Abstract

Earlier snowmelt changes spring stress exposure and growing-season length, possibly causing shifts in plant species dominance. If such shifts involve trees, this may lead to changes in treeline position. We hypothesized that earlier snowmelt would negatively affect the performance of tree seedlings near the treeline due to higher spring stress levels, but less so if seedlings were protected from the main stress factors of night frosts and excess solar radiation. We exposed seedlings of five European treeline tree species: Larix decidua, Picea abies, Pinus cembra, Pinus uncinata, and Sorbus aucuparia to two snow-cover treatments (early and late melting, with about two weeks difference) combined with reduced sky exposure during the day (shading) or night (night warming), repeated in two years, at a site about 200 m below the regional treeline elevation. Physiological stress levels (as indicated by lower Fv/Fm) in the first weeks after emergence from snow were higher in early-emerging seedlings. As expected, shade reduced stress, but contrary to expectation, night warming did not. However, early- and late-emerging seedlings did not differ overall in their growth or survival, and the interaction with shading was inconsistent between years. Overall, shading had the strongest effect, decreasing stress levels and mortality (in the early-emerging seedlings only), but also growth. A two-week difference in snow-cover duration did not strongly affect the seedlings, although even smaller differences have been shown to affect productivity in alpine and arctic tundra vegetation. Still, snowmelt timing cannot be discarded as important for regeneration in subalpine conditions, because (1) it is likely more critical in very snow-rich or snow-poor mountains or landscape positions; and (2) it can change (sub)alpine vegetation phenology and productivity, thereby affecting plant interactions, an aspect that should be considered in future studies.

Highlights

  • Changes in snow-cover duration are one of the ecologically most influential consequences of global climate change in high-mountain ecosystems

  • In the European Alps, snow-cover duration is clearly decreasing: snowmelt in spring has advanced by about 26 days, on average, between

  • We explicitly studied two potential stress factors after emergence from snow cover: cold-induced photoinhibition and freezing damage

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Summary

Introduction

Changes in snow-cover duration are one of the ecologically most influential consequences of global climate change in high-mountain ecosystems. Snow cover in the northern hemisphere has been decreasing in the last decades [1]. This trend is observed in many mountain areas [2,3,4,5], but depending on the local climate, some mountain ranges have experienced increases [6]. In the European Alps, snow-cover duration is clearly decreasing: snowmelt in spring has advanced by about 26 days, on average, between. This trend is observed across elevations up to 2500~3000 m, so including the current treeline and adjoining alpine areas, and is expected to continue in the coming decades [8,9]

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