Abstract

Drought is a major constraint of forest productivity and tree growth across diverse habitat types. In this study, we investigated the drought responses of four conifer species growing within two locations of differing elevation and climatic conditions in northern Mexico. Two species were selected at a mesic site (Cupressus lusitanica Mill., Abies durangensis Martínez) and the other two species were sampled at a xeric site (Pinus engelmannii Carr., Pinus cembroides Zucc.). Using a dendrochronological approach, we correlated the radial-growth series of each species and the climatic variables. All study species positively responded to wet-cool conditions during winter and spring. Despite the close proximity of species at a mesic site, A. durangensis had high responsiveness to hydroclimatic variability, but C. lusitanica was not responsive. At the xeric site, P. engelmannii and P. cembroides were very responsive to drought severity, differentiated only by the longer time scale of the response to accumulated drought of P. engelmannii. The responsiveness to hydroclimate and drought of these tree species seems to be modulated by site conditions, or by the functional features of each species that are still little explored. These findings indicate that differentiating between mesic and xeric habitats is a too coarse approach in diverse forests with a high topographic heterogeneity.

Highlights

  • The hydroclimatic variability experienced by forests has shown differential responsiveness in recent decades as a consequence of global climate change [1]

  • We found that a fir (Abies) species dominant in mesic habitats (A. durangensis) showed the highest responsiveness to drought and water availability, refuting our main hypothesis and highlighting the relevance of dry spells as drivers of forest dynamics in sites where water availability is usually high

  • The suitability of the species for dendrochronology was adequate, except for C. lusitanica (Table 1), which proved to be a complacent species with little responsiveness to hydroclimatic variability

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Summary

Introduction

The hydroclimatic variability experienced by forests has shown differential responsiveness in recent decades as a consequence of global climate change [1]. Among the effects of climate warming, there has been an increase in water deficit, both in intensity and duration [2]. Droughts reduce radial growth and alter the hydraulic conductivity of trees [6,7,8], with a negative impact on carbon sequestration [9,10] and forest productivity [11,12]. Given that aridity is expected to intensify in the future in many forested areas, this may have negative and long-term implications on forest productivity [7,13]. These effects of drought stress on growth and productivity may differ between forest type and tree species [7].

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