Stable Isotopes in Tree Rings of Boreal Forests

• Main Authors: Churakova, Olga V., Porter, Trevor J., Kirdyanov, Alexander V., Myglan, Vladimir S., Fonti, Marina V., Vaganov, Eugene A.
• Format: Book Part
• Language: unknown
• Published: Springer International Publishing 2022
• Subjects: Canada; Norway; Fennoscandia; Subarctic; Tundra; Alaska
• Online Access: http://dx.doi.org/10.1007/978-3-030-92698-4_20; https://link.springer.com/content/pdf/10.1007/978-3-030-92698-4_20

Abstract The boreal forests are widely expanded from subarctic forest to tundra, and from taigato forest-steppe zone (from 50 °N to 70 °N). We reviewed available stable isotope chronologies in tree-ring cellulose (δ 13 C, δ 18 O and δ 2 H) from 16 sites located in the Russian Federation; 4 research sites from Fennoscandia (Finland, Sweden and Norway); 5 sites from Canada, and 1 site from Alaska (USA) to evaluate impact of climatic changes from seasonal to annual scale across boreal forest ecosystems. Results of our review of carbon isotope data showed that droughtconditions (mainly high vapour pressure deficit) are prevalent for western and central regions of Eurasia, Alaska and Canada, while northeastern and eastern sites of Eurasian subarctic are showing water shortage developments resulting from decreasing precipitation. Oxygen isotopechronologies show increasing trends towards the end of the twentieth century mainly for all chronologies, except for the Siberian northern and southern sites. The application of the multiple stable isotope proxies (δ 13 C, δ 18 O, δ 2 H) is beneficial to study responses of boreal forests to climate change in temperature-limited environments. However, a deeper knowledge of hydrogen isotope fractionation processes at the tree-ring cellulose level is needed for a sound interpretation and application of δ 2 H for climate reconstructions, especially for the boreal forest zone where forest ecosystems are more sensitive to climatic and environmental changes.