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Kangyao, Baicheng, Jilin, China

FormationKangyao
Age:479 - 466 Ma
Ordovician
IntervalArenig
Lithologylimestone
Number of Collections1
Number of Occurrences12

Recorded Sample Locations

LocationRegionStratigraphic Name
Half mile west of Shang-kang-yaoBaicheng, Jilin, ChinaKangyao

Associated Units

Stratigraphic NameAgeLithologyOccurrence Records
Wuting466 - 461 Ma
Middle Ordovician
limestone16

Recorded Fossils

Accepted NameHierarchyAge
Orthambonites calligramma
species
7Animalia : Brachiopoda : Rhynchonellata : Orthida : Orthidae : Orthambonites : Orthambonites calligramma478.6 - 466 Ma
Ordovician
Liospira barbouri
species
7Animalia : Mollusca : Gastropoda : Holopeidae : Raphistomina : Liospira barbouri478.6 - 466 Ma
Ordovician
Eotomaria ulrichi
species
7Animalia : Mollusca : Gastropoda : Pleurotomariida : Eotomariidae : Eotomaria : Eotomaria ulrichi478.6 - 466 Ma
Ordovician
Donaldiella cicelia
species
7Animalia : Mollusca : Gastropoda : Lophospiridae : Donaldiella : Donaldiella cicelia478.6 - 466 Ma
Ordovician
Ectomaria sp.
genus
6Animalia : Mollusca : Gastropoda : Lophospiridae : Ectomaria478.6 - 466 Ma
Ordovician
Murchisonia perangulata
species
7Animalia : Mollusca : Gastropoda : Lophospiridae : Lophospira : Murchisonia perangulata478.6 - 466 Ma
Ordovician
Lophospira rectistriata
species
7Animalia : Mollusca : Gastropoda : Lophospiridae : Lophospira : Lophospira rectistriata478.6 - 466 Ma
Ordovician
Lophospira selecta
species
7Animalia : Mollusca : Gastropoda : Lophospiridae : Lophospira : Lophospira selecta478.6 - 466 Ma
Ordovician

References

Endo R. (1932) The Canadian and Ordovician formations and fossils of South Manchuria, United States National Museum Bulletin 164, 1-149
Wagner P. J. (2017) Paleozoic Gastropod, Rostroconch, Helcionelloid and Tergomyan Database
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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