The link between the Permian–Triassic mass extinction (252 million years ago) and the
emplacement of the Siberian Traps Large Igneous Province (STLIP) was first proposed in …

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

Nonmarine biostratigraphic/biochronologic schemes have been created for all or parts of the
late Carboniferous–Middle Triassic using palynomorphs, megafossil plants, conchostracans …

Abstract The Permian–Triassic mass extinction was marked by a massive release of carbon
into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …

The end-Permian mass extinction is the greatest biotic crisis in Earth history causing the
extinction of a large number of marine and terrestrial animals globally. However, how land …

The collapse of late Permian (Lo**ian) Gondwanan floras, characterized by the extinction
of glossopterid gymnosperms, heralded the end of one of the most enduring and extensive …

Abstract The Permian-Triassic mass extinction is widely attributed to the global
environmental changes caused by the eruption of the Siberian Traps. However, the precise …

Global warming is inferred to have been one of the main causes of the Permian-Triassic (P-
Tr) boundary mass extinction. Although a strong temperature rise in tropical sea-surface …

The Triassic rocks are widespread in China, and both marine and terrestrial strata are well
developed. The Triassic stratigraphic architecture of China is very complex in both spatial …

This study reviews plant species richness and abundance change from the End Permian to
Middle Triassic in South China and examines the co-evolutionary relationship between the …