Hu Anyi, Hou Liyuan, Yu Chang-Ping
Key Laboratory of Urban Pollutant Conversion, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, People's Republic of China.
Microb Ecol. 2015 Aug;70(2):322-35. doi: 10.1007/s00248-015-0597-4. Epub 2015 Mar 25.
Mounting evidence suggests that Archaea are widespread and abundant in aquatic and terrestrial habitats and play fundamental roles in global biogeochemical cycles, yet the pattern and its ecological drivers of biogeographic distribution of archaeal community in estuarine ecosystem are still not well understood. Here, we investigated planktonic and benthic archaeal communities in the human-impacted Jiulong River estuary (JRE), southern China by using real-time PCR (RT-PCR) and Illumina 16S ribosomal RNA (rRNA) amplicon sequencing. RT-PCR analysis indicated that Archaea accounted for an average of 0.79 and 5.31 % of prokaryotic biomass in water and sediment samples of the JRE, respectively. The diversity of planktonic archaeal community decreased gradually from the river runoff to seawater, whereas that of benthic community did not show the similar pattern. The results of taxonomic assignments indicated that Thaumarchaeota (Nitrosopumilus and Cenarchaeum), Methanocorpusculum, and Methanospirillum were significantly more abundant in planktonic than benthic communities, whereas the relative abundances of Miscellaneous Crenarchaeotic Group, Marine Benthic Group-B/-D, anaerobic methane-oxidizing Archaea -1/-2D, and South Africa Gold Mine Euryarchaeotic Group 1 were higher in sediments than in surface waters. Moreover, planktonic archaeal community composition varied significantly at broad and finer-scale taxonomic levels along the salinity gradient. Multivariate statistical analyses revealed that salinity is the main factor structuring the JRE planktonic but not benthic archaeal community at both total community and population level. SourceTrakcer analysis indicated that river might be a major source of archaea in the freshwater zone of the JRE. Overall, this study advances our understanding of the biogeographic patterns and its ecological drivers of estuarine archaeal communities.
越来越多的证据表明古菌在水生和陆地生境中广泛分布且数量丰富,在全球生物地球化学循环中发挥着重要作用,然而河口生态系统中古菌群落生物地理分布的模式及其生态驱动因素仍未得到很好的理解。在此,我们通过实时定量聚合酶链反应(RT-PCR)和Illumina 16S核糖体RNA(rRNA)扩增子测序,对受人类活动影响的中国南方九龙江河口(JRE)的浮游和底栖古菌群落进行了调查。RT-PCR分析表明,古菌分别占JRE水样和沉积物样品中总原核生物量的0.79%和5.31%。浮游古菌群落的多样性从河流径流到海水逐渐降低,而底栖古菌群落的多样性则没有呈现出类似的模式。分类学分析结果表明,奇古菌门(亚硝化侏儒菌属和泉古菌属)、甲烷微菌属和甲烷螺菌属在浮游群落中的丰度显著高于底栖群落,而杂项泉古菌组、海洋底栖类群B/-D、厌氧甲烷氧化古菌-1/-2D和南非金矿广古菌组1在沉积物中的相对丰度高于表层水体。此外,浮游古菌群落组成在较宽泛和较精细的分类水平上均随盐度梯度发生显著变化。多变量统计分析表明,在群落总体和种群水平上,盐度是构建JRE浮游古菌群落而非底栖古菌群落的主要因素。溯源分析表明,河流可能是JRE淡水区古菌的主要来源。总体而言,本研究增进了我们对河口古菌群落生物地理模式及其生态驱动因素的理解。