Blue growth rings in woody plant stems indicate years when cells failed to lignify properly due to summers that were too cold for normal growth.
When temperatures drop, even tough trees face challenges in growing. Trees require a specific number of warm days during their growing season to develop properly. Without enough warmth, the cell walls in new growth fail to lignify properly, resulting in “blue rings” that become visible when wood samples are dyed.
Because trees and shrubs can live for centuries, these blue rings provide a valuable record of past cold summers. By studying pine trees and juniper shrubs from northern Norway, scientists identified two exceptionally cold summers in 1902 and 1877, likely linked to volcanic eruptions from Mount Pelée on Martinique and Cotopaxi in Ecuador.
“Blue rings look like unfinished growth rings, and are associated with cold conditions during the growing season,” said Dr Agata Buchwal of Adam Mickiewicz University, Poland, lead author of the article in Frontiers in Plant Science. “In general, we found more blue rings in trees than in shrubs. Shrubs seem to be more adapted to cooling events than trees, which is probably why shrubs are found further north. That is why I love to study shrubs; they seem to be the true heroes of the north.”
Growing pains
The scientists sampled cores from 25 Scots pine trees and stem-base discs from 54 common juniper shrubs at a site high on the treeline of Mount Iškoras in northern Norway. The team cross-sectioned and stained these samples, then photographed them under a microscope so that growth ring widths could be measured and cross-dated, and blue rings identified.
“Blue ring studies require a much longer protocol than classical dendrochronological studies,” Buchwal noted. “We are grateful to work with dedicated, highly-qualified lab technicians. Only together we can explore the blue ring world in high resolution using microscope slides!”
Overall, only 2.1% of the pine trees’ rings and 1.3% of the juniper shrubs’ rings were blue; the cells which hadn’t lignified properly were mainly found at the end of growth rings, in latewood. Blue rings occurred most frequently in 1902 — 96% of pine trees and 68% of juniper shrubs — followed by 1877 — 84% of pine trees and 36% of juniper shrubs. Pine trees seemed to be more vulnerable to blue ring formation than juniper shrubs, which could make them a more sensitive indicator of cold summers.
“In the case of pine trees in boreal regions, blue rings have the potential to weaken the tree, making it more susceptible to mechanical damage or disease,” explained Dr Pawel Matulewski of Adam Mickiewicz University, second author of the article. “If this phenomenon persists over several years, it can impede the tree’s recovery in following years.”
Comparing this data with local weather records showed that 1902 and 1877 were characterized by very low summer temperatures. In 1902 the coldest June ever recorded delayed the growing season, so a low total number of days in that year were warm enough for tree growth. This could explain why earlywood formed almost normally in 1902, but latewood didn’t, creating many blue latewood cells: the growing season was too short, so the latewood didn’t have time to develop properly.
Comparing the cooling events — the 1902 event fell in June, when the growth season usually begins, and the 1877 event in August — suggests it may even be possible to differentiate between cooling at different times. Late cooling events may lead to more lignified cell walls and a ‘less blue’ ring.
Volcanoes’ long shadow
Other studies have linked blue rings to global climatic events, such as cooling after large volcanic eruptions. 1902’s cold June could be related to the eruption of Mount Pelée in May. Similarly, the late June eruption of Cotopaxi aligns with 1877’s cold August — but there is no other reported evidence for related cooling in northern Norway after this eruption. This blue ring could also be due to another, as-yet unidentified, factor.
Looking at other blue rings, the scientists identified more potential cold summer periods — but the weather seems to have been less cold, and some temperature data were missing, preventing analysis. The scientists also cautioned that temperatures among the trees might have been different to those recorded at the Mount Iškoras weather station: future research will need in-situ weather data.
“We hope to inspire other research groups to look for the blue rings in their material,” said Buchwal. “It would be great to establish a blue ring network based on trees and shrubs to reconstruct cooling events at the northern treeline over long timescales.”
Reference: “Blue rings in trees and shrubs as indicators of early and late summer cooling events at the northern treeline” by Agata Buchwal, Pawel Matulewski, Ylva Sjöberg, Alma Piermattei, Alan Crivellaro, Angela Balzano, Maks Merela, Luka Krže, Katarina Čufar, Alexander V. Kirdyanov, Tatiana Bebchuk, Tito Arosio and Ulf Büntgen, 29 October 2024, Frontiers in Plant Science.
DOI: 10.3389/fpls.2024.1487099
Funding: National Science Centre, Poland, Bekker Scholarship, ID-UB UAM, Javna Agencija za Raziskovalno Dejavnost RS, Swiss National Science Foundation
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