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 …

The early Toarcian oceanic anoxic event (T-OAE,~ 183 Ma), also known as the Jenkyns
Event, was one of the most important hyperthermal events of the Phanerozoic, caused by the …

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 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 …

The sources of isotopically light carbon released during the end-Triassic mass extinction
remain in debate. Here, we use mercury (Hg) concentrations and isotopes from a pelagic …

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 …

Abstract The Permian–Triassic mass extinction is the most severe biotic crisis identified in
Earth history. Over 90% of marine species were eliminated,, causing the destruction of the …

Plants first colonized the land over 430 million years ago, having evolved from some of the
most primitive forms of life. Since then, plants have played a major role in supplying the …

Periods of oceanic anoxia have had a major influence on the evolutionary history of Earth
and are often contemporaneous with mass extinction events. Changes in global (as …

Abstract The Permian-Triassic mass extinction was the most severe biotic crisis in the past
500 million years. Many hypotheses have been proposed to explain the crisis, but few …