Skip to main content
Dryad

Long-term low-level nutrient additions significantly impact a low arctic mesic tundra plant community, but species responses differ from high-level fertilization: Implications for predicting climate warming impacts

Data files

Abstract

Arctic climate warming is expected to enhance the soil’s supply of growth-limiting nutrients, resulting in changes in plant community composition. Much of our understanding of nutrient influences on tundra plants is derived from experiments with very high levels of fertilization. Here, aboveground biomass of all species in a mesic birch hummock community, and shoot extension of Betula glandulosa, were measured in response to 11-19 years of factorial annual low-level nitrogen (N) and phosphorus (P) additions that simulate climatically realistic anticipated increases in soil fertility. Only the low N addition treatment had significant effects, enhancing the mosses and some infrequent vascular species’ biomass, reducing others, while the dominant shrubs were unaffected. Hence, overall community composition was altered, but in markedly different ways than classic high-level fertilization responses. By contrast, when measured in much larger sampling areas (9 m2), birch shrub new shoot extension was clearly stimulated by the separate low-level N and P additions, and even more so by their combination, indicating that its growth was NP co-limited. Overall, our results demonstrate that this tundra plant community is sensitive to low-level (climatically-realistic) increases in nutrient availability, and suggest that changes will be slow (multiple decades), and likely to favour species whose growth is primarily N-limited.