Siliceous ooze are modified and transformed during burial into bedded cherts.
2.
Sediments are mainly turbidites interspersed with oceanic deposits of clay, volcanic ash and siliceous ooze.
3.
Pelagic sediments, containing significant quantities of siliceous biogenic remains, are commonly referred to as siliceous ooze.
4.
Siliceous ooze are particularly abundant in the modern ocean at high latitudes in the northern and southern hemispheres.
5.
A striking feature of siliceous ooze distribution is a ca . 200 km wide belt stretching across the Southern Ocean.
6.
Below this depth, calcium carbonate begins to dissolve in the ocean, and only non-calcareous sediments are stable, such as siliceous ooze or pelagic red clay.
7.
"Siliceous ooze " is ooze that is composed of at least 30 % of the siliceous microscopic " shells " of plankton, such as diatoms and radiolaria.
8.
Siliceous ooze accumulates on the ocean floor where the bottom waters are close to saturation with respect to silica, and the opaline remains of either diatoms, radiolarians, silicoflagellates, and sponge spicules, or combinations of these are rapidly buried.
9.
Decomposition and decay of diatoms leads to organic and inorganic ( in the form of silicates ) sediment, the inorganic component of which can lead to a method of analyzing past marine environments by corings of ocean floors or bay muds, since the inorganic matter is embedded in deposition of clays and silts and forms a permanent geological record of such marine strata . ( See siliceous ooze ).
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