Whether interstitial space features were the main factors affecting sediment microbial community structures in Chaohu Lake

• Published in: Frontiers in microbiology Vol. 13; p. 1024630
• Main Authors: Lu, Xiang, Zhou, Xiaotian, von Sperber, Christian, Xu, Yaofei, Wei, Zhipeng, Li, Siyan, Ruan, Aidong
• Format: Journal Article
• Language: English
• Published: Switzerland Frontiers Media S.A 14-12-2022
• Subjects: gas space; microbial community structures; Microbiology; particle features; sediment depth; total interstitial space; volumetric water content; total interstitial space; sediment depth; gas space; particle features; microbial community structures; volumetric water content
• ISSN: 1664-302X; 1664-302X
• DOI: 10.3389/fmicb.2022.1024630

Sediments cover a majority of Earth's surface and are essential for global biogeochemical cycles. The effects of sediment physiochemical features on microbial community structures have attracted attention in recent years. However, the question of whether the interstitial space has significant effects on microbial community structures in submerged sediments remains unclear. In this study, based on identified OTUs (operational taxonomic units), correlation analysis, RDA analysis, and Permanova analysis were applied into investigating the effects of interstitial space volume, interstitial gas space, volumetric water content, sediment particle features (average size and evenness), and sediment depth on microbial community structures in different sedimentation areas of Chaohu Lake (Anhui Province, China). Our results indicated that sediment depth was the closest one to the main environmental gradient. The destruction effects of gas space on sediment structures can physically affect the similarity of the whole microbial community in all layers in river dominated sedimentation area (where methane emits actively). However, including gas space, none of the five interstitial space parameters were significant with accounting for the microbial community structures in a sediment layer. Thus, except for the happening of active physical destruction on sediment structures (for example, methane ebullition), sediment interstitial space parameters were ineffective for affecting microbial community structures in all sedimentation areas.