Abstract

Hydrothermal vents release reduced compounds and small organic carbon compounds into the surrounding seawater, providing essential substrates for microbial growth and bioenergy transformations. Despite the wide distribution of the marine benthic group E archaea (referred to as Hydrothermarchaeota) in the hydrothermal environment, little is known about their genomic repertoires and biogeochemical significance. Here, we studied four highly complete (>80%) metagenome-assembled genomes (MAGs) from a black smoker chimney and the surrounding sulfur-rich sediments on the South Atlantic Mid-Ocean Ridge and publicly available data sets (the Integrated Microbial Genomes system of the U.S. Department of Energy-Joint Genome Institute and NCBI SRA data sets). Genomic analysis suggested a wide carbon metabolic diversity of Hydrothermarchaeota members, including the utilization of proteins, lactate, and acetate; the anaerobic degradation of aromatics; the oxidation of C1 compounds (CO, formate, and formaldehyde); the utilization of methyl compounds; CO2 incorporation by the tetrahydromethanopterin-based Wood-Ljungdahl pathway; and participation in the type III ribulose-1,5-bisphosphate carboxylase/oxygenase-based Calvin-Benson-Bassham cycle. These microbes also potentially oxidize sulfur, arsenic, and hydrogen and engage in anaerobic respiration based on sulfate reduction and denitrification. Among the 140 MAGs reconstructed from the black smoker chimney microbial community (including Hydrothermarchaeota MAGs), community-level metabolic predictions suggested a redundancy of carbon utilization and element cycling functions and interactive syntrophic and sequential utilization of substrates. These processes might make various carbon and energy sources widely accessible to the microorganisms. Further, the analysis suggested that Hydrothermarchaeota members contained important functional components obtained from the community via lateral gene transfer, becoming a distinctive clade. This might serve as a niche-adaptive strategy for metabolizing heavy metals, C1 compounds, and reduced sulfur compounds. Collectively, the analysis provides comprehensive metabolic insights into the Hydrothermarchaeota IMPORTANCE This study provides comprehensive metabolic insights into the Hydrothermarchaeota from comparative genomics, evolution, and community-level perspectives. Members of the Hydrothermarchaeota synergistically participate in a wide range of carbon-utilizing and element cycling processes with other microorganisms in the community. We expand the current understanding of community interactions within the hydrothermal sediment and chimney, suggesting that microbial interactions based on sequential substrate metabolism are essential to nutrient and element cycling.

Highlights

  • IMPORTANCE This study provides comprehensive metabolic insights into the Hydrothermarchaeota from comparative genomics, evolution, and community-level perspectives

  • We analyzed the metagenomes from sulfur-rich hydrothermal sediments at an active deep-sea hydrothermal vent site in the southern Mid-Atlantic Ridge of the South Atlantic Ocean

  • Genomic predictions in the current study indicated that while the genomes of Hydrothermarchaeota from clades 1 and 3 encode various peptide/amino acid transporters, the genomes of the three major clades encode the genes of six groups of aminotransferases to transfer amino residues (Tables S4 and S5) and the genes for pyruvate ferredoxin oxidoreductase (Por), indolepyruvate ferredoxin oxidoreductase (Ior), 2-oxoglutarate/2-oxoacid ferredoxin oxidoreductase (Kor), pyruvate dehydrogenase, and dihydrolipoamide dehydrogenase to assimilate 2-oxo acids to succinyl-coenzyme A (CoA) and replenish the energy pool of reducing equivalents

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Summary

Introduction

IMPORTANCE This study provides comprehensive metabolic insights into the Hydrothermarchaeota from comparative genomics, evolution, and community-level perspectives. We expand the current understanding of community interactions within the hydrothermal sediment and chimney, suggesting that microbial interactions based on sequential substrate metabolism are essential to nutrient and element cycling. De novo metagenome assembly and binning resulted in 140 MAGs (Ͼ50% genome completeness) from 24 microbial groups (Table S1), including 5 archaeal MAGs and 135 bacterial MAGs. The metabolic prediction from the resolved MAGs revealed the functional redundancy and syntrophic substrate-utilizing interactions among the microorganisms. Based on the four Hydrothermarchaeota genomes of relatively high completeness (Ͼ80%) obtained in the current study, the results of a previous publication [9], and data in publicly available data sets (Table S2), we propose a metabolic scheme for this archaeal lineage. The current study provides an in-depth insight into the genomics, community-level interactions, and evolution of Hydrothermarchaeota

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