Figure 5. Regional stratigraphic correlation chart for Sites 897 to 900. The lower contourite-turbidite-pelagite sequence contains abundant siliceous allochems and reworked carbonate grains. The upper turbidite-pelagite sequence shows no evidence of reworking by contour currents.

Figure 5. Regional stratigraphic correlation chart for Sites 897 to 900. The lower contourite-turbidite-pelagite sequence contains abundant siliceous allochems and reworked carbonate grains. The upper turbidite-pelagite sequence shows no evidence of reworking by contour currents.