囊霉科的相对丰度, 降低了球囊霉科相对丰度, 并显著提升了AMF群落网络的复杂性, 可能增强了植物对水分和养分的获取能力。综上, 该研究揭示了降水增加背景下植物功能群生长、根系性状、AMF群落组成及植物水分和养分获取策略之间的潜在联系。这些结果表明降水增加可能通过调控植物-AMF互作网络, 对草地生态系统的养分循环产生深远影响。
何堂庆, 王变变, 曹鑫鑫, 张康成, 汪晓东, 王浩, 白彤硕, 赵叶新, 张艺, 王益, 仇云鹏, 胡水金. 半干旱草地植物和丛枝菌根真菌群落对长期降水增加的响应. 植物生态学报, 2026, 50(3): 674-684. DOI: 10.17521/cjpe.2025.0083
HE Tang-Qing, WANG Bian-Bian, CAO Xin-Xin, ZHANG Kang-Cheng, WANG Xiao-Dong, WANG Hao, BAI Tong-Shuo, ZHAO Ye-Xin, ZHANG Yi, WANG Yi, QIU Yun-Peng, HU Shui-Jin. Responses of plants and arbuscular mycorrhizal fungal communities to long-term precipitation increase in a semi-arid grassland. Chinese Journal of Plant Ecology, 2026, 50(3): 674-684. DOI: 10.17521/cjpe.2025.0083
图1 降水增加对2021-2023年禾草类生物量(A-C)及半灌木和杂类草生物量(D-F)的影响(平均值±标准误)。图中圆圈表示数据点, *表示不同处理间差异显著(p < 0.05)。Con, 环境降水处理; Pi, 降水增加处理。
Fig. 1 Effects of precipitation increase on grass biomass (A-C) and on subshrub and forb biomass (D-F) in 2021-2023 (mean ± SE). Dots represent replicate samples. * denote significant differences between treatments at p < 0.05 level. Con, ambient precipitation; Pi, precipitation increase.
| 年份 Year | 处理 Treatment | 土壤含水量 Soil moisture (%) | 铵态氮含量 NH4+-N content (mg·kg-1) | 硝态氮含量 NO3--N content (mg·kg-1) | 可溶性有机碳含量 Dissolved organic carbon content (mg·kg-1) | 速效磷含量 Available phosphorus content (mg·kg-1) | 微生物生物量碳含量 Microbial biomass carbon content (mg·kg-1) |
|---|---|---|---|---|---|---|---|
| 2021 | Con | 8.09 ± 0.19 | 2.80 ± 0.12 | 14.70 ± 1.49 | 185.56 ± 12.58 | - | 628.60 ± 54.70 |
| Pi | 9.48 ± 0.34 | 3.23 ± 0.09 | 16.06 ± 1.16 | 187.79 ± 12.33 | - | 727.32 ± 76.42 | |
| 2022 | Con | 12.67 ± 0.14 | 1.39 ± 0.10 | 8.87 ± 0.15 | 133.96 ± 5.40 | 8.29 ± 0.84 | 708.17 ± 9.17 |
| Pi | 14.01 ± 0.07 | 1.53 ± 0.02 | 9.68 ± 0.58 | 177.05 ± 10.58 | 9.31 ± 0.08 | 740.86 ± 56.27 | |
| 2023 | Con | 8.11 ± 0.15 | 1.82 ± 0.16 | 20.83 ± 4.20 | 152.42 ± 7.50 | - | 656.60 ± 51.97 |
| Pi | 9.26 ± 0.19 | 2.25 ± 0.17 | 21.42 ± 6.62 | 153.31 ± 11.18 | - | 601.09 ± 19.27 |
表1 降水增加对土壤理化性质和微生物生物量碳含量的线性混合效应模型分析结果(平均值±标准误)
Table 1 Results of the linear mixed-effects model analysis on the effects of precipitation increase on soil abiotic properties and microbial biomass carbon content (mean ± SE)
| 年份 Year | 处理 Treatment | 土壤含水量 Soil moisture (%) | 铵态氮含量 NH4+-N content (mg·kg-1) | 硝态氮含量 NO3--N content (mg·kg-1) | 可溶性有机碳含量 Dissolved organic carbon content (mg·kg-1) | 速效磷含量 Available phosphorus content (mg·kg-1) | 微生物生物量碳含量 Microbial biomass carbon content (mg·kg-1) |
|---|---|---|---|---|---|---|---|
| 2021 | Con | 8.09 ± 0.19 | 2.80 ± 0.12 | 14.70 ± 1.49 | 185.56 ± 12.58 | - | 628.60 ± 54.70 |
| Pi | 9.48 ± 0.34 | 3.23 ± 0.09 | 16.06 ± 1.16 | 187.79 ± 12.33 | - | 727.32 ± 76.42 | |
| 2022 | Con | 12.67 ± 0.14 | 1.39 ± 0.10 | 8.87 ± 0.15 | 133.96 ± 5.40 | 8.29 ± 0.84 | 708.17 ± 9.17 |
| Pi | 14.01 ± 0.07 | 1.53 ± 0.02 | 9.68 ± 0.58 | 177.05 ± 10.58 | 9.31 ± 0.08 | 740.86 ± 56.27 | |
| 2023 | Con | 8.11 ± 0.15 | 1.82 ± 0.16 | 20.83 ± 4.20 | 152.42 ± 7.50 | - | 656.60 ± 51.97 |
| Pi | 9.26 ± 0.19 | 2.25 ± 0.17 | 21.42 ± 6.62 | 153.31 ± 11.18 | - | 601.09 ± 19.27 |
图2 降水增加对2021和2022年丛枝菌根真菌物种相对丰度(A, B), 以及2021和2022年(C, D)巨孢囊霉科(Giga)、类球囊霉科(Para)和球囊霉科(Glomeraceae)相对丰度的影响(平均值±标准误)。*, p < 0.05; **, p < 0.01。
Fig. 2 Effects of precipitation increase on the relative abundance of arbuscular mycorrhizal fungi species (A, B) and on the relative abundance of Gigasporaceae, Paraglomeraceae, and Glomeraceae (C, D) in 2021 and 2022 (mean ± SE). *, p < 0.05; **, p < 0.01. Con, ambient precipitation; Pi, precipitation increase.
图3 降水增加对2021和2022年丛枝菌根真菌群落组成的影响。*表示不同处理间差异显著(p < 0.05)。
Fig. 3 Effects of precipitation increase on arbuscular mycorrhizal fungal community composition in 2021 and 2022. Con, ambient precipitation; Pi, precipitation increase. * denote significant differences between treatments at p < 0.05 level.
图4 降水增加对丛枝菌根真菌群落网络结构的影响。
Fig. 4 Effect of precipitation increase on co-occurrence network structure of arbuscular mycorrhizal fungal communities. Con, ambient precipitation; Pi, precipitation increase.
| 处理 Treatment | 平均度 Average degree | 网络直径 Network diameter | 网络密度 Network density | 聚类系数 Clustering coefficient |
|---|---|---|---|---|
| Con | 10.196 | 6.46 | 0.101 | 0.754 |
| Pi | 18.358 | 6.57 | 0.195 | 0.824 |
表2 不同处理下丛枝菌根真菌群落的网络拓扑特性
Table 2 Topological properties of the arbuscular mycorrhizal fungi co-occurrence networks under different treatments
| 处理 Treatment | 平均度 Average degree | 网络直径 Network diameter | 网络密度 Network density | 聚类系数 Clustering coefficient |
|---|---|---|---|---|
| Con | 10.196 | 6.46 | 0.101 | 0.754 |
| Pi | 18.358 | 6.57 | 0.195 | 0.824 |
图5 2021年根系性状与巨孢囊霉科、类球囊霉科和球囊霉科相对丰度的关系。实线表示相关性显著(*, p < 0.05; **, p < 0.01), 阴影部分表示95%置信区间。
Fig. 5 Relationships between root traits and the relative abundances of Gigasporaceae (Giga), Paraglomeraceae (Para), and Glomeraceae in 2021. Con, ambient precipitation; Pi, precipitation increase. Solid lines indicate significant correlations (*, p < 0.05; **, p < 0.01), and shaded areas represent 95% confidence intervals.
图6 土壤湿度与2021年(A, B)和2022年(C, D)巨孢囊霉科、类球囊霉科和球囊霉科相对丰度的关系。实线表示相关性显著(p < 0.05), 阴影部分表示95%置信区间。
Fig. 6 Relationships between soil moisture and the relative abundances of Gigasporaceae (Giga), Paraglomeraceae (Para), and Glomeraceae in 2021 (A, B) and 2022 (C, D). Con, ambient precipitation; Pi, precipitation increase. Solid lines indicate significant correlations (p < 0.05), and shaded areas represent 95% confidence intervals.
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