Microbial Interactions Drive Distinct Taxonomic and Potential Metabolic Responses to Habitats in Karst Cave Ecosystem

• Published in: Microbiology spectrum Vol. 9; no. 2; p. e0115221
• Main Authors: Ma, Liyuan, Huang, Xinping, Wang, Hongmei, Yun, Yuan, Cheng, Xiaoyu, Liu, Deng, Lu, Xiaolu, Qiu, Xuan
• Format: Journal Article
• Language: English
• Published: United States American Society for Microbiology 31-10-2021
• Subjects: Actinobacteria - classification; Actinobacteria - isolation & purification; Actinobacteria - metabolism; Bacterial Physiological Phenomena; Carbon Cycle - physiology; Caves - microbiology; cooccurrence network; Ecosystem; functional prediction; Geologic Sediments - microbiology; karst cave; keystone species; Microbial Ecology; microbial interactions; Microbial Interactions - physiology; Nitrogen Fixation - physiology; Proteobacteria - classification; Proteobacteria - isolation & purification; Proteobacteria - metabolism; Research Article; Soil Microbiology; microbial interactions; keystone species; cooccurrence network; functional prediction; karst cave
• ISSN: 2165-0497; 2165-0497
• DOI: 10.1128/Spectrum.01152-21

The geological role of microorganisms has been widely studied in the karst cave ecosystem. However, microbial interactions and ecological functions in such a dark, humid, and oligotrophic habitat have received far less attention, which is crucial to understanding cave biogeochemistry. Herein, microorganisms from weathered rock and sediment along the Heshang Cave depth were analyzed by random matrix theory-based network and Tax4Fun functional prediction. The results showed that although the cave microbial communities have spatial heterogeneity, differential habitats drove the community structure and diversity.
were predominant in weathered rock, whereas
dominated the sediment. The sediment communities presented significantly higher alpha diversities due to the relatively abundant nutrition from the outside by the intermittent stream. Consistently, microbial interactions in sediment were more complex, as visualized by more nodes and links. The abundant taxa presented more positive correlations with other community members in both of the two networks, indicating that they relied on promotion effects to adapt to the extreme environment. The keystones in weathered rock were mainly involved in the biodegradation of organic compounds, whereas the keystone
in sediment contributed to carbon/nitrogen fixation. Collectively, these findings suggest that microbial interactions may lead to distinct taxonomic and functional communities in weathered rock and sediment in the subsurface Heshang Cave.
In general, the constant physicochemical conditions and limited nutrient sources over long periods in the subsurface support a stable ecosystem in karst cave. Previous studies on cave microbial ecology were mostly focused on community composition, diversity, and the relationship with local environmental factors. There are still many unknowns about the microbial interactions and functions in such a dark environment with little human interference. Two representative habitats, including weathered rock and sediment in Heshang Cave, were selected to give an integrated insight into microbial interactions and potential functions. The cooccurrence network, especially the subnetwork, was used to characterize the cave microbial interactions in detail. We demonstrated that abundant taxa primarily relied on promotion effects rather than inhibition effects to survive in Heshang Cave. Keystone species may play important metabolic roles in sustaining ecological functions. Our study provides improved understanding of microbial interaction patterns and community ecological functions in the karst cave ecosystem.