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Widespread thermophilization but weak link to climate warming in Europe’s summit plant communities

  • Johannes Hausharter
  • , Johannes Wessely
  • , Norbert Helm
  • , Kryštof Chytrý
  • , Karl Hülber
  • , Dietmar Moser
  • , Mary Carolina García Lino
  • , Katharina Kagerl
  • , Andrea Lamprecht
  • , Jonathan Lenoir
  • , Andreas Kollert
  • , Andreas Mayr
  • , Martin Rutzinger
  • , Philippe Choler
  • , Pieter De Frenne
  • , Jonas J. Lembrechts
  • , Otar Abdaladze
  • , Chris Andrews
  • , Peter Barančok
  • , José Luis Benito-Alonso
  • Eva M. Cañadas, Michele Carbognani, Pau Carnicero, Emmanuel Corcket, Michele Di Musciano, Jan Dick, Khatuna Gigauri, Andreas Hilpold, Juan J. Jiménez, Juan Lorite, Umberto Morra di Cella, Panagiotis Nyktas, Simone Orsenigo, Andrej Palaj, Martina Petey, Mihai Pușcaș, Christophe Randin, Ilektra Remoundou, Christian Rixen, Patrick Saccone, Angela Stanisci, Jean Paul Theurillat, Tudor Mihai Ursu, Thomas Vanneste, Raphael S. von Büren, Sonja Wipf, Manuela Winkler, Harald Pauli, Stefan Dullinger

Publications: Contribution to journal › Article › Peer Reviewed

Abstract

Recent changes in alpine vegetation are often attributed to climate warming, particularly community composition shifts towards more warmth-associated species, or thermophilization. Here we assess the link between thermophilization and warming across 53 European mountain summits. We combine long-term macroclimatic and microclimatic temperature time series with vegetation surveys in 724 permanent plots, monitored over 21 years, to evaluate a possible thermophilization signal and relate it to rates of change in 10 temperature metrics. We find evidence of both thermophilization of alpine plant communities and an increase in temperatures. However, although these two trends are related when averaged across mountain regions, their relationship is weak at the individual plot scale, especially when considering microclimatic temperature metrics. Instead, substrate conditions and particularly the availability of thermophilic colonizers in the surrounding vegetation have a major influence on plot-level thermophilization rates. We conclude that the response of plant communities to climate change strongly depends on the abiotic and biotic context, and intensified monitoring efforts are needed to reduce the resulting uncertainties.

Original languageEnglish
JournalNature Ecology and Evolution
DOIs
Publication statusPublished - 14 Aug 2026

Funding

This study was funded by the European Research Council under the European Union Horizon 2020 Research and Innovation programme (MICROCLIM; grant agreement ID 883669). A.P. and P.B. were financially supported by the VEGA grant agency (project no. 2/0026/25). A.S. received funding by Biodiversa+, the European Biodiversity Partnership, in the context of the PRESINMED project under the 2023–2024 BiodivNBS joint call (CUP: H43C25000280001). C. Randin was financially supported by Communes d’Orsières et de Val de Bagne; Département de la culture et des sports du Valais, Service de la Culture; Fondation Ignace Mariétan; Service des forêts, de la nature et du paysage du canton du Valais; Société académique de Genève; Swiss National Science Foundation; Swiss Federal Office for the Environment; University of Lausanne. P.D.F. received funding from the European Research Council under the European Union Horizon 2020 Research and Innovation program (ERC Consolidator Grant, CanopyChange; grand agreement ID 101124948). T.-M.U. was supported through the Nucleu program as part of the 2022–2027 National RDI Plan, funded by MCID (project no. PN23020401, contract no. 7 N/03.01.2023) and through the RECOVER project, funded by UEFISCDI.

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action

Austrian Fields of Science 2012

  • 106003 Biodiversity research
  • 106050 Vegetation science
  • 106030 Plant ecology

Keywords

  • Alpine plants
  • Climate Change
  • Europe
  • Mountain summits
  • Thermophilization

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