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Bioturbation is extensive in all the facies cored during DSDP Leg 58 in the Philippine Sea, and cores not disturbed by drilling contain several distinctive trace-fossil types. Terrigenous turbidites show little, if any, bioturbation in their lower sub-units, although the upper, fine-grained sub-units commonly contain burrowed horizons. Pelagic biogenic oozes contain a typically deep-sea trace-fossil assemblage dominated by Planolites, Zoophycos, and Chondrites. Pelagic brown clays contain an abundance of smeared and deformed burrows, suggesting deposition of low-strength sediment at or below the carbonate-compensation depth.

Trace Fossils in Deep Sea Drilling Project Leg 58 Cores