The Cretaceous oceanic red bed (CORB) is a newly opened window on global oceanic and
climate changes during the Cretaceous greenhouse world. As a result of the International …

Analysis of maximum depth of occurrence of 11 952 marine fish species shows a global
decrease in species number (N) with depth (x; m): log10 N=− 0· 000422 x+ 3· 610000 (r 2 …

A new lithostratigraphy scheme has been compiled for the Western Black Sea Basin and a
new geological history scheme from Middle Jurassic till Neogene is suggested for the entire …

Abstract The Pontides in northern Turkey constituted part of the southern active margin of
Eurasia during the Mesozoic. In the Early Cretaceous, a large submarine turbidite fan …

We provide a synthesis of stratigraphic data to unravel the history of the geological evolution
of South Crimea in the Mesozoic and Cenozoic. The South Crimea Orogen consists of three …

Abstract The deep sea (> 200 m) is home to a surprisingly rich biota, which in some cases
compares to that found in shallow areas. Scleractinian corals are an example of this–they …

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

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 …

The eastern part of the Sakarya Zone, known as the Eastern Pontides, is represented by a
south-facing carbonate platform during the Late Jurassic-Early Cretaceous. The shallow …

Abstract The Cenomanian‐Turonian period recorded one of the largest disruptions to the
oxygen and carbon cycles, the Oceanic Anoxic Event 2 (OAE2, 94 Ma). This event is global …