2021
DOI: 10.1016/j.dendro.2021.125812
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Drought and cold spells trigger dieback of temperate oak and beech forests in northern Spain

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Cited by 29 publications
(16 citation statements)
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“…In contrast, D trees showed higher iWUE (Figure 2a) and higher responsiveness to summer temperatures (Figure 4b) and steeper increases over the last decades, suggesting more severe drought stress in this tree class [82]. These results are consistent with previous studies of drought-induced dieback on broadleaf [83,84] and conifer species [85]. However, the opposite pattern has been also found [86,87], evidencing the insufficient information provided by tree-ring carbon isotopes alone to elucidate the mechanisms prompting dieback.…”
Section: Discussionsupporting
confidence: 91%
“…In contrast, D trees showed higher iWUE (Figure 2a) and higher responsiveness to summer temperatures (Figure 4b) and steeper increases over the last decades, suggesting more severe drought stress in this tree class [82]. These results are consistent with previous studies of drought-induced dieback on broadleaf [83,84] and conifer species [85]. However, the opposite pattern has been also found [86,87], evidencing the insufficient information provided by tree-ring carbon isotopes alone to elucidate the mechanisms prompting dieback.…”
Section: Discussionsupporting
confidence: 91%
“…Nevertheless, there are still few study cases testing the models' assumptions and predictions (e.g., hydraulic failure would correspond to rapid drops in both stomatal conductance and growth rates prior to death). For instance, in temperate hardwood forests in northern Spain, declining Fagus sylvatica trees showed higher water-use efficiency in contrast to declining Quercus pubescens trees which showed lower growth rates and were less efficient in their water use (Camarero et al 2020), Q. pubescens being in agreement with the conceptual model proposed by Gessler et al (2018). There is still a large research gap regarding the testing of predictions derived from the isotope model of dieback across tree species, drought types (differing in duration, severity and seasonality) and dieback episodes as has been done with tree-ring width data (Cailleret et al 2017(Cailleret et al , 2018.…”
Section: Reconciling Process-based and Empirical Approachessupporting
confidence: 81%
“…As a result, plants have to form some physiological adaptation mechanisms in response to climate change. The change in WUE by adjusting plant stomatal conductance (g s ) and CO 2 assimilation rate (A) [ 5 ] is one of the adaptation mechanisms by which plants can better cope with climate change [ 6 ]. Therefore, investigating the variations in plant WUE under climate change will serve to deepen the understanding of the response of vegetation to global climate change.…”
Section: Introductionmentioning
confidence: 99%
“…The carbon isotope discrimination (Δ 13 C) in plant leaves depends on the ratio of intercellular and environmental CO 2 concentrations (c i /c a ), and this ratio is regulated by g s and A [ 4 , 12 ]. The intrinsic WUE of plants is defined by the ratio of A to g s , which is also associated with c i /c a [ 6 ]. Therefore, foliar Δ 13 C is a useful proxy of plant intrinsic WUE, and there is a negative correlation between leaf Δ 13 C and intrinsic WUE [ 13 , 14 , 15 ].…”
Section: Introductionmentioning
confidence: 99%