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应用生态学报 ›› 2025, Vol. 36 ›› Issue (3): 762-770.doi: 10.13287/j.1001-9332.202503.008

• 研究论文 • 上一篇    下一篇

岩溶区不同石漠化生境优势木本植物叶片功能性状变异及适应策略

李梦妮, 蒋勇军*, 程钰瑞, 吴泽, 贺秋芳, 李佳彬, 赵春峰, 钱凤   

  1. 西南大学地理科学学院/岩溶环境重庆市重点实验室, 重庆 400715
  • 收稿日期:2024-11-08 接受日期:2025-01-19 出版日期:2025-03-18 发布日期:2025-05-15
  • 通讯作者: * E-mail: jiangjyj@swu.edu.cn
  • 作者简介:李梦妮, 女, 1999年生, 硕士研究生。主要从事岩溶植物生态研究。E-mail: Limengni0423@163.com
  • 基金资助:
    西南大学创新研究2035先导计划项目(SWU-XDZD22003)、重庆市硕士研究生科研创新项目(CYS23195)和西南大学实验技术研究项目(SYJ2025016)

Variation of leaf functional traits and adaptive strategies of dominant woody species in rocky desertification habitats in karst area

LI Mengni, JIANG Yongjun*, CHENG Yurui, WU Ze, HE Qiufang, LI Jiabin, ZHAO Chunfeng, QIAN Feng   

  1. School of Geographical Sciences, Southwest University/Chongqing Key Laboratory of Karst Environment, Chongqing 400715, China
  • Received:2024-11-08 Accepted:2025-01-19 Online:2025-03-18 Published:2025-05-15

摘要: 为明确岩溶区优势木本植物叶片性状对不同石漠化生境土壤特性的响应,本研究运用以空间代替时间的方法,研究典型原生林(石漠化特征极弱的石漠化前期)、次生林生境(石漠化特征较弱的石漠化中期)和石漠化生境(石漠化特征较高的石漠化后期)5种优势乔木和3种优势灌木的9种叶片功能性状特征及变异程度,分析其对生境变化的适应策略。结果表明: 相较于原生林生境,石漠化生境的土壤含水量显著降低60.4%,土壤C和N含量、C:N及N:P分别显著降低72.8%、35.8%、55.1%和56.7%。3种生境中,优势乔木的叶片含水量和比叶面积均低于灌木,叶干物质含量和叶C含量高于灌木,其中,比叶面积变异最大,叶C含量变异最小,且灌木叶性状总变异幅度高于乔木。叶片性状间具有普遍的相关性,比叶面积、叶片含水量与叶干物质含量呈显著负相关。土壤含水量对叶片性状的解释度为48.6%,是影响岩溶优势木本植物变异的主要土壤因子。在干旱贫瘠的石漠化生境,植物叶片呈现出高叶片含水量、比叶面积,低叶片厚度、叶干物质含量、叶C含量和叶N:P的性状组合,采取“快速投资-收益”的获取型资源利用策略,而相对湿润多养分的原生林生境呈现出与石漠化生境相反的性状组合,采取“慢速投资-收益”的保守型资源利用策略。

关键词: 岩溶区, 石漠化, 叶片功能性状, 土壤因子, 适应策略

Abstract: To clarify the response of leaf functional traits of dominant woody plants in karst areas to variations of soil characteristics across different rocky desertification habitats, we used the method of substituting space for time to examine the characteristics and variation of nine leaf functional traits of five dominant tree species and three domi-nant shrub species in typical primary forest (the early stage of rocky desertification with extremely weak rocky desertification characteristics), secondary forest habitat (the middle stage of rocky desertification with weak rocky desertification characteristics), and rocky desertification habitat (the late stage of rocky desertification with high rocky desertification characteristics), and analyzed the adaptation strategies of those species to habitat change. The results showed that compared with the primary forest habitat, soil water content in the rocky desertification habitat decreased significantly by 60.4%, and soil carbon and nitrogen contents, C:N, and N:P decreased significantly by 72.8%, 35.8%, 55.1% and 56.7%, respectively. Across the three habitats, leaf water content and specific leaf area of dominant tree species were lower than those of shrub species, while leaf dry matter content and leaf carbon content were higher. Among these traits, the variation of specific leaf area was the largest, and that of leaf carbon content was the smallest. The overall variations of leaf traits of shrubs were higher than that of tree species. There were general correlations among leaf traits. The specific leaf area and leaf water content were significantly negatively correlated with leaf dry matter content. Soil water content accounted for 48.6% of the variation in leaf traits, being the main soil factor affecting the variation of karst dominant woody plants. In the dry and barren rocky desertification habitat, leaves presented a combination of high leaf water content, high specific leaf area, low leaf thickness, low leaf dry matter content, low leaf carbon content and low leaf N:P. They adopted a “fast investment-benefit” resource acquisition strategy. In contrast, the combination of leaf traits in the relatively humid and nutrient-rich primary forest habitat was opposite to that in the rocky desertification habitat, adopting a “slow investment-benefit” resource conservative strategy.

Key words: karst area, rocky desertification, leaf functional trait, soil factor, adaptive strategy