Evidence map›Paper›PMID 32286253›Full record

ArticleNature communications2020

Persistent global marine euxinia in the early Silurian.

Richard G Stockey, Devon B Cole, Noah J Planavsky, David K Loydell, Jiří Frýda, Erik A Sperling

Abstract read
In one paragraph

Article in Nature communications, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.

0numbers the graph read from it
0cells of the map it votes in
8citing papers in PubMed
–field-weighted citation impact
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

8 citing papers in PubMed.

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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

6 authors.

Richard G StockeyStanford University, Department of Geological Sciences, Stanford, CA, 94305, USA. rstockey@stanford.edu.ORCID http://orcid.org/0000-0001-5541-7987
Devon B ColeSchool of Earth & Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, 30332, USA.ORCID http://orcid.org/0000-0002-5669-3817
Noah J PlanavskyDepartment of Geology and Geophysics, Yale University, New Haven, CT, 06511, USA.
David K LoydellSchool of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, PO1 3QL, UK.ORCID http://orcid.org/0000-0003-3967-0047
Jiří FrýdaFaculty of Environmental Sciences, Czech University of Life Sciences Prague, Prague, Czech Republic.
Erik A SperlingStanford University, Department of Geological Sciences, Stanford, CA, 94305, USA.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The second pulse of the Late Ordovician mass extinction occurred around the Hirnantian-Rhuddanian boundary (~444 Ma) and has been correlated with expanded marine anoxia lasting into the earliest Silurian. Characterization of the Hirnantian ocean anoxic event has focused on the onset of anoxia, with global reconstructions based on carbonate δ

Identifiers

PMID32286253
PMCPMC7156380

What OpenQuestion holds

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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.