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Diagnostic Description

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A member of the group of species with complete or nearly complete lateral line, 8 1/2 branched dorsal rays, 9+8 branched caudal rays and no sexual dimorphism. It can be distinguished by its complete lateral line and inflated cheeks (Ref. 39226). Absence or small median notch in upper lip; head length 3.7-4.0 times in SL; body depth 5.7-6.1 times in SL; caudal peduncle with a low adipose keel, length 6.4-6.8 times in SL, depth 7.4-8.1 times in SL, 1.1-1.3 times in length (for individuals 5-7 cm SL); top of head vermiculated; body with 9-13 bars, slightly wider than interspaces, somewhat irregularly set, continuous across back; black bar at caudal base usually complete, sometimes not reaching ventral mid-line, bent forwards at upper extremity; dorsal base with a black spot anteriorly, followed by orange patch and a low elongate grey blotch (Ref. 43281).
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Recorder
Armi G. Torres
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Morphology

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Dorsal soft rays (total): 12; Analsoft rays: 8
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Biology

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Found in riffles (Ref. 43281). Inhabits mountain streams over sandy and gravelly bottom (Ref. 51717).
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Schistura bucculenta

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Schistura bucculenta is a species of ray-finned fish in the stone loach genus Schistura. It has been recorded from the Mekong basin in Laos and Thailand, records elsewhere being due to misidentification. It has been recorded in streams and forest creeks which have a moderate to fast current running over a gravel to stone substrate. It is threatened by deforestation and agriculture.[1]

References

  1. ^ a b Juffe Bignoli, D. (2012). "Schistura bucculenta". IUCN Red List of Threatened Species. 2012: e.T181049A1692747. doi:10.2305/IUCN.UK.2012-1.RLTS.T181049A1692747.en. Retrieved 18 November 2021.
  2. ^ Froese, Rainer; Pauly, Daniel (eds.) (2006). "Schistura bucculenta" in FishBase. April 2006 version.
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Schistura bucculenta: Brief Summary

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Schistura bucculenta is a species of ray-finned fish in the stone loach genus Schistura. It has been recorded from the Mekong basin in Laos and Thailand, records elsewhere being due to misidentification. It has been recorded in streams and forest creeks which have a moderate to fast current running over a gravel to stone substrate. It is threatened by deforestation and agriculture.

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