Evidence map›Paper›PMID 42481466›Full record

ArticleNature communications2026

Widespread tropical cyclone activity during the Late Paleozoic Ice Age.

Qing Yan, Sophia Macarewich, Nanxuan Jiang, David B Kemp, Dubin Huan, Christopher J Poulsen, Jinzhe Zhang, Zhongshi Zhang, Huijun Wang

Abstract 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. 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

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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

9 authors.

Qing YanState Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China. yanqing@mail.iap.ac.cn.ORCID http://orcid.org/0000-0001-5299-7824
Sophia MacarewichClimate and Global Dynamics Laboratory, NSF National Center for Atmospheric Research, Boulder, CO, USA.ORCID http://orcid.org/0000-0002-6263-3044
Nanxuan JiangNansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.
David B KempState Key Laboratory of Geomicrobiology and Environmental Changes and Hubei Key Laboratory of Critical Zone Evolution, School of Earth and Planetary Sciences, China University of Geosciences, Wuhan, China.ORCID http://orcid.org/0000-0002-5116-5046
Dubin HuanState Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.
Christopher J PoulsenDepartment of Earth Sciences, University of Oregon, Eugene, OR, USA.ORCID http://orcid.org/0000-0001-5104-4271
Jinzhe ZhangState Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.ORCID http://orcid.org/0000-0003-3951-6146
Zhongshi ZhangDepartment of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China.ORCID http://orcid.org/0000-0002-2354-1622
Huijun WangState Key Laboratory of Climate System Prediction and Risk Management, Nanjing University of Information Science and Technology, Nanjing, China.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Whether tropical cyclone (TC) activity prevailed during the Late Paleozoic Ice Age (LPIA)-the longest icehouse of the Phanerozoic-remains debated, owing to the paucity and ambiguity of sedimentary evidence. To help resolve this conflict, we combine a global compilation of 126 storm records spanning the LPIA ( ~ 360-260 Ma) with high-resolution (~25-km) TC-resolving simulations. We reveal a quasi-symmetric meridional distribution of TC genesis across the tropics during the LPIA, with TC tracks extending into high latitudes (>60°N/°S). This pattern aligns with the compiled widespread storm deposits from subtropical and tropical regions. During CO₂-driven glacial-interglacial transitions within the LPIA, we observe reduced global TC frequency and enhanced intensity, coinciding with poleward shifts in TC activity. The shifts are linked to spatially heterogeneous warming patterns and associated changes in atmospheric circulation. Our results help reconcile controversies regarding icehouse TC behavior and highlight that warming-induced poleward migration of TC activity is likely a climate state-independent characteristic of the Earth system.

Identifiers

PMID42481466
PMCPMC13500696

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