Elimia tenera
Artist’s reconstruction of Elimia tenera, note the sculptured shell not found in individuals preserved in chalcedony
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Mollusca
Class: Gastropoda
Subclass: Caenogastropoda
Family: Pleuroceridae
Genus: Elimia
Species:
E. tenera
Binomial name
Elimia tenera
(Hall, 1845)
Elimia tenera in chalcedony from Wyoming


Elimia tenera, formerly known as Goniobasis tenera, is an extinct species of freshwater snail with an operculum, in the aquatic gastropod mollusk family Pleuroceridae.[1] This species flourished during the Eocene and is now known only from the fossil record.

Elimia tenera from the Green River Formation, showing ostracods packed inside and around the gastropods' shells

The genus name Elimia was restored to this species in 1975;[2] formerly it was placed in Goniobasis.

Green River Formation deposits

Fossilized Elimia tenera shells occur in a region which is now southern Wyoming, northern Colorado and northeastern Utah. The best preserved Elimia tenera are from Lake Gosiute which fossils occur in the Fort Laclede Bed of the Laney Member at outcrops in Sweetwater County, in southwestern Wyoming.[3]

'Turritella agate'

The fossils are hosted in chalcedony-rich sedimentary rock. This rock was originally incorrectly called Turritella agate.[4] It was named after the sea snail genus Turritella because of the resemblance of the freshwater snail shells to the Turritella fossils that are found in agate in Texas and California. The Wyoming fossil shells, however, are in a freshwater sedimentary deposit and identifiable as the genus Elimia, and are less-silicified than those in Texas and California.

Paleoecology and paleogeology

The fossil beds are approximately 46 to 51 million years old and occur in the Laney Member of the Green River Formation.[5] Evidence suggests that the Elimia tenera were deposited nearshore in a series of shallow lakes, which geologists have named the Fossil, Uinta and Gosiute Lakes.[6] The climate was subtropical and there were intermittent volcanic eruptions.[7]

References

  1. ↑ Burch, J. B. (1989). North American Freshwater Snails. Malacological Publications, Hamburg, Michigan, OCLC 20559611
  2. ↑ Hartman, Joseph H. and Roth, Barry (1998) "Late Paleocene and Early Eocene Nonmarine Molluscan Faunal Change in the Bighorn Basin, Northwestern Wyoming and South-Central Montana" pp. 358-359 in Aubry, Marie-Pierre; Lucas, Spencer G. and Berggren, William A. (Eds.) (1998). Late Paleocene-early Eocene climatic and biotic events in the marine and biotic events in the marine and terrestrial records Columbia University Press, New York, pp. 323-379, ISBN 0-231-10238-0
  3. ↑ Graham, Kenneth Lee (1996). Rockhounding Wyoming. Falcon, Guilford, Connecticut, ISBN 1-56044-445-2
  4. ↑ Dolenc, A. (1979). "Turritella agate - a new find in southwest Wyoming". Lapidary Journal 33(8): p. 1692
  5. ↑ "Laney Member of Green River Formation", United States Geological Survey
  6. ↑ "Green River Lakes", greenrivereocene.com
  7. ↑ Carroll, A. R. & Bohacs, K. M. (1999). "Stratigraphic classification of ancient lakes: Balancing tectonic and climatic controls". Geology. 27: pp. 99-102
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.