Puglia 2003 -Final Conference Project IGCP 437 Coastal Environmental Change During Sea-Level Highstands: A Global Synthesis with implications for management of future coastal change Project 437 Molluscs, Palaeoenvironments and Palaeoclimates during late P

warm highstand acknowledged for MOIS11 (MTIII) can help objective comparisons with pre-Quaternary terraces in Patagonia (MTI-II and Salamanca Fm.). Abstract The Quaternary sea level history along the Patagonian coastal area has been explained by several factors (i.e., eustasy, sediment supply, wave action, current energy)