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Microbial diversity and function in crystalline basement beneath the Deccan Traps explored in a 3 km borehole at Koyna,western India
Authors:Rajendra Prasad Sahu  Sufia K Kazy  Himadri Bose  Sunanda Mandal  Avishek Dutta  Anumeha Saha  Sukanta Roy  Srimanti Dutta Gupta  Abhijit Mukherjee  Pinaki Sar
Institution:1. Environmental Microbiology and Genomics Laboratory, Department of Biotechnology, Indian Institute of Technology Kharagpur, Kharagpur, WB, 721302 India;2. Department of Biotechnology, National Institute of Technology Durgapur, Durgapur, WB, 713209 India;3. Ministry of Earth Sciences, Borehole Geophysics Research Laboratory, Karad, MH, 415114 India;4. School of Environmental Science and Engineering, Indian Institute of Technology Kharagpur, Kharagpur, WB, 721302 India;5. School of Environmental Science and Engineering, Indian Institute of Technology Kharagpur, Kharagpur, WB, 721302 India

Department of Geology and Geophysics, Indian Institute of Technology Kharagpur, Kharagpur, WB, 721302 India

Abstract:Deep terrestrial subsurface represents a huge repository of global prokaryotic biomass. Given its vastness and importance, microbial life within the deep subsurface continental crust remains under-represented in global studies. We characterize the microbial communities of deep, extreme and oligotrophic realm hosted by crystalline Archaean granitic rocks underneath the Deccan Traps, through sampling via 3000 m deep scientific borehole at Koyna, India through metagenomics, amplicon sequencing and cultivation-based analyses. Gene sequences 16S rRNA (7.37 × 106) show considerable bacterial diversity and the existence of a core microbiome (5724 operational taxonomic units conserved out of a total 118,064 OTUs) across the depths. Relative abundance of different taxa of core microbiome varies with depth in response to prevailing lithology and geochemistry. Co-occurrence network analysis and cultivation attempt to elucidate close interactions among autotrophic and organotrophic bacteria. Shotgun metagenomics reveals a major role of autotrophic carbon fixation via the Wood–Ljungdahl pathway and genes responsible for energy and carbon metabolism. Deeper analysis suggests the existence of an ‘acetate switch’, coordinating biosynthesis and cellular homeostasis. We conclude that the microbial life in the nutrient- and energy-limited deep granitic crust is constrained by the depth and managed by a few core members via a close interplay between autotrophy and organotrophy.
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