Evidence map›Paper›PMID 41093843›Full record

ArticleNature communications2025

Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum.

Guang-Yi Wei, Alexandre Pohl, Shijun Jiang, Hua Zhang, Wenqian Wang, Philip A E Pogge von Strandmann, Pierre Maffre, Guolin Xiong, Shu-Zhong Shen, Feifei Zhang

Abstract read
PubMed Full text at PMC Publisher
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. 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

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

10 authors.

Guang-Yi WeiState Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, Frontiers Science Center for Critical Earth Material Cycling, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China.ORCID http://orcid.org/0000-0002-0995-8923
Alexandre PohlUniversité Bourgogne Europe, CNRS, Biogéosciences, Dijon, France.ORCID http://orcid.org/0000-0003-2328-351X
Shijun JiangState Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, Haikou, China.ORCID http://orcid.org/0000-0001-6259-7912
Hua ZhangState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, China.ORCID http://orcid.org/0000-0002-5871-8264
Wenqian WangState Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, Frontiers Science Center for Critical Earth Material Cycling, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China.
Philip A E Pogge von StrandmannMIGHTY, Institute of Geosciences, Johannes Gutenberg University, Mainz, Germany.ORCID http://orcid.org/0000-0001-7181-4165
Pierre MaffreAix Marseille Univ, CNRS, IRD, INRAE, CEREGE, Aix-en-Provence, France.
Guolin XiongState Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, Frontiers Science Center for Critical Earth Material Cycling, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China.
Shu-Zhong ShenState Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, Frontiers Science Center for Critical Earth Material Cycling, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China.ORCID http://orcid.org/0000-0001-8380-0692
Feifei ZhangState Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, Frontiers Science Center for Critical Earth Material Cycling, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China. fzhang@nju.edu.cn.ORCID http://orcid.org/0000-0003-3277-445X

Funding

National Natural Science Foundation of China (National Science Foundation of China) 42322304
6 · The paper itself

Abstract

The moderate impact of rapid global warming on oceanic redox and biodiversity during the Paleocene-Eocene thermal maximum (PETM; ~55.9 Ma) contrasts with other hyperthermal events in Earth's history, and remains mostly unexplained. Here, we use lithium isotope (δ

Identifiers

PMID41093843
PMCPMC12528694

What OpenQuestion holds

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LicenceCC BY-NC-ND
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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.