Evidence map›Paper›PMID 41038815›Full record

ArticleNature communications2025

Tectonic-astronomical interactions in shaping late Paleozoic climate and organic carbon burial.

Ren Wei, Zhijun Jin, Mingsong Li, Shuai Yuan, Yongyun Hu, Lin Dong, Rui Zhang, Juye Shi

Erratum issuedAbstract 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. An erratum has been issued. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing 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

1 citing paper in PubMed.

  1. Article
4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

8 authors.

Ren WeiInstitute of Energy, Peking University, Beijing, China.ORCID http://orcid.org/0000-0002-9133-1301
Zhijun JinInstitute of Energy, Peking University, Beijing, China. jinzj1957@pku.edu.cn.ORCID http://orcid.org/0000-0001-9739-981X
Mingsong LiSchool of Earth and Space Sciences, Peking University, Beijing, China.ORCID http://orcid.org/0000-0002-5542-8106
Shuai YuanLaboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China.ORCID http://orcid.org/0000-0002-8154-4899
Yongyun HuLaboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China.ORCID http://orcid.org/0000-0002-4003-4630
Lin DongSchool of Earth and Space Sciences, Peking University, Beijing, China.ORCID http://orcid.org/0000-0003-1754-842X
Rui ZhangCollege of Geosciences, China University of Petroleum (Beijing), Beijing, China.
Juye ShiSchool of Energy Resources, China University of Geosciences (Beijing), Beijing, China.

Funding

China Postdoctoral Science Foundation BX20240020National Natural Science Foundation of China (National Science Foundation of China) 42090025National Natural Science Foundation of China (National Science Foundation of China) 42488101National Natural Science Foundation of China (National Science Foundation of China) 42488201
6 · The paper itself

Abstract

Tectonic processes and astronomical cycles are key drivers of Earth's climate and carbon systems. However, their interplay in shaping late Paleozoic climate variability remains poorly constrained. Here, we divide the late Paleozoic (~360-250 Ma) into three distinct tectonic phases based on full-plate tectonic reconstructions, geochemical datasets, and carbon cycle modeling, thereby elucidating how global sea levels and organic carbon burial responded to astronomically forced climate fluctuations under different tectonic phases. Our results show that intervals spanning ~360-330 Ma and ~280-250 Ma were characterized by elevated atmospheric CO

Identifiers

PMID41038815
PMCPMC12491408

What OpenQuestion holds

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LicenceCC BY-NC-ND
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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.