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001-es BibID:BIBFORM107748
035-os BibID:(cikkazonosító)126014 (WOS)000899737200004 (Scopus)85140069263
Első szerző:Mészáros Ilona (biológus)
Cím:Long-term radial growth and climate-growth relationships of Quercus petraea (Matt.) Liebl. and Quercus cerris L. in a xeric low elevation site from Hungary / Ilona Mészáros, Balázs Adorján, Balázs Nyitrai, Péter Kanalas, Viktor Oláh, Tom Levanic
Dátum:2022
ISSN:1125-7865 1612-0051
Megjegyzések:Sessile oak (Quercus petraea [Matt.] Liebl.) and Turkey oak (Quercus cerris L.) dominated mixed forests are common in low montane and hilly regions in Hungary. Here, we aimed to describe the long-term pattern and climatic responses of the radial growth of Q. petraea and Q. cerris in a xeric low-elevation forest, using retrospective tree-ring analysis for the period 1910?2019. We performed separate analyses with time series of full tree-ring (TRW), earlywood (EW) and latewood (LW) widths. Our results showed that the radial growth of the two species was largely synchronous over time, but became transiently divergent for a 20-year period after a drought in 1968, due to the greater-than-expected growth of Q. cerris and the supressed growth of Q. petraea. Precipitation was the major growth-limiting factor for both species, with a strong positive influence on LW particularly during the current early growing season (March-June), on EW in the previous late summer (August-September) and in the current early spring (March), and on all tree-ring traits in the previous December. The radial growth of both species was negatively related to temperature in the spring (May) and late summer (August) of both current and previous years. The climate-growth relationships showed general instability over time: the most striking temporal change was a gradual shift of positive correlations with precipitation and SPEI during the growing season from spring (March-May) to summer (June-August) since the 1980s over the analysed period. The two species had similarly low growth resistance to droughts in four studied pointer years (1968, 1993, 2002 and 2012), but Q. cerris exhibited a greater capacity to recover over the four post-drought years, and thus higher growth resilience, particularly after the drought of 1968. Our results contribute to the better understanding of the role of climate variability and droughts in the growth of the two co-existing species in transitional locations between closed forests and forest-steppes.
Tárgyszavak:Természettudományok Biológiai tudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
Megjelenés:Dendrochronologia. - 76 (2022), p. 1-13. -
További szerzők:Adorján Balázs (1985-) (környezettudomány) Nyitrai Balázs (1987-) (ökológus) Kanalas Péter (1983-) (biológus) Oláh Viktor (1980-) (biológus) Levanic, Tom
Pályázati támogatás:OTKA-101552
OTKA
SNN 125652
OTKA
2018-2.1.11-TÉT-SI-2018-00012
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001-es BibID:BIBFORM118615
035-os BibID:(cikkazonosító)126168 (Scopus)85184010062
Első szerző:Sochová, Irena
Cím:The palaeoclimatic potential of recent oak tree-ring width chronologies from Southwest Ukraine / I. Sochová, T. Kolář, M. Arvai, M. Bošeľa, K. Čufar, Z. Kern, J. Kyncl, P. Marčiš, I. Mészáros, A. Morgós, A. Mursa, A. Popa, C.-C. Roibu, I. Sopushynskyy, M. Rybníček
Dátum:2024
ISSN:1125-7865 1612-0051
Megjegyzések:Better insights into spatio-temporal climate signals are needed to understand more clearly the applicability to palaeoclimatic analysis and dendrochronological dating of the long tree-ring oak chronologies currently being compiled in Eastern Europe. This study investigates the climate sensitivity of two recent oak tree-ring width (TRW) chronologies from Transcarpathian and Ciscarpathian Ukraine and their coherence with 35 oak chronologies from Ukraine, Poland, Slovakia, Romania, and Hungary. The new Transcarpathian chronology consists of 247 TRW series of living trees from 13 sites covering the period 1836?2020, while the new Ciscarpathian chronology consists of 215 TRW series from 13 sites and spans the period 1775?2020. Despite the strong similarity between these two chronologies, their responses to climate differ significantly. Growing-season precipitation and particularly drought (three-month SPEI index) were found to be the primary drivers of oak growth on the border between the Carpathians and the northeastern Pannonian Basin. Spatial correlations of the Transcarpathian chronology show particularly high explained variability in the April-August SPEI index, roughly between 18.5?28.5?E and 45?52?N. In the Ciscarpathian, June precipitation primarily influenced oak radial growth but the spatial correlation was quite low. While the Transcarpathian TRW chronology was strongly correlated with eastern Slovakian and northwestern Romanian chronologies, the Ciscarpathian chronology revealed very low correlations with surrounding chronologies. This study indicates the great dendroarchaeological and palaeoclimatic potential of the Transcarpathian chronology and points to the need to analyse additional living trees from the Ciscarpathian region to understand the spatial variability of oak growth and its climate signal better.
Tárgyszavak:Természettudományok Biológiai tudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
Carpathian mountains
Eastern Europe
Hydroclimate
Quercus spp.
Teleconnection
Tree-ring width chronology
Megjelenés:Dendrochronologia. - 84 (2024), p. 1-11. -
További szerzők:Kolář, T. Árvai Mátyás Bošeľa, Michal Čufar, Katarina Kern Zoltán Kyncl, J. Marčiš, P. Mészáros Ilona (1952-) (biológus) Morgós, A. Mursa, A. Popa, A. Roibu, C.C. Sopushynskyy, I. Rybníček, M.
Pályázati támogatás:K 101552
Egyéb
SNN 125652
2018-2.1.11-TET-SI-2018-00012
Egyéb
Internet cím:Szerző által megadott URL
DOI
Intézményi repozitóriumban (DEA) tárolt változat
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