Figure 4From: Reconstruction of productivity signal and deep-water conditions in Moroccan Atlantic margin (~35°N) from the last glacial to the Holocene Comparison of the total organic carbon (TOC) and the TOC mass accumulation rates (TOCMAR) of Geob 9064 with the sedimentation rate pattern, the planktonic δ 18 O and the terrigenous inputs (Fe). The aeolian input record (EM1+EM2) refers to Wienberg et al. (2010).Back to article page