Abstract

QuestionsHow do plant communities on zonal loamy vs. sandy soils vary across the full maritime Arctic bioclimate gradient? How are plant communities of these areas related to existing vegetation units of the European Vegetation Classification? What are the main environmental factors controlling transitions of vegetation along the bioclimate gradient?Location1700‐km Eurasia Arctic Transect (EAT), Yamal Peninsula and Franz Josef Land (FJL), Russia.MethodsThe Braun‐Blanquet approach was used to sample mesic loamy and sandy plots on 14 total study sites at six locations, one in each of the five Arctic bioclimate subzones and the forest–tundra transition. Trends in soil factors, cover of plant growth forms (PGFs) and species diversity were examined along the summer warmth index (SWI) gradient and on loamy and sandy soils. Classification and ordination were used to group the plots and to test relationships between vegetation and environmental factors.ResultsClear, mostly non‐linear, trends occurred for soil factors, vegetation structure and species diversity along the climate gradient. Cluster analysis revealed seven groups with clear relationships to subzone and soil texture. Clusters at the ends of the bioclimate gradient (forest–tundra and polar desert) had many highly diagnostic taxa, whereas clusters from the Yamal Peninsula had only a few. Axis 1 of a DCA was strongly correlated with latitude and summer warmth; Axis 2 was strongly correlated with soil moisture, percentage sand and landscape age.ConclusionsSummer temperature and soil texture have clear effects on tundra canopy structure and species composition, with consequences for ecosystem properties. Each layer of the plant canopy has a distinct region of peak abundance along the bioclimate gradient. The major vegetation types are weakly aligned with described classes of the European Vegetation Checklist, indicating a continuous floristic gradient rather than distinct subzone regions. The study provides ground‐based vegetation data for satellite‐based interpretations of the western maritime Eurasian Arctic, and the first vegetation data from Hayes Island, Franz Josef Land, which is strongly separated geographically and floristically from the rest of the gradient and most susceptible to on‐going climate change.

Highlights

  • Arctic tundra ecosystems occur in a broad circumpolar belt that extends from areas north of 80°N to forest–tundra areas south of 60°N, with mean July temperatures that vary from near 0°C to over 12°C

  • Examples exist for the Taymyr Peninsula, Russia (Matveyeva, 1998), the North America Arctic Transect (NAAT; Walker, Kuss, et al, 2011) and the

  • We describe the vegetation along the 1700-­km Eurasia Arctic Transect (EAT) that includes the Yamal Peninsula and Franz Josef Land (Figure 1)

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Summary

Introduction

Arctic tundra ecosystems occur in a broad circumpolar belt that extends from areas north of 80°N to forest–tundra areas south of 60°N, with mean July temperatures that vary from near 0°C to over 12°C. Cluster 2 contains the six tundra plots in the forest–tundra transition at Nadym with three highly diagnostic taxa (Carex globularis, Andromeda polifolia, Rubus chamaemorus) and one other diagnostic taxon (Rhododendron tomentosum) This cluster aligns with Cl. Oxycocco–Sphagnetea Br.-Bl. et Tx. ex Westhoff et al 1946, which contains dwarf shrub, sedge and peat moss vegetation of the Holarctic ombrotrophic bogs and wet heaths on extremely acidic soils.

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