We review available data constraining the extent, volume, age and duration of all major
Phanerozoic continental flood basalts (CFB or traps) and oceanic plateaus (OP), together …

The climate of the Triassic period was characterized by a non-zonal pattern, dictated by a
strong global monsoon system with effects that are most evident in the Tethys realm. This …

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 …

Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

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 …

A new oxygen isotope (δ 18 O) record derived from conodont apatite reveals variable long-
term climate trends throughout the Triassic period. This record shows several major, first …

Current chemostratigraphical studies of the Jurassic System primarily involve the use of one
sedimentary component (marine organic carbon), one divalent transition metal substituted in …