Environmental crises at the Permian–Triassic mass extinction
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 …
emplacement of the Siberian Traps Large Igneous Province (STLIP) was first proposed in …
Carboniferous and Permian integrative stratigraphy and timescale of North China Block
Abstract The Carboniferous-Permian strata in the North China Block (NCB) contain
abundant fossils, coals and natural gases. Establishing a high-resolution timescale for the …
abundant fossils, coals and natural gases. Establishing a high-resolution timescale for the …
Felsic volcanism as a factor driving the end-Permian mass extinction
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 …
driver of global environmental changes that triggered the end-Permian mass extinction …
[HTML][HTML] Six-fold increase of atmospheric pCO2 during the Permian–Triassic mass extinction
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 …
into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope …
Massive and rapid predominantly volcanic CO2 emission during the end-Permian mass extinction
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 …
global carbon cycle perturbations in the Phanerozoic and is thought to be triggered by the …
The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction
The end-Permian mass extinction was the most severe ecological event during the
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …
Phanerozoic and has long been presumed contemporaneous across terrestrial and marine …
Volcanic CO2 degassing postdates thermogenic carbon emission during the end-Permian mass extinction
Massive carbon dioxide (CO2) emissions are widely assumed to be the driver of the end-
Permian mass extinction (EPME). However, the rate of and total CO2 released, and whether …
Permian mass extinction (EPME). However, the rate of and total CO2 released, and whether …
[HTML][HTML] Permo–Triassic boundary carbon and mercury cycling linked to terrestrial ecosystem collapse
Records suggest that the Permo–Triassic mass extinction (PTME) involved one of the most
severe terrestrial ecosystem collapses of the Phanerozoic. However, it has proved difficult to …
severe terrestrial ecosystem collapses of the Phanerozoic. However, it has proved difficult to …
[HTML][HTML] End-Permian terrestrial ecosystem collapse in North China: evidence from palynology and geochemistry
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 …
biocrisis of the Phanerozoic in both the oceans and on land. The crisis saw the collapse of …
Climate and biotic evolution during the Permian-Triassic transition in the temperate Northern Hemisphere, Kuznetsk Basin, Siberia, Russia
Abstract The Siberian Traps volcanism is widely considered the main cause of the end-
Permian mass extinction, the greatest biological crisis in the Earth history. While the …
Permian mass extinction, the greatest biological crisis in the Earth history. While the …