Understanding of the role of ocean circulation on climate during the Late Cretaceous is
contingent on the ability to reconstruct its modes and evolution. Geochemical proxies used …

Regional (2D) seismic-reflection profiles and borehole data are used to characterise the syn-
to post-rift transition in the shallow offshore Porto Basin, and in deep-offshore regions of …

The last 8 Myr of the Cretaceous greenhouse interval were characterized by a progressive
global cooling with superimposed cool/warm fluctuations. The mechanisms responsible for …

Abstract The latest Cenomanian to Santonian sedimentary record recovered at IODP
Expedition 369 Site U1513 in the Mentelle Basin (SE Indian Ocean, paleolatitude 60° S at …

The Cretaceous opening of the Equatorial Atlantic gateway (EAG) is considered a driver of
major changes in global oceanography, carbon cycling, and climate. However, the early …

Circulation in the North Atlantic during the Late Cretaceous has implications for poleward
heat transport and nutrient distribution during an extreme greenhouse interval with episodes …

Nd isotopes of fish debris collected from the English Chalk at Eastbourne (Sussex, UK) are
used to reconstruct the history of ocean circulation in the NW European shelf sea during …

Here, we compare the ocean overturning circulation of the early Eocene (47–56 Ma) in eight
coupled climate model simulations from the Deep‐Time Model Intercomparison Project …

Abstract The Late Cretaceous is considered to have been a time of greenhouse climates,
although evidence from Maastrichtian sediments for rapid and significant sea-level changes …

Abstract The Late Cretaceous was a greenhouse world, characterized by elevated
temperatures and high atmospheric pCO2. Even in the context of an extreme greenhouse …