A significant number of new palaeomagnetic poles have become available since the last
time a compilation was made (assembled in 2005, published in 2008) to indicate to us that a …

Abstract The Central Atlantic magmatic province (CAMP) consists of basic rocks emplaced
as shallow intrusions and erupted in large lava flow fields over a land surface area in excess …

Angiosperms are by far the most species-rich clade of land plants, but their origin and early
evolutionary history remain poorly understood. We reconstructed angiosperm phylogeny …

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-Triassic extinction is one of the Phanerozoic's largest mass extinctions. This
extinction is typically attributed to climate change associated with degassing of basalt flows …

The end-Triassic extinction is characterized by major losses in both terrestrial and marine
diversity, setting the stage for dinosaurs to dominate Earth for the next 136 million years …

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 Central Atlantic Magmatic Province (CAMP) has long been proposed as having a
causal relationship with the end-Triassic extinction event (∼ 201.5 Ma). In North America …

Paleomagnetic and cycle stratigraphic analyses of nearly 7000 m of section from continuous
cores in the Newark basin and an overlap** 2500 meter-thick composite outcrop and core …

Ammonites underwent an evolutionary diversification after the mass extinction of the end
Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …