Sea levels shape the face of the Earth, define processes of sedimentation, and influence the
evolution of life via the distribution of habitats. Ancient topographies can be reconstructed …

Global mean sea level is a key component within the fields of climate and oceanographic
modelling in the Anthropocene. Hence, an improved understanding of eustatic sea level in …

2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …

We present an updated oceanic crustal age grid and a set of complementary grids including
spreading rate, asymmetry, direction, and obliquity. Our data set is based on a selected set …

The tectonics, geography and climate of the Cretaceous world were very different from the
modern world. At the start of the Cretaceous, the supercontinent of Pangaea had just begun …

In order to facilitate the search for new play concepts and exploration opportunities, a
sequence stratigraphic synthesis of the Cenomanian–Turonian interval of the Arabian Plate …

Retrograde clay mineral reactions (reverse weathering), including glauconite formation, are
first-order controls on element sequestration in marine sediments. Here, we report …

The evolving mosaic of tectonic plates across the surface of the Earth sets boundary
conditions for the evolution of biotic and abiotic processes and helps shape the dynamics of …

The sedimentary rock record suggests that global sea levels may have fluctuated by
hundreds of meters throughout Phanerozoic times. Long-term (10–80 Myr) sea level change …

The validity of sea level estimates based on stratigraphic correlations has been debated
since the 1990 s as relative sea level curves differ between sites due to local tectonics …