Eratotrivia, SACCO, 1894

Groves, Lindsey & Squires, Richard L., 2023, Revision of northeast Pacific Paleogene cypraeoidean gastropods, including recognition of three new species: implications for paleobiogeographic distribution and faunal turnover, PaleoBios 40 (10), pp. 1-52 : 37

publication ID

https://doi.org/ 10.5070/P9401057774

publication LSID

lsid:zoobank.org:pub:11600574-2B0E-4C13-BC08-A3A5EF9EE562

persistent identifier

https://treatment.plazi.org/id/921FD94C-FFF5-FF8E-FE86-F990FA51FC0B

treatment provided by

Felipe

scientific name

Eratotrivia
status

 

ERATOTRIVIA SACCO, 1894 View in CoL

Type Species— Erato crenata (Deshayes, 1835) [= Eratotrivia crenularis Schilder, 1927 View in CoL , non Oppenheim, 1901], by original designation (of Sacco, 1894: p. 62), Eocene (Lutetian), Chaumont, Haute-Marne Department, France

Diagnosis— Shell small, ob-ovate; spire concealed; columella region attenuated; slight canal; aperture nar- row; outer lip thickened, crenulated internally; surface ornamented by spiral ribs which anastomose in the dorsal region; along the mid-dorsal line, the ribs are interrupted more or less by a shallow groove.

Geologic Range— Early Eocene (Ypresian Stage), Washington ( Squires and Goedert 1994) to late Eocene (Bartonian Stage), Italy ( Dolin and Pacaud 2009).

Remarks — In the NEP region, Eratotrivia occurs as Eratotrivia crescentensis ( Weaver and Palmer 1922) of early Eocene age (“Capay Stage”) in Washington.

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF