The early Toarcian biotic crisis (∼ 183 Ma), characterized in marine environments by abrupt
temperature fluctuations, included a hyperthermal event (Jenkyns Event) with sea-level …

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 …

The tectonic development of the northeast margin of the Korabi-Pelagonian continent and
the adjacent Vardar ocean is discussed based on study of nine traverses across the former …

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

During the Oxfordian, sea-level rise created widespread carbonate platform deposition on
the margins of Neotethys, although some areas remain poorly described. One such area is …

Palaeocene reef complexes are among the rarely preserved geologic structures on Earth. In
the Western Carpathians traces of one of the most northern shallow-water reef complexes …

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 …

Three sections (Rebro, Lyalintsi and Velinovo) of the Upper Jurassic-Lower Cretaceous
carbonate sequences from the Lyubash unit (Srednogorie, Balkanides, SW Bulgaria) have …

The lowermost Cretaceous carbonate deposits of the Carpatho–Balkanides (Eastern
Serbia), which crop out in the Kučaj zone, were studied in three sections: Kamenica …

Abstract Piatra Craiului Massif is situated in the easternmost part of the Southern
Carpathians, Romania. The Kimmeridgian–lowermost Valanginian carbonate succession …