Paleoceanographic and paleoclimatic analyses throughout the MIS 5 interval: preliminary results from calcareous nannoplankton

New insights about the Marine Isotope Stage (MIS) 5 over the North Atlantic area are presented in this study. The MIS 5 interval covers a timeframe from ̴130 ka to 70 ka and it has been the last major interglacial interval occurred on Earth. In particular, the MIS 5e sub-interval, is a key period to study the possible evolution for human induced climate changes. It also represents an opportunity to interpret the natural climate evolution beyond the anthropic impact being interested by global temperatures assumed to be warmer than the pre-anthropogenic ones (e.g. Kopp et al., 2009). Likewise, the North Atlantic region is interesting for climatic studies being involved in the modulation of the global climate and in particular the Iberian margin is a well-known source of rapidly accumulating sediment offering a high-fidelity record of millennial climate variability. With this contribution we show preliminary results concerning changes in hydrography and coccolithophores productivity from two sites recovered on the Promontorio dos Principes de Avis, SW Iberian Margin: U1385 (37°34.285’N; 10°7.562’W – 2585 meters below sea level), drilled during the Integrated Ocean Drilling Program Expedition 339, and U1586 (37º37.283’N; 10º42.628’W - 4691 meters below sea level), drilled during the International Ocean Discovery Program Expedition 397. The phytoplankton group of coccolithophores has proved to be a high-quality environmental proxy since their geographic distribution and abundance is strongly influenced by parameters such as sea-surface temperature, salinity, sunlight and nutrient availability. Accordingly, coccolithophores are here used to describe paleoproductivity fluctuations in surface waters and upwelling strength as well as paleoceanographic changes linked to global climate evolution. References Kopp, R.E., Simons, F.J., Mitrovica, J.X., Maloof, A.C. & Oppenheimer, M. (2009). Probabilistic assessment of sea level during the last interglacial stage. Nature, 462 (863-867)