Abstract

To anticipate European climate scenarios for the end of the century, we explored the climate gradient within the REINFFORCE (RÉseau INFrastructure de recherche pour le suivi et l’adaptation des FORêts au Changement climatiquE) arboreta network, established in 38 sites between latitudes 37° and 57°, where 33 tree species are represented. We aim to determine which climatic variables best explain their survival and growth, and identify those species that are more tolerant of climate variation and those of which the growth and survival future climate might constrain. We used empirical models to determine the best climatic predictor variables that explain tree survival and growth. Precipitation-transfer distance was most important for the survival of broadleaved species, whereas growing-season-degree days best explained conifer-tree survival. Growth (annual height increment) was mainly explained by a derived annual dryness index (ADI) for both conifers and broadleaved trees. Species that showed the greatest variation in survival and growth in response to climatic variation included Betula pendula Roth, Pinus elliottii Engelm., and Thuja plicata Donn ex D.Don, and those that were least affected included Quercus shumardii Buckland and Pinus nigra J.F.Arnold. We also demonstrated that provenance differences were significant for Pinus pinea L., Quercus robur L., and Ceratonia siliqua L. Here, we demonstrate the usefulness of infrastructures along a climatic gradient like REINFFORCE to determine major tendencies of tree species responding to climate changes.

Highlights

  • Predicted scenarios for the European climate at the end of the century point to a slight reduction in annual precipitation and an extension of rain seasons

  • Eucalyptus spp. and Quercus shumardii Buckland are represented by only one provenance

  • In the present climate range, we concluded that the best predictors for plant survival differed between conifer and broadleaf

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Summary

Introduction

Predicted scenarios for the European climate at the end of the century point to a slight reduction in annual precipitation and an extension of rain seasons. The frequency of occurrence of extreme events is expected to increase, the number of days with spring frost and periods of water stress for plants, leading to a decrease in productivity, and an increase in pest and disease activity [2,3,4]. Extreme events, such as drought and heat waves, have already been identified as a major cause of forest dieback [5,6,7]. Temperate plants are vulnerable to frost damage in spring, when leaves and flowers are developing after bud burst [9]

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