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Conference on Carbonate Platform and Dolomitization , Ortisei , pp. 3 – 43 . Budai , T. , A. Vörös 2006 : Middle Triassic platform and basin evolution of the Southern Bakony

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and their correlation with the Germanic Middle Triassic. — Zentralblatt für Geologie und Paläontologie, Teil I, 199 8( 7 – 8 ), pp. 853 – 876 . Brack , P. , H. Rieber , A. Nicora , R. Mundil

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The Middle Triassic Wetterstein Limestone was investigated on the Feuerkogel, in the eastern Höllengebirge area, Austria. Cephalopod-bearing coquina interbeds consisting predominantly of orthocone cephalopods were found within the dasycladacean inner platform lagoon facies. Based on sedimentological studies the coquina beds are interpreted as storm accumulations. Dasycladacean biostratigraphic data permit assigning the studied succession to the Late Anisian-Early Ladinian interval. Ammonites of age-diagnostic value found in the coquina horizon suggest the Avisianum Subzone of the Reitzi Zone that corresponds to the upper part of the Anisian.

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H. Rieber A. Nicora 2003 The Global Stratigraphic Section and Point (GSSP) of the base of the Ladinian Stage (Middle Triassic). A proposal for the

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. Budai A. Vörös 1992 Middle Triassic history of the Balaton Highland: extensional tectonics and basin evolution Acta Geologica Hungarica

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. T. Budai A. Vörös 1993 The Middle Triassic events of the Transdanubian Central Range in the frame of the Alpine evolution

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Authors: Attila Ősi, Gábor Botfalvai, Edina Prondvai, Zsófia Hajdu, Gábor Czirják, Zoltán Szentesi, Emília Pozsgai, Annette E. Götz, László Makádi, Dóra Csengődi and Krisztina Sebe

Middle Triassic fish teeth from the Kalapani Limestone of Malla Johar, Chamoli district (Uttaranchal) Journal of the Palaeontological Society of India 47 151 155

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Authors: Sándor Kovács, János Haas, Péter Ozsvárt, Ladislav A. Palinkaš, Gabriella Kiss, Ferenc Molnár, Sándor Józsa and Szilvia Kövér

. Ozsvárt , P. , L. Dosztály , G. Migiros , V. Tselepidis , S. Kovács (in press): New radiolarian biostratigraphic age constraints on Middle Triassic basalts and radiolarites from the Inner Hellenides (Northern Pindos and Othris Mountains, Northern

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In the area of the Aggtelek-Rudabánya Mts, limestone and dolomite of reefal and lagoonal facies were formed on a platform, which was continuously deepening from the beginning of the Middle Triassic. The bulk of the limestone is represented by lagoonal formations, extremely rich in dasycladaceans. The reefal formations are of patch reef origin. The almost continuous development and the remarkable abundance of fossils permitted the elaboration of an Anisian-Carnian dasycladacean biostratigraphy. On the basis of investigations 4 assemblage zones could be separated in the Anisian, and 6 in the Ladinian-Carnian. In establishing this biostratigraphy dasycladacean investigations of similar facies areas of the Silica Plateau and the Northern Calcareous Alps were also taken into account.

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Farabegoli, E., M. C. Perri 1998 b: Stop 3.3B - Middle Triassic conodonts at the Pelsonian/Illyrian boundary of the Nosgieda section (Southern Alps, Italy). - In: M. Perri C., C. Spalletta (Eds): ECOS VII Southern Alps Field

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