Difference between revisions of "Foraminifera"

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{{Definition|title=Foraminifera
 
{{Definition|title=Foraminifera
|definition= (= foraminiferans) phylum of mainly marine unicellular protists (classified as protozoans of class Sarcodina in older zoological classifications), having a highly vacuolated outer layer of cytoplasm and a calcareous, siliceous or composite shell through which project fine pseudopodia. Chalk is largely composed of foraminiferan shells and they are also major components of many deep-sea oozes.<ref name="Hendersons"> Lawrence, E. (2005). ''Henderson’s dictionary of biology.'' Pearson Education Limited, 13th ed., Harlow. 748 p. </ref>.}}
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|definition= (= foraminiferans) phylum of mainly marine unicellular protists (classified as protozoans of class Sarcodina in older zoological classifications), having a highly vacuolated outer layer of cytoplasm and a calcareous, siliceous or composite shell through which project fine pseudopodia. <ref name="Hendersons"> Lawrence, E. (2005). ''Henderson’s dictionary of biology.'' Pearson Education Limited, 13th ed., Harlow. 748 p. </ref>.}}
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==Notes==
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Most foraminifera live on or within the seafloor sediment; they are a major components of many deep-sea oozes. Chalk is largely composed of foraminiferan shells. Most foraminifera are heterotrophic organisms (microzooplankton).
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See also [https://en.wikipedia.org/wiki/Foraminifera wikipedia].
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==Related article==
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[[Marine Plankton]]
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==References==
 
==References==
 
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Latest revision as of 12:14, 25 December 2023

Definition of Foraminifera:
(= foraminiferans) phylum of mainly marine unicellular protists (classified as protozoans of class Sarcodina in older zoological classifications), having a highly vacuolated outer layer of cytoplasm and a calcareous, siliceous or composite shell through which project fine pseudopodia. [1].
This is the common definition for Foraminifera, other definitions can be discussed in the article


Notes

Most foraminifera live on or within the seafloor sediment; they are a major components of many deep-sea oozes. Chalk is largely composed of foraminiferan shells. Most foraminifera are heterotrophic organisms (microzooplankton). See also wikipedia.


Related article

Marine Plankton


References

  1. Lawrence, E. (2005). Henderson’s dictionary of biology. Pearson Education Limited, 13th ed., Harlow. 748 p.