4.6 Article

Growth and community responses of alpine dwarf shrubs to in situ CO2 enrichment and soil warming

Journal

NEW PHYTOLOGIST
Volume 191, Issue 3, Pages 806-818

Publisher

WILEY
DOI: 10.1111/j.1469-8137.2011.03722.x

Keywords

alpine treeline; dwarf shrub; elevated CO2; Empetrum hermaphroditum (crowberry); free air CO2 enrichment (FACE); soil warming; Vaccinium gaultherioides (northern bilberry); Vaccinium myrtillus (bilberry)

Categories

Funding

  1. Swiss National Science Foundation [31-061428.00, 315200-116861]
  2. Velux Foundation
  3. ANR-biodiversite
  4. CCES-ETH-Project
  5. Swiss State Secretariat for Education and Research [C07.0032]
  6. WSL
  7. University of Basel Botanical Institute
  8. Swiss Federal Office for the Environment
  9. 'Fonds quebecois de recherche sur la nature et les technologies'

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Rising CO2 concentrations and the associated global warming are expected to have large impacts on high-elevation ecosystems, yet long-term multifactor experiments in these environments are rare. We investigated how growth of dominant dwarf shrub species (Vaccinium myrtillus, Vaccinium gaultherioides and Empetrum hermaphroditum) and community composition in the understorey of larch and pine trees responded to 9 yr of CO2 enrichment and 3 yr of soil warming at the treeline in the Swiss Alps. Vaccinium myrtillus was the only species that showed a clear positive effect of CO2 on growth, with no decline over time in the annual shoot growth response. Soil warming stimulated V. myrtillus growth even more than elevated CO2 and was accompanied by increased plant-available soil nitrogen (N) and leaf N concentrations. Growth of Vaccinium gaultherioides and E. hermaphroditum was not influenced by warming. Vascular plant species richness declined in elevated CO2 plots with larch, while the number of moss and lichen species decreased under warming. Ongoing environmental change could lead to less diverse plant communities and increased dominance of the particularly responsive V. myrtillus in the studied alpine treeline. These changes are the consequence of independent CO2 and soil warming effects, a result that should facilitate predictive modelling approaches.

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