THE CLIMATE VARIABILITY DURING MARINE ISOTOPE STAGE 19: EVIDENCES FROM A WEST-EAST MEDITERRANEAN TRANSECT
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New high temporal resolution data on calcareous nannofossil and planktonic foraminifera assemblages, alkenone-derived sea surface temperature and stable oxygen and carbon isotopes are acquired on the Montalbano Ideale section (southern Italy) and at the Ocean Drilling Program (ODP) sites 975 and 976 through Marine Isotope Stages (MIS) 20-18. Results describe accurate climate pattern and distinct orbital-suborbital up to millennia-scale oscillations across the investigated interval. MIS 19
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