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Oozes on the seafloor mostly consist of the remains of microscopic plankton, such as diatoms and foraminifera. These plankton produce shells or skeletons that accumulate on the ocean floor over time, forming a soft, sedimentary layer known as ooze.

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Microcrystalline quartz formed by recrystallization of silicaeous oozes in seafloor sediments?

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