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Rasmussen, 1991

Conodont stratigraphy of the Lower Ordovician Huk Formation at Slemmestad, southern Norway

Rasmussen, J. A.
URL
Year1991
JournalNorsk Geologisk Tidsskrift
Volume71
Number4
Pages265-288
Typearticle in journal
LanguageEnglish
Id3978

Abstract

Conodonts are present throughout the Lower Ordovician Huk Formation (previously the "Orthoceras Limestone') at Slemmestad, southern Norway. Eighteen genera and 34 species are present. Drepanoistodus stougei n.sp. is described and taxonomic notes are included. The Huk Formation comprises, in ascending order, four conodont zones: The B. navis, P. originalis, M. parva and E.? variabilis zones, although only the E.? variabilis-M. parva Subzone of the latter zone is present. It is suggested that the Arenig-Llanvirn boundary is situated within the lowest 1 m of the Svartodden Member, the uppermost member of the Huk Formation.

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