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Nekton or necton (from the ) is any that can actively and persistently propel itself through a (i.e. swim) without touching the . Nekton generally have powerful and (e.g. , , flippers or jets) that make them strong enough swimmers to counter , and have mechanisms for sufficient lift and/or to prevent sinking. Examples of nekton include most (especially like and ), (, and ) and (specifically ), , ( and ) and several species of decapod crustaceans (specifically , and ).

The term was proposed by German biologist to differentiate between the active swimmers in a body of water, and the that are passively carried along by the current. As a guideline, nektonic organisms have a high (greater than 1000) and planktonic organisms a low one (less than 10). Some organisms begin their life cycle as , and transition to nektonic juveniles and later in life. This may make distinction difficult when attempting to classify certain plankton-to-nekton species as one or the other. For this reason, some biologists avoid using this term.


History
The term was first proposed and used by the German biologist in 1891 in his article Plankton-Studien where he contrasted it with , the aggregate of passively floating, drifting, or somewhat motile organisms present in a body of water, primarily tiny and , small eggs and larvae of marine organisms, and and other minute consumers. Today it is sometimes considered an obsolete term because it often does not allow for a meaningful quantifiable distinction between these two groups. The colonization of the water column is very important for the evolution of marine animals. The Devonian Nekton Revolution (DNR), well known as the Age of Fishes, accounted for more than eighty-five percent of nekton, which were widespread during the Carboniferous period that took place during the . Some biologists no longer use the term.
(1977). 9789401013260
Haeckel, E. 1891. Plankton-Studien. Jenaische Zeitschrift für Naturwissenschaft 25 / (Neue Folge) 18: 232–336. BHL.


Definition
As a guideline, nekton are larger and tend to swim largely at biologically high (>1000 to beyond 109), where inertial flows are the rule, and eddies (vortices) are easily shed. Plankton on the other hand are small, and if they swim at all, do so at biologically low Reynolds numbers (0.001 to 10), where the viscous behavior of water dominates, and reversible flows are the rule. Organisms such as and others are considered plankton when they are very small and swim at low Reynolds numbers, and considered nekton as they grow large enough to swim at high Reynolds numbers. Many animals considered classic examples of nekton (e.g., , , ) start out life as tiny members of the plankton and then, it is argued, gradually transition to nekton as they grow.


Oceanic nekton
Oceanic nekton comprises largely from three :

There are organisms whose initial life stage is identified as planktonic, but when they grow and increase in body size they become gradually more nektonic. A typical example is the medusa of the jellyfish, which can actively propel itself (though generally insufficient to overcome strong currents).


See also
  • (organisms, including microscopic, living at the surface of the water)
  • (organisms, including microscopic, living at the bottom of a body of water)


External links
  • Stefan Nehring and Ute Albrecht (1997): "Hell und das redundante Benthon: Neologismen in der deutschsprachigen Limnologie". In: Lauterbornia H. 31: 17–30, Dinkelscherben, December 1997 E-Text (PDF-Datei)

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