continental Faunal succession and with the Cordylodus angulatus Zone of the Baltic-Scania succession.

Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected by J. C. Troelsen in 1941 at Kap Qay, Washington Land, western North Greenland. The samples probably derived from the Cape Clay Formation which is exposed in the steep coastal cliff. The macrofauna o...

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Bibliographic Details
Main Authors: Western North Greenl, Svend Stouge, Gabriella Bagnoli Stouge, Roberto Albani
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Island
Canadian Arctic Archipelago
Arctic
Greenland
Kap
Washington Land
Arctic Archipelago
North Greenland
Washington land
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.515.9305
http://2dgf.dk/xpdf/bull33-03-04-261-272.pdf
Description
Summary:Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected by J. C. Troelsen in 1941 at Kap Qay, Washington Land, western North Greenland. The samples probably derived from the Cape Clay Formation which is exposed in the steep coastal cliff. The macrofauna of the samples includes Symphysurina sp. of Early Ordovician age. The conodont fauna comprises "Paltodus" bassleri Furnish, Utahconus oneotensis (Furnish), "Oistodus " triangularis Furnish, and species of Cordylo-dus Pander and "Acontiodus " Pander. The fauna correlates with Fauna C of the North American Mid-

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