4.7 Article

Community assembly, potential functions and interactions between fungi and microalgae associated with biodeterioration of sandstone at the Beishiku Temple in Northwest China

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 835, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2022.155372

关键词

Phototrophic microorganisms; Fungal guilds; Bioweathering; Caves temple; Environmental factors

资金

  1. National Natural Science Foundation of China [32060258, 32100101]
  2. National Key R&D Plan Project of China [2020YFC1522200]
  3. Science and Technology Plan of Gansu Province, China [21JR11RA218, 18JR3RA004, 18ZD2FA001]

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This study investigated the diversity, distributions, ecological functions, and interaction patterns of fungal and microalgal communities on sandstone in the Beishiku Temple using high-throughput sequencing analysis. The results showed that the core phyla of fungi were affiliated with unclassified Lecanoromycetes, Engyodontium, Knufia, Epicoccum, Endocarpon, and Cladosporium of Ascomycota whereas the phyla of microalgae were dominated by prokaryotic Cyanobacteria and eukaryotic Chlorophyta. The study also found that the structure of microbial communities on the weathered sandstone was more strongly shaped by soluble Cl-, Na+, NO3- ions than by other environmental factors. The co-occurrence network analysis suggested a more stable community structure outside the caves.
Fungi, cyanobacteria and algae are specific microbial groups associated with the deterioration and safety of stone monuments. In this study, high-throughput sequencing analysis was used to investigate the diversity, distributions, ecological functions, and interaction patterns of both the fungal and microalgal (including cyanobacteria and algae) communities on sandstone in the Beishiku Temple, located on the ancient Silk Road. The results showed that the core phyla of fungi were affiliated with unclassified Lecanoromycetes, Engyodontium, Knufia, Epicoccum, Endocarpon, and Cladosporium of Ascomycota whereas the phyla of microalgae were dominated by prokaryotic Cyanobacteria and eukaryotic Chlorophyta. The environmental factors of temperature, relative humidity, and light intensity were monitored simultaneously. The structure of the microbial communities was much more strongly shaped by soluble Cl-, Na+, NO3- ions than by the light intensity, moisture content or temperature, especially for the weathered sandstone located outside the caves. The co-occurrence network analysis suggested that a more stable community structure was evident outside the caves than inside. The stronger positive connections and coexistence patterns that were detected indicate a strong adaptability of fungi and microalgae to the distinct oligotrophic microhabitats on sandstone.

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