Garra dunsirei Banister, 1987
publication ID |
https://doi.org/ 10.11646/zootaxa.5134.4.1 |
publication LSID |
lsid:zoobank.org:pub:47796EB6-B7FE-4442-AED3-E664DCC9A9B4 |
DOI |
https://doi.org/10.5281/zenodo.6543059 |
persistent identifier |
https://treatment.plazi.org/id/03FBBC4B-095B-B205-EC95-FF4B233C4D7C |
treatment provided by |
Plazi |
scientific name |
Garra dunsirei Banister, 1987 |
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4. Garra dunsirei Banister, 1987 View in CoL , Endemic
Fig. 16 View FIGURE 16
Etymology: Garra : named based on a vernacular Indian name, a fish living in mud; dunsirei : named after Mr. A. Dunsirei who collected the fishes.
Common name: Tawi Atair Garra .
Taxonomy: Garra dunsirei was originally described by Banister 1987:59, figs. 1, 2a, 3-5 [Bulletin of the British Museum (Natural History) Zoology v. 52 (no. 1) from a Sinkhole, Tawi Atair [or Attair], 17°06’N, 54°34’E, in the Jabal Qara (Jabal Samhan) mountains , Dhofar, Oman. GoogleMaps
Holotype: BMNH 1984 .3.6.571 . Paratypes: BMNH 1984.3.6.572-576 (6) .
Short description: It is distinguished from the other Garra species in the region by having the highly unusual shape of neural spines below the dorsal fin, being very short and not penetrating between dorsal pterygiophores, whitish or pink body, very small eye, absence or reduction of scales on breast and abdomen.
Distribution: Garra dunsirei is restricted to a sinkhole at Tawi Attair, in the Jabal Qara (Jabal Samhan) mountains, Dhofar, Oman ( Fig. 17 View FIGURE 17 ). Tawi Atair is a very impressive limestone formation at the surface level (680 m above the sea level) with a depth of about 211 m.
Examined material: Based on holotype and paratypes.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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