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词汇 coccolith
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Examples of coccolith


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Banding within the unit, composed of organicrich mudstone finely intercalated with the coccolith laminae, may relate to the seasonal nature of the blooms.
Immediately below the cementstone there is a bed approximately 3 cm thick that appears to have been fluidized; it is a coccolith-rich mudstone run through with mini-sediment-filled fissures.
They produce calcified scales, known as coccoliths, which are deposited on the surface of the cell resulting in the formation of a coccosphere.
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This means that the most recently produced coccoliths may lie beneath older coccoliths.
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The two coccolith types were originally thought to be produced by different families of coccolithophores.
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The coccoliths are either dispersed following death and breakup of the coccosphere, or are shed continually by some species.
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Chalk is a limestone that consists of coccolith biomicrite.
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The majority of the fossil debris comprising chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores.
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These limestone cliffs are formed from the skeletons of marine plankton called coccoliths.
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It consists of minute calcite plates (coccoliths) shed from micro-organisms called coccolithophores.
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Its coccoliths are transparent and commonly colourless, but are formed of calcite which refracts light very efficiently in the water column.
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The production of coccoliths requires the uptake of dissolved inorganic carbon and calcium.
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The best-known haptophytes are coccolithophores, which have an exoskeleton of calcareous plates called coccoliths.
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When the coccolith is complete these vesicles fuse with the cell wall and the coccolith is exocytosed and incorporated in the coccosphere.
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In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks.
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It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite plates (coccoliths) shed from micro-organisms called coccolithophores.
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Hence, a high concentration of coccoliths leads to a simultaneous increase in surface water temperature and decrease in the temperature of deeper waters.
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Coccolithophorids are distinguished by special calcium carbonate plates (or scales) of uncertain function called "coccoliths", which are also important microfossils.
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The calcareous particles include coccoliths, bivalve, and gastropod fragments, and calcispheres.
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Coccolithophores are of particular interest to those studying global climate change because as ocean acidity increases, their coccoliths may become even more important as a carbon sink.
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