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Costatoria (Costatoria?) subrotunda (BITTNER, 1901) a Smithian (Lower Triassic) marker from Tethys
No full textThe authors erect Costatoria costata var. subrotunda (Bittner) from Hungarian Lower Triassic to species level. Its subgeneric position is also discussed here. Thus, Costatoria is represented in the Werfen Formation of Dolomites area by two species: C. (Costatoria?) subrotunda (Bittner) from the upper part of Campil Member (Smithian) and C. (Costatoria) costata (Zenker) from Cencenighe and S. Lucano Members (Spathian). C. subrotunda shows a wide geographic distribution and could be considered as a helpful marker of Smithian age.-Author
Large foraminiferal facies in the Middle and Upper Eocene of Northeastern Italy (Colli Berici, Vicenza)
No full textNutrient regimes and euphotic habitats: the response of larger foraminifera and coralline red algae in Eocene and Oligocene rhodolith facies (north-eastern Italy)
No full textOligocene, paleoecolog
I banchi a bivalvi del Giurassico Inferiore (Piattaforma di Trento): dinamica deposizionale, modalità di insediamento e sviluppo
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The early macrofaunas of the Werfen Formation and the Permian-Triassic boundary in the Dolomites (Southern Alps, Italy)
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Banchi a Cornucardia nell’Unità di San Donato (Triassico Superiore, Calabria settentrionale)
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Marine fossil assemblages from Upper Permian to lowermost Triassic in the western Dolomites (Italy)
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Ostracod-bivalve response to shallow water poikiloaerobic conditions: Lower Jurassic black-shales (Veneto, northern Italy).
No full textMicro- and macrofossils as palaeoenvironmental proxies in Liassic oligohaline ecosystem (Trento Platform, north-eastern Italy).
No full textJurassic ostracod
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