Evidence map›Paper›PMID 41271769›Full record

ArticleNature communications2025

Origin of Earth's hydrogen and carbon constrained by their core-mantle partitioning and bulk Earth abundance.

Yutaro Tsutsumi, Naoya Sakamoto, Kei Hirose, Shuhei Mita, Shunpei Yokoo, Han Hsu, Hisayoshi Yurimoto

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. 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

7 authors.

Yutaro TsutsumiDepartment of Earth and Planetary Science, The University of Tokyo, Bunkyo, Tokyo, Japan.
Naoya SakamotoInstitute for Integrated Innovations, Hokkaido University, Sapporo, Hokkaido, Japan.ORCID http://orcid.org/0000-0003-2335-1359
Kei HiroseDepartment of Earth and Planetary Science, The University of Tokyo, Bunkyo, Tokyo, Japan. kei@eps.s.u-tokyo.ac.jp.ORCID http://orcid.org/0000-0003-4366-7721
Shuhei MitaDepartment of Earth and Planetary Science, The University of Tokyo, Bunkyo, Tokyo, Japan.ORCID http://orcid.org/0009-0006-6153-4833
Shunpei YokooDepartment of Earth and Planetary Science, The University of Tokyo, Bunkyo, Tokyo, Japan.ORCID http://orcid.org/0000-0001-8081-5194
Han HsuDepartment of Physics, National Central University, Taoyuan City, Taiwan.ORCID http://orcid.org/0000-0003-1205-4770
Hisayoshi YurimotoInstitute for Integrated Innovations, Hokkaido University, Sapporo, Hokkaido, Japan.ORCID http://orcid.org/0000-0003-0702-0533

Funding

MEXT | Japan Society for the Promotion of Science (JSPS) 21H04968MEXT | Japan Society for the Promotion of Science (JSPS) 21H04985MEXT | Japan Society for the Promotion of Science (JSPS) 23KJ0479
6 · The paper itself

Abstract

Hydrogen and carbon concentrations in the Earth's core are yet known. Here we determined their metal/silicate partition coefficients (D) simultaneously under typical conditions of core formation and found that D

Identifiers

PMID41271769
PMCPMC12638987

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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.