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 …

Sea-level changes exert an important control on oceanic circulation and climate evolution.
Researchers have proposed that sea-level rise favored accumulation of sediments enriched …

Abstract Before the Late Cretaceous opening of the Black Sea, the Central Pontides
constituted part of the southern margin of Laurasia. Two features that distinguish the Central …

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

Widespread accumulation of thick carbonates is not typical of orogenic settings. During the
mid-Cretaceous, near the Bangong suture in the northern Lhasa terrane, the shallow-marine …

Abstract Upper Jurassic-lowermost Cretaceous carbonate build-ups are imaged on seismic
data in the Black Sea. They form important, untested, hydrocarbon reservoirs that are the …

The Pontides forming the southern continental margin of the Black Sea consist of the
Strandja, İstanbul and Sakarya zones. The Zonguldak-Ulus Basin, located in the NE part of …

The carbonate sediments of the Polish part of Tethys shelf contain Crescentiella-microbial-
cement facies. The facies is associated with Middle Oxfordian-Lower Kimmeridgian …

The controversial nature of Iberopora bodeuri is discussed. This microfossil presents striking
similarities with Acervulinidae, more specifically with the latest Cretaceous-Miocene genus …