It is well established that greenhouse conditions prevailed during the Cretaceous Period (~
145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming …

Sequence stratigraphic studies consider relative change in sea level (as regulated by
eustasy, local tectonics and sediment supply) as the main builder of the stratigraphic record …

The studies of past climatic changes form the basis for predicting our future anthropogenic
world and are among the most prominent topics in current Earth sciences. Although the …

A 101 m thick stratigraphically complete late Coniacian–early Santonian (ca 89 to 83 Ma)
sedimentary sequence drilled in Tanzania (Tanzania Drilling Project Site 39) allows, for the …

Early Jurassic marine palaeotemperatures have been typically quantified by oxygen‐isotope
palaeothermometry of benthic and nektonic carbonate and phosphatic macrofossils …

The Campanian–Maastrichtian (83–66 Ma) was a period of global climate cooling, featuring
significant negative carbon-isotope (δ13C) anomalies, such as the Late Campanian Event …

Marine mudstone sediments recovered from multiple boreholes drilled in southeast
Tanzania yield some of the best preserved Turonian microfossils in the world, and these …

Little is known about the impact of the mid-Cretaceous Oceanic Anoxic Events (OAEs) on the
neritic carbonate systems in South America. In order to fill this knowledge gap, the present …

Biotic perturbations and changes in ocean circulation during the Maastrichtian stage of the
latest Cretaceous raise questions about whether the biosphere was preconditioned for the …

Integrated framework of calcareous nannofossil biostratigraphy and carbon isotope
stratigraphy for the upper Albian to upper Turonian succession has been made in the …