Evidence map›Paper›PMID 41417910›Full record

ArticleScience advances2025

The asynchronous rise of Northern Hemisphere alpine floras reveals general responses of biotic assembly to orogeny and climate change.

Wenna Ding, Richard H Ree, Michael R May, Philipp Brun, Oskar Hagen, Dirk N Karger, Alexander Skeels, Loïc Pellissier, Yaowu Xing, Niklaus E Zimmermann

Abstract read
In one paragraph

Article in Science advances, 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

10 authors.

Wenna DingState Key Laboratory of Plant Diversity and Specialty Crops, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, China.ORCID 0000-0002-0446-8431
Richard H ReeDepartment of Collections, Conservation, and Research, Field Museum, 1400 S DuSable Lake Shore Drive, Chicago, IL 60605, USA.ORCID 0000-0003-1898-3335
Michael R MayDepartment of Evolution and Ecology, University of California Davis, 2320 Storer Hall, One Shields Avenue, Davis, CA 95616, USA.ORCID 0000-0002-5031-4820
Philipp BrunSwiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, 8903 Zürich, Switzerland.ORCID 0000-0002-2750-9793
Oskar HagenCenter for Critical Computational Studies (C3S), Goethe University Frankfurt, Theodor-W.-Adorno-Platz 1, 60629 Frankfurt am Main, Germany.ORCID 0000-0002-7931-6571
Dirk N KargerSwiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, 8903 Zürich, Switzerland.ORCID 0000-0001-7770-6229
Alexander SkeelsResearch School of Biology, Australian National University, Canberra 0200, Australia.ORCID 0000-0002-9973-4703
Loïc PellissierSwiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, 8903 Zürich, Switzerland.ORCID 0000-0002-2289-8259
Yaowu XingState Key Laboratory of Plant Diversity and Specialty Crops, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, China.ORCID 0000-0001-6709-4492
Niklaus E ZimmermannSwiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, 8903 Zürich, Switzerland.ORCID 0000-0003-3099-9604

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Understanding how biotic assembly processes responded to past geoclimatic changes is key to explaining the origins of mountain biodiversity and the causes of regional disparities in species richness. Here, we jointly reconstructed geographic ranges and biome-niche evolution for 34 diverse plant clades across five major Northern Hemisphere mountain systems and quantified how late Neogene cooling increased arctic-alpine habitat connections across regions. We reveal that, while alpine floras originated asynchronously and were assembled through distinct evolutionary processes over the past 30 million years, general biological responses to orogeny and environmental change are apparent. Across regions, in situ diversification was consistently elevated during heightened phases of tectonic activity. Over the past 5 million years, enhanced arctic-alpine connectivity facilitated biotic interchange and positioned the boreal-arctic region as a major biogeographic crossroads linking Eurasia and North America.

Indexed as

Climate ChangePlantsArctic RegionsBiodiversityBiological EvolutionEcosystemGeographyPhylogeny

Identifiers

PMID41417910
PMCPMC12716423

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.