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生态学杂志 ›› 2024, Vol. 43 ›› Issue (6): 1747-1755.doi: 10.13292/j.1000-4890.202406.034

• 湿地生态 • 上一篇    下一篇

四川南莫且湿地国家级自然保护区沼泽湿地景观格局变化

吕旭湘1,苟安颖2,陈章敏1,张塔星1,谭进波1*,冉江洪1*
  

  1. 1四川大学生命科学学院, 生物资源与生态环境教育部重点实验室, 成都 610065; 2四川南莫且高原湿地自然保护区管理处, 四川壤塘 624300)

  • 出版日期:2024-06-10 发布日期:2024-06-18

Landscape pattern change of marsh in the Nanmoqie Wetland National Nature Reserve of Sichuan Province.

LYU Xuxiang1, GOU Anying2, CHEN Zhangmin1, ZHANG Taxing1, TAN Jinbo1*, RAN Jianghong1*   

  1. (1Key Laboratory of Bio-Resources and Eco-Environment of Ministry of Education, College of Life Sciences, Sichuan University, Chengdu 610065, China; 2Sichuan Nanmoqie Plateau Wetland Nature Reserve Administrative Office, Rangtang 624300, Sichuan, China).

  • Online:2024-06-10 Published:2024-06-18

摘要: 高寒湿地是青藏高原典型的湿地类型,具有重要的生物多样性维持和水源涵养作用,了解其景观格局变化及其影响因素对我国高寒湿地的保护与恢复具有重要意义。本研究基于GEE和Landsat卫星影像,采用随机森林分类方法提取了1987—2022年12期四川南莫且湿地国家级自然保护区沼泽湿地分布信息,分析了沼泽湿地景观格局时空变化及其影响因素。结果表明:(1)保护区沼泽湿地面积先减少再增加,整体减少了10.29%;(2)沼泽湿地与草甸的面积转换最剧烈,沼泽湿地累计向草甸转移4349.44 hm2;(3)沼泽湿地重心先向东北再向西南方向迁移,沼泽湿地分布范围整体向西南方向迁移;(4)沼泽湿地景观格局表现为破碎化程度先下降再升高,连通性先升高再下降,斑块形状趋于复杂,湿地景观趋向离散化发展;(5)生长季累积降水量、生长季均温是影响保护区沼泽湿地变化的主要影响因素。研究结果可为保护区高寒湿地的保护与恢复以及青藏高原高寒湿地生态安全建设提供科学依据。


关键词: 沼泽湿地, 景观格局变化, 保护区, 青藏高原

Abstract: Alpine wetlands are typical wetland types on the Qinghai-Tibet Plateau, playing important roles in biodiversity maintenance and water conservation. Understanding the changes and driving factors for their landscape pattern is of great significance for the conservation and restoration of alpine wetlands in China. Based on GEE and Landsat satellite images, we used the random forest classification method to extract information on the distribution of marsh in the Sichuan Nanmoqie Wetland National Nature Reserve, for 12 periods from 1987 to 2022, and analyzed the spatial and temporal marsh landscape patterns and the driving factors. The results showed that: (1) the area of marsh first decreased and then increased, with an overall decrease of 10.29%; (2) the area conversion between marsh and meadow was highest, with a cumulative shift of 4349.44 hm2 from marsh to meadow; (3) the centroid of marsh moved to the northeast first and then to the southwest, and the distribution range of marsh moved to the southwest as a whole; (4) the degree of fragmentation decreased and then increased, and the connectivity increased and then decreased instead. The shape of patches tended to be complex, and the landscape tended to develop from a compact state to a dispersed state; (5) the cumulative precipitation and average temperature during the growing season were the main factors affecting the pattern of marsh distribution. The results can provide a scientific basis for the conservation and restoration of alpine wetlands in the reserve and for the ecological security construction of alpine wetlands on the Qinghai-Tibet Plateau.


Key words: marsh, landscape pattern change, nature reserve, Qinghai-Tibet Plateau