General trends in climate proxy data for the southern Pannonian Plain.

This table is based on data from Demény et al. 2019 and supported by data from Drăguşin et al. 2014. Demeny et al. is based primarily on data from Trio Cave and Dragusin et al. focus on Ascunsă, Poleva, and Ursilor caves. These are located ca. 200 km to the west-north-west and east-north-east of the centre of the TSG network respectively. All conditions in the figure are relative to those of 2000–1900 BC when this timeline begins. As the dating of changes is broadly construed within century blocks, when peaks occur within a block, the following trajectory is opposite to the preceding one, i.e. if preceded by cooling then following the peak, prevailing conditions shifted to warming.