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Age-effect on intra-annual d13C-variability within Scots pine tree-rings from Central Siberia

Response of Four Tree Species to Changing Climate in a Moisture-Limited Area of South SiberiaResponse of Four Tree Species to Changing Climate in a Moisture-Limited Area of South Siberia

Small fluctuations in cell wall thickness in pine and spruce xylem: Signal from cambium? of the small fluctuations in the latewood cell wall thickness of rapidly growing tree rings, which exhibit a

Response of four tree species to changing climate in 2 a moisture-limited area of South Siberia, and (2) optimization of the parameters of the Vaganov-Shashkin tree growth simulation model to assess

To which side are the scales swinging? Growth stability of Siberian larch under 1 permanent moisture deficit with periodic droughtsIn moisture-limited regions in which droughts leave a significant “footprint”, monitoring

Xylogenesis of Scots Pine in an uneven-aged stand of the Minusinsk Depression (Southern Siberia) sylvestris L.) of different age (two classes of 30 and 95 years) from a forest-steppe zone in Southern

What prevails in climatic response of Pinus sylvestris in-between its range limits in mountains: slope aspect or elevation?

DYNAMICS OF THE SOIL CO2 EMISSION DURING SNOW-FREE PERIOD IN THE IN MIDDLE TAIGA FORESTS IN CENTRAL SIBERIA

Warming induced changes in wood matter accumulation in tracheid walls of spruce, the Borus Ridge of the Western Sayan Mountains (South Siberia) was considered as a forest area under rapid

Методология получения 600-летней многоэлементной летописи на основе годичных колец лиственницы с полуострова Таймыр, РоссияWe developed a long (600-year) dataset for the concentrations of 26 elements in tree rings of larch

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