This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …

Oceanic anoxic events (OAEs) record profound changes in the climatic and
paleoceanographic state of the planet and represent major disturbances in the global …

The temporal link between large igneous province (LIP) eruptions and at least half of the
major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …

Patterns of uranium–molybdenum covariation in marine sediments have the potential to
provide insights regarding depositional conditions and processes in paleoceanographic …

The temporal link between mass extinctions and large igneous provinces is well known.
Here, we examine this link by focusing on the potential climatic effects of large igneous …

Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

Abstract The Jurassic (∼ 201–145 Myr ago) was long considered a warm
'greenhouse'period; more recently cool, even 'icehouse'episodes have been postulated …

The tropical, warm, and equable climate of the Jurassic world is regularly challenged by
geoscientists, especially since oxygen isotopes (δ18O) of fossil hardparts have been used to …

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 …

Abstract The Early Jurassic Toarcian oceanic anoxic event (∼ 183 Ma) was marked by
marine anoxia–euxinia and globally significant organic-matter burial, accompanied by a …