Evidence map›Paper›PMID 36399571›Full record

ArticleScience advances2022

Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction.

Nevin P Kozik, Seth A Young, Sean M Newby, Mu Liu, Daizhao Chen, Emma U Hammarlund, David P G Bond, Theodore R Them, Jeremy D Owens

Open access · goldAbstract read
In one paragraph

Article in Science advances, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
4.5field-weighted citation impact, top 5% 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

3 citing papers in PubMed, 34 citations in OpenAlex.

  1. 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

9 authors at 5 institutions in 5 countries.

Nevin P KozikDepartment of Earth, Ocean and Atmospheric Science - National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32306, USA.ORCID 0000-0001-7759-7552
Seth A YoungDepartment of Earth, Ocean and Atmospheric Science - National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32306, USA.ORCID 0000-0001-6885-4780
Sean M NewbyDepartment of Earth, Ocean and Atmospheric Science - National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32306, USA.ORCID 0000-0002-6585-095X
Mu LiuKey Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
Daizhao ChenKey Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.ORCID 0000-0002-1131-3630
Emma U HammarlundTissue Development and Evolution (TiDE) Division, Department of Laboratory Medicine, Lund University, Lund, Sweden.ORCID 0000-0001-7625-4793
David P G BondDepartment of Geography, Geology and Environment, University of Hull, Hull HU6 7RX, UK.
Theodore R ThemDepartment of Geology and Environmental Geosciences, College of Charleston, Charleston, SC 29424, USA.ORCID 0000-0003-3986-8520
Jeremy D OwensDepartment of Earth, Ocean and Atmospheric Science - National High Magnetic Field Laboratory, Florida State University, Tallahassee, FL 32306, USA.ORCID 0000-0002-0530-2177
Florida State University · USChinese Academy of Sciences · CNCollege of Charleston · USLund University · SEUniversity of Hull · GB

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The timing and connections between global cooling, marine redox conditions, and biotic turnover are underconstrained for the Late Ordovician. The second most severe mass extinction occurred at the end of the Ordovician period, resulting in ~85% loss of marine species between two extinction pulses. As the only "Big 5" extinction that occurred during icehouse conditions, this interval is an important modern analog to constrain environmental feedbacks. We present a previously unexplored thallium isotope records from two paleobasins that record global marine redox conditions and document two distinct and rapid excursions suggesting vacillating (de)oxygenation. The strong temporal link between these perturbations and extinctions highlights the possibility that dynamic marine oxygen fluctuations, rather than persistent, stable global anoxia, played a major role in driving the extinction. This evidence for rapid oxygen changes leading to mass extinction has important implications for modern deoxygenation and biodiversity declines.

Identifiers

PMID36399571
PMCPMC9674285
OpenAlexW4309468427

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.