Drought constrains acorn production and tree growth in the Mediterranean holm oak and triggers weak legacy effects

Abstract

Droughts are becoming more frequent in the Mediterranean basin due to warmer conditions. Droughts negatively impact forests growth for several years, often generating negative legacies or carryover effects. However, these legacies differ among tree species, sites and drought characteristics and have been mainly studied considering tree growth or canopy greenness, but ignoring reproductive phenomena. Here, we compare the legacy effects of drought on acorn and male inflorescence production and radial growth by using a 19-year series of 150 Quercus ilex individuals in three stands located in north-eastern Spain. We evaluate the relationships between monthly climate variables, tree-ring width, acorn production and male inflorescence production. For the two driest years considered (2005 and 2012), when very few acorns were produced, we did not find negative legacy effects on acorn production in the three years following droughts. The production of male inflorescences did not show any significant legacy after drought, although its annual variation was related to the climatic conditions of the year before acorn ripening. Acorn production was higher than expected for some of these years, apparently following the pattern of tree growth recovery with a certain lag. This compensatory response of acorn production differed between the two analysed droughts, in accordance with different conditions of drought timing and post-drought climate conditions. Even though few negative legacy effects of growth and acorn production were found, we confirmed the negative effect of drought stress on tree growth and acorn production, linked to dry winter conditions. Our findings confirm that drought features (timing, d

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Keywords

Bibliographic citation

Agricultural And Forest Meteorology, 2023, 334, 109435
AGROVOC subjects
Sequía
Bosques
Bellotas
Condiciones ambientales
Quercus ilex

Sponsorship

This research was funded by Spanish Ministry of Science, Innovation and Universities, grant number FORMAL (RTI2018-096884-B-C31) to JJC. We acknowledge the E-OBS dataset from the EU-FP6 project UERRA (http://www.uerra.eu) and the Copernicus Climate Change Service, and the data providers in the ECA&D project (https://www. ecad.eu). We also thank Gabriel Montserrat Martí, Gabriel Sangüesa Barreda, Michele Colangelo, Jos´e Manuel Altarriba and Pedro S´ anchez for their help in the field.