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青海湖河口及近岸湿地中甲烷营养菌群落特征及其理化驱动机制

Characteristics of methanotrophic communities and their physicochemical driving mechanisms in estuarine and nearshore wetlands of Qinghai Lake.

作者信息

Ji Wei, Ren Likai, Zhou Zhiyun, Yang Jianpeng, Yang Ziwei, Zhang Ni, Sun Jianqing, Chen Kelong, Chai Wenbo

机构信息

Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining 810008, China.

Lianyungang Academy of Agricultural Sciences, Lianyungang 222006, China.

出版信息

iScience. 2025 Jul 1;28(8):113040. doi: 10.1016/j.isci.2025.113040. eCollection 2025 Aug 15.

Abstract

Methanotrophic communities play a vital role in regulating methane fluxes in wetland ecosystems. This study examined the composition and environmental drivers of methanotrophs in estuarine and nearshore wetlands of the Qinghai Lake basin. Soil samples from six sites across three tributaries showed clear spatial and vertical variation in organic matter, nitrogen forms, and salinity. The Heima River estuarine wetland exhibited the highest methanotrophic diversity and functional potential. Dominant genera included , , and , with site-specific distributions. Redundancy analysis identified soil organic matter, nitrate nitrogen, pH, and electrical conductivity as key factors shaping community structure. These findings reveal how water-salt interactions and nutrient status influence methane-oxidizing microbes, offering insights into carbon cycling dynamics in high-altitude wetlands and supporting ecological restoration efforts in plateau regions.

摘要

甲烷营养群落对调节湿地生态系统中的甲烷通量起着至关重要的作用。本研究调查了青海湖流域河口和近岸湿地中甲烷氧化菌的组成及环境驱动因素。来自三条支流六个地点的土壤样本在有机质、氮形态和盐度方面呈现出明显的空间和垂直变化。黑马河河口湿地表现出最高的甲烷营养多样性和功能潜力。优势属包括 、 和 ,具有特定地点分布。冗余分析确定土壤有机质、硝态氮、pH值和电导率是塑造群落结构的关键因素。这些发现揭示了水盐相互作用和养分状况如何影响甲烷氧化微生物,为高海拔湿地的碳循环动态提供了见解,并为高原地区的生态恢复工作提供了支持。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5ac8/12283554/a3f86f42667c/fx1.jpg

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