Ocean acidification may have severe consequences for marine ecosystems; however,
assessing its future impact is difficult because laboratory experiments and field observations …

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 …

The temporal link between large igneous province (LIP) eruptions and at least half of the
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …

The end-Permian mass extinction was the most severe in the Phanerozoic, extinguishing
more than 90% of marine and 75% of terrestrial species in a maximum of 61±48 ky. Because …

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 temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …

INTRODUCTION Climate change triggered by volcanic greenhouse gases is hypothesized
to have caused the largest mass extinction in Earth's history at the end of the Permian Period …

Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for
the Permo-Triassic Boundary mass extinction, but direct evidence for an acidification event …

Delayed Earth system recovery following the end-Permian mass extinction is often attributed
to severe ocean anoxia. However, the extent and duration of Early Triassic anoxia remains …

Previous studies of the end-Permian mass extinction have established that it was
geologically rapid, but condensed sections have made it difficult to establish the exact timing …