Figure 9. CaCO3 and Corg time series for Site 1019, shown as weight percent and as mass accumulation rate (MAR). This site had major variations in sedimentation rate caused by highly variable sedimentation of terrigenous aluminosilicates. The sedimentation rate changes masked the flux variations of CaCO3 and Corg. 175

Figure 9. CaCO₃ and C_org time series for Site 1019, shown as weight percent and as mass accumulation rate (MAR). This site had major variations in sedimentation rate caused by highly variable sedimentation of terrigenous aluminosilicates. The sedimentation rate changes masked the flux variations of CaCO₃ and Corg.