The Late Triassic Carnian Pluvial Episode (CPE) saw a dramatic increase in global humidity
and temperature that has been linked to the large-scale volcanism of the Wrangellia large …

The breakup of Pangaea and the rapid opening of the Ligurian and Central Atlantic oceans
during the Middle Jurassic resulted in widespread volcanism accompanied by significant …

Massive carbon dioxide (CO2) emissions are widely assumed to be the driver of the end-
Permian mass extinction (EPME). However, the rate of and total CO2 released, and whether …

The late Paleozoic ice age (LPIA) was the longest-lived glaciation of the Phanerozoic, and
the demise of LPIA is the Earth's only recorded transition from an icehouse to a greenhouse …

Abstract The Permian-Triassic Mass Extinction (PTME) is the greatest biodiversity crisis in
Earth history and while the marine crisis is increasingly well constrained, the timing and …

The End-Triassic Mass Extinction (ETME) saw the catastrophic loss of ca. 50% of marine
genera temporally associated with emplacement of the Central Atlantic Magmatic Province …

The late Paleozoic ice age (LPIA) during the Carboniferous and Permian (ca. 360–260 Ma)
was vegetated Earth's only recorded icehouse-to-greenhouse transition and provides a …

The deep-time geological record can provide insights into the processes and mechanisms of
glacier retreat. Ice sheets of the Late Paleozoic Ice Age (LPIA) collapsed extensively during …

Future environmental change may profoundly affect oceanic ecosystems in a complex way,
due to the synergy between rising temperatures, reduction in mixing and upwelling due to …

Abstract The Early Jurassic break-up of Pangea and the formation of the Central Atlantic
Ocean are associated with changes to the atmosphere, climate, and environment, as …