1,721,095 research outputs found

    Age-dependent tree-ring growth responses to climate in Larix decidua and Pinus cembra

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    Dendrochronology generally operates under the assumption that climate– growth relationships are age independent, once growth trends and/or disturbance pulses have been accounted for. However, several studies have demonstrated that tree physiology undergoes changes with age. This may cause growth-related climate signals to vary over time. Using chronology statistics and response functions, we tested the consistency of climate–growth responses in tree-ring series from Larix decidua and Pinus cembra trees of four age classes. Tree-ring statistics (mean sensitivity, standard deviation, correlation between trees, and first principal component) did not change significantly with age in P. cembra, whereas in L. decidua they appeared to be correlated with age classes. Response function analysis indicated that climate accounts for a high amount of variance in tree-ring widths in both species. The older the trees are, the higher the variance explained by climate, the significance of the models, and the percentage of trees with significant responses. Age influence on climate sensitivity is likely to be non-monotonic. In L. decidua, the most important response function variables changed with age according to a twofold pattern: increasing for trees younger than 200 years and decreasing or constant for older trees. A similar pattern was observed in both species for the relationship between tree height and age. It is hypothesized that an endogenous parameter linked to hydraulic status becomes increasingly limiting as trees grow and age, inducing more stressful conditions and a higher climate sensitivity in older individuals. The results of this study confirm that the climate signal is maximized in older trees, but also that a sampling procedure non-stratified by age (especially in multi-aged forests) could lead to biased mean chronologies due to the higher amount of noise present in younger trees. The issue requires more extensive research as there are important ecological implications both at small and large geographic scales. Predictive modeling of forest dynamics and paleo-climate reconstructions may be less robust if the age effect is not accounted for

    Assetto strutturale e qualità dei fusti - Studio su cedui di faggio in conversione in un parco nazionale

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    In three sites correspondent to different steps of the conversion process (abandoned coppice, stands with first and second thinning) we have measured forest structure and assessed timber quality of stems. The vertical structure is very similar in the three sites, but stem domages increase with the number of thinnings. Current management does not seem suitable both timber supply (mainly fuelwood) and nature conservation

    Dating and explanation of Late Glacial – Holocene landslides: a case study from the Southern Alps

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    Landslide chronologies are essential both for understanding the causes of mass movements and for the assessment of landslide hazards. The Fadalto landslide (Venetian Prealps, Italy) studied in this paper has been active, as shown by morphological and stratigraphical data, for several thousands years since the Late Glacial. The chronology of this large and complex landslide was significantly improved through identification and radiocarbon and dendrochronological dating of several mass movements which occurred during the Holocene: one in the late Atlantic (5375 ± 95 years BP) and others in historical times (within the last 14 centuries). Understanding the specific causes of these landslides, and establishing a relationship between landslides and climate (or earthquakes) in particular turned out to be a difficult task (mainly due to the imprecision of radiocarbon dating). It can not be ruled out that the landslides occurred under colder and more changeable climate or during a transition between climatic spells with different characteristics. Dendrochronological analyses, on the other hand, show no relationship between one of these historical landslides and climate (or earthquakes). Reactivations of movements involved both the main scarp and the accumulation zone; besides, it was recognised that the landslide can be reactivated through a rock avalanche, a type of complex landsliding not uncommon in the southern Alps

    Rescuing defective CFTR applying a drug repositioning strategy based on computational studies, surface plasmon resonance and cell-based assays

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    Cystic Fibrosis (CF) is caused by mutations (mainly F508del) of the cystic fibrosis transmembrane conductance regulator (CFTR). Current CF therapies are aimed at symptoms alleviation, calling for new drugs to rescue CFTR function. Hypothesis and objectives Drug repositioning is aimed at finding new applications for already marketed drugs, reducing cost and duration and the likelihood of unforeseen adverse events. In this project we have integrated drug repositioning with computational studies, surface plasmon resonance (SPR) [1] and well-tried cellular models [2] to identify new CF drugs and to comprehend their mechanism of action. Methods and results We have prepared a new structural homology model of intact human F508del-CFTR embedded in a phospholipid bilayer and a SPR biosensor containing the same protein in a cell membrane-mimicking lipid film. These tools, along with appropriate cell-based assays, have been firstly used to analyze a mixed library of well-known and new compounds that allowed the validation of the system and the identification of a promising molecule endowed with a F508del-binding and rescuing capacity that is higher than those of drugs already in use. With the computational model we have then performed a virtual drug repositioning on a library of 846 drugs, identifying 10 drugs that were reduced to 4 on the basis of toxicity profile and patient compliance. These drugs will be now subjected to experimental analysis by cell-based and SPR assays for their effective capacity to bind F508del-CFTR and rescue its activity. Also, we will proceed to the virtual repositioning of a library of natural compounds. Spin-off for research & clinical purposes The novel computational models and biosensors will widen the study of CF drugs and made available to other research groups in the field of CF. References 1. Rusnati M, Sala D, Orro A, Bugatti A, Trombetti G, Cichero E, Urbinati C, Di Somma M, Millo E, Galietta LJV, Milanesi L, Fossa P, D'Ursi P. Speeding Up the Identification of Cystic Fibrosis Transmembrane Conductance Regulator-Targeted Drugs: An Approach Based on Bioinformatics Strategies and Surface Plasmon Resonance. Molecules. 2018 Jan 8;23(1). pii: E120. doi: 10.3390/molecules23010120. 2. Tomati V, Pesce E, Caci E, Sondo E, Scudieri P, Marini M, Amato F, Castaldo G, Ravazzolo R, Galietta LJV, Pedemonte N. High-throughput screening identifies FAU protein as a regulator of mutant cystic fibrosis transmembrane conductance regulator channel. J Biol Chem. 2018 Jan 26;293(4):1203-1217. doi: 10.1074/jbc.M117.816595. Epub 2017 Nov 20. Acknowledgment FFC#11/2018 funded by FFC and supported by Delegazione FFC di Torin

    Testing for tree-ring divergence in the European Alps

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    Evidence for reduced sensitivity of tree growth to temperature has been reported from multiple forests along the high northern latitudes. This alleged circumpolar phenomenon described the apparent inability of temperature-sensitive tree-ring width and density chronologies to parallel increasing instrumental temperature measurements since the mid-20th century. In addition to such low-frequency trend offset, the inability of formerly temperature-sensitive tree growth to reflect high-frequency temperature signals in a warming world is indicated at some boreal sites, mainly in Alaska, the Yukon and Siberia. Here, we refer to both of these findings as the ‘divergence problem’ (DP), with their causes and scale being debated. If DP is widespread and the result of climatic forcing, the overall reliability of tree-ring-based temperature reconstructions should be questioned. Testing for DP benefits from well-replicated tree-ring and instrumental data spanning from the 19th to the 21st century. Here, we present a network of 124 larch and spruce sites across the European Alpine arc. Tree-ring width chronologies from 40 larch and 24 spruce sites were selected based on their correlation with early (1864–1933) instrumental temperatures to assess their ability of tracking recent (1934–2003) temperature variations. After the tree-ring series of both species were detrended in a manner that allows low-frequency variations to be preserved and scaled against summer temperatures, no unusual late 20th century DP is found. Independent tree-ring width and density evidence for unprecedented late 20th century temperatures with respect to the past millennium further reinforces our results
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