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The effects of this Dansgaard—Oeschger D—O type climatic variability have been found in a number of European and Asian terrestrial paleoclimate archives, including speleothems, lakes and loess deposits.

However, only very few of the already sparse precisely dated records provide quantitative information on stadial-interstadial temperature variations over this time period.

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This is a major impediment to resolving the cause and geographical propagation of D-O events, as well as to understanding the impact they have on continental climates and environments. Stadial ASTs of the investigated periods were found to be in the range of 7—13 °C, corresponding to Tannual of 0—6 °C and TJuly of 11—17 °C, agreeing well with the range of model simulation results for the region.

The PK-6 flowstone δ18Ocalcite-based temperature change estimates ~0.

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Our results show that stadial-interstadial online dating study variability in East Central Europe was of comparable magnitude to that in Greenland. We propose that large scale ocean-atmospheric variability NAO-AMO imparts a major control on transmitting abrupt North Atlantic climate event signals into continental Europe during the last glacial. TS is grateful for the support of the Swedish Research Council How to cite: Ujvari, G.

We employ state-of-the-art analyses of trace elements, cryptoptephra and sulphur isotopes Burke et al.

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Finally, based on these comparisons, we propose a number of stratigraphic age tie-points to anchor ice-core chronologies from Greenland GICC05 and Ismerősök olpe WD to the absolute dated tree-ring chronology.

We thereby aim to improve proxy synchronization throughout the Holocene -- a prerequisite for detection and attribution studies -- and invite the paleo-climate community to update climate proxy records based on ice cores to the latest chronologies. References: Burke, A. McConnell, J. How to cite: Sigl, M.

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