Event stratigraphy is used to help characterise the Anthropocene as a chronostratigraphic
concept, based on analogous deep-time events, for which we provide a novel …

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 …

The end-Triassic mass extinction was one of the big five crises of the fossil record. It affected
diverse marine groups, including bivalves, brachiopods, ostracods, calcareous algae …

The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …

During the past 600 million years of Earth history, four of five major extinction events were
synchronous with volcanism in large igneous provinces. Despite improved temporal …

Abstract The Triassic–Jurassic transition, which is here broadly defined as extending from
the Late Triassic through the Early Jurassic (~ 237 Ma to 174 Ma), was an important interval …

There is an apparent temporal correlation between large igneous province (LIP)
emplacement and global environmental crises, including mass extinctions. Advances in the …

The Triassic was a time of diversification of the global floras following the mass-extinction
event at the close of the Permian, with floras of low-diversity and somewhat uniform aspect …

Abstract The Central Atlantic Magmatic Province (CAMP) is a large igneous province (LIP)
composed of basic dykes, sills, layered intrusions and lava flows emplaced before Pangea …

One of the most severe extinctions of complex marine life in Earth's history occurred at the
end of the Triassic period (~ 201.4 million years ago). The marine extinction was initiated by …