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      Growth and resilience responses of Scots pine to extreme droughts across Europe depend on predrought growth conditions

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          Abstract

          Global climate change is expected to further raise the frequency and severity of extreme events, such as droughts. The effects of extreme droughts on trees are difficult to disentangle given the inherent complexity of drought events (frequency, severity, duration, and timing during the growing season). Besides, drought effects might be modulated by trees’ phenotypic variability, which is, in turn, affected by long‐term local selective pressures and management legacies. Here we investigated the magnitude and the temporal changes of tree‐level resilience (i.e., resistance, recovery, and resilience) to extreme droughts. Moreover, we assessed the tree‐, site‐, and drought‐related factors and their interactions driving the tree‐level resilience to extreme droughts. We used a tree‐ring network of the widely distributed Scots pine ( Pinus sylvestris) along a 2,800 km latitudinal gradient from southern Spain to northern Germany. We found that the resilience to extreme drought decreased in mid‐elevation and low productivity sites from 1980–1999 to 2000–2011 likely due to more frequent and severe droughts in the later period. Our study showed that the impact of drought on tree‐level resilience was not dependent on its latitudinal location, but rather on the type of sites trees were growing at and on their growth performances (i.e., magnitude and variability of growth) during the predrought period. We found significant interactive effects between drought duration and tree growth prior to drought, suggesting that Scots pine trees with higher magnitude and variability of growth in the long term are more vulnerable to long and severe droughts. Moreover, our results indicate that Scots pine trees that experienced more frequent droughts over the long‐term were less resistant to extreme droughts. We, therefore, conclude that the physiological resilience to extreme droughts might be constrained by their growth prior to drought, and that more frequent and longer drought periods may overstrain their potential for acclimation.

          Abstract

          We examined tree growth resilience of Scots pine along a 2,800 km latitudinal gradient from southern Spain to north‐eastern Germany using 615 adult trees from 30 different sites. We found that the resilience of Scots pine to extreme drought decreased in mid‐elevation and low productivity sites from 1980–1999 to 2000–2011 due to more frequent and severe droughts in the later period. We showed that the impact of drought on tree‐level resilience was not dependent on its latitudinal location, but rather on the type of sites trees were growing at and on their growth performances during the pre‐drought period.

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          Plant Ecological Strategies: Some Leading Dimensions of Variation Between Species

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            Conserving biodiversity under climate change: the rear edge matters.

            Modern climate change is producing poleward range shifts of numerous taxa, communities and ecosystems worldwide. The response of species to changing environments is likely to be determined largely by population responses at range margins. In contrast to the expanding edge, the low-latitude limit (rear edge) of species ranges remains understudied, and the critical importance of rear edge populations as long-term stores of species' genetic diversity and foci of speciation has been little acknowledged. We review recent findings from the fossil record, phylogeography and ecology to illustrate that rear edge populations are often disproportionately important for the survival and evolution of biota. Their ecological features, dynamics and conservation requirements differ from those of populations in other parts of the range, and some commonly recommended conservation practices might therefore be of little use or even counterproductive for rear edge populations.
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              Regional vegetation die-off in response to global-change-type drought.

              Future drought is projected to occur under warmer temperature conditions as climate change progresses, referred to here as global-change-type drought, yet quantitative assessments of the triggers and potential extent of drought-induced vegetation die-off remain pivotal uncertainties in assessing climate-change impacts. Of particular concern is regional-scale mortality of overstory trees, which rapidly alters ecosystem type, associated ecosystem properties, and land surface conditions for decades. Here, we quantify regional-scale vegetation die-off across southwestern North American woodlands in 2002-2003 in response to drought and associated bark beetle infestations. At an intensively studied site within the region, we quantified that after 15 months of depleted soil water content, >90% of the dominant, overstory tree species (Pinus edulis, a piñon) died. The die-off was reflected in changes in a remotely sensed index of vegetation greenness (Normalized Difference Vegetation Index), not only at the intensively studied site but also across the region, extending over 12,000 km2 or more; aerial and field surveys confirmed the general extent of the die-off. Notably, the recent drought was warmer than the previous subcontinental drought of the 1950s. The limited, available observations suggest that die-off from the recent drought was more extensive than that from the previous drought, extending into wetter sites within the tree species' distribution. Our results quantify a trigger leading to rapid, drought-induced die-off of overstory woody plants at subcontinental scale and highlight the potential for such die-off to be more severe and extensive for future global-change-type drought under warmer conditions.
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                Author and article information

                Contributors
                arun.bose@wsl.ch
                Journal
                Glob Chang Biol
                Glob Chang Biol
                10.1111/(ISSN)1365-2486
                GCB
                Global Change Biology
                John Wiley and Sons Inc. (Hoboken )
                1354-1013
                1365-2486
                08 June 2020
                August 2020
                : 26
                : 8 ( doiID: 10.1111/gcb.v26.8 )
                : 4521-4537
                Affiliations
                [ 1 ] WSL Swiss Federal Institute for Forest, Snow and Landscape Research Birmensdorf Switzerland
                [ 2 ] Forestry and Wood Technology Discipline Khulna University Khulna Bangladesh
                [ 3 ] Institute of Terrestrial Ecosystems ETH Zurich Zurich Switzerland
                [ 4 ] SwissForestLab Birmensdorf Switzerland
                [ 5 ] Thünen Institute of Forest Ecosystems Eberswalde Germany
                [ 6 ] Land Surface‐Atmosphere Interactions Technische Universitat München Freising Germany
                [ 7 ] UMR RECOVER/Ecosystèmes Méditerranéens et Risques INRAE Aix‐en‐Provence cedex 5 France
                [ 8 ] Instituto Pirenaico de Ecologıa (IPE‐CSIC) Zaragoza Spain
                [ 9 ] Department of Forest Sciences Transilvania University of Braşov Braşov Romania
                [ 10 ] BC3 ‐ Basque Centre for Climate Change Scientific Campus of the University of the Basque Country Leioa Spain
                [ 11 ] Departamento de Ciencias Agroforestales Universidad de Huelva Palos de la Frontera Spain
                [ 12 ] Depto. Sistemas Físicos, Químicos y Naturales Universidad Pablo de Olavide Sevilla Spain
                [ 13 ] CREAF Bellaterra (Cerdanyola del Vallès) Spain
                [ 14 ] Universitat Autònoma de Barcelona Bellaterra (Cerdanyola del Vallès) Spain
                [ 15 ] Departamento de Biología Vegetal y Ecología Facultad de Biología Universidad de Sevilla Sevilla Spain
                [ 16 ] Ecoclimatology Technische Universität München Freising Germany
                [ 17 ] Institute for Advanced Study Technische Universität München Garching Germany
                [ 18 ] Faculty of Forest and Environment Eberswalde University for Sustainable Development Eberswalde Germany
                Author notes
                [*] [* ] Correspondence

                Arun K. Bose, WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Zürcherstrasse 111, CH‐8903 Birmensdorf, Switzerland.

                Email: arun.bose@ 123456wsl.ch

                Author information
                https://orcid.org/0000-0001-8581-1651
                https://orcid.org/0000-0002-1910-9589
                https://orcid.org/0000-0003-4106-0387
                https://orcid.org/0000-0003-2179-0681
                https://orcid.org/0000-0001-6561-1943
                https://orcid.org/0000-0003-2436-2922
                https://orcid.org/0000-0002-1839-1770
                https://orcid.org/0000-0001-6352-1442
                https://orcid.org/0000-0003-0273-510X
                https://orcid.org/0000-0001-8375-6353
                https://orcid.org/0000-0002-2332-7298
                https://orcid.org/0000-0001-5603-5390
                https://orcid.org/0000-0002-7175-2512
                https://orcid.org/0000-0002-6545-5810
                https://orcid.org/0000-0003-3977-2166
                https://orcid.org/0000-0001-9031-051X
                https://orcid.org/0000-0003-1944-4042
                Article
                GCB15153
                10.1111/gcb.15153
                7383776
                32388882
                488d68d5-9237-4e19-bf7a-f3c16e3ab8e3
                © 2020 The Authors. Global Change Biology published by John Wiley & Sons Ltd

                This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc-nd/4.0/ License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.

                History
                : 18 October 2019
                : 19 March 2020
                : 30 April 2020
                Page count
                Figures: 6, Tables: 2, Pages: 17, Words: 13037
                Funding
                Funded by: Marie Skłodowska‐Curie
                Award ID: 749051‐REFOREST
                Funded by: FEDER , open-funder-registry 10.13039/501100002924;
                Award ID: IJCI‐2015‐25845
                Funded by: Ministry of Science, Innovation and Universities
                Award ID: RTI2018‐096884‐B‐C31
                Award ID: RTI2018‐096884‐B‐C33
                Funded by: VULBOS
                Award ID: UPO‐1263216
                Funded by: PinCaR
                Award ID: UHU‐1266324
                Funded by: Bavarian Climate Research Network
                Funded by: German Waldklimafond
                Award ID: FKZ 28W‐C‐4‐077‐01
                Funded by: Bavarian State Ministry for Food, Agriculture, and Forestry
                Award ID: ST327
                Categories
                Primary Research Article
                Primary Research Articles
                Custom metadata
                2.0
                August 2020
                Converter:WILEY_ML3GV2_TO_JATSPMC version:5.8.5 mode:remove_FC converted:27.07.2020

                acclimation,latitudinal gradient,pinus sylvestris,predisposition,tree rings

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