Peer review report 1 on “Intra-annual variability of wood formation and δ 13 C in tree-rings at Hyytiälä, Finland”

2016 ◽  
Vol 217 ◽  
pp. 310-312
Author(s):  
Anonymous
2016 ◽  
Vol 224 ◽  
pp. 17-29 ◽  
Author(s):  
Alex Soudant ◽  
Neil J. Loader ◽  
Janna Bäck ◽  
Janne Levula ◽  
Natascha Kljun

2015 ◽  
Vol 40 (2) ◽  
pp. 315-340 ◽  
Author(s):  
B. A. Molski

The corewood of pine ds very prone to compression wood formation, this changing the whole pattern of the tree ring structure and the siz.es of early and late wood. Compression wood always increases the formation of late wood at the expense of early wood. Tree rings with compression wood are generally wider than those without it, but there occur also tree rings wihout compression wood wider than those in which it is present, formed in the same year and in the same tree.


Forests ◽  
2020 ◽  
Vol 11 (2) ◽  
pp. 146 ◽  
Author(s):  
Franco Biondi

The contribution of tree-ring analysis to other fields of scientific inquiry with overlapping interests, such as forestry and plant population biology, is often hampered by the different parameters and methods that are used for measuring growth. Here I present relatively simple graphical, numerical, and mathematical considerations aimed at bridging these fields, highlighting the value of crossdating. Lack of temporal control prevents accurate identification of factors that drive wood formation, thus crossdating becomes crucial for any type of tree growth study at inter-annual and longer time scales. In particular, exactly dated tree rings, and their measurements, are crucial contributors to the testing and betterment of allometric relationships.


2021 ◽  
Author(s):  
Gonzalo Pérez‐de‐Lis ◽  
Cyrille B. K. Rathgeber ◽  
Laura Fernández‐de‐Uña ◽  
Stéphane Ponton
Keyword(s):  

IAWA Journal ◽  
2019 ◽  
Vol 40 (2) ◽  
pp. 155-182 ◽  
Author(s):  
Veronica De Micco ◽  
Marco Carrer ◽  
Cyrille B.K. Rathgeber ◽  
J. Julio Camarero ◽  
Jordi Voltas ◽  
...  

ABSTRACTIt is noteworthy that the largest part of global vegetation biomass depends on a thin layer of cells: the vascular cambium. Understanding the wood formation processes and relationships with environmental factors is a crucial and timely research question requiring interdisciplinary efforts, also to upscale the information gained and to evaluate implications for tree growth and forest productivity.We provide an overview of wood formation processes up to tree-ring development, bearing in mind that the combined action of intrinsic factors and environmental drivers determines the anatomical traits of a tree ring formed at a specific time and position within the tree’s architecture. After briefly reviewing intrinsic factors, we focus attention on environmental drivers highlighting how a correct interpretation of environmental signals in tree rings must be grounded in a deep knowledge of xylogenesis and consequent wood anatomical traits. We provide guidelines on novel methods and approaches recently developed to study xylem formation. We refer to existing literature on established techniques for retrospective analyses in tree-ring series of anatomical and isotopic traits, to assess long-term ecophysiological responses to environmental variations, also giving advice on possible bias because of interand within-tree variability.Finally, we highlight that, once the temporal axis of intra-annual tree-ring variability of xylem traits is established by xylogenesis analysis, a multidisciplinary approach linking classical dendro-ecology, wood functional traits (dendro-anatomy) and eco-physiology (here focusing on dendro-isotopes) allows a better interpretation of past environmental events hidden in tree rings, and more reliable forecasts of wood growth in response to climate change.


2013 ◽  
Vol 11 (4) ◽  
pp. 583-592 ◽  

The relationships between the annual variability of the Aleppo pine tree-ring widths and the variability of the main climatic parameters in the Attica basin are analysed in the present study for a 45-year period (1959-2003). The Principal Components Analysis was applied to the times-series of the tree-rings indices (12 populations) as well as to the residual timeseries of the monthly precipitation, maximum and minimum temperatures derived from 5 meteorological stations located in the study region. The results showed that the 64% of the total variance of the tree-rings of the Aleppo pine could be attributed to the common variability of the climatic parameters: for precipitation with 82.6%, for minimum temperature with 88.2% and for maximum temperature with 88.5% of the total variance of each parameter. Characteristic narrow and wide tree-rings were observed during the hydrological years with extreme rainfall or temperature conditions. Finally the study of the climate – growth links, on a local basis, showed that the growth of the Aleppo pine is related positively (positive correlations) with the winter and spring precipitations. On the other hand negative correlations were found with the temperatures of the spring months.


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