Chert is derived from a siliceous ooze. Siliceous oozes are formed under upwelling zones. (B) Siliceous oozes: These pelagic deposits are formed by a large percentage of siliceous skeletal material produced by planktonic plants and animals. Siliceous ooze, Foraminifera, Diatoms, Radiolaria, Carbonate compensation depth Grade Level: 9-12 Lesson Time: 1 hr. ), surface sediments vary between calcareous oozes and siliceous muds. They are even found at depth of 4-5km covering extensive areas in abyssal plains for which the sediments found there are termed as siliceous ooze. Siliceous oozes often contain lesser proportions of either sponge spicules, silicoflagellates or both. Materials Required: global map, Sediment Distribution Patterns map Science as Inquiry Abilities necessary to do scientific inquiry (K -4, 5 -8, 9 -12) The composition of ooze depends on details of geography: ocean currents, the availability of nutrients in the water, world climate, depth in the ocean, and other factors. Carbonate oozes dominate the deep Atlantic seafloor, while siliceous oozes are most common in the Pacific; the floor of the Indian Ocean is covered by a combination of the two. WikiMatrix Ooze is pelagic sediment that consists of at least 30% of microscopic remains of either calcareous or siliceous planktonic debris organisms. Further, factors such as depth, temperature, and pressure can affect the ability of calcium carbonate to dissolve. - Siliceous ooze is found on deeper sea floor, below the level where carbonates have dissolved. An ooze that is primarily calcium carbonate (aragonite or calcite), a calcareous ooze, typically turns into a rock of the limestone group. They are overlain by foraminiferal ooze deposited on the shallower seafloor of the mid-ocean ridge, with the sedimentation rate and the proportion of siliceous organisms depending on latitude. Eventually, subsidence of the oceanic crust may bring the seafloor below the carbonate compensation depth, and abyssal brown clays accumulate. (ii) Pteropod ooze contains protective shells of pelagic molluscs; (iii) Coccolith ooze contains large number of coccoliths and rhabdoliths that form the protective structures of the minute coccolithophoridae. This type of ooze accumulates on the ocean floor at depths below the carbonate compensation depth. - siliceous material also dissolves a bit in seawater, but much more slowly than carbonate material. Areas of the ocean that lie beneath the carbonate compensation depth (CCD), below which calcium carbonate dissolves, typically beneath 4-5 km, will be dominated by Because of the proximity of the basin to the Carbonate Compensation Depth (C.C.D. The top of the opal-A dominated siliceous ooze is at ∼1,745 m. The opal-CT contact is at ∼1,993 m (Table 1). As a result, the majority of deep marine deposits are of siliceous ooze, which lithifies as chert. Below the CCD, only dust and silica can deposit, as the calcareous organisms dissolve before reaching the sea floor, and siliceous ooze accumulates more quickly than red clays. The ooze composed of their hard parts accumulates at a rate of about 10mm - 50mm per thousand years, varying from location to location; which doesn't sound like much, but is actually a faster rate than other marine sediments such as siliceous ooze or pelagic clay. 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