Evidence map›Paper›PMID 40395648›Full record

ArticleNational science review2025

Magnesium and boron isotope evidence for the generation of arc magma through serpentinite-mélange melting.

Xin-Yue Qiao, Jia-Wei Xiong, Yi-Xiang Chen, Jan C M De Hoog, Julian Pearce, Fang Huang, Zi-Fu Zhao, Kun Chen

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in National science review, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.

0numbers the graph read from it
0cells of the map it votes in
5citing 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

5 citing papers in PubMed.

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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

8 authors.

Xin-Yue QiaoState Key Laboratory of Lithospheric and Environmental Co-evolution, University of Science and Technology of China, Hefei 230026, China.
Jia-Wei XiongSchool of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
Yi-Xiang ChenState Key Laboratory of Lithospheric and Environmental Co-evolution, University of Science and Technology of China, Hefei 230026, China.
Jan C M De HoogSchool of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh EH9 3FE, UK.
Julian PearceSchool of Earth and Ocean Sciences, Cardiff University, Cardiff CF10 3AT, UK.
Fang HuangState Key Laboratory of Lithospheric and Environmental Co-evolution, University of Science and Technology of China, Hefei 230026, China.
Zi-Fu ZhaoState Key Laboratory of Lithospheric and Environmental Co-evolution, University of Science and Technology of China, Hefei 230026, China.
Kun ChenState Key Laboratory of Lithospheric and Environmental Co-evolution, University of Science and Technology of China, Hefei 230026, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Serpentinites play a crucial role in mass transport and volatile recycling in subduction zones, yet the mechanism for their contribution to the formation of arc magma remains elusive. Here, we investigate this issue by examining the magnesium (Mg) and boron (B) isotope compositions of volcanic rocks and forearc serpentinites from the South Sandwich Island arc. The volcanic rocks display δ

Indexed as

arc magmaB isotopecrust–mantle interactionMg isotopeserpentinite

Identifiers

PMID40395648
PMCPMC12089755

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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.