Zhu Xinshu, Deng Yongcui, Huang Tao, Han Cheng, Chen Lei, Zhang Zhigang, Liu Keshao, Liu Yongqin, Huang Changchun
School of Geography, Nanjing Normal University, Nanjing, China.
Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing, China.
Front Microbiol. 2023 Mar 8;14:1118892. doi: 10.3389/fmicb.2023.1118892. eCollection 2023.
Microbial communities in freshwater lake sediments exhibit a distinct depth-dependent variability. Further exploration is required to understand their biodiversity pattern and microbial interactions in vertical sediments. In this study, sediment cores from two freshwater lakes, Mugecuo (MGC) and Cuopu (CP), on the Tibetan plateau were sampled and subsequently sliced into layers at a depth of every centimeter or half a centimeter. Amplicon sequencing was used to analyze the composition, diversity, and interaction of microbial communities. Results showed that sediment samples of both lakes could be clustered into two groups at a sediment depth of about 20 cm, with obvious shifts in microbial community compositions. In lake MGC, the richness component dominated β-diversity and increased with depth, indicating that the microbial communities in the deep layer of MGC was selected from the surface layer. Conversely, the replacement component dominated β-diversity in CP, implying a high turnover rate in the surface layer and inactive seed banks with a high variety in the deep layer. A co-occurrence network analysis showed that negative microbial interactions were prevalent in the surface layers with high nutrient concentrations, while positive microbial interactions were more common in the deep layers with low nutrient concentrations, suggesting that microbial interactions are influenced by nutrient conditions in the vertical sediments. Additionally, the results highlight the significant contributions of abundant and rare taxa to microbial interactions and vertical fluctuations of β-diversity, respectively. Overall, this work deepens our understanding of patterns of microbial interactions and vertical fluctuation in β-diversity in lake sediment columns, particularly in freshwater lake sediments from the Tibetan plateau.
淡水湖沉积物中的微生物群落呈现出明显的深度依赖性变化。需要进一步探索以了解其生物多样性模式以及垂直沉积物中的微生物相互作用。在本研究中,采集了青藏高原上两个淡水湖——木格措(MGC)和措普(CP)的沉积物岩芯,随后将其切成每厘米或半厘米深度的分层。采用扩增子测序分析微生物群落的组成、多样性和相互作用。结果表明,两个湖泊的沉积物样本在约20厘米的沉积物深度处可聚类为两组,微生物群落组成有明显变化。在木格措湖,丰富度成分主导β多样性并随深度增加,表明木格措湖深层的微生物群落是从表层筛选出来的。相反,替代成分在措普湖主导β多样性,这意味着表层的周转率高,而深层有高多样性的不活跃种子库。共现网络分析表明,在高营养浓度的表层,负向微生物相互作用普遍存在,而在低营养浓度的深层,正向微生物相互作用更为常见,这表明微生物相互作用受垂直沉积物中营养条件的影响。此外,结果突出了丰富和稀有分类群分别对微生物相互作用和β多样性垂直波动的重要贡献。总体而言,这项工作加深了我们对湖泊沉积物柱中微生物相互作用模式和β多样性垂直波动的理解,特别是对青藏高原淡水湖沉积物的理解。