What is it about?
A hydroclimate reconstruction is presented from an ombrotrophic mountain bog in Romania. Five major hydroclimatic shifts are identified over the past 1000 years. Good correlation exists with other palaeohydrological records from central eastern Europe. Contrasting conditions with others estimates from northwest Europe.
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Why is it important?
This dataset represents one of the few last millennium reconstructions from central-eastern Europe.
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This page is a summary of: A multi-proxy analysis of hydroclimate trends in an ombrotrophic bog over the last millennium in the Eastern Carpathians of Romania, Palaeogeography Palaeoclimatology Palaeoecology, January 2020, Elsevier,
DOI: 10.1016/j.palaeo.2019.109390.
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