What is it about?
We look at the climate changes and events, affecting the Adriatic Sea in a time span that goes from 20k to 10k years ago. To do so we look at the fossil planktonic assemblages and the chemical proxies in a deep sea core sediment.
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Why is it important?
This is a very detailed look at the climate events during the last deglaciation taking place in the Central Mediterranean.
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This page is a summary of: Climate evolution in the Adriatic Sea across the last deglaciation: A multiproxy approach combining biomarkers and calcareous plankton, Palaeogeography Palaeoclimatology Palaeoecology, December 2022, Elsevier,
DOI: 10.1016/j.palaeo.2022.111291.
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