The Late Triassic timescale is poorly constrained due largely to the dearth of reliable
radioisotopic ages that can be related precisely to biostratigraphy combined with evident …

The time span between the Variscan and Alpine cycles is not devoid of any major tectonic
activity, and corresponds to the Cimmerian cycle. Between the Early Permian and Late …

This paper summarizes 30 years of research on the biostratigraphy of Triassic radiolarians
and presents a correlation of currently-used radiolarian zonations established in North …

The catalogue of Mesozoic radiolarian genera is a revision of all described genera with re-
illustration of their type species. This project was organized under the auspices of the …

A review of marine and terrestrial animal and plant fossils fails to reveal convincing evidence
of a global catastrophe at the Triassic‐Jurassic boundary, although this time marked the final …

The break‐up of Pangea began during the Triassic and was preceded by a generalized
Permo‐Triassic formation of continental rifts along the future margins between Africa and …

Abstract The Carnian Pluvial Episode (CPE) was a global environmental change and biotic
crisis that occurred during the Carnian (Late Triassic). The climate during the CPE was …

The Beyşehir–Hoyran–Hadim Nappes crop out over 700 km from NW to SE. Above a
regionally autochthonous Tauride carbonate platform the Beyşehir–Hoyran Nappes begin …

Within the Late Cretaceous mélange complex of the Izmir–Ankara suture zone in central
Sakarya area, north-western Turkey, a megablock with radiolarian cherts associated with …

Abstract The Isparta Angle has played a critical role in the development of concepts
concerning the tectonic evolution of the Mesozoic–Tertiary Neotethys in the Eastern …