A series of global major geological and biological events occurred during the Permian
Period. Establishing a highresolution stratigraphic and temporal framework is essential to …

The latest Permian mass extinction (LPME) coincided with major changes in the composition
of marine plankton communities, yet little is known about concurrent changes in primary …

The Siberian Traps large igneous province (STLIP) is commonly invoked as the primary
driver of global environmental changes that triggered the end-Permian mass extinction …

The end-Permian mass extinction was the most severe biodiversity crisis in Earth history. To
better constrain the timing, and ultimately the causes of this event, we collected a suite of …

The end-Permian mass extinction was the most severe ecological event during the
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …

The greatest loss of biodiversity in the history of animal life occurred at the end of the
Permian Period (∼ 252 million years ago). This biotic catastrophe coincided with an interval …

The end-Permian mass extinction event (∼ 252 Mya) is associated with one of the largest
global carbon cycle perturbations in the Phanerozoic and is thought to be triggered by the …

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 …

Understanding the interplay of climatic and biological events in deep time requires resolving
the precise timing and pattern of paleotemperature changes and their temporal relationship …

The Permian marine lithostratigraphy, biostratigraphy and faunal compositions among all
the major tectonic blocks in the Qinghai–Tibet Plateau are synthesised based on published …