( January 2023) ( Learn how and when to remove this template message) You may improve this section, discuss the issue on the talk page, or create a new section, as appropriate. The examples and perspective in this section may not represent a worldwide view of the subject. Because of its extremely small grain size, oolitic sand has a lot of surface area, which promotes high bacterial growth. This unusually smooth sand promotes the growth of bacteria, which are important biofilters in home aquaria. Also known as "oolitic" sand, the sugar-sized round grains of this sand pass easily through the gills of gobies and other sand-sifting organisms. Oolites are often used in the home aquarium industry because their small grain size (0.2 to 1.22 mm) is ideal for shallow static beds and bottom covering of up to 1" in depth. The size of the oolites reflect the time that they were exposed to the water before they were covered with later sediment. The oolites are commonly found in large current bedding structures that resemble sand dunes.
Strong intertidal currents wash the 'seeds' around on the seabed, where they accumulate layers of chemically precipitated calcite from the supersaturated water. The mechanism of formation starts with a small fragment of sediment acting as a 'seed', such as a piece of a shell.
They are usually formed in warm, supersaturated, shallow, highly agitated marine water intertidal environments, though some are formed in inland lakes. Oolitic hematite occurs at Red Mountain near Birmingham, Alabama, along with oolitic limestone. Dolomitic and chert ooids are most likely the result of the replacement of the original texture in limestone. Ooids are most commonly composed of calcium carbonate ( calcite or aragonite), but can be composed of phosphate, clays, chert, dolomite or iron minerals, including hematite. The term oolith can refer to oolite or individual ooids. Strictly, oolites consist of ooids of diameter 0.25–2 millimetres rocks composed of ooids larger than 2 mm are called pisolites. Oolite or oölite (from Ancient Greek ᾠόν (ōión) 'egg stone') is a sedimentary rock formed from ooids, spherical grains composed of concentric layers. Modern ooids from a beach on Joulter Cays, The Bahamas Ooids on the surface of a limestone Carmel Formation (Middle Jurassic) of southern Utah Thin-section of calcitic ooids from an oolite within the Carmel Formation (Middle Jurassic) of southern Utah The highly porous and permeable Miami Limestone forms much of the Biscayne Aquifer of the surficial aquifer system.For the video game, see Oolite (video game). Fossils present include mollusks, bryozoans, and corals. Beds of quartz sand are also present as unindurated sediments and indurated limey sandstones. The bryozoan facies consists of white to orangish gray, poorly to well indurated, sandy, fossiliferous limestone (grainstone and packstone). The oolitic facies consists of white to orangish gray, poorly to moderately indurated, sandy, oolitic limestone (grainstone) with scattered concentrations of fossils. The Miami Limestone consists of two facies, an oolitic facies and a bryozoan facies (Hoffmeister et al. To the north, in Palm Beach County, the Miami Limestone grades laterally northward into the Anastasia Formation. From Big Pine Key to the mainland, the Miami Limestone is replaced by the Key Largo Limestone. The Miami Limestone occurs on the mainland and in the southern Florida Keys from Big Pine Key to the Marquesas Keys. It forms the Atlantic Coastal Ridge and extends beneath the Everglades where it is commonly covered by thin organic and freshwater sediments. The Miami Limestone (formerly the Miami Oolite), named by Sanford (1909), occurs at or near the surface in southeastern peninsular Florida from Palm Beach County to Dade and Monroe Counties.
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