Table_1_Epilithic Microbial Community Functionality in Deep Oligotrophic Continental Bedrock.XLSX

• Main Authors: Maija Nuppunen-Puputti, Riikka Kietäväinen, Mari Raulio, Aino Soro, Lotta Purkamo, Ilmo Kukkonen, Malin Bomberg
• Format: Dataset
• Language: unknown
• Published: 2022
• Subjects: Microbiology; Microbial Genetics; Microbial Ecology; Mycology; crystalline bedrock; deep biosphere; Fennoscandian Shield; sessile microbial communities; the Outokumpu deep drill hole; metagenome-assembled genomes; microbe-mineral interactions; sulfate reduction; Fennoscandian
• Online Access: https://doi.org/10.3389/fmicb.2022.826048.s002; https://figshare.com/articles/dataset/Table_1_Epilithic_Microbial_Community_Functionality_in_Deep_Oligotrophic_Continental_Bedrock_XLSX/19254113

The deep terrestrial biosphere hosts vast sessile rock surface communities and biofilms, but thus far, mostly planktic communities have been studied. We enriched deep subsurface microbial communities on mica schist in microcosms containing bedrock groundwater from the depth of 500 m from Outokumpu, Finland. The biofilms were visualized using scanning electron microscopy, revealing numerous different microbial cell morphologies and attachment strategies on the mica schist surface, e.g., bacteria with outer membrane vesicle-like structures, hair-like extracellular extensions, and long tubular cell structures expanding over hundreds of micrometers over mica schist surfaces. Bacterial communities were analyzed with amplicon sequencing showing that Pseudomonas, Desulfosporosinus, Hydrogenophaga, and Brevundimonas genera dominated communities after 8–40 months of incubation. A total of 21 metagenome assembled genomes from sessile rock surface metagenomes identified genes involved in biofilm formation, as well as a wide variety of metabolic traits indicating a high degree of environmental adaptivity to oligotrophic environment and potential for shifting between multiple energy or carbon sources. In addition, we detected ubiquitous organic carbon oxidation and capacity for arsenate and selenate reduction within our rocky MAGs. Our results agree with the previously suggested interaction between the deep subsurface microbial communities and the rock surfaces, and that this interaction could be crucial for sustaining life in the harsh anoxic and oligotrophic deep subsurface of crystalline bedrock environment.