(Table 2) Terrigenous, authigenic and biogenic composition of sediments at DS...

Pelagic sedimentation during the Early Cretaceous at Site 603 produced alternations of laminated marly limestone and bioturbated limestone--a facies typical of the "Blake-Bahama...

早白垩世时期，603站位（Site 603）的远洋沉积（pelagic sedimentation）作用形成了纹层状泥灰岩（laminated marly limestone）与生物扰动灰岩（bioturbated limestone）的互层沉积——该岩相（facies）为"布莱克-巴哈马（Blake-Bahama）"典型的沉积相。