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Recent changes in high-mountain plant community functional composition in contrasting climate regimes
K Steinbauer1, A Lamprecht2, M Winkler2
1GLORIA Coordination, Department of Integrative Biology and Biodiversity Research, University of Natural Resources and Life Sciences, 1190 Vienna, Austria; GLORIA Coordination, Institute for Interdisciplinary Mountain Research, Austrian Academy of Sciences, 1190 Vienna, Austria; UNESCO-Chair on Sustainable Management of Conservation Areas, Carinthia University of Applied Science, 9524 Villach, Austria; E.C.O. - Institut für Ökologie, 9020 Klagenfurt, Austria.
Alpine plant communities face climate warming. Studies show a shift from temperature to drought as the main driver, with vegetation changes observed across European mountains over 14 years.
Area of Science:
- Ecology
- Climate Change Biology
- Plant Community Ecology
Background:
- High-mountain plant communities are sensitive to abiotic factors, particularly temperature, making them vulnerable to climate warming.
- Rising temperatures increase evapotranspiration and alter precipitation, potentially causing severe water deficiencies in alpine ecosystems.
- Understanding these impacts requires comparing plant communities across diverse climatic gradients.
Purpose of the Study:
- To compare alpine plant communities along elevation and water availability gradients in the Alps, Apennines, and Crete.
- To identify relationships between community indices (traits, cover, diversity) and soil temperature/snow duration.
- To assess vegetation changes over a 14-year period (2001-2015) in response to climate change.
Main Methods:
- Field study comparing alpine plant communities across three distinct regions: NE-Alps (humid), Central Apennines (moderate), and Lefka Ori, Crete (summer-dry).
- Analysis of community-based indices: plant functional traits (Leaf Dry Matter Content, Specific Leaf Area), thermic vegetation indicator, life forms, vegetation cover, and diversity.
- Correlation with abiotic factors: soil temperature and snow duration, and temporal analysis of changes over 14 years.
Main Results:
- Plant community indices responded to temperature gradients in the Alps and Apennines, but this effect diminished in dry Crete, indicating a shift to drought as the primary filter.
- Leaf trait responses varied, suggesting drought impacts are evident even in the northern Mediterranean.
- Vegetation cover increased slightly across all regions; thermophilisation occurred in the Alps and Apennines, with declines in cold-adapted plants and increases in shrubs on Crete.
Conclusions:
- Alpine vegetation is shifting from temperature-driven to drought-driven dynamics, particularly in drier Mediterranean regions.
- While significant biodiversity loss is not yet observed, ongoing monitoring is crucial due to the threat to vulnerable alpine flora.
- Combined warming and drought impacts necessitate intensified monitoring for threatened alpine plant species, especially those in southern, dry areas or poorly adapted to drought in the north.
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