NATURE CIKK

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Részlet az Abstract- ból:

"Lake Petea’s evolution was mainly controlled by major climate-driven hydrological changes also seen in regional records.
The hydrological changes were mainly controlled by varying input of thermal water due to recurring increased/decreased recharge
of the underground karst water system. The driving factor was warming connected to the interstadial GI 1 increasing recharge
by melting of regional ice sheets in the Late Glacial..."

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