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Geologija  2007 

Triassic conodonts of the Slovenian Basin

Keywords: conodonts , Triassic , Slovenian Basin , Slovenia

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Abstract:

Slovenian Basin was formed during the Ladinian following disintegration of the Slovenian Carbonate Platform. It persisted continuously until the Late Cretaceous. Several conodont asscociations were recognized within the Triassic rocks of the Slovenian Basin. Stratigraphically significant species belong to the genera Budurovignathus, Epigondolella, Gladigondolella, Metapolygnathus, Misikella, Neogondolella, Nicoraella, Norigondolellaand Paragondolella.

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