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Remarkably high blue ring occurrence in Estonian Scots pines in 1976 reveals wood anatomical evidence of extreme autumnal cooling
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SYSNO ASEP 0572173 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Remarkably high blue ring occurrence in Estonian Scots pines in 1976 reveals wood anatomical evidence of extreme autumnal cooling Tvůrce(i) Greaves, C. (GB)
Crivellaro, A. (GB)
Piermattei, A. (GB)
Krusic, P. J. (SE)
Oppenheimer, C. (GB)
Potapov, A. (EE)
Hordo, M. (EE)
Metslaid, S. (EE)
Kask, R. (EE)
Kangur, A. (EE)
Büntgen, Ulf (UEK-B) RID, ORCID, SAIZdroj.dok. Trees: structure and function. - : Springer - ISSN 0931-1890
Roč. 37, č. 2 (2023), s. 511-522Poč.str. 12 s. Jazyk dok. eng - angličtina Země vyd. DE - Německo Klíč. slova Climate change ; Dendrochronology ; Europe ; Lignification ; Pinus sylvestris ; Temperature reconstruction ; Wood anatomy Vědní obor RIV EH - Ekologie - společenstva Obor OECD Forestry CEP EF16_019/0000797 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy Výzkumná infrastruktura CzeCOS IV - 90248 - Ústav výzkumu globální změny AV ČR, v. v. i. Způsob publikování Open access Institucionální podpora UEK-B - RVO:86652079 UT WOS 000886451400001 EID SCOPUS 85142213582 DOI 10.1007/s00468-022-02366-1 Anotace Key message An exceptionally high number of blue rings were formed within and between Scots pine trees from Estonia in 1976: a year that is well known for its outstanding summer heatwave over Western Europe, but its extreme autumnal cooling over Eastern Europe has so far been neglected in scientific literature. 'Blue rings' (BRs) are visual indicators of less lignified cell walls typically formed towards the end of a tree's growing season. Though BRs have been associated with ephemeral surface cooling, often following large volcanic eruptions, the intensity of cold spells necessary to produce BRs, as well as the consistency of their formation within and between trees still remains uncertain. Here, we report an exceptionally high BR occurrence within and between Scots pine (Pinus sylvestris L.) trees at two sites in Estonia, including the first published whole-stem analysis for BRs. Daily meteorological measurements from a nearby station allowed us to investigate the role temperature has played in BR formation since the beginning of the twentieth century. The single year in which BRs were consistently formed within and amongst most trees was 1976. While the summer of 1976 is well known for an exceptional heatwave in Northwest Europe, mean September and October temperatures were remarkably low over Eastern Europe, and 3.8 degrees C below the 1961-1990 mean at our sites. Our findings contribute to a better eco-physiological interpretation of BRs, and further demonstrate their ability to reveal ephemeral cooling not captured by dendrochronological ring width and latewood density measurements. Pracoviště Ústav výzkumu globální změny Kontakt Nikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268 Rok sběru 2024 Elektronická adresa https://link.springer.com/article/10.1007/s00468-022-02366-1
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