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 …

Abstract Analysis of the Lower Triassic sedimentary rock record has revealed a variety of
unusual sedimentary fabrics and features, many of which were more common in the …

The latest Permian mass extinction, the most devastating biocrisis of the Phanerozoic, has
been widely attributed to eruptions of the Siberian Traps Large Igneous Province, although …

Euxinia was widespread during and after the end-Permian mass extinction and is commonly
cited as an explanation for delayed biotic recovery during Early Triassic time. This anoxic …

Fabric and pyrite framboid size analysis of Permian to Jurassic samples from the Mino-
Tamba terrane of Japan provide an 80myr redox history from the Panthalassa Ocean. Fully …

The end of the Permian was a time of crisis that culminated in the Earth's greatest mass
extinction. There is much speculation as to the cause for this catastrophe. Here we provide a …

The current knowledge of Paleozoic radiolarian ranges, proposed zonations, and faunal
assemblages that have been used in biostratigraphy over the past few decades is compiled …

Several new Triassic–Jurassic boundary sections from the Eiberg Basin (Northern
Calcareous Alps, Austria) have been studied at high resolution. We present integrated …

Abstract Analysis of Permian–Triassic brachiopod diversity and body size changes from
different water depths spanning the continental shelf to basinal facies in South China …

We describe variations in trace element compositions that occurred on the deep seafloor of
palaeo-superocean Panthalassa during the end-Permian mass extinction based on samples …