Abstract The early Toarcian Oceanic Anoxic Event (Jenkyns Event) was associated with
major world-wide climatic changes with profound effects on the global carbon cycle. This …

Abstract The Early Jurassic Jenkyns Event (∼ 183 Ma) was characterized in terrestrial
environments by global warming, perturbation of the carbon cycle, enhanced weathering …

The early Toarcian biotic crisis (∼ 183 Ma), characterized in marine environments by abrupt
temperature fluctuations, included a hyperthermal event (Jenkyns Event) with sea-level …

The flooding of the Pliensbachian shelf of the North-South Axis of Central Tunisia during the
early Toarcian favoured the development of organic-rich facies in the most subsiding areas …

Abstract The early Toarcian Oceanic Anoxic Event (T-OAE, or Jenkyns Event,~ 183 million
years ago) was a major hyperthermal and global carbon-cycle perturbation, likely …

Abstract The uppermost Pliensbachian (Margaritatus Zone)-upper Toarcian (Pseudoradiosa
Zone) sediments (silty and variably calcareous claystones, marlstones, silty sandstones, and …

Abstract The Early and Middle Jurassic Marrat Formation in Kuwait was deposited along the
southwestern margin of the Neo-Tethys Ocean. The formation has been extensively cored …

Konservat-Lagerstätten—deposits with exceptionally preserved fossils of articulated multi-
element skeletons and soft tissues—offer the most complete snapshots of ancient organisms …

Abstract The Sogno Core represents one of the deepest pelagic records of the Toarcian
Oceanic Anoxic Event (T-OAE) in the Alpine-Mediterranean Tethys. New sedimentological …

Environmental changes governed the diversity of marine ecosystems and the evolution of
marine reptiles during the Jurassic. Abrupt climatic changes, mainly cooling, produced …