Microbial diversity and function in crystalline basement beneath the Deccan Traps explored in a 3 km borehole at Koyna, western India. (20th December 2021)

• Record Type: Journal Article
• Authors: Sahu, Rajendra Prasad; Kazy, Sufia K.; Bose, Himadri; Mandal, Sunanda; Dutta, Avishek; Saha, Anumeha; Roy, Sukanta; Dutta Gupta, Srimanti; Mukherjee, Abhijit; Sar, Pinaki
• Is Part Of: Environmental microbiology. Volume 24:Number 6(2022)
• Page Start: 2837
• Page End: 2853
• Publication Date: 2021-12-20
• Subjects: Microbial ecology -- Periodicals; Environmental Microbiology -- Periodicals; 579.17
• DOI: 10.1111/1462-2920.15867
• Languages: English
• ISSNs: 1462-2912

Abstract

Summary: 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 × 10 6 ) 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.