Although ocean circulation plays a vital role in the climate system, its response to major
carbon-cycle perturbations during the mid-Cretaceous, including mid-Cenomanian event I …

Abstract The Cretaceous Period is particularly well represented by a thick sequence of
clastic sedimentary rocks exposed in the Antarctic Peninsula region of western Antarctica …

Abstract The Santonian–Campanian interval is of particular interest as it encompasses a
cooling trend after the Late Cretaceous greenhouse maximum warmth of the Turonian as …

Abstract The Albian–Cenomanian breakup sequence (BS) offshore Northwest Iberia is
mapped, described and characterised for the first time in terms of its seismic and …

Neodymium isotopic compositions (ε Nd) have been largely used for the last fifty years as a
tracer of past ocean circulation, and more intensively during the last decade to investigate …

New clay mineralogical analyses have been performed on Campanian sediments from the
Tethyan and Boreal realms along a palaeolatitudinal transect from 45° to 20° N (Danish …

Fossil fish teeth from pelagic open ocean settings are considered a robust archive for
preserving the neodymium (Nd) isotopic composition of ancient seawater. However, using …

The role that meridional overturning circulation (MOC) patterns played in poleward heat
transport during the extreme warmth of the Early to Late Cretaceous is a fundamental and …

Submarine lobes form at the distal end of sediment gravity flow systems and are globally
important sinks for sediment, anthropogenic pollutants and organic carbon, as well as …

International Ocean Discovery Program (IODP) Expedition 392 Site U1579 is located on the
shallowest part of the central Agulhas Plateau (39° 57.0725′ S, 26° 14.1793′ E) at 2492 …