Abstract

DPANN archaea account for half of the archaeal diversity of the biosphere, but with few cultivated representatives, their metabolic potential and environmental functions are poorly understood. The extreme geochemical and environmental conditions in meromictic ice-capped Lake A, in the Canadian High Arctic, provided an isolated, stratified model ecosystem to resolve the distribution and metabolism of uncultured aquatic DPANN archaea living across extreme redox and salinity gradients, from freshwater oxygenated conditions, to saline, anoxic, sulfidic waters. We recovered 28 metagenome-assembled genomes (MAGs) of DPANN archaea that provided genetic insights into their ecological function. Thiosulfate oxidation potential was detected in aerobic Woesearchaeota, whereas diverse metabolic functions were identified in anaerobic DPANN archaea, including degradation and fermentation of cellular compounds, and sulfide and polysulfide reduction. We also found evidence for “vampiristic” metabolism in several MAGs, with genes coding for pore-forming toxins, peptidoglycan degradation, and RNA scavenging. The vampiristic MAGs co-occurred with other DPANNs having complementary metabolic capacities, leading to the possibility that DPANN form interspecific consortia that recycle microbial carbon, nutrients and complex molecules through a DPANN archaeal shunt, adding hidden novel complexity to anaerobic microbial food webs.

Highlights

  • Archaea are found across global ecosystems, carrying out diverse functions, including ammonium oxidation in aerobic environments, and sulfur, methane, and hydrocarbon cycling in anoxic environments [1,2,3,4,5]

  • Archaeal community composition was investigated by DNA and cDNAbased 16 S rRNA amplicon sequencing, qPCR and primer-free metagenomic sequencing on the discrete samples collected down the water column

  • 16 S rRNA genes related to Methanofastidiosales and Thermoplasmatales, detected by amplicon sequencing were rare in the metagenomes (Fig. 1, Supplementary Fig. 1)

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Summary

Introduction

Archaea are found across global ecosystems, carrying out diverse functions, including ammonium oxidation in aerobic environments, and sulfur, methane, and hydrocarbon cycling in anoxic environments [1,2,3,4,5]. The monophyletic super-phylum DPANN, named by the initials of the first five phyla level taxa in the cluster (Diapherotrites, Parvarchaeota, Aenigmarchaeota, Nanohaloarchaeota, and Nanoarchaeota phyla), includes Woesearchaeota (formerly named Deep-sea Hydrothermal Vent Euryarchaeota Group 6, DHVEG-6 [7]), Micrarchaeota, Altiarchaeota (formerly known as SM1 Euryarchaeon), Huberarchaeota, and Undinarchaeota [8, 9]. This super-phylum is estimated to account for approximately half of all the archaeal diversity of the planet [10]. Despite this recent progress exploring archaeal ecology, the biodiversity and metabolism of the DPANN super-phylum still remains largely unknown, leaving their ecosystem-level importance nebulous

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