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生态学杂志 ›› 2026, Vol. 45 ›› Issue (9): 2913-2921.doi: 10.13292/j.1000-4890.202609.026

• ·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

莆田木兰溪入海河口蓝碳生态系统碳储量

吕静1,雷鹏2,陈恩1,王聪敏1,陈鹭真2*,吴秋华1,刘耀辉1,陈强1   

  1. 1福建省水利水电勘测设计研究院有限公司, 福州 350001; 2厦门大学环境与生态学院, 福建厦门 361102)
  • 出版日期:2026-09-10 发布日期:2026-09-07

Blue carbon stocks in the estuary of Mulan River in Putian City.

LYU Jing1, LEI Peng2, CHEN En1, WANG Congmin1, CHEN Luzhen2*, WU Qiuhua1, LIU Yaohui1, CHEN Qiang1   

  1. (1Fujian Provincial Investigation, Design & Research Institute of Water Conservancy & Hydropower Co., Ltd., Fuzhou 350001, China; 2College of the Environment and Ecology, Xiamen University, Xiamen 361102, Fujian, China).

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

摘要: 为探明莆田市木兰溪入海河口蓝碳生态系统植被结构及碳汇功能,对该区域修复5年的红树林和盐沼群落开展野外调查、沉积物采样与室内测定,结合植被异速生长方程和碳密度测算方法,定量分析不同植被群落的碳储量。结果表明:研究区红树林和盐沼总碳储量分别为8158.57和5289.62 t C,重点研究的3种红树植物群落中,白骨壤(Avicennia marina)碳密度最高,为121.03 t C·hm-2,其次为秋茄(Kandelia obovata),为100.87 t C·hm-2,桐花树(Aegiceras corniculatum)最低,为98.07 t C·hm-2;在盐沼植物群落中,芦苇(Phragmites australis)碳密度为99.46 t C·hm-2,盐地碱蓬(Suaeda salsa)和南方碱蓬(Suaeda australis)组成的碱蓬群落为94.03 t C·hm-2。从碳库构成看,红树和盐沼植物群落均以沉积物碳库为主,其碳密度分别为82.54~97.23和93.10~94.32 t C·hm-2,明显高于植被和枯落层碳密度。整体来看,该修复区红树林碳密度低于全国平均水平和天然红树林水平,群落仍处于修复初期;对比国内滨海湿地,研究区盐沼沉积物碳密度处于中等水平,但植被碳密度相对偏低。研究结果可为开展滨海湿地生态修复实践和区域碳汇能力评估提供参考。


关键词: 红树林, 盐沼, 碳密度, 碳库构成, 沉积物碳库

Abstract: To investigate vegetation structure and carbon sink function of blue carbon ecosystems at the Mulan River estuary in Putian City, we conducted field surveys, sediment sampling, and laboratory analyses on mangrove and salt marsh communities that had been restored for five years. Combined with vegetation allometric growth equations and carbon density estimation methods, carbon storage of different communities was quantitatively analyzed. The results showed that the total carbon stocks of mangroves and salt marshes reached 8158.57 and 5289.62 t C, respectively. Among the three mangrove species investigated, Avicennia marina exhibited the highest carbon density (121.03 t C·hm-2), followed by Kandelia obovata (100.87 t C·hm-2), while Aegiceras corniculatum was the lowest (98.07 t C·hm-2). In the salt marsh plant communities, carbon density was 99.46 t C·hm-2 for Phragmites australis and 94.03 t C·hm-2 for Suaeda community. In terms of carbon pool composition, both mangrove and salt marsh communities were dominated by sediment carbon pools, with carbon density of 82.54-97.23 and 93.10-94.32 t C·hm-2, respectively, which were significantly higher than those of vegetation and litter carbon pools. Overall, the carbon density of the restored mangroves was lower than the national average and the level of natural mangroves, indicating that the communities were still at the early stages of restoration. Compared with other coastal wetlands in China, the sediment carbon density of salt marshes in the study area was at a moderate level, while vegetation carbon density was relatively low. These findings provide a scientific reference for the ecological restoration practices in coastal wetlands and the assessment of regional carbon sequestration capacity.

Key words: mangrove, salt marsh, carbon density, carbon pool composition, sediment carbon pool