EGU26-2968, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-2968
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 04 May, 16:35–16:45 (CEST)
 
Room 1.85/86
Winter climate or species-specific traits? Controls on tundra winter nitrogen uptake along an Arctic climate gradient
Laura Helene Rasmussen1,2, Louise Rütting3, and Anders Michelsen4
Laura Helene Rasmussen et al.
  • 1University of Copenhagen, Institute for Mathematical Sciences, Data science laboratory, København K, Denmark (lhr@ign.ku.dk)
  • 2University of Tromsø, Institute for Geosciences, Tromsø, Norway
  • 3Chair of Soil and Plant Systems, Brandenburg University of Technology Cottbus-Senftenberg, Cottbus, Germany
  • 4University of Copenhagen, Institute for Biology, Terrestrial ecosystem sciences, København Ø, Denmark

Nitrogen (N) availability is a point of competition between tundra plants in a warming Arctic, where shrubs are spreading. Soil N mobilization from microbial mineralization can happen year round, and if some plants are able to access N during winter, they will have competitive advantages during warming winters with more N turnover. We therefore compared access to and retention of N during freeze-in to late winter in tundra plants from different tundra sites and explored how this may be linked to root biomass and plant functional type specific traits.

 We used 15N tracers in mesocosms from around Greenland, spanning a climate gradient from High- to Subarctic climates, and analyzed N uptake and retention species-specifically in stems and leaves, and in roots, microbes and in soil solution at four different winter stages along the climate gradient. We further measured the N uptake during a simulated late winter warming event.

We found that roots and aboveground biomass took up and retained 3-8 % of the early winter-released tracer N, but that early microbial N recovery of up to 50% dominated the ecosystem N retention. Most root N uptake was found in the Low Arctic, where continuous uptake was indicated. Least winter-released 15N overall was recovered in the High Arctic ecosystem, whereas the Subarctic ecosystem had the highest 15N recovery in plant biomass, especially in stems of deciduous shrubs. While evergreen shrubs, especially Empetrum nigrum, were overall most successful at acquiring and retaining winter-released  N with the current vegetation composition, the deciduous shrub Salix arctica stood out as most effective per unit biomass. 

We conclude that plant-specific traits and strategies, as well as climate, controlled tundra plant N access and retention during winter. Our results reveal that tundra plants access N during winter, but that plants in the Subarctic could be better adapted to access future increased winter N compared to the High Arctic. Across climates, species-specific winter N acquisition must be considered when explaining the expansion of shrubs in the Arctic tundra.

tundra plant N access and retention during winter is controlled by plant-specific traits and strategies as well as climate. Furthermore,  species-specific winter N access and acquisition must be considered when explaining the expansion of shrubs in the Arctic tundra.

How to cite: Rasmussen, L. H., Rütting, L., and Michelsen, A.: Winter climate or species-specific traits? Controls on tundra winter nitrogen uptake along an Arctic climate gradient, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-2968, https://doi.org/10.5194/egusphere-egu26-2968, 2026.