ABSTRACT The Tethys Ocean existed between the continents of Gondwana and Laurasia
from the Triassic to the Pliocene. Analyses of multiple biogeographic and phylogenetic …

This review aims to present an updated lithostratigraphic framework of the northern Danube
Basin in Slovakia, consistent with recent shifts in geochronology and depositional system …

The large number and distribution of rollback systems in Mediterranean orogens infer the
possibility of interacting extensional back‐arc deformation driven by different slabs. The …

Depositional sequences originating in semi-enclosed basins with endemic biota, partly or
completely isolated from the open ocean, frequently do not allow biostratigraphic …

Abstract The Tokaj Mts. volcanism occurred in a thinning continental lithosphere regime at
the final stage of the subduction process. Using high-precision zircon U-Pb dating, four …

Marine gateways prove to be important factors for changes in the ecology and biochemistry
of marginal seas. Changes in gateway configuration played a dominant role in the Middle …

Clinoforms and clinothems are important and common architectural elements in the
sedimentary record of many basins worldwide. The influence that they exert on …

The youngest regional chronostratigraphic unit of the Central Paratethys, the Pannonian
Stage, is benchmarked by the deposits of Lake Pannon, containing a highly endemic …

In this paper we establish when and how the Pannonian basin and associated Central
Paratethys basins were isolated from the remainder of the Paratethys, a system of back-arc …

Abstract The Badenian–Sarmatian boundary interval is marked by a major extinction event
of marine species in the Central Paratethys. The exact age of the boundary is debated …