The latest Triassic was an interval of prolonged biotic extinction culminating in the end-
Triassic Extinction (ETE). The ETE is now associated with a perturbation of the global carbon …

Abstract The Dinarides and Carpathian-Balkans, the western Balkan Peninsula, form an
essential link between the Paleotethyan branches of the Adriatic Sea (Montenegro, Croatia) …

The late Norian “chaotic carbon episode” in the Late Triassic has been identified in North
America, Italy, and China, reflecting a global carbon isotope perturbation. Although it has …

The biostratigraphy and carbon stable isotopes of the Norian Stage (Upper Triassic) are well
studied in the western Tethys, but little information is available from the eastern Tethys …

We investigated for magnetostratigraphy the Rio Nigra and Rio Frommer stratigraphic
sections from Alpe di Siusi/Seiser Alm (Dolomites, northern Italy) in order to improve the …

Abstract The Late Triassic time interval witnessed several important biological turnovers,
extinctions and onset of new life forms. Therefore, it is crucial to better constrain the tectonic …

The geochemistry of Mariana forearc serpentinites sheds light on how the subducting slab
starts to devolatilize. International Ocean Discovery Program Expedition 366 targeted three …

The numerous discoveries of disintegrated skeletons of large terrestrial vertebrates within
several thin levels of the Upper Silesian Keuper initiated broad investigations into the …

A total of 125 samples from core from the Csővár borehole (north-central Hungary) were
investigated for conodont bio-and carbon-isotope chemostratigraphy. This 620 m thick …

Abstract For the Upper Triassic, conodonts are the primary tools utilized in biostratigraphic
investigations. For an effective biostratigraphic zonation, the species should be constrained …