EGU22-4024
https://doi.org/10.5194/egusphere-egu22-4024
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Does vegetation shift in Arctic tundra upon permafrost degradation influence mineral element recycling in the topsoil?

Maëlle Villani1, Elisabeth Mauclet1, Yannick Agnan1, Arsène Druel2, Briana Jasinski3, Meghan Taylor4, Edward A.G. Schuur3, and Sophie Opfergelt1
Maëlle Villani et al.
  • 1Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium
  • 2Ecologie des Forêts Méditerranéennes (URFM), Institut national de recherche pour l'agriculture, l'alimentation et l'environnement (INRAE), Avignon, France
  • 3Center for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, USA
  • 4University of Vermont, Burlington, VT, USA

Climate change affects the Arctic and Subarctic regions by exposing previously frozen permafrost to thaw, unlocking nutrients, changing hydrological processes, and boosting plant growth. As a result, Arctic tundra is subject to a shrub expansion, called “shrubification” at the expense of sedge species. Depending on intrinsic foliar properties of these plant species, changes in foliar fluxes with shrubification in the context of permafrost degradation may influence topsoil mineral element composition. Despite the potential implications for the fate of organic carbon in the topsoil, this remains poorly quantified. Here, we investigate vegetation foliar and topsoil mineral element composition (mineral elements that influence organic carbon decomposition: Si, K, Ca, P, Mn, Zn, Cu, Mo and V) from a typical Arctic tundra at Eight Mile Lake (Alaska, USA) across a natural gradient of permafrost degradation. Results show that foliar element concentrations are higher (up to 9 times; Si, K, Mo, and for some species Zn) or lower (up to 2 times; Ca, P, Mn, Cu, V, and for some species Zn) in sedge than in shrub species. This induces different foliar flux with permafrost degradation and shrubification. As a result, a vegetation shift over ~40 years from sedges to shrubs has resulted in lower topsoil concentrations in Si, K, Zn and Mo (respectively of 52, 24, 20 and 51%) in poorly degraded permafrost sites compared to highly degraded permafrost sites. For other mineral elements (Ca, P, Mn, Cu and V), the vegetation shift has not induced a marked changed in topsoil concentrations at this stage of permafrost degradation. This observed change in topsoil composition involving beneficial or toxic elements for decomposers is likely to influence organic carbon decomposition. These data can serve as a first estimate to assess the influence of other shifts in vegetation in Arctic tundra such as sedge expansion with wildfires.

How to cite: Villani, M., Mauclet, E., Agnan, Y., Druel, A., Jasinski, B., Taylor, M., Schuur, E. A. G., and Opfergelt, S.: Does vegetation shift in Arctic tundra upon permafrost degradation influence mineral element recycling in the topsoil?, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-4024, https://doi.org/10.5194/egusphere-egu22-4024, 2022.

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