Data about <i>Folifer brevifilis</i>

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Distribution

 
geographic distribution includes
Additional detail
Asia: China, Viet Nam, Laos, Thailand and Myanmar
FishBase  

Ecology

 
habitat
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drainage basin
  • drainage basin
    A regions or area bounded by drainage divides and occupied by a drainage system; specifically the tract of country that gathers water originating as precipitation and contributes it to a particular stream channel or system of channels, or to a lake, reservoir, or other body of water.
    http://purl.obolibrary.org/obo/ENVO_00000291
Environments - EOL project  
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fresh water
Environments - EOL project  
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headwater
  • headwater
    The upper part of a river system, denoting the upper basin and source streams of a river.
    http://purl.obolibrary.org/obo/ENVO_00000153
Environments - EOL project  
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Large river biome
Environments - EOL project  
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river
  • river
    Natural freshwater surface streams of considerable volume and a permanent or seasonal flow, moving in a definite channel toward a sea, lake, or another river; any large streams, or ones larger than brooks or creeks, such as the trunk stream and larger branches of a drainage system.
    http://purl.obolibrary.org/obo/ENVO_00000022
Environments - EOL project  
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river mouth
  • river mouth
    The end of a stream where it enters a standing water body such as a lake, sea or ocean.
    http://purl.obolibrary.org/obo/ENVO_00000386
Environments - EOL project  
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sea
  • sea
    A large expanse of saline water usually connected with an ocean.
    http://purl.obolibrary.org/obo/ENVO_00000016
Environments - EOL project  
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tributary
  • tributary
    A stream or river which flows into another river (a parent river) or body of water but which may not flow directly into the sea.
    http://purl.obolibrary.org/obo/ENVO_00000495
Environments - EOL project  
Additional detail
brackish water environment
FishBase  
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freshwater environment
FishBase  
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oceanic benthopelagic zone biome
  • oceanic benthopelagic zone biome
    The benthopelagic zone biome comprises regions of the marine water column which usually coincide with the benthic boundary layer (BBL) - the layer of isothermal and isohaline water contiguous to the sea floor. A general reversal in the declining gradient of pelagic biomass may be observed here, perhaps explained by viable nutrition on the sea floor being resuspended by bottom currents. This zone typically extends 100 m above the seafloor, but may reach upto1000 m during benthic storms.
    http://purl.obolibrary.org/obo/ENVO_01000040
FishBase  

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