Abstract

Extreme climatic events that are expected under global warming expose forest ecosystems to drought stress, which may affect the growth and productivity. We assessed intra-annual growth responses of trees to soil water content in species belonging to different functional groups of tree-ring porosity. We pose the hypothesis that species with contrasting carbon allocation strategies, which emerge from different relationships between wood traits and canopy architecture, display divergent growth responses to drought. We selected two diffuse-porous species (Acer saccharum and Betula alleghaniensis) and two ring-porous species (Quercus rubra and Fraxinus americana) from the mixed forest of Quebec (Canada). We measured anatomical wood traits and canopy architecture in eight individuals per species and assessed tree growth sensitivity to water balance during 2008–2017 using the standardized precipitation evapotranspiration index (SPEI). Stem elongation in diffuse-porous species mainly depended upon the total number of ramifications and hydraulic diameter of the tree-ring vessels. In ring-porous species, stem elongation mainly depended upon the productivity of the current year, i.e., number of vessels and basal area increment. Diffuse-porous and ring-porous species had similar responses to soil water balance. The effect of soil water balance on tree growth changed during the growing season. In April, decreasing soil temperature linked to wet conditions could explain the negative relationship between SPEI and tree growth. In late spring, greater water availability affected carbon partitioning, by promoting the formation of larger xylem vessels in both functional groups. Results suggest that timings and duration of drought events affect meristem growth and carbon allocation in both functional groups. Drought induces the formation of fewer xylem vessels in ring-porous species, and smaller xylem vessels in diffuse-porous species, the latter being also prone to a decline in stem elongation due to a reduced number of ramifications. Indeed, stem elongation of diffuse-porous species is influenced by environmental conditions of the previous year, which determine the total number of ramifications during the current year. Drought responses in different functional groups are thus characterized by different drivers, express contrasting levels of resistance or resilience, but finally result in an overall similar loss of productivity.

Highlights

  • A reliable understanding of tree growth responses to environmental conditions is important in confronting the changes caused by the global warming

  • The mean maximum SPEI3 was 1.31, with peaks observed in April during 2011 (SPEI3 = 1.7) and 2016 (SPEI3 = 1.8), in February of 2008 (SPEI3 = 2.1) and 2013 (SPEI3 = 0.9), and in October during 2010 (SPEI3 = 1.8) and 2012 (SPEI3 = 0.5)

  • The maximum standardized precipitation evapotranspiration index (SPEI) was observed in June (2014, SPEI3 = 1.0), July (2009, SPEI3 = 1.3), and August (2015, SPEI3 = 0.6)

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Summary

Introduction

A reliable understanding of tree growth responses to environmental conditions is important in confronting the changes caused by the global warming. Allometric scaling among the different plant organs drives primary and secondary growth toward convergent patterns to changing environmental conditions, leading to adjustments in biomass allocation and sapwood area (Petit et al, 2018). Ring-porous and diffuse-porous species are expected to undergo contrasting growth responses to seasonal stresses, such as drought events. Given that these groups demonstrate divergent seasonal patterns in their developmental phases (Barbaroux and Bréda, 2002; Delpierre et al, 2016), they could manifest contrasting consequences in terms of resource partitioning between radial growth and stem elongation

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