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Elita fimbriata (Conrad, 1842)

Elita fimbriata
Elita fimbriata

Scientific Classification

Kingdom: Animalia
Phylum: Brachiopoda
Class: Rynchonellata
Order: Spiriferida
Family: Elythidae
Genus: Elita
Species: Elita fimbriata (Conrad, 1842)

Information

Geological Range

Middle Devonian

Lower Devonian

Paleogeographic Distribution

Indiana

Kentucky

Michigan

New York

Ohio

Ontario

Pennsylvania

Stratigraphic Occurrences

Tully Formation
Upperville Member
Long Hill Member
West Brook Beds
Moscow Formation
Garrattsville Member
Windom Member
Mahantango Formation
Clearville Member
Pokejoy Member
Montebello Member
Upper Shale Member
Ludlowville Formation
Wanakah Member
Ivy Point Member
Otisco Member
Centerfield Member
Beechwood Member
Boyle Formation
Prout Formation
Hungry Hollow Member
Traverse Group
Four mile Dam Formation
Skaneateles Formation
Ashantee Member
Mottville Member
Plum Brook Formation
North Vernon Formation
Swanville Member
Oatka Creek Formation
Cardiff Member
Mount Marion Formation
Otsego Member
Onondaga Formation
Edgecliff Member
Moorehouse Member
Columbus Formation
Jeffersonville Formation
Grand Tower Formation
Schoharie Formation

References

Hall, J., 1867 (as Spirifera fimbriata): p. 214, pl. 33.

Wilson, K., 2014: pp. 112, 113.

Linsley, D., 1994: p. 202.

Remarks

Originally described as Delthyris fimbriata by Conrad in 1842. Recombined as Spirifer fimbriatus by Billings in 1861. Recombined as Reticularis fimbriata by Schuchert in 1897. Recombined as Elita fimbriata by Frederiks in 1918.

From Wilson (2014, p. 112): “Shell with hinge line less than shell width. Both valves strongly convex. Pedicle valve with rounded sinus and high, incurved beak. Brachial valve with distinct fold. Shell surface covered with regular array of tubercles or spine bases. To 25-35 mm.”

From Carlton Brett and Gordon Baird: A very distinctive brachiopod with surface covered in small spines; this is a long ranging (Emsian-Givetian, possibly Famennian?) Eastern Americas Realm species. It was generally though to have its last major occurrence in the paper part of the Tully Formation (West Brook Beds which was called the E. fimbriata Zone by Cooper and Williams (1935, GSA Bull.)). However, rare specimens of a reticularacean brachiopod nearly identical to E. fimbriata have recently been found in high Famennian strata in western Pennsylvania (G.C. Baird, unpublished data). Elita is characteristic of high diversity brachiopod and even coral-dominated assemblages of carbonates and calcareous mudstones (Pseudoatrypa-Megastrophia Biofacies of Brett et al., 2007, Palaios). However, occasional specimens are present in the mudstone facies of Tropidoleptus-Nucleospira and Athyris-Mediospirifer biofacies. It is rare in heavy siliciclastic facies. Probably a pedically attached epifaunal brachiopod, the function of the long spines is unclear, possibly to trap sediment and make the surface less attractive to predators; nonetheless, specimens of E. fimbriata with boreholes are not uncommon (Smith et al., 1985, Science).

Online Resources

Paleobiology Database

Media

Images

Photography of Elita fimbriata PRI109542
Elite fimbriata from the Ludlowville Fm. (Wanakah Mbr.) of Erie County, New York (PRI 109542).
Illustrations of Elita fimbriata
Illustrations of Elita fimbriata from Hall (1867)

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