Figure 2From: Reconstruction of productivity signal and deep-water conditions in Moroccan Atlantic margin (~35°N) from the last glacial to the Holocene Correlation of the gravity cores using the isotopic data (planktonic δ 13 C and δ 18 O), the organic carbon (TOC), the carbonate (CaCO 3 ) and the Fe content. Geob 9064 was chosen as reference.Back to article page