Evidence map›Paper›PMID 40155613›Full record

ArticleNature communications2025

Astronomically calibrating early Ediacaran evolution.

Tan Zhang, Chao Ma, Yifan Li, Chao Li, Anne-Christine Da Silva, Tailiang Fan, Qi Gao, Mingzhi Kuang, Wangwei Liu, Mingsong Li and 1 more

Abstract read
In one paragraph

Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

11 authors.

Tan ZhangState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China.ORCID http://orcid.org/0000-0002-8547-5798
Chao MaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China. machao@cdut.edu.cn.ORCID http://orcid.org/0000-0002-0122-5696
Yifan LiSchool of Energy Resources, China University of Geosciences (Beijing), Beijing, 100083, China. yifangeosci@gmail.com.ORCID http://orcid.org/0000-0003-2756-6146
Chao LiState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China.ORCID http://orcid.org/0000-0001-9861-661X
Anne-Christine Da SilvaSedimentary Petrology Laboratory, University of Liege, Sart Tilman B20, Allée du Six Août 12, Liège, 4000, Belgium.ORCID http://orcid.org/0000-0003-4191-7600
Tailiang FanSchool of Energy Resources, China University of Geosciences (Beijing), Beijing, 100083, China.
Qi GaoCollege of Geography and Planning, Chengdu University of Technology, Chengdu, 610059, China.
Mingzhi KuangCollege of Energy, Chengdu University of Technology, Chengdu, 610059, China.
Wangwei LiuWuxi Research Institute of Petroleum Geology, Research Institute of Petroleum Exploration and Production, SINOPEC, Wuxi, 214151, China.
Mingsong LiKey Laboratory of Orogenic Belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University, Beijing, 100871, China.ORCID http://orcid.org/0000-0002-5542-8106
Mingcai HouState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation & Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, 610059, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The current low-resolution chronostratigraphic framework for the early Ediacaran Period hampers a comprehensive understanding of potential trigger mechanisms for environmental upheavals and their connections to evolutionary innovation. Here, we establish a high-resolution astrochronological framework spanning ~57.6 million years of the early Ediacaran, anchored by the radioisotopic date of the Gaskiers glaciation onset, based on key sections from South China. Constrained by multiple radioisotopic dates, this framework precisely constrains the timing of the Marinoan deglaciation, Ediacaran Negative carbon isotope excursions 1 and 2 (EN1 and EN2), and key fossil assemblages (acanthomorphic acritarchs, Weng'an and Lantian biotas). These dates indicate the rapid termination of the Marinoan glaciation in South China within 10

Identifiers

PMID40155613
PMCPMC11953472

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