Radial growth of Pinus sylvestris L. in island bores of Northern Kazakhstan in the context of climate and geomorphological conditions

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Tree-ring chronologies based on the width of the annual ring of Scots pine (Pinus sylvestris L.) were studied at 8 test sites in island forests in the north of the Republic of Kazakhstan from the Turgai trough to the eastern part of the Kazakh small hills. An analysis of the relationships between the radial growth of pine and climate showed that the climate signal in chronologies can change depending on geomorphological conditions determined by the edaphic factor, relief and absolute elevations. These features must be taken into account when using tree-ring chronologies for spatiotemporal climate reconstructions.

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M. Gurskaya

Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: marina_gurskaya@mail.ru
俄罗斯联邦, 620144, Ekaterinburg

L. Agafonov

Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences

Email: lagafonovc@ipae.uran.ru
俄罗斯联邦, 620144, Ekaterinburg

V. Kukarskih

Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences

Email: marina_gurskaya@mail.ru
俄罗斯联邦, 620144, Ekaterinburg

A. Surkov

Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences

Email: marina_gurskaya@mail.ru
俄罗斯联邦, 620144, Ekaterinburg

Feng Chen

Yunnan University

Email: marina_gurskaya@mail.ru

Institute of Transboundary River Basins and Ecological Security

中国, 650500, Kunming Yunnan

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2. Fig. 1. Geographical location of dendrochronological test sites (1–8) in Northern Kazakhstan.

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3. Fig. 2. Climate data for the studied test sites. Average values ​​for 1901–2019 (according to CRU TS 4.04): average annual temperature (a); average temperature of the growing season (b); annual precipitation (c); precipitation of the growing season (d).

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4. Fig. 3. Deviations in air temperature during the year (a) and in May–September (b) and precipitation (c, d) at test sites in the period 1990–2019 relative to 1901–1930. Significant changes (p < 0.05) are marked with *. For the color coding of test sites, see Fig. 2.

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5. Fig. 4. Measured generalized chronologies of TP 1–8: the black line corresponds to the average values ​​of radial increment in mm, the standard deviations are shown in gray.

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6. Fig. 5. Factor analysis of tree-ring chronologies from test sites 1–8 using the principal component method.

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7. Fig. 6. Results of cluster analysis of the chronologies of the studied test sites – diagram of Euclidean distances.

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8. Fig. 7. Correlation coefficients between the generalized indexed chronologies of test sites and air temperature (a) and precipitation (b). The horizontal line is the significance level (p < 0.05). For the color coding of test sites, see Fig. 2.

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9. Fig. 8. Analysis of the stability of the relationship between pine growth in the studied test sites for the period May–July (5, 6, 7, respectively) with air temperature (a), precipitation (b), and the Palmer drought severity index (c). Horizontal lines correspond to the significance level of p < 0.05. Color designations of the test sites correspond to Fig. 2.

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