Figure F6. Close-up photographs of representative lithologies for the transition from calcareous nannofossil clay in lithostratigraphic Unit III to black shale in lithostratigraphic Unit IV. A. The transition from calcareous nannofossil clay of Unit III (25–31 cm) (note the distinct burrows) into the basal glauconitic interval of Unit III (31–40 cm) (interval 207-1258B-44R-2, 25–40 cm). B. The transition from glauconitic interval via leached brownish laminated sediments (Unit III) into black shale (Unit IV; note burrows with glauconite in laminated black shale) (interval 207-1258B-44R-2, 50–70 cm). C. Gravity flow deposit without obvious internal fabric in the uppermost part of Unit IV (interval 207-1258B-44R-3, 7898 cm). The sediment contains phosphatic nodules, a clast of laminated black shale, and shell fragments. D. Sharp contact (96 cm) between calcareous nannofossil clay of Unit III and laminated black shale of Unit IV (interval 207-1258C-15R-3, 85100 cm). The basal sediment of Unit III contains poorly preserved radiolarians, glauconite, quartz, and feldspar. The fabric of the black shale in the topmost few centimeters is strongly disturbed.