Abstract

Arctic and subarctic ecosystems are changing rapidly in species composition and functioning as they warm twice as fast as the global average. It has been suggested that tree-less boreal landscapes may shift abruptly to tree-dominated states as climate warms. Yet, we insufficiently understand the conditions and mechanisms underlying tree establishment in the subarctic and arctic regions to anticipate how climate change may further affect ecosystem structure and functioning. We conducted a field experiment to assess the role of permafrost presence, micro-topography and shrub canopy on tree establishment in almost tree-less subarctic peatlands of northern Finland. We introduced seeds and seedlings of four tree-line species and monitored seedling survival and environmental conditions for six growing seasons. Our results show that once seedlings have emerged, the absence of permafrost can enhance early tree seedling survival, but shrub cover is the most important driver of subsequent tree seedling survival in subarctic peatlands. Tree seedling survival was twice as high under an intact shrub canopy than in open conditions after shrub canopy removal. Under unclipped control conditions, seedling survival was positively associated with dense shrub canopies for half of the tree species studied. These strong positive interactions between shrubs and trees may facilitate the transition from today’s treeless subarctic landscapes towards tree-dominated states. Our results suggest that climate warming may accelerate this vegetation shift as permafrost is lost, and shrubs further expand across the subarctic.

Highlights

  • Climate warming of arctic and subarctic ecosystems is advancing twice as fast as the global average (IPCC 2019)

  • Our results suggest that climate warming may accelerate this vegetation shift as permafrost is lost, and shrubs further expand across the subarctic

  • We report on a long-term field experiment aiming to understand the mechanisms that could facilitate tree expansion on currently almost tree-less permafrost peatlands at the southern edge of the permafrost distribution which is most vulnerable to climate warming (Sollid and Sørbel 1998; Luoto and Seppala 2003; Fronzek and others 2010)

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Summary

Introduction

Climate warming of arctic and subarctic ecosystems is advancing twice as fast as the global average (IPCC 2019). Permafrost degradation facilitates organic matter decomposition and the release of stored soil carbon as carbon dioxide (CO2) and methane (CH4) (Goulden and others 1998; Betts 2000; Schuur and others 2015). This can be relevant for permafrost peatlands that store approximately 14% of the global soil carbon (Malmer and others 2005; Tarnocai and others 2009; Olefeldt and others 2016). Woody plant canopies trap thicker snow layers than herbaceous plants, and because snow insulates the soil more effectively, this results in higher soil temperature and enhanced microbial activity that may further enhance decomposition rates and woody plant expansions (Sturm and others 2005; Zhang and others 2013; Hagedorn and others 2014)

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