Chen Ying, Qiu Kairui, Zhong Ziyuan, Zhou Tao
School of Biotechnology, Guilin Medical University, Guilin, China.
Front Microbiol. 2021 Sep 3;12:675665. doi: 10.3389/fmicb.2021.675665. eCollection 2021.
Archaea are ubiquitous and play an important role in elemental cycles in Earth's biosphere; but little is known about their diversity, distribution, abundance, and impact in karst environments. The present study investigated the effect of environmental factors on the variability of archaeal communities in the sediment of the Huixian karst wetland, the largest karst wetland in South China. Sediment cores were obtained from four sampling sites with different water depths and macrophyte inhabitants in both the winter of 2016 and the summer of 2018. The community analysis was based on PacBio sequencing and quantitative PCR of the archaeal 16S rRNA gene. The results showed that Euryarchaeota (57.4%) and Bathyarchaeota (38.7%) were dominant in all the samples. Methanogenic Methanosarcinales (25.1%) and Methanomicrobiales (13.7%), and methanotrophic archaea ANME-2d (9.0%) were the dominant Euryarchaeota; MCG-11 (16.5%), MCG-6 (9.1%), and MCG-5b (5.5%) were the dominant Bathyarchaeota. The community composition remained stable between summer and winter, and the vertical distributions of the archaeal phyla conformed to two patterns among the four sampling sites. In the winter samples, the archaeal 16S rRNA gene abundance was approximately 1.0E+10 copies/g of wet sediment and the Shannon index was 7.3±5, which were significantly higher than in the summer samples and in other karst environments. A correlation analysis showed that the moisture content and pH were the factors that mostly affected the archaeal communities. The prevalence of nitrate in the summer may be a key factor causing a significant decrease in archaeal abundance and diversity. Two features specific to karst environments, calcium-richness and weak alkalescence of the water supplies, may benefit the prevalence of bathyarchaeotal subgroups MCG-11, MCG-5b, and MCG-6. These results suggest that in karst wetlands, most of the archaea belong to clades that have significant roles in carbon turnover; their composition remains stable, but their abundance and diversity vary significantly from season to season.
古菌广泛存在,在地球生物圈的元素循环中发挥着重要作用;但对于它们在喀斯特环境中的多样性、分布、丰度和影响,人们却知之甚少。本研究调查了环境因素对中国南方最大的喀斯特湿地——会仙喀斯特湿地沉积物中古菌群落变异性的影响。在2016年冬季和2018年夏季,从四个具有不同水深和大型植物群落的采样点获取了沉积物岩芯。群落分析基于古菌16S rRNA基因的PacBio测序和定量PCR。结果表明,广古菌门(57.4%)和深古菌门(38.7%)在所有样本中占主导地位。产甲烷的甲烷八叠球菌目(25.1%)和甲烷微菌目(13.7%),以及甲烷营养古菌ANME-2d(9.0%)是广古菌门中的优势类群;MCG-11(16.5%)、MCG-6(9.1%)和MCG-5b(5.5%)是深古菌门中的优势类群。群落组成在夏季和冬季之间保持稳定,古菌门的垂直分布在四个采样点中符合两种模式。在冬季样本中,古菌16S rRNA基因丰度约为1.0E+10拷贝/克湿沉积物,香农指数为7.3±5,显著高于夏季样本和其他喀斯特环境。相关性分析表明,含水量和pH值是对古菌群落影响最大的因素。夏季硝酸盐的普遍存在可能是导致古菌丰度和多样性显著下降的关键因素。喀斯特环境特有的两个特征,即水源的富钙性和弱碱性,可能有利于深古菌门亚群MCG-11、MCG-5b和MCG-6的普遍存在。这些结果表明,在喀斯特湿地中,大多数古菌属于在碳周转中具有重要作用的进化枝;它们的组成保持稳定,但其丰度和多样性随季节变化显著。