Hinnites

Summary

Hinnites is a genus of rock scallops, marine bivalve mollusks in the family Pectinidae, the scallops.[1]

Hinnites
Temporal range: Triassic - Recent
Fossil valve of Hinnites crispus from Pliocene of Italy
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Order: Pectinida
Family: Pectinidae
Genus: Hinnites
DeFrance, 1821

These mollusks have been recorded as fossils from the Triassic to the Quaternary (from 235.0 to 0.126 Ma). Fossils have been found in the sediments of Algeria, Angola, Tanzania, Ethiopia, South Africa, Oman, Saudi Arabia, United States, Australia and of various European countries.[2]

Description edit

This genus include scallops with thick shells resembling that of an oyster.[3]

Hinnites is unusual in that, like the extant taxon Crassadoma gigantea, it was free-swimming as a juvenile, but subsequently cemented itself to a hard substrate.

Species edit

Species within the genus Hinnites include:[2]

  • Hinnites corallinus G. B. Sowerby I, 1827
  • Hinnites crispus(Brocchi, 1814)
  • Hinnites denticostatusKlipstein 1843
  • Hinnites distortus (da Costa, 1778) [4]
  • Hinnites ercolanianusCocconi 1873
  • Hinnites granulosusKlipstein 1843
  • Hinnites obliquusMünster 1841
Species brought into synonymy
  • Hinnites cortesyi Defrance 1821: synonym of Hinnites crispus (Brocchi, 1814)
  • Hinnites giganteus (Gray, 1825) (synonym of Crassadoma gigantea)[5]
  • Hinnites multirugosus (Gale, 1928):[6] synonym of Crassadoma gigantea (J.E. Gray, 1825)

References edit

  1. ^ ITIS
  2. ^ a b Paleobiology Database
  3. ^ Merrian-webster
  4. ^ Femorale
  5. ^ "Wallawalla". Archived from the original on 2015-06-26. Retrieved 2015-06-26.
  6. ^ D.L.Leighton A growth profile for the rock scallop Hinnites multirugosus held at several depths off La Jolla, California
  • Vaught, K.C.; Tucker Abbott, R.; Boss, K.J. (1989). A classification of the living Mollusca. American Malacologists: Melbourne. ISBN 0-915826-22-4. XII, 195 pp.