An intensification of the hydrological cycle is an expected consequence of global warming,
and this will likely lead to spatially variable precipitation and drought extremes, and more …

Abstract The Karoo Large Igneous Province (K-LIP) is considered to have substantially
influenced global warming, marine anoxia, and concomitant marine extinction in the …

Abstract The Toarcian Oceanic Anoxic Event (T-OAE;~ 183 Ma) of the Early Jurassic period
is considered a second-order bioevent, of major importance in the Mesozoic. This event …

Causes of the major mass extinction recorded during the Early Toarcian (Early Jurassic) are
controversial. Many authors have concluded that the mass extinction is caused by the …

A better understanding the functioning of Earth System in the context of past climatic
upheavals is essential for predictions about the fate of the diversity of life and the future of …

The analysis of macroinvertebrates, trace fossils, calcareous nannofossils and geochemistry
from Pliensbachian to Lower Toarcian deposits of the Subbetic (Southern Spain) allows us …

We used an integrated analysis of benthic foraminiferal assemblages, geochemical proxies
(paleoproductivity, redox, and detrital proxies), and C and O stable isotopes to characterize …

The bathyal and abyssal environments represent an extent benthic habitat. The deep-sea
floor is a dynamic setting affected by fluctuations of organic-matter deposition, sedimentation …

Abstract The Early Toarcian Oceanic Anoxic Event (T-OAE) is characterised by major
palaeoenvironmental and palaeoceanographical changes (ocean anoxia, global warming …

A geochemical analysis has been conducted in the Fuente de la Vidriera section of the
External Subbetic (Betic Cordillera, southern Spain) in order to interpret the incidence of the …