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Mixed claystones and nannofossil chalks of late Aptian-Cenomanian age rested upon basaltic basement at DSDP Holes 417D, 418A, and 418B. Marine organic matter was largely preserved in the sediments. In addition, continental inputs of organic matter were rhythmically introduced, with detrital reworked material also present. Detrital material characterizes Upper Cretaceous sediments.

Organic Geochemistry of Cretaceous Sediments at DSDP Holes 417D (Leg 51), 418A (Leg 52), and 418B (Leg 53) in the Western North Atlantic