The impacts of climate change on alpine summit floras have been widely investigated. However, only few studies included alpine grasslands and generally concluded that snowbeds, with a long snow cover duration and a short growing season, and windy ridges, with a short snow cover duration and strong winter frosts, are the most sensitive alpine grasslands. However, these habitats were mostly investigated in different regions, where local factors (e.g. nitrogen deposition, grazing) can co-vary with climate changes, potentially obscuring differences between habitats. Here, we focused on the Zermatt region (Swiss Alps) to investigate the impacts of climate change on snowbeds and windy ridges. Forty-three exhaustive historical plant inventories on windy ridges (acidophilic or basophilic) and 31 inventories in snowbeds (typical or wet) were repeated in quasi-permanent plots after approximately 23 years. Historical and recent records were compared with the Simpson index, Bray–Curtis dissimilarity, a PCA, ecological indicator values and the frequency and cover changes of species. There was a general increase in α-diversity and a decrease in β-diversity (homogenisation). Most of the new species in the plots were generalists from surrounding grasslands. The plant composition tended to be more thermophilous on acidophilic windy ridges and in typical snowbeds. The flora of acidophilic windy ridges became more similar to that of basophilic windy ridges and more eutrophic. We interpreted this as possibly arising from fertilisation by the aeolian dust deposition coming from the expanding glacial moraine in the valley. In snowbeds, the species indicated increasingly drier conditions, especially in wet snowbeds. Warming climate induces lower snowfall and earlier snowmelt, leading to a shorter snow cover duration. Hence, wet snowbeds are certainly among the most threatened plant communities by climate change in the Alps.
Salicion herbaceaeElynionSnow cover Temperature Quasi-permanent plots Vegetation dynamics Switzerland
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We are grateful to J.-L. Richard, B. Bressoud, C. Käsermann, S. Krähenmann, F. Meyer and S. Reist who collected the historical data, to A. Steiner who transmitted them to us, to M. Vust for his help in lichen identification and to J. Alexander for English editing. We also thank the Burgergemeinde Zermatt for authorising this study on their properties and the Zermatt Bergbahnen AG for offering the travelling costs for the cable cars during fieldwork.
Compliance with ethical standards
Conflict of interest
The authors declare that they have no conflict of interest.
Declaration of authorship
All authors designed the study, LL and SM inventoried the plots in the fields and analysed the data under the advices of MM and PV, and all authors contributed to the manuscript.
The authors declare that they respected ethical standards.
The investigation in the field was conducted with authorisation of the Burgergemeinde Zermatt.
Klein G, Rebetez M, Rixen C, Vitasse Y (2018) Unchanged risk of frost exposure for subalpine and alpine plants after snowmelt in Switzerland despite climate warming. Int J Biometeorol 62:1755–1762CrossRefGoogle Scholar
Maliniemi T, Kapfer J, Saccone P, Skog A, Virtanen R (2018) Long-term vegetation changes of treeless heath communities in northern Fennoscandia: links to climate change trends and reindeer grazing. J Veg Sci 29:469–479CrossRefGoogle Scholar
Steiner A (2002) Die Vegetation der Gemeinde Zermatt. Geobot Helvet 74:1–204Google Scholar
Stevens CJ, Thompson K, Grime JP, Long CJ, Gowing DJG (2010) Contribution of acidification and eutrophication to declines in species richness of calcifuge grasslands along a gradient of atmospheric nitrogen deposition. Funct Ecol 24:478–484CrossRefGoogle Scholar
Stocker TF, Qin D, Plattner GK et al (2013) Technical Summary. In: Stocker TF, Qin D, Plattner GK (eds) Climate change 2013: the physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, CambridgeGoogle Scholar
R Core Team (2017) R: a language and environment for statistical computing. R Foundation for Statistical Computing, Vienna. http://www.r-project.org/. Accessed 17 Apr 2019
Virtanen R, Eskelinen A, Gaare E (2003) Long-term changes in alpine plant communities in Norway and Finland. In: Nagy L, Grabherr G, Körner C, Thompson DBA (eds) Alpine biodiversity in Europe. Springer, Berlin, pp 411–422CrossRefGoogle Scholar
Vitasse Y, Rebetez M, Filippa G, Cremonese E, Klein G, Rixen C (2017) ‘Hearing’ alpine plants growing after snowmelt: ultrasonic snow sensors provide long-term series of alpine plant phenology. Int J Biometeorol 61:349–361CrossRefGoogle Scholar
Vittoz P, Bodin J, Ungricht S, Burga C, Walther GR (2008) One century of vegetation change on Isla Persa, a nunatak in the Bernina massif in the Swiss Alps. J Veg Sci 19:671–680CrossRefGoogle Scholar
Vittoz P, Dussex N, Wassef J, Guisan A (2009a) Diaspore traits discriminate good from weak colonisers on high-elevation summits. Basic Appl Ecol 10:508–515CrossRefGoogle Scholar
Vittoz P, Randin CF, Dutoit A, Bonnet F, Hegg O (2009b) Low impact of climate change on subalpine grasslands in the Swiss Northern Alps. Glob Change Biol 15:209–220CrossRefGoogle Scholar
Vonlanthen CM, Bühler A, Veit H, Kammer PM, Eugster W (2006a) Alpine plant communities: a statistical assessment of their relation to microclimatological, pedological, geomorphological, and other factors. Phys Geogr 27:137–154CrossRefGoogle Scholar
Vonlanthen CM, Kammer PM, Eugster W, Bühler A, Veit H (2006b) Alpine vascular plant species richness: the importance of daily maximum temperature and pH. Plant Ecol 184:13–25CrossRefGoogle Scholar