Triassic conodonts of the Slovenian Basin
AbstractSlovenian 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, Norigondolella and Paragondolella.
How to Cite
Buser, S., Kolar-Jurkovšek, T., & Jurkovšek, B. (2007). Triassic conodonts of the Slovenian Basin. Geologija, 50(1), 19–28. https://doi.org/10.5474/geologija.2007.002