Eratotrivia, SACCO, 1894
publication ID |
https://doi.org/ 10.5070/P9401057774 |
publication LSID |
lsid:zoobank.org:pub:11600574-2B0E-4C13-BC08-A3A5EF9EE562 |
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https://doi.org/10.5281/zenodo.13887917 |
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https://treatment.plazi.org/id/921FD94C-FFF5-FF8E-FE86-F990FA51FC0B |
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Felipe |
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Eratotrivia |
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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 narrow; 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.
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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