Abstract The Late Jurassic–Early Cretaceous is an interval of unstandardized stages and
includes the only Mesozoic system boundary without a Global Boundary Stratotype Section …

Limestones designated the Štramberk-type are the most common carbonate exotic clasts
(exotics) embedded in the uppermost Jurassic–Miocene flysch deposits of the Polish Outer …

Lithocodium aggregatum and Bacinella irregularis are now extinct, shallow marine life forms
of unknown taxonomic origin. Forming part of the tropical platform biota during much of the …

Abundant lagoonal oncoids occur in the Late Oxfordian Hauptmumienbank Member of the
Swiss Jura Mountains. Four oncoid types are observed in the studied sections and classified …

The closure of the western part of the Neotethys Ocean started in late Early Jurassic. The
Middle to early Late Jurassic contraction is documented in the Berchtesgaden Alps by the …

Although many case studies describe stromatoporoid-rich Jurassic reefs, there are only few
reliable data as to their distribution pattern. This is in part due to a largely taxonomic and …

Abstract The Štramberk Limestone (Tithonian–lower Berriasian) was developed on a
northerly located, isolated intra-Tethyan carbonate platform. It is composed of various facies …

Sažetak Several organisms or interaction of organisms have been described over a long
time interval from the Late Palaeozoic to Cretaceous as Tubiphytes, with the type species …

Abstract The Late Jurassic–Lower Cretaceous microorganisms incertae sedis Lithocodium
aggregatum Elliott and Bacinella irregularis Radoičić are taxonomically studied based on …

Abstract Late Jurassic–Early Cretaceous Štramberk-type reef limestones are known from
some parts of the Southern Carpathians in Romania. The Upper Jurassic deposits mainly …