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Oriskany - Glenerie Limestone, Ulster County, New York, USA

GroupOriskany
FormationGlenerie Limestone
Age:411 - 408 Ma
Early/Lower Devonian
IntervalPragian
Lithologylimestone
Number of Collections1
Number of Occurrences8

Recorded Sample Locations

LocationRegionStratigraphic Name
Glen Erie FallsUlster County, New York, USAOriskany - Glenerie Limestone

Recorded Fossils

Accepted NameHierarchyAge
Paciphacops logani
species
7Animalia : Arthropoda : Trilobita : Phacopida : Phacopidae : Paciphacops : Paciphacops logani410.8 - 407.6 Ma
Early/Lower Devonian
Coelospira dichotoma
species
7Animalia : Brachiopoda : Rhynchonellata : Athyridida : Anoplothecidae : Coelospira : Coelospira dichotoma410.8 - 407.6 Ma
Early/Lower Devonian
Floweria becraftensis
species
7Animalia : Brachiopoda : Strophomenata : Orthotetida : Areostrophiidae : Floweria : Floweria becraftensis410.8 - 407.6 Ma
Early/Lower Devonian
Platyceras reflexum
species
7Animalia : Mollusca : Gastropoda : Platyceratidae : Platyceras : Platyceras reflexum410.8 - 407.6 Ma
Early/Lower Devonian
Diaphorostoma desmatum
species
7Animalia : Mollusca : Gastropoda : Platyceratidae : Platyostoma : Diaphorostoma desmatum410.8 - 407.6 Ma
Early/Lower Devonian
Platyostoma gebhardi
species
7Animalia : Mollusca : Gastropoda : Euomphalina : Platyceratidae : Platyceras : Platyostoma gebhardi410.8 - 407.6 Ma
Early/Lower Devonian
Platyostoma ventricosum
species
7Animalia : Mollusca : Gastropoda : Platyceratidae : Platyostoma : Platyostoma ventricosum410.8 - 407.6 Ma
Early/Lower Devonian
Cyrtolites sp.
genus
6Animalia : Mollusca : Tergomya : Cyrtonellida : Cyrtolitidae : Cyrtolites410.8 - 407.6 Ma
Early/Lower Devonian

References

Clarke J. M. The Oriskany fauna of Becraft Mountain, Columbia County, N. Y., New York State Museum Bulletin 3 3, 1-128
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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