The Carnian Pluvial Episode (Late Triassic) was a time of global environmental changes
and possibly substantial coeval volcanism. The extent of the biological turnover in marine …

Abstract The Carnian Pluvial Episode was a phase of global climatic change and biotic
turnover that occurred during the early Late Triassic. In marine sedimentary basins, the …

The Triassic is bound by two mass extinctions that coincide with vast outpourings of volcanic
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …

Conodonts are biostratigraphically very important microfossils in the Upper Triassic,
occurring in different marine habitats, from deep-ocean to shallow-shelf waters. Because of …

Conodonts are tooth-like elements of a primitive chordate and are generally abundant in
many marine sedimentary rocks deposited from the late Cambrian to the latest Triassic. For …

Abstract The Carnian Pluvial Episode (CPE) was a short interval of extreme rainfall in the
Late Triassic that caused significant changes in marine ecosystems. Global warming …

In this paper we study the Lilang Super Group in the Spiti area, Indian Himalaya to
understand environmental changes in the aftermath of the end-Permian mass extinction. We …

The opening of the Neo‐Tethys started in the Middle Anisian and is recorded in the
drowning succession of the shallow‐water Ravni/Steinalm Carbonate Ramp and the …

The contribution to Tethyan and global Triassic studies from the Australian sector of
southeastern Tethys is limited relative to that from the Himalayan sector. Whilst many of the …

Abstract The Middle Triassic volcano-sedimentary successions deposited on the passive
continental margin during a period of intense extensional tectonics related to the opening of …