Abstract The Early Jurassic Toarcian oceanic anoxic event (T-OAE) is characterized by an extinction event, a major sea-level rise, enhanced marine primary productivity, elevated …
The Earth's cryosphere represents a huge climate-sensitive carbon reservoir capable of releasing carbon dioxide (CO 2) and methane (CH 4) from permafrost soils or gas reservoirs …
Ammonites underwent an evolutionary diversification after the mass extinction of the end Triassic induced by the formation of a Large Igneous province (LIP), and this group provides …
The geochemistry and mineralogy of organic-rich sediments of the Rietheim succession in northern Switzerland were studied to evaluate the main impacts of the early Toarcian …
Abstract The Early Jurassic was marked by multiple periods of major global climatic and palaeoceanographic change, biotic turnover and perturbed global geochemical cycles …
Throughout Earth's history, variations in atmospheric CO2 concentration modulated climate. Understanding changes in atmospheric carbon cycle is therefore pivotal in predicting …
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 …
Abstract The Pliensbachian–Toarcian boundary interval is characterized by a~ 3‰ negative carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from …
Abstract The Toarcian Oceanic Anoxic Event (T‐OAE,∼ 183 Myr) was a long‐lasting episode of ocean deoxygenation during the Early Jurassic. The event is related to a period …