Evidence map›Paper›PMID 29968714›Full record

ArticleNature communications2018

Coupling of ocean redox and animal evolution during the Ediacaran-Cambrian transition.

Dan Wang, Hong-Fei Ling, Ulrich Struck, Xiang-Kun Zhu, Maoyan Zhu, Tianchen He, Ben Yang, Antonia Gamper, Graham A Shields

Erratum issuedAbstract read
In one paragraph

Article in Nature communications, 2018. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 12 papers.

0numbers the graph read from it
0cells of the map it votes in
12citing 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

12 citing papers in PubMed.

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4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

9 authors.

Dan WangMNR Key Laboratory of Isotope Geology, MNR Key Laboratory of Deep-Earth Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China. njuwangdan@gmail.com.
Hong-Fei LingState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China. hfling@nju.edu.cn.
Ulrich StruckMuseum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, 10115, Berlin, Germany.
Xiang-Kun ZhuMNR Key Laboratory of Isotope Geology, MNR Key Laboratory of Deep-Earth Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China.
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, 210008, Nanjing, China.
Tianchen HeSchool of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK.
Ben YangMNR Key Laboratory of Stratigraphy and Palaeontology, Institute of Geology, Chinese Academy of Geological Sciences, 100037, Beijing, China.
Antonia GamperMuseum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, 10115, Berlin, Germany.
Graham A ShieldsDepartment of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, UK.ORCID http://orcid.org/0000-0002-7828-3966

Funding

Chinese Academy of Sciences (CAS) XDB18000000Deutsche Forschungsgemeinschaft (German Research Foundation) Projectnumber 21910049National Natural Science Foundation of China (National Science Foundation of China) 41430104National Natural Science Foundation of China (National Science Foundation of China) 41603023National Natural Science Foundation of China (National Science Foundation of China) 41661134048Natural Environment Research Council (NERC) NE/P013643/1
6 · The paper itself

Abstract

The late Ediacaran to early Cambrian interval witnessed extraordinary radiations of metazoan life. The role of the physical environment in this biological revolution, such as changes to oxygen levels and nutrient availability, has been the focus of longstanding debate. Seemingly contradictory data from geochemical redox proxies help to fuel this controversy. As an essential nutrient, nitrogen can help to resolve this impasse by establishing linkages between nutrient supply, ocean redox, and biological changes. Here we present a comprehensive N-isotope dataset from the Yangtze Basin that reveals remarkable coupling between δ

Identifiers

PMID29968714
PMCPMC6030108

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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.