The Cretaceous provides us with an excellent case history of ocean-climate-biota system
perturbations. Such perturbations occurred several times during the Cretaceous, such as …

The mid-Maastrichtian carbon isotope event (MME), dated at∼ 69 Ma, reflects a perturbation
of the global carbon cycle that, in part, correlates with the enigmatic global extinction of …

A multi-disciplinary approach, based on faunal, isotopic, geochemical and mineralogical
analyses, reveals a complex Maastrichtian paleoenvironment characterized by major …

During the mid-Cretaceous the Earth was characterized by peculiar climatic and
oceanographic features, such as very high temperatures, smooth thermal meridional …

Upper Maastrichtian chalks form important hydrocarbon reservoirs in the Danish sector of
the North Sea and have been intensively studied, yet their lithological uniformity can …

This work presents high-resolution palynological and micropalaeontological analyses of a
cored succession across the upper Maastrichtian from a well in the Møre Basin (Norwegian …

A multi-proxy study of four sediment cores from the Eastern (Caucasian) Black Sea shelf
revealed five transgressive–regressive cycles overprinted on the general trend of …

The Maastrichtian was a time of a high variability in the climate/ocean system. Most studies
on Maastrichtian palaeoenvironment fluxes have been based on evidence from the open …

Foraminiferal stable isotopes and assemblages from Franz Victoria and St. Anna troughs
provide a valuable record of freshwater and Atlantic Water flows to the northern Barents and …

Analysis of 944 single specimens of three species of late Maastrichtian planktonic
foraminifera (Racemiguembelina fructicosa, Contusotruncana contusa, and …