TY - JOUR
T1 - No systematic effects of sampling direction on climate-growth relationships in a large-scale, multi-species tree-ring data set Dendrochronologia
AU - Gut, Urs
AU - Árvai, Mátyás
AU - Bijak, Szymon
AU - Camarero, J. Julio
AU - Cedro, Anna
AU - Cruz-García, Roberto
AU - Garamszegi, Balázs
AU - Hacket-Pain, Andrew
AU - Hevia, Andrea
AU - Huang, Weiwei
AU - Isaac-Renton, Miriam
AU - J.Kaczka, Ryszard
AU - Kazimirović, Marko
AU - Kędziora, Wojciech
AU - Kern, Zoltán
AU - Klisz, Marcin
AU - Kolář, Tomáš
AU - Körner, Michael
AU - Kuznetsova, Veronica
AU - Montwé, David
AU - Mary Petritan, Any
AU - Petritan, Ion Catalin
AU - Plavcová, Lenka
AU - Rehschuh, Romy
AU - Rocha, Eva
AU - Rybníček, Michal
AU - Sánchez-Salguero, Raúl
AU - Schröder, Jens
AU - Schwab, Niels
AU - Stajić, Branko
AU - Tomusiak, Robert
AU - Wilmking, Martin
AU - Sass-Klaassen, Ute
AU - Buras, Allan
PY - 2019/10
Y1 - 2019/10
N2 - Ring-width series are important for diverse fields of research such as the study of past climate, forest ecology, forest genetics, and the determination of origin (dendro-provenancing) or dating of archaeological objects. Recent research suggests diverging climate-growth relationships in tree-rings due to the cardinal direction of extracting the tree cores (i.e. direction-specific effect). This presents an understudied source of bias that potentially affects many data sets in tree-ring research. In this study, we investigated possible direction-specific growth variability based on an international (10 countries), multi-species (8 species) tree-ring width network encompassing 22 sites. To estimate the effect of direction-specific growth variability on climate-growth relationships, we applied a combination of three methods: An analysis of signal strength differences, a Principal Component Gradient Analysis and a test on the direction-specific differences in correlations between indexed ring-widths series and climate variables. We found no evidence for systematic direction-specific effects on tree radial growth variability in high-pass filtered ring-width series. In addition, direction-specific growth showed only marginal effects on climate-growth correlations. These findings therefore indicate that there is no consistent bias caused by coring direction in data sets used for diverse dendrochronological applications on relatively mesic sites within forests in flat terrain, as were studied here. However, in extremely dry, warm or cold environments, or on steep slopes, and for different life-forms such as shrubs, further research is advisable.
AB - Ring-width series are important for diverse fields of research such as the study of past climate, forest ecology, forest genetics, and the determination of origin (dendro-provenancing) or dating of archaeological objects. Recent research suggests diverging climate-growth relationships in tree-rings due to the cardinal direction of extracting the tree cores (i.e. direction-specific effect). This presents an understudied source of bias that potentially affects many data sets in tree-ring research. In this study, we investigated possible direction-specific growth variability based on an international (10 countries), multi-species (8 species) tree-ring width network encompassing 22 sites. To estimate the effect of direction-specific growth variability on climate-growth relationships, we applied a combination of three methods: An analysis of signal strength differences, a Principal Component Gradient Analysis and a test on the direction-specific differences in correlations between indexed ring-widths series and climate variables. We found no evidence for systematic direction-specific effects on tree radial growth variability in high-pass filtered ring-width series. In addition, direction-specific growth showed only marginal effects on climate-growth correlations. These findings therefore indicate that there is no consistent bias caused by coring direction in data sets used for diverse dendrochronological applications on relatively mesic sites within forests in flat terrain, as were studied here. However, in extremely dry, warm or cold environments, or on steep slopes, and for different life-forms such as shrubs, further research is advisable.
U2 - 10.1016/j.dendro.2019.125624
DO - 10.1016/j.dendro.2019.125624
M3 - Journal article
SN - 1125-7865
VL - 57
JO - Dendrochronologia
JF - Dendrochronologia
M1 - 125624
ER -