Evidence map›Paper›PMID 41564180›Full record

ArticleScience advances2026

Dynamic redox-promoted iron and nutrient cycling drove graptolite evolution across the Ordovician-Silurian transition.

Zhen Qiu, Caineng Zou, Jiaqiang Zhang, Aiguo Dong, Weiliang Kong, Yijun Xiong, Paul B Wignall, Ming Li, Zaicong Wang, Xiangkun Zhu and 1 more

Abstract read
In one paragraph

Article in Science advances, 2026. 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.

Zhen QiuResearch Institute of Petroleum Exploration & Development, China National Petroleum Corporation, Beijing, China.ORCID 0000-0003-1886-1821
Caineng ZouResearch Institute of Petroleum Exploration & Development, China National Petroleum Corporation, Beijing, China.ORCID 0009-0002-2331-5278
Jiaqiang ZhangSchool of Geoscience and Technology, Southwest Petroleum University, Chengdu, China.
Aiguo DongInstitute of Earth Sciences, China University of Geosciences (Beijing), Beijing, China.ORCID 0000-0002-0633-4904
Weiliang KongResearch Institute of Petroleum Exploration & Development, China National Petroleum Corporation, Beijing, China.
Yijun XiongSchool of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.ORCID 0009-0004-7689-7157
Paul B WignallSchool of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.ORCID 0000-0003-0074-9129
Ming LiState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan, China.ORCID 0000-0001-8517-2933
Zaicong WangState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan, China.ORCID 0000-0002-3584-1673
Xiangkun ZhuMNR Key Laboratory of Isotope Geology, MNR Key Laboratory of Deep-Earth Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China.ORCID 0000-0002-8407-6883
Simon W PoultonSchool of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK.ORCID 0000-0001-7621-189X

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Graptolites were abundant and cosmopolitan zooplankton in Early Paleozoic oceans, but a prominent change in species occurred across the Late Ordovician mass extinction. We use ocean redox, iron isotope (δ

Identifiers

PMID41564180
PMCPMC12822635

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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.