000131801 001__ 131801
000131801 005__ 20241125101158.0
000131801 0247_ $$2doi$$a10.1016/j.dendro.2023.126135
000131801 0248_ $$2sideral$$a137113
000131801 037__ $$aART-2023-137113
000131801 041__ $$aeng
000131801 100__ $$aDolar, Nina Škrk
000131801 245__ $$aSpatial and temporal variation of Fagus sylvatica growth in marginal areas under progressive climate change
000131801 260__ $$c2023
000131801 5060_ $$aAccess copy available to the general public$$fUnrestricted
000131801 5203_ $$aThe escalating decline in growth trends of European beech (Fagus sylvatica) observed across its distribution area pose a major ecological and economic challenge for countries with a high proportion of beech, such as Slovenia. In this study, the effects of climate change were examined at a high-resolution scale, encompassing the large climatic, orographic, and ecological variability of beech forests in Slovenia. Using basal area increment data (BAI) from a tree-ring network (48 sites in Slovenia), modelled climate data, and generalized linear mixed models (GLMM), we found an average growth decline of 11% between the 1953–1985 and 1986–2018 subperiods, affecting 90.5% of the forest stands. Based on climate data, we defined two contrasted marginal areas of beech presence (warm and cold) and analysed the growth changes over time. The warm marginal areas, which predominate near the geographical margin of beech distribution with a sub-Mediterranean climatic regime, were most affected by growth decline, threatening the survival of beech populations in the area. In contrast, cold marginal areas, mainly at high elevations in the Alps, where beech growth had previously been limited by low temperatures, turned out to be the only ones where growth of beech increased under prevailing warming conditions. Consequently, high elevation regions harbour climatic potential for increased beech growth performance, and may represent areas of future expansion of the species.
000131801 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000131801 590__ $$a2.7$$b2023
000131801 592__ $$a0.849$$b2023
000131801 591__ $$aFORESTRY$$b15 / 89 = 0.169$$c2023$$dQ1$$eT1
000131801 593__ $$aPlant Science$$c2023$$dQ1
000131801 591__ $$aGEOGRAPHY, PHYSICAL$$b26 / 65 = 0.4$$c2023$$dQ2$$eT2
000131801 593__ $$aEcology$$c2023$$dQ1
000131801 594__ $$a5.5$$b2023
000131801 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000131801 700__ $$aCastillo, Edurne Martinez del
000131801 700__ $$0(orcid)0000-0001-7663-1202$$aSerrano-Notivoli, Roberto$$uUniversidad de Zaragoza
000131801 700__ $$aArrillaga, Martín de Luis
000131801 700__ $$aNovak, Klemen
000131801 700__ $$aMerela, Maks
000131801 700__ $$aCufar, Katarina
000131801 7102_ $$13006$$2430$$aUniversidad de Zaragoza$$bDpto. Geograf. Ordenac.Territ.$$cÁrea Geografía Física
000131801 773__ $$g81 (2023), 126135 [10 pp.]$$pDendrochronologia$$tDENDROCHRONOLOGIA$$x1125-7865
000131801 8564_ $$s12437559$$uhttps://zaguan.unizar.es/record/131801/files/texto_completo.pdf$$yVersión publicada
000131801 8564_ $$s2418524$$uhttps://zaguan.unizar.es/record/131801/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000131801 909CO $$ooai:zaguan.unizar.es:131801$$particulos$$pdriver
000131801 951__ $$a2024-11-22-12:10:12
000131801 980__ $$aARTICLE