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 …

Abstract The Triassic Period records important ecological transitions in the aftermath of the
end-Permian mass extinction and is a key interval in the evolution of modern coral reefs …

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 …

Industrialization has raised the concentration of carbon dioxide (CO2) in Earth's atmosphere
by half since 1770, posing a risk from ocean acidification to global biodiversity, including …

Abstract The end-Triassic (also Triassic-Jurassic) mass extinction severely affected life on
planet Earth 200 million years ago. Paleoclimate change triggered by the volcanic eruptions …

The end‐Triassic extinction coincided with an increase in marine black shale deposition and
biomarkers for photic zone euxinia, suggesting that anoxia played a role in suppressing …

Severe global climate change led to the deterioration of environmental conditions in the
oceans during the Toarcian Stage of the Jurassic. Carbonate platforms of the Western …

Mass extinctions have profoundly influenced the history of life, not only through the death of
species but also through changes in ecosystem function and structure. Importantly, these …

Throughout the history of complex life, Earth's climate and biogeochemical cycles have been
perturbed by Large Igneous Province (LIP) volcanism, with several LIP episodes correlating …

The cause-and-effect relationship between the c. 201 Ma eruption of the Central Atlantic
magmatic province (CAMP) and the end-Triassic abrupt climate change and mass extinction …