Evidence map›Paper›PMID 39583328›Full record

ArticleCommunications earth & environment2024

The climatic pattern of East Asia shifted in response to cratonic thinning in the Early Cretaceous.

Wenbo Wang, Xu Chu, Jian Zhang, Ying Cui, Xuegen Chen, Yue Wang, Shangguo Su

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Communications earth & environment, 2024. 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.

Wenbo WangSchool of Earth Sciences and Resources, China University of Geosciences, Beijing, 100010 China.ORCID 0009-0001-0774-1114
Xu ChuDepartment of Earth Sciences, University of Toronto, Toronto, ON M5S 3B1 Canada.ORCID 0000-0002-6816-1076
Jian ZhangDepartment of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871 China.ORCID 0000-0002-5728-9066
Ying CuiDepartment of Earth and Environmental Studies, Montclair State University, Montclair, NJ 07043 USA.ORCID 0000-0003-1057-4369
Xuegen ChenSchool of Earth Sciences and Resources, China University of Geosciences, Beijing, 100010 China.
Yue WangResearch School of Earth Sciences, The Australian National University, Canberra, ACT 0200 Australia.
Shangguo SuSchool of Earth Sciences and Resources, China University of Geosciences, Beijing, 100010 China.ORCID 0000-0002-0812-672X

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

In response to westward subduction of the Paleo-Pacific, the North China Craton experienced the uplift of an eastern coastal plateau followed by subsidence in the Early Cretaceous, which potentially drove a shift in climatic patterns. Here we use the oxygen isotope ratios of garnets from magmatic-hydrothermal ore systems to infer the origins and signatures of mineralization fluids during this tectonic transition. The garnet oxygen isotope values range from approximately -11.4 to +13.5‰, with extremely depleted oxygen isotope ratios exclusively found in the northern margin, indicating extensive involvement of meteoric and lacustrine fluid in the back-arc hinterland. This geological record aligns with climate modeling exhibiting that the coastal plateau amplified northeastward transport of moisture from tropical Tethyan Ocean. The long-distance transport strongly depleted

Indexed as

GeochemistryGeology

Identifiers

PMID39583328
PMCPMC11581977

What OpenQuestion holds

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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.