Abstract

SummaryObligate acidophilic members of the thaumarchaeotal genus Candidatus Nitrosotalea play an important role in nitrification in acidic soils, but their evolutionary and physiological adaptations to acidic environments are still poorly understood, with only a single member of this genus (Ca. N. devanaterra) having its genome sequenced. In this study, we sequenced the genomes of two additional cultured Ca. Nitrosotalea strains, extracted an almost complete Ca. Nitrosotalea metagenome‐assembled genome from an acidic fen, and performed comparative genomics of the four Ca. Nitrosotalea genomes with 19 other archaeal ammonia oxidiser genomes. Average nucleotide and amino acid identities revealed that the four Ca. Nitrosotalea strains represent separate species within the genus. The four Ca. Nitrosotalea genomes contained a core set of 103 orthologous gene families absent from all other ammonia‐oxidizing archaea and, for most of these gene families, expression could be demonstrated in laboratory culture or the environment via proteomic or metatranscriptomic analyses respectively. Phylogenetic analyses indicated that four of these core gene families were acquired by the Ca. Nitrosotalea common ancestor via horizontal gene transfer from acidophilic representatives of Euryarchaeota. We hypothesize that gene exchange with these acidophiles contributed to the competitive success of the Ca. Nitrosotalea lineage in acidic environments.

Highlights

  • Nitrification, the oxidation of ammonia to nitrate via nitrite, is a central process within the terrestrial nitrogen cycle, determining the form of inorganic nitrogen available to plants, decreasing nitrogen fertilizer utilization efficiency and contributing to atmospheric and groundwater pollution by nitrous oxide and nitrate respectively (Robertson and Vitousek, 2009)

  • Net rates of nitrification do not show a strong correlation with soil pH and some of the highest rates are found in acidic soils (Booth et al, 2005), which comprise approximately 30% of all soils

  • Surveys of 16S rRNA and ammonia monooxygenase subunit A genes demonstrate that ammonia oxidising archaea (AOA) are distributed globally in soils, with pH being an important

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Summary

Introduction

Nitrification, the oxidation of ammonia to nitrate via nitrite, is a central process within the terrestrial nitrogen cycle, determining the form of inorganic nitrogen available to plants, decreasing nitrogen fertilizer utilization efficiency and contributing to atmospheric and groundwater pollution by nitrous oxide and nitrate respectively (Robertson and Vitousek, 2009). Nitrification in soil is generally limited by the initial oxidation of ammonia to nitrite, in which archaeal ammonia oxidisers play a significant role (e.g., Lu et al, 2015; Hink et al, 2017). Surveys of 16S rRNA and ammonia monooxygenase subunit A (amoA) genes demonstrate that ammonia oxidising archaea (AOA) are distributed globally in soils, with pH being an important. Environmental Microbiology published by Society for Applied Microbiology and John Wiley & Sons Ltd. Environmental Microbiology published by Society for Applied Microbiology and John Wiley & Sons Ltd

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