Abstract

Climate change modifies the distribution and dominance of forest tree species, particularly near their distribution limits. This study used tree-ring width data for Pinus cembroides Zucc. at its distribution limits in Mexico and the SW USA to assess how tree populations responded to hydroclimatic variability. Indexed ring-width chronologies were built and correlated with climate and drought records at four marginal stands. We found that P. cembroides responds differently to climatic conditions depending on the bioclimatic and biogeographic conditions, with the forests situated in the driest area (Nuevo León) presenting the highest growth association to maximum temperatures and drought, while the forest situated in the wettest area (Puebla) was the least correlated to these hydroclimatic factors. In particular, dry and hot conditions, during the prior autumn and winter, reduced radial growth. Drought conditions could result in more vulnerable forests at the driest sites. These results advance our understanding of the radial growth responses of P. cembroides and similar widely distributed trees to climatic change near their biogeographical limits.

Highlights

  • Global climate change is predicted to have consequences for vegetation dynamics, causing profound changes in the distribution and mortality of trees and producing considerable alterations in forest structure, composition, and functioning [1,2]

  • This study evaluates the association of Pinus cembroides to climate variables in radial growth in four sites forming the species’ latitudinal and longitudinal distribution limits

  • Tree-ring widths ranged from 1.47 mm (Nuevo León) to 2.03 mm (California Sur)

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Summary

Introduction

Global climate change is predicted to have consequences for vegetation dynamics, causing profound changes in the distribution and mortality of trees and producing considerable alterations in forest structure, composition, and functioning [1,2]. Significant changes in the distribution and functioning of conifer forests (growth, mortality, reproduction) associated with altered precipitation regimes, severe droughts, and a notable increase in terrestrial temperature have recently been observed [3,4,5]. The natural variability of the climatic system depends, among other factors, on latitude, which determines the biogeographical frontiers or distribution limits of many trees [6]. The northern (leading edge) and southern (rear edge) distribution limits of a tree species should present different responses to climatic constraints, be it through local adaptations or by locally adjusting the phenotypic plasticity of the trees [7,8]. The vulnerability of certain trees, in terms of adaptation of their physiological functions to climatic and environmental

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