Data about <i>Creagrutus amoenus</i>

TraitBank assembles data records from many providers. Select a row for more details about the record, or search within Creagrutus amoenus.

Distribution

Data about <i>Creagrutus amoenus</i>
geographic distribution includes
Additional detail South America: Andean foothill rivers of eastern Ecuador and southeastern Colombia. FishBase  

Physical Description

Data about <i>Creagrutus amoenus</i>
body length (CMO)
Additional detail 9.1 cm male or unsexed FishBase  

Ecology

Data about <i>Creagrutus amoenus</i>
habitat
Additional detail Large river biome Environments - EOL project  
Additional detail mountain
  • mountain
    A landform that extends above the surrounding terrain in a limited area. A mountain is generally steeper than a hill, but there is no universally accepted standard definition for the height of a mountain or a hill although a mountain usually has an identifiable summit and a local relief of more than 300m.
    http://purl.obolibrary.org/obo/ENVO_00000081
Environments - EOL project  
habitat
Additional detail freshwater environment FishBase  
Additional detail non-marine IRMNG - Interim Register of Marine and Nonmarine Genera.  
Additional detail 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  

Conservation

Data about <i>Creagrutus amoenus</i>
extinction status
Additional detail extant IRMNG - Interim Register of Marine and Nonmarine Genera.  

Disclaimer

EOL content is automatically assembled from many different content providers. As a result, from time to time you may find pages on EOL that are confusing.

To request an improvement, please leave a comment on the page. Thank you!