The Palaeozoic–Mesozoic transition is marked by distinct perturbations in the global carbon
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …

Brachiopod faunas in Lower Triassic deposits from Spitzbergen, Primorye of Russia, Japan,
Mangyslak of Kazakhstan, Alpine Europe, the Caucasus, the Middle East, the Himalaya …

The latest Permian mass extinction (LPE), just prior to the Permian–Triassic boundary at~
252Ma, resulted in the disappearance of~ 90% of skeletonized marine taxa and the …

Early Triassic animal body fossils and trace fossils are small relative to those in older and
younger intervals. Size decreases sharply through the end-Permian extinction event and …

The Khunamuh Formation of the Guryul Ravine section in Kashmir provides one of the most
detailed deep-water records of the end-Permian mass extinction in Perigondwanan …

Ammonoids recovered much faster than other marine shelly invertebrates after the end-
Permian mass extinction. Based on a refined global data set at the basin level, we …

A new Early Triassic marine fauna is described from the Central Oman Mountains. The
fauna is Griesbachian in age, on the basis of abundant conodonts and ammonoids, and was …

Abstract Earliest Triassic microbialites (ETMs) and inorganic carbonate crystal fans formed
after the end-Permian mass extinction (ca. 251.4 Ma) within the basal Triassic Hindeodus …

A distinct negative δ13C excursion is documented in two Permian–Triassic sections (He**
and Tai**) in shallow marine carbonate platform deposits in the Nanpanjiang Basin, south …

Stable carbon isotope curves derived from Lower Triassic carbonate rocks from three Iranian
sections are established to investigate changes in the carbon cycle during the Early Triassic …