Soil water content and pH drive archaeal distribution patterns in sediment and soils of water-level-fluctuating zones in the East Dongting Lake wetland, China

被引:13
作者
Li, Wei [1 ,2 ,3 ,4 ]
Feng, Defeng [5 ]
Yang, Gang [6 ]
Deng, Zhengmiao [7 ]
Rui, Junpeng [1 ,2 ]
Chen, Huai [1 ,2 ]
机构
[1] Chinese Acad Sci, Chengdu Inst Biol, Key Lab Mt Ecol Restorat & Bioresource Utilizat, Chengdu 610041, Sichuan, Peoples R China
[2] Chinese Acad Sci, Chengdu Inst Biol, Ecol Restorat Biodivers Conservat Key Lab Sichuan, Chengdu 610041, Sichuan, Peoples R China
[3] Yunnan Univ, Sch Ecol & Environm Sci, Kunming 650091, Yunnan, Peoples R China
[4] Yunnan Univ, Yunnan Key Lab Plateau Mt Ecol & Restorat Degrade, Kunming 650091, Yunnan, Peoples R China
[5] Chinese Acad Forestry, Res Inst Resource Insects, Kunming 650224, Yunnan, Peoples R China
[6] Southwest Univ Sci & Technol, Sch Life Sci & Engn, Mianyang 621010, Sichuan, Peoples R China
[7] Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, Changsha 410125, Hunan, Peoples R China
基金
中国国家自然科学基金;
关键词
Abundance; Diversity; pH; Water content; Wetland; AMMONIA-OXIDIZING ARCHAEA; BACTERIAL COMMUNITY STRUCTURE; NITROSOSPHAERA-VIENNENSIS; ALTITUDINAL DISTRIBUTION; MICROBIAL COMMUNITIES; SPATIAL-DISTRIBUTION; DIVERSITY; ABUNDANCE; TEMPERATURE; METHANOGEN;
D O I
10.1007/s11356-019-06109-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Archaea play a vital role in Earth's geochemical cycles, but the factors that drive their distribution between sediments and water-level-fluctuating zones in the East Dongting Lake (EDL) wetland are poorly understood. Here, we used Illumina MiSeq to investigate the variation in the soil archaeal community structure and diversity among sediments and four water-level-fluctuating zones (mudflat, sedge, sedge-Phragmites, and Phragmites) in the EDL wetland. Diverse archaeal assemblages were found in our study, Crenarchaeota, Euryarchaeota, and ammonia-oxidizing and methanogenic subset were the dominant groups, and all their abundances shifted from sediment to water-level-fluctuating zones. The principal coordinates analysis and cluster analysis showed that the overall archaeal community structure was separated into two clusters: cluster I contained nine samples from sediment, mudflat, and sedge zones, whereas cluster II contained six samples from sedge-Phragmites and Phragmites zones. Archaeal diversity was significantly highest in sediment and lowest in Phragmites zone soils. The Mantel test showed that the variation in archaeal community structure was significantly positively correlated with soil water content and pH. The relative abundances of Crenarchaeota and Nitrososphaerales decreased with soil water content, while Euryarchaeota and Methanomicrobiales increased with soil water content. The relative abundance of Methanomicrobiales significantly decreased with pH (R-2 = 0.34-0.48). Chao 1, observed operational taxonomic units, Shannon index, and Simpson index all correlated significantly positively with water content (R-2 = 0.40-0.60), while Shannon and Simpson indexes both correlated significantly negatively with pH (R-2 = 0.20-0.37). Our results demonstrated that the variations in the archaeal community structure were markedly driven by soil water content and pH in the EDL wetland. Our findings suggested that archaeal communities shifted among sediment and four water-level-fluctuating zones, highlighting that the spatiotemporal heterogeneity of greenhouse gas flux in small scale should be taken into account for accurate prediction of greenhouse gas emissions in the Dongting Lake area, especially on the background of climate change and human activities.
引用
收藏
页码:29127 / 29137
页数:11
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