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Ostracoda from the Ellis Bay Formation (Ordovician), Anticosti Island, Quebec

Murray John Copeland

出版	Department of Energy, Mines and Resources, 1973
URL	http://books.google.com.hk/books?id=D7v-Gu6OHx8C&hl=&source=gbs_api

註釋

The 200- to 300- foot-thick Ellis Bay Formation on Anticosti Island has yielded a well preserved and distinctive ostracode fauna. This fauna is closely related to that of the underlying Vaureal Formation and contains elements common to the Porkuni beds of Estonia and the Dalmanitina Series (5a, 5b) of Norway. The Late Ordovician age of these faunas is indicted.