The Aalenian was a time marked by profound environmental and carbon cycle changes.
Still, the scarcity of detailed studies hinders a better understanding of the triggering …

Calcareous nannoplankton were profoundly affected by environmental perturbations
coincident with the early Toarcian oceanic anoxic event (T‐OAE). We quantify the …

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

Benthic foraminiferal assemblages belonging to a mixed carbonate–siliciclastic shelf
succession of the Oxfordian (Upper Jurassic) in the Prebetic, southern Spain, were …

Major, trace (Y, Zr, Pb, Th and U), rare earth element (REE) and Sm–Nd isotope analyses
were carried out on microbialites and detrital carbonate sediments collected in Upper …

The analysis of macroinvertebrate and foraminiferal assemblages from Upper Jurassic
(Middle Oxfordian to Lower Kimmeridgian) epicontinental shelf deposits in the Prebetic …

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 …

Calcareous nannoplankton experienced rapid diversification at the Jurassic/Cretaceous
boundary, including the appearance of several highly successful and long-ranging …

Many studies relating to long-term global change and climate variability rely on proxy data
from fossils and geochemistry to reconstruct paleoenvironments. Such data can also …

Foraminiferal assemblages from the neritic environment reveal the palaeoecological impact
of nutrient types in relation to shore distance and sedimentary setting. Comparatively …