We reconstructed 3300 years of the development history of the peatland, central Poland.
We use high-resolution multi-proxy palaeoecological approaches.
Our results demonstrate the high potential peat record to reconstruct palaeohydrological dynamics.
The studied time interval is characterised by two pronounced dry periods 2500–1700 BCE and 700–500 BCE.
Only current observations from peatlands and lake ecosystems may lead to a better interpretation of past climate changes.