Evidence map›Paper›PMID 35173296›Full record

ArticleThe ISME journal2022

Active anaerobic methane oxidation and sulfur disproportionation in the deep terrestrial subsurface.

Emma Bell, Tiina Lamminmäki, Johannes Alneberg, Chen Qian, Weili Xiong, Robert L Hettich, Manon Frutschi, Rizlan Bernier-Latmani

Open access · hybridAbstract read
In one paragraph

Article in The ISME journal, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 23 papers.

0numbers the graph read from it
0cells of the map it votes in
23citing papers in PubMed
5.9field-weighted citation impact, top 3% 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

23 citing papers in PubMed, 58 citations in OpenAlex.

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  12. Growth physiology, genomics, and proteomics ofFrontiers in microbiology · 2025
    Article
  13. Article
  14. Microorganisms · 2024
    Article
  15. Groundwater chromate removal by autotrophic sulfur disproportionation.Environmental science and ecotechnology · 2024
    Article
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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

8 authors at 4 institutions in 4 countries.

Emma BellEnvironmental Microbiology Laboratory, Environmental Engineering Institute, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, Lausanne, 1015, Switzerland. emma.bell1@ucalgary.ca.ORCID http://orcid.org/0000-0002-2064-6496
Tiina LamminmäkiPosiva Oy, Eurajoki, 27160, Finland.ORCID http://orcid.org/0000-0003-3581-5181
Johannes AlnebergScience for Life Laboratory, School of Engineering Sciences in Chemistry, Biotechnology and Health, Department of Gene Technology, KTH Royal Institute of Technology, Stockholm, SE-17121, Sweden.
Chen QianChemical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37830, USA.
Weili XiongChemical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37830, USA.ORCID http://orcid.org/0000-0001-7208-917X
Robert L HettichChemical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37830, USA.ORCID http://orcid.org/0000-0001-7708-786X
Manon FrutschiEnvironmental Microbiology Laboratory, Environmental Engineering Institute, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, Lausanne, 1015, Switzerland.
Rizlan Bernier-LatmaniEnvironmental Microbiology Laboratory, Environmental Engineering Institute, School of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, Lausanne, 1015, Switzerland. rizlan.bernier-latmani@epfl.ch.ORCID http://orcid.org/0000-0001-6547-722X
École Polytechnique Fédérale de Lausanne · CHOak Ridge National Laboratory · USPosiva (Finland) · FIScience for Life Laboratory · SE

Funding

U.S. Department of Energy (DOE) DE-AC02-05CH11231
6 · The paper itself

Abstract

Microbial life is widespread in the terrestrial subsurface and present down to several kilometers depth, but the energy sources that fuel metabolism in deep oligotrophic and anoxic environments remain unclear. In the deep crystalline bedrock of the Fennoscandian Shield at Olkiluoto, Finland, opposing gradients of abiotic methane and ancient seawater-derived sulfate create a terrestrial sulfate-methane transition zone (SMTZ). We used chemical and isotopic data coupled to genome-resolved metaproteogenomics to demonstrate active life and, for the first time, provide direct evidence of active anaerobic oxidation of methane (AOM) in a deep terrestrial bedrock. Proteins from Methanoperedens (formerly ANME-2d) are readily identifiable despite the low abundance (≤1%) of this genus and confirm the occurrence of AOM. This finding is supported by

Indexed as

ArchaeaMethaneAnaerobiosisCarbonGeologic SedimentsMethanosarcinalesOxidation-ReductionPhylogenySulfatesSulfurCarbonMethaneSulfatesSulfur

Identifiers

PMID35173296
PMCPMC9123182
OpenAlexW4226033138

What OpenQuestion holds

Textmetadata
LicenceCC BY
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.