Abstract
The distribution of corals within the paleo-geotectonic units of Yugoslavia is varying during the Cretaceous period. Lower Cretaceous corals are restricted to the Dinarid Platform and to the Carpathian-Balcanid unit. Cenomanian-Turonian-Coniacian corals occur exclusively in the Drina-Ivanjica unit. The Santonian-Campanian and Maastrichtian corals are restricted to the northern part of the Inner Dinarids. The prosperity and obliteration of corals on the paleo-geotectonic units of Yugoslavia was caused by environmental changes due to tectonic activities.
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© 1992 Österreichische Akademie der Wissenschaften
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Turnšek, D. (1992). Tethyan Cretaceous corals in Yugoslavia. In: Kollmann, H.A., Zapfe, H. (eds) New Aspects on Tethyan Cretaceous Fossil Assemblages. Österreichische Akademie der Wissenschaften Schriftenreihe der Erdwissenschaftlichen Kommissionen, vol 9. Springer, Vienna. https://doi.org/10.1007/978-3-7091-5644-5_9
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