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Stable Isotopes in Tree Rings of Pinus heldreichii Can Indicate Climate Variability over the Eastern Mediterranean Region

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    SYSNO ASEP0542633
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleStable Isotopes in Tree Rings of Pinus heldreichii Can Indicate Climate Variability over the Eastern Mediterranean Region
    Author(s) Lukac, L. (HR)
    Mikac, S. (HR)
    Urban, Otmar (UEK-B) RID, ORCID, SAI
    Kolář, Tomáš (UEK-B) RID, ORCID, SAI
    Rybníček, Michal (UEK-B) RID, ORCID, SAI
    Ač, Alexander (UEK-B) RID, ORCID, SAI
    Trnka, Miroslav (UEK-B) RID, ORCID, SAI
    Marek, Michal V. (UEK-B) RID, ORCID, SAI
    Number of authors8
    Article number350
    Source TitleForests. - : MDPI
    Roč. 12, č. 3 (2021)
    Number of pages14 s.
    Languageeng - English
    CountryCH - Switzerland
    Keywordstree-ring width ; carbon and oxygen isotopes ; sub-Adriatic climate ; drought ; climate signal ; Bosnian pine
    Subject RIVGK - Forestry
    OECD categoryClimatic research
    R&D ProjectsEF16_019/0000797 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Research InfrastructureCzeCOS III - 90123 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Method of publishingOpen access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000633679300001
    EID SCOPUS85103479494
    DOI10.3390/f12030350
    AnnotationA long-term context is important for understanding past climatic variability. Although tree-ring widths (TRWs) are widely used as a proxy for reconstructing past climate, the use of annually-resolved values of delta C-13 and delta O-18 tree-ring stable isotopes (TRSIs) is increasing and may provide further valuable information. Here, we present a 487-year-long TRW chronology and 240-year-long TRSI chronology for Bosnian pine (Pinus heldreichii H. Christ) and compare them to each other. We demonstrate that both delta C-13 and delta O-18 values are better proxies for temperature, precipitation, and drought than TRW. The correlations between these climate parameters and TRSIs are strongest for the combined summer (JJA) period. The results of temporal and spatial field correlation indicate that TRSI chronologies are stable, reliable proxies for JJA precipitation reconstruction over the whole Balkan Peninsula and surrounding eastern Mediterranean region. However, the stability of the temperature signal of the both delta C-13 and delta O-18 chronologies declines after the 1950s. Our work supports the emerging evidence that TRSI data track climate variability more accurately than a conventional TRW approach and can be subsequently used for the reconstruction of past climate.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2022
    Electronic addresshttps://www.mdpi.com/1999-4907/12/3/350
Number of the records: 1  

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