Evidence map›Paper›PMID 33398096›Full record

ArticleNature microbiology2021

Trace gas oxidizers are widespread and active members of soil microbial communities.

Sean K Bay, Xiyang Dong, James A Bradley, Pok Man Leung, Rhys Grinter, Thanavit Jirapanjawat, Stefan K Arndt, Perran L M Cook, Douglas E LaRowe, Philipp A Nauer and 2 more

Open access · greenAbstract read
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In one paragraph

Article in Nature microbiology, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 92 papers.

0numbers the graph read from it
0cells of the map it votes in
92citing papers in PubMed
15.8field-weighted citation impact, top 1% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

92 citing papers in PubMed, 214 citations in OpenAlex.

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  20. First isolation of a methanotrophicApplied and environmental microbiology · 2025
    Article

32 more citing papers are in PubMed but not listed here.

4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

12 authors at 7 institutions in 5 countries.

Sean K BaySchool of Biological Sciences, Monash University, Clayton, Victoria, Australia.
Xiyang DongSchool of Marine Sciences, Sun Yat-Sen University, Zhuhai, China.ORCID http://orcid.org/0000-0002-9224-5923
James A BradleySchool of Geography, Queen Mary University of London, London, UK.ORCID http://orcid.org/0000-0003-3640-208X
Pok Man LeungSchool of Biological Sciences, Monash University, Clayton, Victoria, Australia.ORCID http://orcid.org/0000-0002-5382-827X
Rhys GrinterDepartment of Microbiology, Biomedicine Discovery Institute, Monash University, Clayton, Victoria, Australia.
Thanavit JirapanjawatSchool of Biological Sciences, Monash University, Clayton, Victoria, Australia.
Stefan K ArndtSchool of Ecosystem and Forest Sciences, University of Melbourne, Richmond, Victoria, Australia.ORCID http://orcid.org/0000-0001-7086-9375
Perran L M CookSchool of Chemistry, Monash University, Clayton, Victoria, Australia.ORCID http://orcid.org/0000-0002-0444-3488
Douglas E LaRoweDepartment of Earth Sciences, University of Southern California, Los Angeles, CA, USA.
Philipp A NauerSchool of Chemistry, Monash University, Clayton, Victoria, Australia.
Eleonora ChiriSchool of Biological Sciences, Monash University, Clayton, Victoria, Australia. eleonora.chiri@monash.edu.ORCID http://orcid.org/0000-0002-6627-0762
Chris GreeningSchool of Biological Sciences, Monash University, Clayton, Victoria, Australia. chris.greening@monash.edu.ORCID http://orcid.org/0000-0001-7616-0594
Australian Regenerative Medicine Institute · AUDiscovery Institute · USMonash University · AUQueen Mary University of London · GBSun Yat-sen University · CNThe University of Melbourne · AUUniversity of Southern California · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Soil microorganisms globally are thought to be sustained primarily by organic carbon sources. Certain bacteria also consume inorganic energy sources such as trace gases, but they are presumed to be rare community members, except within some oligotrophic soils. Here we combined metagenomic, biogeochemical and modelling approaches to determine how soil microbial communities meet energy and carbon needs. Analysis of 40 metagenomes and 757 derived genomes indicated that over 70% of soil bacterial taxa encode enzymes to consume inorganic energy sources. Bacteria from 19 phyla encoded enzymes to use the trace gases hydrogen and carbon monoxide as supplemental electron donors for aerobic respiration. In addition, we identified a fourth phylum (Gemmatimonadota) potentially capable of aerobic methanotrophy. Consistent with the metagenomic profiling, communities within soil profiles from diverse habitats rapidly oxidized hydrogen, carbon monoxide and to a lesser extent methane below atmospheric concentrations. Thermodynamic modelling indicated that the power generated by oxidation of these three gases is sufficient to meet the maintenance needs of the bacterial cells capable of consuming them. Diverse bacteria also encode enzymes to use trace gases as electron donors to support carbon fixation. Altogether, these findings indicate that trace gas oxidation confers a major selective advantage in soil ecosystems, where availability of preferred organic substrates limits microbial growth. The observation that inorganic energy sources may sustain most soil bacteria also has broad implications for understanding atmospheric chemistry and microbial biodiversity in a changing world.

Indexed as

MicrobiotaSoilSoil MicrobiologyBacteriaCarbon MonoxideHydrogenMetagenomicsOxidation-ReductionPhylogenyCarbon MonoxideHydrogenSoil

Identifiers

PMID33398096
OpenAlexW3120760289

What OpenQuestion holds

Textmetadata
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.