Evidence map›Paper›PMID 33097795›Full record

ArticleScientific reports2020

Carbon isotope evidence for large methane emissions to the Proterozoic atmosphere.

Pierre Cadeau, Didier Jézéquel, Christophe Leboulanger, Eric Fouilland, Emilie Le Floc'h, Carine Chaduteau, Vincent Milesi, Julia Guélard, Gérard Sarazin, Amandine Katz and 3 more

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.

0numbers the graph read from it
0cells of the map it votes in
9citing papers in PubMed
13.3field-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

9 citing papers in PubMed, 50 citations in OpenAlex.

  1. Timing and magnitude of the Lomagundi-Jatuli carbon isotope excursion.Proceedings of the National Academy of Sciences of the United States of America · 2026
    Article
  2. Revisiting the greatness of Earth's great oxidation.Communications earth & environment · 2026
    Review
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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

13 authors at 4 institutions in 1 country.

Pierre CadeauUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France. pierre.cadeau@gmail.com.
Didier JézéquelUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Christophe LeboulangerMARBEC Sète, France, Univ Montpellier, CNRS, Ifremer, IRD, Sète, France.
Eric FouillandMARBEC Sète, France, Univ Montpellier, CNRS, Ifremer, IRD, Sète, France.
Emilie Le Floc'hMARBEC Sète, France, Univ Montpellier, CNRS, Ifremer, IRD, Sète, France.
Carine ChaduteauUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Vincent MilesiUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Julia GuélardUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Gérard SarazinUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Amandine KatzUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Sophie d'AmoreUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Cécile BernardUMR 7245 MCAM, Muséum National D'Histoire Naturelle - CNRS, Paris, France.
Magali AderUniversité de Paris, Institut de physique du globe de Paris, CNRS, 75005, Paris, France.
Centre National de la Recherche Scientifique · FRInstitut de physique du globe de Paris · FRUniversité Paris Cité · FRUniversité de Montpellier · FR

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Proterozoic Era records two periods of abundant positive carbon isotope excursions (CIEs), conventionally interpreted as resulting from increased organic carbon burial and leading to Earth's surface oxygenation. As strong spatial variations in the amplitude and duration of these excursions are uncovered, this interpretation is challenged. Here, by studying the carbon cycle in the Dziani Dzaha Lake, we propose that they could be due to regionally variable methane emissions to the atmosphere. This lake presents carbon isotope signatures deviated by ~  + 12‰ compared to the modern ocean and shares a unique combination of analogies with putative Proterozoic lakes, interior seas or restricted epireic seas. A simple box model of its Carbon cycle demonstrates that its current isotopic signatures are due to high primary productivity, efficiently mineralized by methanogenesis, and to subsequent methane emissions to the atmosphere. By analogy, these results might allow the reinterpretation of some positive CIEs as at least partly due to regionally large methane emissions. This supports the view that methane may have been a major greenhouse gas during the Proterozoic Era, keeping the Earth from major glaciations, especially during periods of positive CIEs, when increased organic carbon burial would have drowned down atmospheric CO

Identifiers

PMID33097795
PMCPMC7585424
OpenAlexW3093614820

What OpenQuestion holds

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LicenceCC BY
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Registered trials

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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.