|—vb (often foll by away)|
|1.||(intr) to flow or leak out slowly, as through pores or very small holes|
|2.||to exude or emit (moisture, gas, etc)|
|3.||(tr) to overflow with: to ooze charm|
|4.||to disappear or escape gradually|
|5.||a slow flowing or leaking|
|6.||an infusion of vegetable matter, such as sumach or oak bark, used in tanning|
|[Old English wōs juice]|
pelagic (deep-sea) sediment of which at least 30 percent is composed of the skeletal remains of microscopic floating organisms. Oozes are basically deposits of soft mud on the ocean floor. They form on areas of the seafloor distant enough from land so that the slow but steady deposition of dead microorganisms from overlying waters is not obscured by sediments washed from the land. The oozes are subdivided first into calcareous oozes (containing skeletons made of calcium carbonate) and siliceous oozes (containing skeletons made of silica) and then are divided again according to the predominant skeleton type. Thus, the calcareous oozes include globigerina ooze, containing the shells of planktonic foraminifera, and pteropod ooze, made up chiefly of the shells of pelagic mollusks. The siliceous oozes include radiolarian ooze, comprising essentially brown clay with more than 30 percent of the skeletons of warm-water protozoa, and diatom ooze, containing the frustules (tiny shells) of diatoms. The siliceous oozes exist only where the rate of deposition of diatoms or radiolarians is greater than the rate at which their silica content is dissolved in the deep waters; thus the diatom oozes are confined to belts in the North Pacific and Antarctic, and the radiolarian oozes are found only under the eastern part of the North Pacific. Globigerina ooze is the most widespread of the oozes and occurs in both the Atlantic and Indian oceans. Pteropod ooze is found only in the mid-Atlantic.
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