The Triassic is bound by two mass extinctions that coincide with vast outpourings of volcanic
flood basalts. The Mesozoic begins with a gradual recovery of plant and animal life after the …

The Triassic is bounded by two mass extinctions that coincide with vast outpourings of
volcanic flood basalts. Ammonoids and conodonts are the main correlation tools for marine …

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 Early Triassic interval is dominated by unusual oceanic and climatic conditions that are
perhaps unique to the Phanerozoic. Early Triassic oceans were likely anoxic and possibly …

The transition from the Triassic to Jurassic Period, initiating the 'Age of the dinosaurs',
approximately 200Ma, is marked by a profound mass extinction with more than 50% genus …

The latest Triassic was an interval of prolonged biotic extinction culminating in the end-
Triassic Extinction (ETE). The ETE is now associated with a perturbation of the global carbon …

Abstract The Late Triassic was a prolonged episode characterized by high rates of biotic
turnover and discrete extinction events due to elevated extinction rates for some biotic …

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 …

The Triassic has long been recognized as a time during which marine and terrestrial
ecosystems modernized dramatically, and it seems to have been a two-step process. First …

Approximately 230 million years ago in the middle of the Carnian stage of the Upper
Triassic, the sedimentary records in different regional basins display dramatic changes …