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 …

Stratigraphic sections in the Bogda Mountains, NW China, provide detailed records of late
Permian–Early Triassic terrestrial paleoenvironmental and paleoclimatic evolution at the …

Current large-scale deforestation poses a threat to ecosystems globally, and imposes
substantial and prolonged changes on the hydrological and carbon cycles. The tropical …

Rapid climate change was a major contributor to the end-Permian extinction (EPE).
Although well constrained for the marine realm, relatively few records document the pace …

Harmful algal and bacterial blooms linked to deforestation, soil loss and global warming are
increasingly frequent in lakes and rivers. We demonstrate that climate changes and …

Abstract Eruption of the Siberian Traps large igneous province (LIP) is thought to have
triggered the Permian-Triassic biological crisis, the largest of the Phanerozoic mass …

The current model for the end-Permian terrestrial ecosystem crisis holds that systematic loss
exhibited by an abrupt turnover from the Daptocephalus to the Lystrosaurus Assemblage …

Wildfire has been implicated as a potential driver of deforestation and continental
biodiversity loss during the end-Permian extinction event (EPE;∼ 252 Ma). However, it …

Abstract Upper Permian to Lower Triassic coastal plain successions of the Sydney Basin in
eastern Australia have been investigated in outcrop and continuous drillcores. The purpose …

Abstract The Permian-Triassic Mass Extinction (ca. 252 Ma; PTME) is the most severe
biocrisis of the Phanerozoic in both the oceans and on land. The crisis saw the collapse of …