Informace o publikaci
Oak tree-ring carbon stable isotopes from eastern Europe reveal significant drought signals along elevational gradients
| Autoři | |
|---|---|
| Rok publikování | 2024 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | Science of the Total Environment |
| Fakulta / Pracoviště MU | |
| Citace | |
| www | https://doi.org/10.1016/j.scitotenv.2024.177114 |
| Doi | https://doi.org/10.1016/j.scitotenv.2024.177114 |
| Klíčová slova | Dendrochronology; Eastern Europe; Hydroclimate; Paleoclimate; Stable isotopes; Tree rings |
| Přiložené soubory | |
| Popis | The importance of stable carbon and oxygen isotopes in tree-ring-based climate reconstructions is increasingly recognized, especially in regions where traditional dendrochronological parameters, such as tree-ring width, usually fail. However, the effects of elevation and other site conditions on climate signals in tree-ring stable isotope (TRSI) chronologies remain unclear. Here, we assess the sensitivities to precipitation and drought of tree-ring width (TRW) and ?13C and ?18O TRSI chronologies of 136 living oaks (Quercus spp.) from five different elevational zones between 130 and 630 m asl in eastern Slovakia. Our results show that while the mean ?13C values were stable across the elevational gradient, TRW gradually decreased with increasing elevation, and the mean ?18O values significantly differed between the lower and higher sites. Despite these variations, we observed strong coherency among all the elevation-specific TRW and TRSI chronologies. We also found that mainly mid-May to July precipitation and mid-May to August drought controlled TRW and the ?13C values, whereas the ?18O reflected an overall lower climate signal. Our results show a relatively stable drought signal across the elevational range, with shorter seasonal response windows at higher elevations. Furthermore, our study indicates that carbon TRSI and TRW oak chronologies capture distinct summer drought signals independently of elevation and therefore have a strong paleoclimatic potential across eastern Europe. |