4.8 Article

Termite gas emissions select for hydrogenotrophic microbial communities in termite mounds

Publisher

NATL ACAD SCIENCES
DOI: 10.1073/pnas.2102625118

Keywords

hydrogen; lithoautotrophy; termite; Actinobacteria; trace gas

Funding

  1. Swiss National Science Foundation [P2EZP3_178421, P2EZP3_155596]
  2. ARC DECRA Fellowship [DE170100310]
  3. NHMRC EL2 Fellowship [APP1178715]
  4. Australian Research Council [DP120101735, LP100100073, DP180101762, DP210101595]
  5. Genomic Aotearoa grant [1806]
  6. Terrestrial Ecosystem Research Network (TERN) OzFlux
  7. TERN Australian SuperSite Network
  8. Swiss National Science Foundation (SNF) [P2EZP3_178421, P2EZP3_155596] Funding Source: Swiss National Science Foundation (SNF)
  9. Australian Research Council [LP100100073] Funding Source: Australian Research Council

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Organoheterotrophs are dominant in most soils, but termite mounds feature a unique community dominated by diverse hydrogenotrophic Actinobacteriota and Dormibacterota. These bacteria efficiently consume termite-derived H2 emissions and act as net sinks of atmospheric H2, while also releasing small amounts of methane. The availability of H2 shapes microbial communities and activities, highlighting a unique arthropod-bacteria interaction dependent on H2 transfer.
Organoheterotrophs are the dominant bacteria in most soils worldwide. While many of these bacteria can subsist on atmospheric hydrogen (H-2), levels of this gas are generally insufficient to sustain hydrogenotrophic growth. In contrast, bacteria residing within soil-derived termite mounds are exposed to high fluxes of H-2 due to fermentative production within termite guts. Here, we show through community, metagenomic, and biogeochemical profiling that termite emissions select for a community dominated by diverse hydrogenotrophic Actinobacteriota and Dormibacterota. Based on metagenomic short reads and derived genomes, uptake hydrogenase and chemosynthetic RuBisCO genes were significantly enriched in mounds compared to surrounding soils. In situ and ex situ measurements confirmed that high-and low-affinity H-2-oxidizing bacteria were highly active in the mounds, such that they efficiently consumed all termite-derived H-2 emissions and served as net sinks of atmospheric H-2. Concordant findings were observed across the mounds of three different Australian termite species, with termite activity strongly predicting H-2 oxidation rates (R-2 = 0.82). Cell-specific power calculations confirmed the potential for hydrogenotrophic growth in the mounds with most termite activity. In contrast, while methane is produced at similar rates to H-2 by termites, mounds contained few methanotrophs and were net sources of methane. Altogether, these findings provide further evidence of a highly responsive terrestrial sink for H-2 but not methane and suggest H-2 availability shapes composition and activity of microbial communities. They also reveal a unique arthropod-bacteria interaction dependent on H-2 transfer between host-associated and free-living microbial communities.

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