Eustatic sea-level changes of the Cretaceous are reevaluated based on a synthesis of
global stratigraphic data. A new terminology for local/regional or relative sea-level changes …

The present work aims to provide a high-resolution stratigraphic range of the planktic
foraminiferal group during the Campanian/Maastrichtian boundary (C/M) of Gebel Owaina …

Carbon stable-isotope stratigraphy provides unique insights into environmental change
during the Campanian, the longest (83.5–71.3 Ma), but least well-understood stage of the …

Data about the stratigraphical and regional distribution of Cretaceous rudist bivalves in the
central-eastern Mediterranean and Middle East from the Barremian to the Maastrichtian …

Study of an upper Santonian to upper Campanian hemipelagic succession from the
southern part of the Romanian Eastern Carpathians enables us to establish an integrated …

Two shallow water late Cenomanian to early Turonian sequences of NE Egypt have been
investigated to evaluate the response to OAE2. Age control based on calcareous …

Relative sea‐level changes on the mixed carbonate–siliciclastic platform of Sinai are
manifested in shifts of distinct facies belts (deep‐water facies, high‐energy subtidal, shallow …

The chronostratigraphy of Coniacian–Maastrichtian platform carbonates exposed on the
island of Brač and the adjacent mainland has been revised, based on numerical ages …

Environmental and depositional changes across the Late Cenomanian oceanic anoxic
event (OAE2) in the Sinai, Egypt, are examined based on biostratigraphy, mineralogy, δ 13 …

Making Upper Cretaceous biostratigraphic correlations between the Northwest Pacific and
Tethyan–Atlantic sections have been difficult because of rare frequencies of age-diagnostic …