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 …

While demonstrating ocean acidification in the modern is relatively straightforward (measure
increase in atmospheric CO2 and corresponding ocean chemistry change), identifying …

Hungary lies in the central part of the Pannonian Basin, surrounded by the ranges of the
Alps, Carpathians, and Dinarides. The geology of the country can be summarized as a …

The history of the Earth system is a story of change. Some changes are gradual and benign,
but others, especially those associated with catastrophic mass extinction, are relatively …

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 …

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 …

Carbon-isotope stratigraphy is a useful tool for stratigraphic correlation, especially for strata
deposited during major perturbations of the carbon cycle that affected the marine, terrestrial …

Conodonts are biostratigraphically very important microfossils in the Upper Triassic,
occurring in different marine habitats, from deep-ocean to shallow-shelf waters. Because of …

The Triassic‐Jurassic boundary mass‐extinction event (T‐J; 199.6 Ma) is associated with
major perturbations in the carbon cycle recorded in stable carbon isotopes. Two rapid …

Summary The Triassic‐Jurassic transition (~ 201.5 Ma) is marked by one of the largest mass
extinctions in Earth's history. This was accompanied by significant perturbations in ocean …