滨海湿地不同水盐生境下芦苇生态化学计量特征变化及其环境解释
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山东省自然科学基金面上项目(ZR2020MD007);国家自然科学基金面上项目(41971126)


Variation in ecological stoichiometric characteristics of Phragmites australis under different water-salt environments and associated environmental explanation in coastal wetland
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    摘要:

    全球变暖后的冰川融化导致海平面上升,会进一步影响滨海湿地的地下水位和土壤水盐条件,明确滨海湿地植物应对土壤水盐环境变化的生态响应策略,可为滨海湿地植被的保护和恢复提供重要理论依据。因而,选择黄河三角洲滨海湿地优势植物芦苇为研究对象,通过调查不同地下水位梯度下芦苇的化学计量特征与土壤理化指标,探讨芦苇化学计量特征与土壤环境因子的响应关系。结果表明:(1)生长季内芦苇叶片N含量与N/P均表现为降低的趋势。生长季中期,芦苇叶片14 < N/P < 16,表明该地区芦苇生长受N和P共同限制。芦苇群落土壤剖面由表层向下C、N、P含量及N/P均表现为逐渐降低的趋势。芦苇群落土壤C、N含量均显著低于全国土壤C、N含量的平均值,但是土壤P含量与全国平均值比较接近,说明本地区土壤N含量相对缺乏,而P含量相对丰富。相关分析表明,叶片C含量与土壤N含量存在极显著正相关关系(P < 0.01),叶片N含量与地下水位存在显著负相关关系(P < 0.05),叶片P含量与土壤电导率之间存在显著正相关关系(P < 0.05),叶片P含量与土壤C、N、P均存在显著相关关系,而叶片C/P、叶片N/P与土壤C、N、P也均存在显著相关关系。冗余分析表明,第一轴的环境因子解释量可达73.22%。相关分析结合冗余分析结果表明,土壤N含量、土壤P含量、土壤电导率及地下水位是影响芦苇生态化学计量特征的重要驱动因素。

    Abstract:

    The melting of glaciers as a result of continued global warming is raising sea levels and further affecting groundwater levels and soil water and salt conditions in coastal wetlands. In recent years, studies on ecological stoichiometry have increased rapidly. Relationships between ecological stoichiometry indicators of plants and soils have been widely investigated. Understanding the ecological response strategies of plants to soil water and salt environment in coastal wetland could provide important theoretical basis for the protection and restoration of coastal wetland vegetation. Therefore, the dominant plant Phragmites australis in coastal wetland was selected as the research object. By investigating the leaf C/N/P stoichiometric characteristics of Phragmites australias and soil under different groundwater levels in the Yellow River Delta, this study analyzed the coupling relationship between the stoichiometric characteristics of Phragmites australias and soil environmental factors. The results showed that: (1) During the growing season, both the leaf N content and leaf N/P of Phragmites australias showed a decreasing trend. In the middle of the growing season, the leaf N/P ratio of Phragmites australias was between 14 and 16, indicating that the growth of Phragmites australias in this area was jointly limited by N and P. The soil C, N, P content and N/P in the Phragmites australias community all showed a decrease trend from the surface to the bottom of soil profile. The soil C and N content in the Phragmites australias community was significantly lower than the average soil C and N content within China. However, the soil P content is relatively close to the average soil P content within China, indicating that the soil N content in this region is relatively lacking, while the P content is relatively abundant. Correlation analysis showed that there was a highly significant positive correlation between leaf C content and soil N content (P < 0.01), and a significant negative correlation between leaf N content and groundwater level (P < 0.05). There was a significant positive correlation between leaf P content and soil conductivity (P < 0.05). There were significant or extremely significant correlations between leaf P content and soil element content (C, N or P), and there were also significant correlations between leaf element ratio (C/P or N/P) and soil element content (C, N or P). Redundancy analysis showed that the explanatory power of environmental factors for the first axis could reach 73.22%. Correlation analysis combined with redundancy analysis indicated that soil P content, soil N content, soil conductivity, and groundwater level were important driving factors affecting the ecological stoichiometric characteristics of Phragmites australias.

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董林水,刘京涛,宋爱云.滨海湿地不同水盐生境下芦苇生态化学计量特征变化及其环境解释.生态学报,2025,45(1):147~156

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