植物生态学报

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不同沼泽湿地芦苇地上-地下性状对水分变化的响应

贾紫璇1,方涛1,张舒欣1,刘一凡1,赵微1,王荣2,昌海超3,郭允倩1,朱耀军4,罗芳丽1,于飞海5   

  1. 1. 北京林业大学
    2. 中国林业科学研究院 森林生态环境与保护研究所
    3. 北京林业大学生态与自然保护学院
    4. 中国林业科学研究院生态保护与修复研究所(湿地研究所)
    5. 台州学院
  • 收稿日期:2024-07-22 修回日期:2025-03-05 发布日期:2025-03-21

Responses of aboveground-belowground traits of Phragmites australis in different marsh wetlands to changes in soil moisture

  • Received:2024-07-22 Revised:2025-03-05

摘要: 芦苇(Phragmites australis)作为典型的根茎型多年生湿地植物,是沼泽湿地生态系统的重要组成部分。然而,随着全球气候变化以及湿地逐渐干旱化,芦苇的生长常常受到水分的限制。研究芦苇对水分变化的响应可为芦苇群落的保护和动态预测以及湿地植物异质生境下响应机制的研究提供理论依据。该研究以北方3个典型沼泽湿地——岱海湿地、科尔沁湿地、青铜峡水库的芦苇群落为对象,分析了高低土壤水分和其它环境因子对芦苇地上性状、地下性状及地上-地下性状关系的影响。结果表明:相对于低土壤水分,高土壤水分显著增加芦苇地上部分的生物量和比叶面积,显著降低芦苇根冠比;高土壤水分显著降低了芦苇的叶非结构性碳水化合物含量、茎的氮磷含量。高土壤水分显著增加了芦苇的根生物量、根表面积和根体积,显著降低了芦苇的根直径。土壤水分不影响根生物量与茎非结构性碳水化合物含量的正相关关系,但土壤水分的降低会逆转高土壤水分下根直径与叶氮含量的负相关关系,以及与叶非结构性碳水化合物含量、茎非结构性碳水化合物含量的正相关关系。高土壤水分下芦苇性状主要受土壤总氮、总磷影响;低土壤水分下芦苇性状主要受温度和降水影响,表明土壤水分可能通过间接影响土壤总氮含量、土壤总磷含量和温度,改变部分地上-地下性状的相关关系。综上,高土壤水分有利于芦苇地上部分和根系生长,但降低芦苇茎氮磷含量和叶非结构性碳水化合物含量。土壤水分可通过影响土壤氮磷含量和温度,间接影响芦苇的地上和地下性状及其关系。

关键词: 沼泽湿地, 湿地植物, 土壤水分, 植物性状, 地上-地下性状关系

Abstract: Aims Phragmites australis, a typical perennial rhizomatic wetland plant, is an important species of marsh wetland ecosystem. However, with the global climate change and the gradual drying of wetlands, the growth of P. australis is often limited by soil moisture. Standing the response of P. australis to changes in soil moisture can provide a theoretical basis for the protection and dynamic prediction of its community, as well as for research on the response mechanisms of wetland plants in heterogeneous habitats. Methods In this study, P. australis communities in three typical marsh wetlands in northern China, i.e., Daihai Wetland, Horqin Wetland and Qingtongxia Reservoir, were studied, and the effects of low and high soil moisture, and other environmental factors on the aboveground traits, belowground traits and their relationships of P. australis were analyzed. Important findings Compared with low soil moisture, high soil moisture significantly increased the aboveground biomass and specific leaf area, and significantly reduced the root to shoot ratio of P. australis. High soil moisture significantly reduced the contents of non-structural carbohydrates in leaves, and nitrogen and phosphorus in stems. High soil moisture significantly increased the root biomass, root surface area and root volume, and significantly decreased the root diameter of P. australis. Soil moisture did not affect the positive correlation between root biomass and stem non-structural carbohydrates content. However, the decrease in soil moisture reversed the negative correlation between root diameter and leaf nitrogen content under high soil moisture, as well as the positive correlations between root diameter and leaf non-structural carbohydrates content, and between root diameter and stem non-structural carbohydrates content. In high soil moisture areas, total soil nitrogen and total soil phosphorus were important factors that affected the aboveground and belowground traits of P. australis; in low soil moisture areas, temperature and precipitation were also important factors. Our results indicate that soil moisture may indirectly affect total soil nitrogen and total soil phosphorus and temperature to change the the correlations between some aboveground and belowground traits. In summary, high soil moisture was beneficial to the growth of aerial parts and roots of P. australis, but it reduced the contents of nitrogen and phosphorus in stems and the content of non-structural carbohydrates in leaves. Soil moisture can influence the aboveground and belowground traits and their relationships of P. australis, by indirectly affecting soil nitrogen and phosphorus contents, as well as temperature.

Key words: marsh wetland, wetland plants, soil moisture, plant traits, aboveground-belowground traits relationship