Evidence map›Paper›PMID 42115597›Full record

ArticleNature communications2026

Coupled sulfur-silicon isotopes reveal supracrustal origin of Archean continents.

Kun Shang, Jian Zhang, Zaicong Wang, Ian Cawood, Yawen Cui, Ming Li, Ruihong Chang, Yanan Shen, Guochun Zhao

Erratum issuedAbstract read
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. 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

5 · Who and what money

Authors and funding

9 authors.

Kun ShangNWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth and Planetary Sciences, The University of Hong Kong, Hong Kong SAR, China.ORCID http://orcid.org/0009-0000-5441-0003
Jian ZhangNWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth and Planetary Sciences, The University of Hong Kong, Hong Kong SAR, China. jian@hku.hk.ORCID http://orcid.org/0000-0002-6311-289X
Zaicong WangState Key Laboratory of Geological Processes and Mineral Resources, School of Earth and Planetary Sciences, China University of Geosciences, Wuhan, China.ORCID http://orcid.org/0000-0002-3584-1673
Ian CawoodNWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth and Planetary Sciences, The University of Hong Kong, Hong Kong SAR, China.ORCID http://orcid.org/0000-0002-3903-8714
Yawen CuiSchool of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.
Ming LiState Key Laboratory of Geological Processes and Mineral Resources, School of Earth and Planetary Sciences, China University of Geosciences, Wuhan, China.
Ruihong ChangNWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth and Planetary Sciences, The University of Hong Kong, Hong Kong SAR, China.ORCID http://orcid.org/0000-0002-1326-3622
Yanan ShenSchool of Earth and Space Sciences, University of Science and Technology of China, Hefei, China.ORCID http://orcid.org/0000-0001-8343-6763
Guochun ZhaoNWU-HKU Joint Centre of Earth and Planetary Sciences, Department of Earth and Planetary Sciences, The University of Hong Kong, Hong Kong SAR, China. gzhao@hku.hk.ORCID http://orcid.org/0000-0002-5429-0758

Funding

National Natural Science Foundation of China (National Science Foundation of China) 42025204National Natural Science Foundation of China (National Science Foundation of China) 42330211
6 · The paper itself

Abstract

The genesis of Archean continental crust through partial melting of hydrous mafic protolith is widely acknowledged, yet the origin of the mafic protolith remains highly contentious. Silicon isotopes and quadruple sulfur isotopes serve as particularly powerful tools in this regard, as they directly trace the source nature of the felsic continent. Here, we integrate whole-rock silicon and sulfur isotopic data of Neoarchean granitoids from the North China Craton to constrain the origin and pathway of their protoliths. These granitoids exhibit non-zero Δ³³S (0.01‰ to - 0.24‰) and elevated δ³⁰Si ( - 0.09‰ to -0.05‰), requiring a supracrustal source and contrasting with the previously reported mantle-like zircon δ

Identifiers

PMID42115597
PMCPMC13161363

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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.