Abstract

Low temperatures are crucial for the formation of the alpine treeline worldwide. Since soil temperature in the shade of tree canopies is lower than in open sites, it was assumed that self-shading may impair the trees’ root growth performance. While experiments with tree saplings demonstrate root growth impairment at soil temperatures below 5–7°C, field studies exploring the soil temperature – root growth relationship at the treeline are missing. We recorded soil temperature and fine root abundance and dynamics in shaded and sun-exposed areas under canopies of isolated Pinus cembra trees at the alpine treeline. In contrast to the mentioned assumption, we found more fine root biomass and higher fine root growth in colder than in warmer soil areas. Moreover, colder areas showed higher fine root turnover and thus lower root lifespan than warmer places. We conclude that P. cembra balances enhanced fine root mortality in cold soils with higher fine root activity and by maintaining higher fine root biomass, most likely as a response to shortage in soil resource supply. The results from our study highlight the importance of in situ measurements on mature trees to understand the fine root response and carbon allocation pattern to the thermal growth conditions at the alpine treeline.

Highlights

  • The alpine treeline is one of the most conspicuous vegetation boundaries on earth, which has been studied by ecologists and geographers for decades

  • The results support our first hypothesis on the biological significance of the afternoon temperature regime, but they do not support the second and third hypothesis concerning the temperature influence on fine root biomass and productivity

  • The size of the soil temperature differences between shaded and sunny patches in the plots is displayed by the temperature maps produced on August 1, and it is evident from the long-term soil temperature measurements in July/August 2012 which show a nearly 2 Kelvin warmer soil in mid-summer in sunny plot areas

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Summary

Introduction

The alpine treeline is one of the most conspicuous vegetation boundaries on earth, which has been studied by ecologists and geographers for decades. Microclimatic measurements at various treelines indicate that the elevational position of the alpine treeline apparently is more closely related to soil than to air temperature (e.g., Sveinbjörnsson, 2000; Körner and Hoch, 2006; Körner, 2012a). According to Körner (2012a), this correlation does not necessarily show a more prominent soil temperature than air temperature effect on tree growth, but may reflect lower diurnal and seasonal variation in soil than air temperature at the treeline (Körner and Paulsen, 2004). The apparently critical temperature of ∼6.7◦C experienced by treeline trees may not directly relate to a low temperature threshold of biological processes at this temperature (Körner, 1998, 2012a)

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