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Confessions of solitary oaks: We grow fast but we fear the drought
Institution:1. Institute of Botany and Landscape Ecology, University of Greifswald, Soldmannstr. 15, 17489, Greifswald, Germany;2. Chair of Forest Growth and Woody Biomass Production, TU Dresden, Germany;1. Tribhuvan University, Kathmandu, Nepal;2. WSL Swiss Federal Research Institute, CH-8903 Birmensdorf, Switzerland;1. Departamento de Ciencias Agropecuarias, Universidad Nacional de San Luis, San Luis, Argentina;2. Instituto de Arqueología, Facultad de Filosofía y Letras, Universidad de Buenos Aires, Buenos Aires, Argentina;3. Departamento de Ciencias Sociales, Universidad Nacional de Luján, Buenos Aires, Argentina;4. Facultad de Agronomía y Facultad de Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, Santa Rosa, La Pampa, Argentina;5. Asentamiento Universitario San Martin de los Andes, Facultad de Ciencias Agrarias, Universidad Nacional del Comahue, San Martin de los Andes, Neuquén, Argentina;6. Instituto de Arqueología, Facultad de Filosofía y Letras, Universidad de Buenos Aires, Buenos Aires, Argentina;7. CONICET – Instituto de Arqueología, Facultad de Filosofía y Letras, Universidad de Buenos Aires, Buenos Aires, Argentina;1. Institute of Botany and Landscape Ecology, University Greifswald, Soldmannstr. 15, 17487 Greifswald, Germany;2. Professor Emeritus of Forest Ecology, School of Natural Resources and Extension, University of Alaska Fairbanks, 99775, USA;1. Department of Earth and Environmental Sciences, KU Leuven, University of Leuven, Celestijnenlaan 200E Box 2411, BE-3001 Leuven, Belgium;2. Agency for Nature and Forests (ANB), Koning Albert II-laan 20 bus 8, BE-1000 Brussels, Belgium;3. AgroParisTech, ENGREF, UMR 1092 Inra, AgroParisTech Laboratoire d’Etude des Ressources Forêt-Bois (LERFoB), 14 rue Girardet, 54000 Nancy, France;4. INRA, Centre de Nancy-Lorraine, UMR 1092 Inra, AgroParisTech Laboratoire d’Etude des Ressources Forêt-Bois (LERFoB), 54280 Champenoux, France;5. European Forest Insitute (EFI), Mediterranean Regional Office (EFIMED), Sant Pau World Heritage Site, Pabellon de Santa Victoria, S. Antoni Maria Claret 167, 08025 Barcelona, Spain;1. Laboratory of Silviculture, Dendrochronology and Climate Change, Department of Forestry Engineering, University of Cordoba. Edf. Leonardo da Vinci, Campus de Rabanales, 14075 Córdoba, Spain;2. Laboratory of Plant Physiology and Soil Culture, Faculty of Nature and Life Sciences, Ibn Khaldoun University, PO Box 80 Zaaroura, Tiaret, Theniet El Had, Tissemsilt, 38200, Algeria;3. Instituto Pirenaico de Ecología (IPE-CSIC), Avda. Montañana 1005, 50192, Zaragoza, Spain;4. Laboratory of Plant Ecology and Environment, Faculty of Biological Sciences, University of Science and Technology HouariBoumediene (USTHB), BP 32 El Alia, Bab Ezzouar, Alger, Algeria
Abstract:Competition effects and management related disturbances can contribute to strong non-climatic signals in ring-width trends of trees from closed canopy forests. Removing this noise comes at the price of losing a considerable amount of (climatic) information on decadal and centennial time scales. Alternatively, open grown solitary trees, which never competed for light or other resources could function as less biased climate proxies. To explore this potential we analysed individual growth trends and climate-growth relationships of solitary oaks, potentially representative of former, open forests, and compared it to those of trees growing in adjacent closed canopy forests. Solitary oaks show differing tree allometry with bigger crowns and lower absolute heights. Their radial growth was significantly higher compared to forest trees. Contrary to our expectations, these solitary oaks show highly individualistic decadal growth trends. Their inter-annual variations are nevertheless in good agreement between individuals and stronger compared to trees from closed canopy forests. Climate –growth analysis revealed a significantly higher drought sensitivity of solitary oaks. Given the typical open medieval forest structure of large trees with extensive crowns growing in a mosaic of grazed woodlands and grasslands, it is likely that these trees contribute to the historical part of tree-ring collections. When trees from today’s denser forests forming the recent parts of the collections are used to calibrate reconstruction models, the differing drought sensitivity might therefore lead to an overestimation of historical droughts.
Keywords:Dendrochronology  Ring-width  Competition  Drought  Oak  Tree-rings
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