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FIGURE 6 Modern examples of burrows in deposits containing organic matter. (A) Core 16867-3
(2.2 S, 5.1 E; 3,894 mwater depth; 1,655-1,695 cm), producers of Zoophycos ( Z ) displacedmaterial
downward as indicated by sediment color; Z 1 fromthe top carbonate ooze layer, Z 2 fromthe blackmud
layer. (B) Core 12337-5 (15 58.4 0 N, 18 07.1 0 W, 3,082 mwater depth; 34-44 cm; X-ray radiograph
negative); cross-cutting relationships suggest a four-tier bioturbated zone. (C and D) Sonne Cruise
187, core 61-2 (11 25.5 0 N, 111 17 0 E, 2,226 m water depth); X-ray-radiograph negative; (C)
487-493 cm core depth; (D) 505-512 cm core depth; bioturbation within the oxygenminimum zone;
lowoxygenation indicatedby the highproportionof biodeformational structures, andby the small size
of traces. h, homogeneous (biodeformational structures); s, shear plane formed during retrieval of the
core; Ch , Chondrites ; P , Planolites ; Sc , Scolicia ; Th , Thalassinoides ; Z , Zoophycos .
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