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Topography modulates climate sensitivity of multidecadal trends of holm oak decline

View ORCID ProfileAna López-Ballesteros, Emilio Rodríguez-Caballero, Gerardo Moreno, Paula Escribano, Ana María Hereş, Jorge Curiel-Yuste
doi: https://doi.org/10.1101/2023.03.09.531879
Ana López-Ballesteros
1Department of Agricultural and Forest Systems and the Environment, Agrifood Research and Technology Centre of Aragon (CITA). Avda. Montañana 930, 50059 Zaragoza, Spain
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  • For correspondence: alpzballesteros@gmail.com
Emilio Rodríguez-Caballero
2Department of Agronomy and Centro de Investigación de Colecciones Científicas (CECOUAL), Universidad de Almería, carretera Sacramento s/n,04120, La Cañada de San Urbano, Almeria, Spain
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Gerardo Moreno
3Faculty of Forestry, Institute for Dehesa Research (INDEHESA), Universidad de Extremadura, Avenida Virgen del Puerto 2, 10600 Plasencia, Cáceres, Spain
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Paula Escribano
4Biodiversity Node S.L., Sector Foresta 17, 28760 Tres Cantos, Madrid, Spain
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Ana María Hereş
5BC3 - Basque Centre for Climate Change, Scientific Campus of the University of the Basque Country, 48940 Leioa, Spain
6Department of Forest Sciences, Transilvania University of Braşov, Sirul Beethoven -1, 500123 Braşov, Romania
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Jorge Curiel-Yuste
5BC3 - Basque Centre for Climate Change, Scientific Campus of the University of the Basque Country, 48940 Leioa, Spain
7IKERBASQUE, Basque Foundation for Science, Bilbao, Bizkaia, Spain
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Abstract

Forest decline events have increased worldwide over the last decades, being holm oak one of the tree species with the most worrying trends across Europe. Previous research identified drought and soil pathogens as the main causes behind holm oak decline. However, despite tree health loss is a multifactorial phenomenon where abiotic and biotic factors interact in time and space, there are some abiotic factors whose influence has been commonly overlooked. Here, we evaluate how land use (forests versus savannas), topography, and climate extremes jointly relate to spatiotemporal patterns of holm oak defoliation over almost three decades (1987-2014) in Spain, where holm oak represents the 25% of the national forested area. We found an increasing defoliation trend in 119 of the total 134 holm oak plots evaluated, being this increase rate significantly higher in forests compared to savannas. Moreover, we have detected that the interaction between topography and summer drought can explain trends of holm oak decline across the Mediterranean region. While a higher occurrence of dry summers increases defoliation trends in complex terrains where forests dominate, an inverse relationship was found at flatter terrains where savannas are located. Our results contribute to growing evidence of the influence of local topography, tightly linked to potential soil water availability, on forest functioning, as it can shape forest vulnerability against climate extremes. The present work could assist the identification of potential tree decline hotspots over the Mediterranean region. Moreover, our findings suggest that forest adaptive management will be key to guarantee the health and future stability of Mediterranean oak ecosystems, especially in the topographically more complex areas where tree vulnerability to climate extremes may be greater.

Competing Interest Statement

The authors have declared no competing interest.

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The copyright holder for this preprint is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under a CC-BY-NC-ND 4.0 International license.
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Posted March 12, 2023.
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Topography modulates climate sensitivity of multidecadal trends of holm oak decline
Ana López-Ballesteros, Emilio Rodríguez-Caballero, Gerardo Moreno, Paula Escribano, Ana María Hereş, Jorge Curiel-Yuste
bioRxiv 2023.03.09.531879; doi: https://doi.org/10.1101/2023.03.09.531879
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Topography modulates climate sensitivity of multidecadal trends of holm oak decline
Ana López-Ballesteros, Emilio Rodríguez-Caballero, Gerardo Moreno, Paula Escribano, Ana María Hereş, Jorge Curiel-Yuste
bioRxiv 2023.03.09.531879; doi: https://doi.org/10.1101/2023.03.09.531879

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