Problem of climate-driven dynamics in the genetic forest typology

• Published in: AIP Conference Proceedings, MODERN SYNTHETIC METHODOLOGIES FOR CREATING DRUGS AND FUNCTIONAL MATERIALS (MOSM2020): PROCEEDINGS OF THE IV INTERNATIONAL CONFERENCE
• Main Authors: Fomin, V., Ivanova, N., Mikhailovich, A., Zolotova, E.
• Format: Conference Object
• Language: English
• Published: American Institute of Physics Inc. 2021
• Subjects: CORPORATE GOVERNANCE; CORPORATE SOCIAL PERFORMANCE; CORPORATE SOCIAL RESPONSIBILITY; CORPORATE SOCIAL RESPONSIBILITY OUTCOMES; FIRM RISK; permafrost; taiga
• Online Access: http://elar.urfu.ru/handle/10995/132446; https://aip.scitation.org/doi/pdf/10.1063/5.0068806; https://doi.org/10.1063/5.0068806

Included is the review of forest typology aimed at issues related to climate-driven dynamics of vegetation. Problem definition and key research were performed under extreme conditions for trees (upper tree-line ecotone). Study of climate factor impacts on forest ecosystems in taiga zone conditions that are optimal for arboreal plants has a number of complications, and required specific data analysis methods. Authors provide examples of using landscape photos taken at different times, ecological scales, DCA-ordination, and catastrophe theory-based modeling. Priority study areas for forest climate-driven dynamics include research on impact of climatic factors on forest structure and diversity, age and recovery dynamics, development of new data analysis methods, and study of phenomena related to permafrost thawing and forest fires. © 2021 Author(s). A.N. Zavaritsky Institute of Geology and Geochemistry of the Ural branch of the Russian Academy of Sciences, (AAAA-A18-118052590028-9) Russian Ministry for Education and Science, (FEUG-2020-0013) Russian Foundation for Basic Research, РФФИ, (18-34-00803 mol_a) Ural Branch, Russian Academy of Sciences, UB RAS The work was carried out within the framework of the state task of the Botanical Garden of the Ural branch of the Russian Academy of Sciences, the A.N. Zavaritsky Institute of Geology and Geochemistry of the Ural branch of the Russian Academy of Sciences (state registration no. AAAA-A18-118052590028-9) and supported by the Russian Foundation for Basic Research (project No. 18-34-00803 mol_a) and a grant of Russian Ministry for Education and Science FEUG-2020-0013.