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Biogeography 2026

Conference at University of Bayreuth, Germany | April 29 – May 2, 2026

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Subarctic cold spot Faroe Islands shows decreasing floristic diversity and no thermophilization in summit vegetation over the past two decades.

Peter Wolff1, Johanna Alberg2, Leander Beierkuhnlein1, Anna-Maria Fossa2, Kolbrun Haraldsstovu2, Andreas von Hessberg1, Stefan Wirth1, Anke Jentsch1
1 Disturbance Ecology and Vegetation Dynamics, University of Bayreuth, Germany
2 Botany, The Faroe Islands National Museum, Faroe Islands

P 22 in Postersession

The Faroe Islands represent a subarctic, mountainous, ‘cold spot’. However, it is currently difficult to predict whether the archipelago’s climate is warming or cooling as a result of global warming (due to a possible weakening of the North-Atlantic-Current).


Here, we present novel data on plant community dynamics from floristic summit monitoring over two decades on weathered basalt volcanic bedrock – as part of the Global Observation Research Initiative on Alpine Environments (GLORIA). Richness and abundance of angiosperm and cryptogam species was recorded across an altitudinal gradient from 372 m - 752 m asl. Floristic pattern was resurveyed between 2005 - 2025. Here, we present plant community dynamics along with novel metrics for analyzing “winner” and “loser” species.


The total summit vegetation species pool of Faroe Islands consists of 80 plant species (50 forbs, 24 graminoids, 6 dwarf shrubs, 20 mosses, 9 lichens). Bryophytes dominate vegetation cover on higher summits, graminoids on lower summits. However, although the rate of richness change across continental European mountain summits is generally increasing, which has been correlated with rising temperatures, our data from the Faroe Islands suggest that more species have disappeared than newly appeared. Thus, we present evidence of local species loss.

Remarkably, species redistribution dynamics at Faroe Islands over the last two decades result in a lower “Thermophilization Indicator” D = -0.023 (S2025 – S2005) than the European average D = 0.054. Such a decrease in thermophilization of mountain summit vegetation has rarely been presented elsewhere so far.

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