Garra dunsirei Banister, 1987

Esmaeili, Hamid Reza, Jufaili, Saud Al, Masoumi, Amir Hassan & Zarei, Fatah, 2022, Ichthyodiversity in southeastern Arabian Peninsula: Annotated checklist taxonomy, short description and distribution of Inland fishes of Oman, Zootaxa 5134 (4), pp. 451-503 : 466

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
status

 

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.

Kingdom

Animalia

Phylum

Chordata

Class

Actinopterygii

Order

Cypriniformes

Family

Cyprinidae

Genus

Garra

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