植物生态学报 ›› 2026, Vol. 50 ›› Issue (3): 731-741.DOI: 10.17521/cjpe.2025.0252 cstr: 32100.14.cjpe.2025.0252
陈淼1,2,3,4, 陈健1,2, 刘顺1,2, 许格希1,2, 冯秋红3,4, 史作民1,2,5,*(
)
收稿日期:2025-07-02
接受日期:2025-12-13
出版日期:2026-03-20
发布日期:2026-04-03
通讯作者:
*史作民(shizm@caf.ac.cn)基金资助:
CHEN Miao1,2,3,4, CHEN Jian1,2, LIU Shun1,2, XU Ge-Xi1,2, FENG Qiu-Hong3,4, SHI Zuo-Min1,2,5,*(
)
Received:2025-07-02
Accepted:2025-12-13
Online:2026-03-20
Published:2026-04-03
Contact:
*SHI Zuo-Min(shizm@caf.ac.cn)
Supported by:摘要:
外生菌根树木既通过细根直接吸收土壤中的氮(根途径), 也通过外生菌根真菌菌丝吸收土壤氮(菌丝途径)后转移到细根中。然而, 目前对于菌丝途径对外生菌根树木氮获取的相对贡献(ffungi)的量化估算仍具有较大的不确定性, 其关键影响因素亦不甚明确。该研究以青藏高原东缘岷江冷杉(Abies fargesii var. faxoniana)和糙皮桦(Betula utilis)为对象, 采用15N自然丰度法量化了菌丝途径对其氮获取的相对贡献, 并进一步分析了ffungi的关键影响因素。研究发现, 岷江冷杉和糙皮桦通过菌丝途径获取的氮在总氮吸收中的贡献与根途径相当, 菌丝途径对岷江冷杉总氮吸收的贡献率为33.6%-71.8%, 对糙皮桦的贡献率为41.6%-63.0%。此外, 土壤碳氮比、年平均温度及土壤pH是ffungi的关键影响因素。该研究为深入理解自然生态系统中外生菌根树木氮获取策略及其影响因素提供了新的思路和见解。
陈淼, 陈健, 刘顺, 许格希, 冯秋红, 史作民. 外生菌根真菌对青藏高原东缘岷江冷杉和糙皮桦氮获取的贡献及其影响因素. 植物生态学报, 2026, 50(3): 731-741. DOI: 10.17521/cjpe.2025.0252
CHEN Miao, CHEN Jian, LIU Shun, XU Ge-Xi, FENG Qiu-Hong, SHI Zuo-Min. Contribution and influencing factors of ectomycorrhizal fungi to nitrogen acquisition for Abies fargesii var. faxoniana and Betula utilis on the eastern Qingzang Plateau. Chinese Journal of Plant Ecology, 2026, 50(3): 731-741. DOI: 10.17521/cjpe.2025.0252
图1 研究区样点分布图。FTZ, 蜂桶寨; MYL, 米亚罗; SDG, 三达古; SPG, 松坪沟; WL, 卧龙。
Fig. 1 Location of the sampling sites in the study area. FTZ, Fengtongzhai; MYL, Miyaluo; SDG, Sandagu; SPG, Songpinggou; WL, Wolong.
图2 不同森林类型土壤氮浓度和同位素特征以及植物氮同位素特征(平均值±标准误)。DON, 可溶性有机氮含量; TDN, 土壤总溶解氮含量。δ15NTDN, 土壤总溶解的氮稳定同位素组成; δ15Nplant, 全株植物的氮稳定同位素组成。不同小写字母表示不同林型间在p < 0.05水平下存在显著差异。不同大写字母表示同一林型内不同形态氮含量在p < 0.05水平下存在显著差异。
Fig. 2 Soil nitrogen (N) concentration and isotopic characteristics and plant nitrogen isotopic characteristics in different forest types (mean ± SE). DON, dissolved organic nitrogen content; TDN, total dissolved nitrogen content. δ15NTDN, the stable nitrogen isotope value of soil total dissolved nitrogen; δ15Nplant, the stable nitrogen isotope value of whole-plant. Different lowercase letters denote significant differences between different forest types at p < 0.05. Different uppercase letters denote significant differences among different forms of N at p < 0.05.
| 森林类型 Forest type | 地点 Site | 不同形态氮含量 Different forms of nitrogen content (mg·kg-1) | 氮同位素特征 Nitrogen isotope characteristics (‰) | ||||
|---|---|---|---|---|---|---|---|
| NH4+-N | NO3--N | DON | TDN | δ15NTDN | δ15Nplant | ||
| 岷江冷杉林 Abies fargesii var. faxoniana forest | WL | 13.79 ± 2.79aB | 4.89 ± 0.79aA | 49.27 ± 3.12aA | 67.93 ± 4.83aB | 2.72 ± 0.64aA | -2.51 ± 0.35aABC |
| MYL | 27.70 ± 1.50aA | 0.75 ± 0.10bA | 53.95 ± 5.44aA | 82.39 ± 4.17aAB | 3.14 ± 0.62aA | -2.71 ± 0.37aBC | |
| FTZ | 24.94 ± 2.62aA | 1.25 ± 0.40bA | 67.71 ± 7.45aA | 93.90 ± 8.55aA | 3.48 ± 0.38aA | -1.59 ± 0.24aA | |
| SDG | 12.48 ± 0.41aB | 0.80 ± 0.17bA | 63.28 ± 8.13aA | 76.54 ± 7.93aAB | 0.93 ± 0.38bB | -2.07 ± 0.04bAB | |
| SPG | 6.72 ± 1.01aC | 3.35 ± 0.97aA | 52.54 ± 3.58aA | 62.60 ± 4.05aB | 3.16 ± 0.59aA | -3.27 ± 0.45aC | |
| 糙皮桦林 Betula utilis forest | WL | 9.09 ± 2.63aBC | 8.20 ± 1.79aB | 32.82 ± 6.16bC | 50.10 ± 7.95bB | 2.37 ± 0.14aAB | -1.35 ± 0.60aA |
| MYL | 27.42 ± 1.30aA | 5.51 ± 0.79aB | 55.28 ± 4.23aAB | 88.20 ± 3.16aA | 1.53 ± 0.60aB | -2.52 ± 0.22aBC | |
| FTZ | 14.18 ± 1.52bB | 10.73 ± 3.15aAB | 72.56 ± 8.35aA | 97.47 ± 5.70aA | 3.01 ± 0.61aAB | -1.90 ± 0.43aAB | |
| SDG | 13.97 ± 2.64aB | 13.63 ± 2.59aA | 51.76 ± 9.51aB | 79.35 ± 14.57aA | 2.42 ± 0.42aAB | -3.21 ± 0.16aC | |
| SPG | 4.93 ± 0.71aC | 5.49 ± 1.33aB | 26.17 ± 5.96bC | 36.58 ± 6.75bB | 3.53 ± 0.77aA | -1.75 ± 0.20bAB | |
表1 不同地点不同形态氮含量及氮同位素特征(平均值±标准误, n=4)
Table 1 Different forms of nitrogen content and nitrogen isotope characteristics in different sites (mean ± SE, n = 4)
| 森林类型 Forest type | 地点 Site | 不同形态氮含量 Different forms of nitrogen content (mg·kg-1) | 氮同位素特征 Nitrogen isotope characteristics (‰) | ||||
|---|---|---|---|---|---|---|---|
| NH4+-N | NO3--N | DON | TDN | δ15NTDN | δ15Nplant | ||
| 岷江冷杉林 Abies fargesii var. faxoniana forest | WL | 13.79 ± 2.79aB | 4.89 ± 0.79aA | 49.27 ± 3.12aA | 67.93 ± 4.83aB | 2.72 ± 0.64aA | -2.51 ± 0.35aABC |
| MYL | 27.70 ± 1.50aA | 0.75 ± 0.10bA | 53.95 ± 5.44aA | 82.39 ± 4.17aAB | 3.14 ± 0.62aA | -2.71 ± 0.37aBC | |
| FTZ | 24.94 ± 2.62aA | 1.25 ± 0.40bA | 67.71 ± 7.45aA | 93.90 ± 8.55aA | 3.48 ± 0.38aA | -1.59 ± 0.24aA | |
| SDG | 12.48 ± 0.41aB | 0.80 ± 0.17bA | 63.28 ± 8.13aA | 76.54 ± 7.93aAB | 0.93 ± 0.38bB | -2.07 ± 0.04bAB | |
| SPG | 6.72 ± 1.01aC | 3.35 ± 0.97aA | 52.54 ± 3.58aA | 62.60 ± 4.05aB | 3.16 ± 0.59aA | -3.27 ± 0.45aC | |
| 糙皮桦林 Betula utilis forest | WL | 9.09 ± 2.63aBC | 8.20 ± 1.79aB | 32.82 ± 6.16bC | 50.10 ± 7.95bB | 2.37 ± 0.14aAB | -1.35 ± 0.60aA |
| MYL | 27.42 ± 1.30aA | 5.51 ± 0.79aB | 55.28 ± 4.23aAB | 88.20 ± 3.16aA | 1.53 ± 0.60aB | -2.52 ± 0.22aBC | |
| FTZ | 14.18 ± 1.52bB | 10.73 ± 3.15aAB | 72.56 ± 8.35aA | 97.47 ± 5.70aA | 3.01 ± 0.61aAB | -1.90 ± 0.43aAB | |
| SDG | 13.97 ± 2.64aB | 13.63 ± 2.59aA | 51.76 ± 9.51aB | 79.35 ± 14.57aA | 2.42 ± 0.42aAB | -3.21 ± 0.16aC | |
| SPG | 4.93 ± 0.71aC | 5.49 ± 1.33aB | 26.17 ± 5.96bC | 36.58 ± 6.75bB | 3.53 ± 0.77aA | -1.75 ± 0.20bAB | |
图3 根途径和菌丝途径对岷江冷杉和糙皮桦氮获取的贡献(平均值±标准误)。FTZ, 蜂桶寨; MYL, 米亚罗; SDG, 三达古; SPG, 松坪沟; WL, 卧龙。不同小写字母表示在给定地点的不同氮吸收途径之间的显著差异(p < 0.05)。不同大写字母表示在给定森林类型的不同地点之间的显著差异(p < 0.05)。
Fig. 3 Contributions of root pathway and mycelia pathway to Abies fargesii var. faxonian and Betula utilis nitrogen acquisition (mean ± SE). FTZ, Fengtongzhai; MYL, Miyaluo; SDG, Sandagu; SPG, Songpinggou; WL, Wolong. Different lowercase letters denote significant differences between different nitrogen (N) uptake pathways in a given site at p < 0.05. Different uppercase letters denote significant differences among different sites in a given forest type at p < 0.05.
图4 同一地点岷江冷杉和糙皮桦的ffungi差异(平均值±标准误)。ffungi, 菌根真菌对树木氮获取的贡献率。FTZ, 蜂桶寨; MYL, 米亚罗; SDG, 三达古; SPG, 松坪沟; WL, 卧龙。不同小写字母表示存在显著差异(p < 0.05)。
Fig. 4 Difference in ffungi between Abies fargesii var. faxoniana and Betula utilis at the same site (mean ± SE). ffungi, the contribution rate of the mycelia pathway to tree nitrogen acquisition. FTZ, Fengtongzhai; MYL, Miyaluo; SDG, Sandagu; SPG, Songpinggou; WL, Wolong. Different lowercase letters denote significant differences at p < 0.05.
图5 ffungi与气候因子、土壤特性、树木年龄之间的关系。AGE, 树木年龄; C:N, 土壤碳氮比; DON, 可溶性有机氮含量; ffungi, 菌根真菌对树木氮获取的贡献率; MAP, 年降水量; MAT, 年平均气温; SBD, 土壤容重; SWC, 土壤含水量。
Fig. 5 Relationship between ffungi and climate factors, soil characteristics, and tree age. AGE, tree age; C:N, soil carbon to nitrogen ratio; DON, dissolved organic nitrogen content; ffungi, the contribution rate of the mycelia pathway to tree nitrogen acquisition; MAP, mean annual precipitation; MAT, mean annual air temperature; SBD, soil bulk density; SWC, soil water content.
图6 解释变量对ffungi变异的相对重要性。AGE, 树木年龄; C:N, 土壤碳氮比; DON, 可溶性有机氮含量; ffungi, 菌根真菌对树木氮获取的贡献率; MAP, 年降水量; MAT, 年平均气温; SBD, 土壤容重; SWC, 土壤含水量。
Fig. 6 Relative importance of explanatory variables to ffungi. AGE, tree age; C:N, soil carbon to nitrogen ratio; DON, dissolved organic nitrogen content; ffungi, the contribution rate of the mycelia pathway to tree nitrogen acquisition; MAP, mean annual precipitation; MAT, mean annual air temperature; SBD, soil bulk density; SWC, soil water content.
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