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单词 coccolith
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Examples ofcoccolith

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Banding within the unit, composed of organicrich mudstone finely intercalated with thecoccolithlaminae, may relate to the seasonal nature of the blooms.
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Immediately below the cementstone there is a bed approximately 3 cm thick that appears to have been fluidized; it is acoccolith-rich mudstone run through with mini-sediment-filled fissures.
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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 twococcolithtypes 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 ofcoccolithbiomicrite.
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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 thecoccolithis complete these vesicles fuse with the cell wall and thecoccolithis 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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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.

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更新时间:2024/12/28 1:20:33