Evidence map›Paper›PMID 31178922›Full record

ArticleNature geoscience2019

Possible links between extreme oxygen perturbations and the Cambrian radiation of animals.

Tianchen He, Maoyan Zhu, Benjamin J W Mills, Peter M Wynn, Andrey Yu Zhuravlev, Rosalie Tostevin, Philip A E Pogge von Strandmann, Aihua Yang, Simon W Poulton, Graham A Shields

Abstract read
In one paragraph

Article in Nature geoscience, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 26 papers.

0numbers the graph read from it
0cells of the map it votes in
26citing papers in PubMed
30.7field-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

26 citing papers in PubMed, 175 citations in OpenAlex.

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  5. Repeated occurrences of marine anoxia under high atmospheric OProceedings of the National Academy of Sciences of the United States of America · 2025
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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

10 authors at 7 institutions in 3 countries.

Tianchen HeLondon Geochemistry and Isotope Centre (LOGIC), Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, London, WC1E 6BT, UK.
Maoyan ZhuState Key Laboratory of Palaeobiology and Stratigraphy & Center for Excellence in Life and Paleoenvironment, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008, China.
Benjamin J W MillsSchool of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK.
Peter M WynnLancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK.
Andrey Yu ZhuravlevDepartment of Biological Evolution, Faculty of Biology, Lomonosov Moscow State University, Leninskie gory 1(12), Moscow 119234, Russia.
Rosalie TostevinDepartment of Earth Sciences, University of Oxford, Oxford, OX1 3AN, UK.
Philip A E Pogge von StrandmannLondon Geochemistry and Isotope Centre (LOGIC), Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, London, WC1E 6BT, UK.
Aihua YangState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210093, China.
Simon W PoultonSchool of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK.
Graham A ShieldsLondon Geochemistry and Isotope Centre (LOGIC), Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, London, WC1E 6BT, UK.
University of Leeds · GBUniversity College London · GBChinese Academy of Sciences · CNLancaster University · GBLomonosov Moscow State University · RUNanjing University · CNUniversity of Oxford · GB

Funding

European Research Council 682760
6 · The paper itself

Abstract

The role of oxygen as a driver for early animal evolution is widely debated. During the Cambrian explosion, episodic radiations of major animal phyla occurred coincident with repeated carbon isotope fluctuations. However, the driver of these isotope fluctuations and potential links to environmental oxygenation are unclear. Here, we report high-resolution carbon and sulphur isotope data for marine carbonates from the southeastern Siberian Platform that document the canonical explosive phase of the Cambrian radiation from ~524 to ~514 Myr ago. These analyses demonstrate a strong positive covariation between carbonate δ

Identifiers

PMID31178922
PMCPMC6548555
OpenAlexW2942544615

What OpenQuestion holds

Textmetadata
LicenceTDM
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.