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Annals of Forest Science

, Volume 70, Issue 8, pp 769–780 | Cite as

Growth response to climate and drought change along an aridity gradient in the southernmost Pinus nigra relict forests

  • J. Julio CamareroEmail author
  • Rubén D. Manzanedo
  • Raúl Sanchez-Salguero
  • Rafael M. Navarro-Cerrillo
Original Paper

Abstract

Context

Tree populations at the rear edge of species distribution are sensitive to climate stress and drought. However, growth responses of these tree populations to those stressors may vary along climatic gradients.

Aims

To analyze growth responses to climate and drought using dendrochronology in rear-edge Pinus nigra populations located along an aridity gradient.

Methods

Tree-ring width chronologies were built for the twentieth century and related to monthly climatic variables, a drought index (Standardized Precipitation–Evapotranspiration Index), and two atmospheric circulation patterns (North Atlantic and Western Mediterranean Oscillations).

Results

Growth was enhanced by wet and cold previous autumns and warm late winters before tree-ring formation. The influence of the previous year conditions on growth increased during the past century. Growth was significantly related to North Atlantic and Western Mediterranean Oscillations in two out of five sites. The strongest responses of growth to the drought index were observed in the most xeric sites.

Conclusion

Dry conditions before tree-ring formation constrain growth in rear-edge P. nigra populations. The comparisons of climate-growth responses along aridity gradients allow characterizing the sensitivity of relict stands to climate warming.

Keywords

Atmospheric circulation patterns Dendroecology Drought Mediterranean forests Standardized Precipitation–Evapotranspiration Index 

Notes

Acknowledgments

This project was funded through a Junta de Andalucía and projects DIVERBOS (CGL2011-30285-C02-02) and XILVA (CGL2011-26654), through the Ministry of Science and Innovation of Spain. RSS acknowledges a FPU grant (AP2007-04747) (Science Ministry, Spain), also the financial support from CEXTREME-FP7-ENV-2008-1-226701 and INIA-RTA (RTA2010-00065-00-00) projects. We also acknowledge the financial support from University of Córdoba-Campus de Excelencia ceiA3 and CRU and S.M. Vicente-Serrano for providing meteorological and drought data. JJC thanks the support of ARAID and collaborative efforts within the Globimed network (www.globimed.net). We thank the editors and reviewers for improving the manuscript.

Supplementary material

13595_2013_321_MOESM1_ESM.doc (3.2 mb)
ESM 1 (DOC 3231 kb)

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Copyright information

© INRA and Springer-Verlag France 2013

Authors and Affiliations

  • J. Julio Camarero
    • 1
    • 2
    Email author
  • Rubén D. Manzanedo
    • 3
    • 4
  • Raúl Sanchez-Salguero
    • 3
    • 5
  • Rafael M. Navarro-Cerrillo
    • 3
  1. 1.ARAID-Instituto Pirenaico de Ecología (IPE-CSIC)ZaragozaSpain
  2. 2.Dept. d’Ecologia, Fac. BiologiaUniv. BarcelonaBarcelonaSpain
  3. 3.Depto. Ingeniería Forestal, Laboratorio de Dendrocronología. DendrodatLab-ERSAFUniversidad de CórdobaCórdobaSpain
  4. 4.Institute of Plant SciencesUniversity of BernBernSwitzerland
  5. 5.INIA-CIFORMadridSpain

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