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单词 contractile vacuole
释义

contractile vacuole


contractile vacuole

n. A membrane-bound organelle found in certain protists that pumps fluid in a cyclical manner from within the cell to the outside by alternately filling and then contracting to release its contents at various points on the surface of the cell. It functions in maintaining osmotic equilibrium.

contractile vacuole


contractile vacuole

[kən′trak·təl ′vak·yə·wōl] (cell and molecular biology) A tiny, intracellular, membranous bladder that functions in maintaining intra- and extracellular osmotic pressures in equilibrium, as well as excretion of water, such as occurs in protozoans.

contractile vacuole


vacuole

 [vak´u-ōl] a space or cavity in the protoplasm of a cell.contractile vacuole a small fluid-filled cavity in the protoplasm of certain unicellular organisms. It gradually increases in size and then collapses; its function is thought to be respiratory and excretory.

con·trac·tile vac·u·ole

a cavity formed by the accumulation of fluid in the ectoplasm of a protozoan; after increasing for a time it empties itself externally by a sudden contraction; it functions as an osmoregulatory mechanism for water balance, especially in freshwater protozoans.

contractile vacuole

n. A membrane-bound organelle found in certain protists that pumps fluid in a cyclical manner from within the cell to the outside by alternately filling and then contracting to release its contents at various points on the surface of the cell. It functions in maintaining osmotic equilibrium.

contractile vacuole

a membrane-surrounded vacuole that periodically fills with liquid, expands and then actively voids the contents to the outside of the organism. Particularly found in protozoans and freshwater sponges, the contractile vacuole appears to have an osmoregulatory function involving active transport. The vacuoles are surrounded by MITOCHONDRIA to produce ATP which drives a sodium pump, enabling water to pass into the vacuole against the osmotic gradient. This theory is supported by the relative absence of such vacuoles in marine amoebae, whereas they are common in freshwater forms that take in water along an osmotive gradient because of the higher (less negative) osmotic pressure inside the cell compared with outside.
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