Spatial-Coherent Dynamics and Climatic Signals in the Radial Growth of Siberian Stone Pine (Pinus sibirica Du Tour) in Subalpine Stands along the Western Sayan Mountains

• Published in: Forests
• Main Authors: Zhirnova, Dina F., Belokopytova, Liliana V., Krutovsky, Konstantin V., Kholdaenko, Yulia A., Babushkina, Elena A., Vaganov, Eugene A.
• Other Authors: Zhirnova, Dina F.; 1Khakass Technical Institute, Siberian Federal University, 655017 Abakan, Russia, Belokopytova, Liliana V.; 1Khakass Technical Institute, Siberian Federal University, 655017 Abakan, Russia, Krutovsky, Konstantin V.; 2Department of Forest Genetics and Forest Tree Breeding, Georg-August University of Göttingen, D-37077 Göttingen, Germany, Kholdaenko, Yulia A.; 1Khakass Technical Institute, Siberian Federal University, 655017 Abakan, Russia, Babushkina, Elena A.; 1Khakass Technical Institute, Siberian Federal University, 655017 Abakan, Russia, Vaganov, Eugene A.; 7Institute of Ecology and Geography, Siberian Federal University, 660036 Krasnoyarsk, Russia
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2022
• Subjects: taiga; Siberia
• Online Access: https://resolver.sub.uni-goettingen.de/purl?gro-2/118472; https://doi.org/10.3390/f13121994

Siberian stone pine (Pinus sibirica Du Tour) is one of the keystone conifers in Siberian taiga, but its radial growth is complacent and thus rarely investigated. We studied its growth in subalpine stands near the upper timberline along the Western Sayan Mountains, Southern Siberia, because climatic responses of trees growing on the boundaries of species distribution help us better understand their performance and prospects under climate change. We performed dendroclimatic analysis for six tree-ring width chronologies with significant between-site correlations at distances up to 270 km (r = 0.57–0.84, p < 0.05). We used ERA-20C (European Reanalysis of the Twentieth Century) daily climatic series to reveal weak but spatially coherent responses of tree growth to temperature and precipitation. Temperature stably stimulated growth during the period from the previous July–August to current August, except for an adverse effect in April. Precipitation suppressed growth during periods from the previous July–September to December (with reaction gradually strengthening) and from the current April to August (weakening), while the snowfall impact in January–March was neutral or positive. Weather extremes probably caused formation of wide tree rings in 1968 and 2002, but narrow rings in 1938, 1947, 1967, 1988, and 1997. A subtle increase in the climatic sensitivity of mature trees was observed for all significant seasonal climatic variables except for the temperature in the previous October–January. The current winter warming trend is supposedly advantageous for young pine trees based on their climatic response and observed elevational advance. Russian Science Foundation