High-resolution carbon isotope (δ13C) profiles from shallow-and deep-water carbonates in
the South Atlantic (Campos and Santos Basins) are here correlated to stratigraphically well …

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 …

We have compiled stratigraphic ranges of genera of calcareous nannofossils, calcispheres,
planktonic foraminifers, larger benthic foraminifers, corals and rudists bivalves, and species …

A high‐resolution carbonate C‐isotope stratigraphy for the Aptian is presented for the Cau
core (Spain). The biostratigraphically calibrated C‐isotope stratigraphy of the core is used to …

The∼ 35-my-long Late Cretaceous greenhouse climate has been the subject of a number of
studies, with emphasis on the Cenomanian–Turonian and late Campanian–Maastrichtian …

Abstract The upper Aptian-lower Albian stratigraphic interval documents important
perturbations in the carbon cycle associated with the Oceanic Anoxic Event 1b (OAE 1b) …

Abstract The Aptian/Albian oceanic anoxic event 1b contains the record of several
perturbations in the global carbon cycle and multiple black shale levels, particularly in the …

An integrated study of multiple geochemical proxies (δ 13 C carb, δ 13 C org, TOC, HI,
CaCO 3, trace elements/Al ratios) of the late Aptian–early Albian oceanic anoxic event …

Organic carbon burial is an important driver of carbon cycle and climate dynamics on
geological and shorter time scales. Ocean basins emerging during the Early Cretaceous …

Upper Aptian planktonic foraminifera assemblages recorded in the post-salt section of the
Santos, Campos and Espírito Santo Brazilian marginal basins are described and interpreted …