Didacna protracta

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Phylum:Mollusca
Class:Bivalvia
Order:Cardiida
Family:Cardiidae
Didacna protracta
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Order: Cardiida
Family: Cardiidae
Genus: Didacna
Species:
D. protracta
Binomial name
Didacna protracta
(Eichwald, 1841)
Synonyms
  • Didacna protracta var. grimmi Andrusov, 1910
  • Didacna protracta var. media Andrusov, 1910
  • Didacna protracta var. submedia Andrusov, 1910

Didacna protracta is a brackish-water bivalve mollusc of the family Cardiidae, the cockles. It has a rounded-trapezoidal, thick, whitish shell, up to 42 mm (1.7 in) in length, with a small umbo and flattened ribs. The species is endemic to the Caspian Sea. It lives in the middle and southern parts of the sea at depths between 25 and 85 m (82–279 ft), rarely deeper.

Similar species

Didacna protracta has a rounded-trapezoidal, thick, moderately convex shell, with a small umbo, 30–40 flattened radial ribs, dense growth lines on the ventral margin and a smooth posterior ridge, which is more distinct near the umbo.[1][2][3][4] The shell length is up to 42 mm (1.7 in).[3][4] The coloration is whitish, with thin pale yellowish gray periostracum.[4] The hinge consists of one or two cardinal teeth in the right valve and one cardinal tooth in the left valve. The right valve sometimes has weakly developed lateral teeth.[3]

Didacna profundicola has a smaller shell, up to 15 mm (0.59 in) in length.[3]

The fossil species Didacna catillus has a less equilateral and usually more convex shell, with a wider posterior slope and without the characteristic dense growth lines on the ventral margin.[3][5]

Distribution and ecology

Didacna protracta is endemic to the Caspian Sea. It lives in the middle and southern parts of the sea at depths between 25 and 85 m (82–279 ft), rarely deeper.[1][6] The species does not occur in waters with salinity of less than 5‰.[7]

Fossil record

Didacna protracta is widespread in the Late Pleistocene (Lower Khvalynian) deposits of the northern Caspian Region. It is less common in the Upper Khvalynian sediments and is also present in the Holocene (Neocaspian) deposits of the Caspian Sea.[3][5]

Taxonomy

References

Cited texts

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