Scientists have quantified dust and iron fluxes deposited in the Antarctic Ocean during the past 4 million years. The research study shows evidence of the close relation between the maximum contributions of dust to this ocean and climate changes occurring in the most intense glaciation periods of the Pleistocene period, some 1.25 million years ago. Data confirms the role of iron in the increase in phytoplankton levels during glacial periods, intensifying the function of this ocean as a carbon dioxide sink....