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生态学杂志 ›› 2026, Vol. 45 ›› Issue (9): 2867-2874.doi: 10.13292/j.1000-4890.202609.025

• ·红树林湿地生态学专栏·(专栏组织专家:曹文志、王文卿、宋长春) • 上一篇    下一篇

海桑属红树植物果实发育中矿质元素的积累规律

刘超1,2,3,张林2,3,4,汤燕娜2,王文卿2,3*   

  1. 1浙江海洋大学水产学院, 浙江舟山 316022; 2厦门大学环境与生态学院, 福建厦门 361102; 3福建台湾海峡海洋生态系统国家野外科学观测研究站(厦门大学), 福建漳州 363000; 4北京大学深圳研究生院环境与能源学院, 广东深圳 518055)
  • 出版日期:2026-09-10 发布日期:2026-09-07

Patterns of mineral element accumulation during fruit development in mangrove species of Sonneratia.

LIU Chao1,2,3, ZHANG Lin2,3,4, TANG Yanna2, WANG Wenqing2,3*   

  1. (1School of Fishery, Zhejiang Ocean University, Zhoushan 316022, Zhejiang, China; 2College of the Environment & Ecology, Xiamen University, Xiamen 361102, Fujian, China; 3National Observation and Research Station for the Taiwan Strait Marine Ecosystem, Xiamen University, Zhangzhou 363000, Fujian, China; 4School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, Guangdong, China).

  • Online:2026-09-10 Published:2026-09-07

摘要: 为揭示红树植物果实发育过程中矿质元素的积累规律,以海南清澜港5种海桑属(Sonneratia)红树植物为对象,测定果实发育过程中Na、K、Ca、Mg和Cl含量,采用幂函数模型分析矿质元素浓度和总量与果实质量之间的关系。结果表明,随着果实质量增加,各矿质元素浓度均显著下降,而总量持续增加。矿质元素总量与果实质量均呈显著异速生长关系,并表现为负异速生长(0.61<b<0.93),表明矿质元素积累速率低于果实质量增长速率。不同功能矿质元素表现出差异化配置,其中Ca具有较强保守性,而Na、K和Cl等渗透调节元素具有更高可塑性;Cl和Mg的种间差异明显。研究表明,海桑属果实发育过程中矿质元素积累普遍遵循负异速生长规律,不同功能元素的分配策略反映了结构构建与盐适应需求之间的资源权衡,表明繁殖体阶段的矿质元素配置可能是红树植物盐适应策略的重要组成部分。


关键词: 红树林, 繁殖体发育, 异速生长关系, 矿质元素分配, 盐适应

Abstract: To elucidate the patterns of mineral element accumulation during fruit development in mangrove plants, we measured the concentrations of Na, K, Ca, Mg, and Cl throughout fruit development of five Sonneratia species from Qinglan Harbor, Hainan, China. Power-function models were used to analyze the relationships between mineral element concentrations, total contents, and fruit mass. The results showed that the concentrations of all mineral elements decreased with increasing fruit mass, whereas their total contents continuously increased. There were significant allometric relationships between total mineral element content and fruit mass, all exhibiting negative allometry (0.61<b<0.93), indicating that mineral element accumulation increased at a slower rate than fruit mass. Different functional mineral elements displayed distinct allocation patterns. Ca exhibited relatively conservative allocation, whereas the osmoregulatory elements Na, K, and Cl showed greater plasticity. In addition, Cl and Mg exhibited pronounced interspecific variation. These findings demonstrate that mineral element accumulation during fruit development in Sonneratia generally follows negative allometric growth patterns. The differential allocation strategies of functional mineral elements reflect trade-offs between structural construction and salt-adaptation requirements, suggesting that mineral element allocation during the propagule stage may contribute to the adaptation of mangrove plants to saline environments.

Key words: mangrove, propagule development, allometric relationship, mineral element allocation, salinity adaptation