It is the very first study concerning the development of a bog in Central-Eastern Europe.
The use of high-quality data set i.e., high-temporal resolution, continuous plant macrofossil record.
Hypothesis testing of a hotly debated subject regarding the driving factors for peatland development and functioning, that is regional climate changes versus autogenic succession from an area where nothing is known about the subject.
Implication of the use of ombrothrophic mountains bog as a palaeoclimatic archive.
Consolidates the geographical coverage of proxy reconstruction of past climate variability in a poorly studied region.