Abstract

Elevation gradients offer excellent opportunities to explore the climate sensitivity of vegetation. Here, we investigated elevation patterns of structural, chemical, and physiological traits in tropical tree species along a 1700–2700 m elevation gradient in Rwanda, central Africa. Two early-successional (Polyscias fulva, Macaranga kilimandscharica) and two late-successional (Syzygium guineense, Carapa grandiflora) species that are abundant in the area and present along the entire gradient were investigated. We found that elevation patterns in leaf stomatal conductance (gs), transpiration (E), net photosynthesis (An), and water-use efficiency were highly season-dependent. In the wet season, there was no clear variation in gs or An with elevation, while E was lower at cooler high-elevation sites. In the dry season, gs, An, and E were all lower at drier low elevation sites. The leaf-to-air temperature difference was smallest in P. fulva, which also had the highest gs and E. Water-use efficiency (An/E) increased with elevation in the wet season, but not in the dry season. Leaf nutrient ratios indicated that trees at all sites are mostly P limited and the N:P ratio did not decrease with increasing elevation. Our finding of strongly decreased gas exchange at lower sites in the dry season suggests that both transpiration and primary production would decline in a climate with more pronounced dry periods. Furthermore, we showed that N limitation does not increase with elevation in the forests studied, as otherwise most commonly reported for tropical montane forests.

Highlights

  • Tropical forests play a significant role as a carbon sink, currently dampening the ongoing rise in atmospheric CO2 [1]

  • The overall aim of this study is to explore how leaf and tree traits and resource use vary with climate along a tropical elevation gradient in Rwanda, located on the Albertine Rift in central Africa

  • Our results indicate that transpiration and CO2 uptake of tropical montane forests may decline in a climate with more pronounced dry periods

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Summary

Introduction

Tropical forests play a significant role as a carbon sink, currently dampening the ongoing rise in atmospheric CO2 [1]. Through their high rates of evapotranspiration, they strongly control land hydrology and energy partitioning, affecting both local and regional climate [2]. In spite of the importance of tropical forests for global, regional, and local climate and climate change, their climate sensitivity is poorly known compared to that of temperate and boreal forests [3,4,5]. The montane tropics are likely to undergo considerable change under global warming, with plants facing dual challenges of climatic change and invading lowland species [8,9]. A better understanding of the climate sensitivity of tropical tree species is fundamental to forecasting these changes

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