W Ruebsam, M Al-Husseini - Gondwana Research, 2020 - Elsevier
Abstract Cyclostratigraphic analyses of Upper Pliensbachian and Lower Toarcian carbon-13 isotope (δ 13 C) data, together with radiometric dating, are used to calibrate biozones and …
Global perturbations to the Early Jurassic environment (∼ 201 to∼ 174 Ma), notably during the Triassic–Jurassic transition and Toarcian Oceanic Anoxic Event, are well studied and …
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 …
Abstract The Early Jurassic was marked by multiple periods of major global climatic and palaeoceanographic change, biotic turnover and perturbed global geochemical cycles …
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 …
Sea-level change is an important parameter controlling the expansion of oxygen-depleted conditions in neritic settings during oceanic anoxic events (OAEs). Despite this fundamental …
A Fantasia, KB Föllmi, T Adatte… - Journal of the …, 2018 - lyellcollection.org
Palaeoenvironmental and palaeoclimatic changes during the Toarcian Oceanic Anoxic Event (T-OAE) are reported from two successions deposited in the Andean Basin (Chile) …
Abstract The late Early Jurassic Toarcian Stage represents the warmest interval of the Jurassic Period, with an abrupt rise in global temperatures of up to∼ 7° C in mid-latitudes at …
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 …