Lower Ordovician conodonts from Washington Land, western North Greenland.

Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected in 1941 at Kap Clay, Washington Land, western North Greenland. The conodont fauna correlates with Fauna C of the North American Midcontinental Faunal succession and with the Cordylodus angulatus Zone...

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Bibliographic Details
Main Authors: STOUGE S., BAGNOLI, GABRIELLA, ALBANI, ROBERTO
Other Authors: Stouge, S., Bagnoli, Gabriella, Albani, Roberto
Format: Article in Journal/Newspaper
Language:English
Published: 1985
Subjects:
Greenland
Kap
Kap Clay
Washington Land
North Greenland
Washington land
Online Access:http://hdl.handle.net/11568/233551
Description
Summary:Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected in 1941 at Kap Clay, Washington Land, western North Greenland. The conodont fauna correlates with Fauna C of the North American Midcontinental Faunal succession and with the Cordylodus angulatus Zone of the Balto-Scanic succession. The conodont fauna is described applying multielement taxonomy.

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