Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

Abstract The Coniacian-Santonian (CS) was a time of differentiation in marine
sedimentation, characterized by organic carbon (OC)-rich black shales and carbonates …

GPlates is an open‐source, cross‐platform plate tectonic geographic information system,
enabling the interactive manipulation of plate‐tectonic reconstructions and the visualization …

The alkenone–p CO2 methodology has been used to reconstruct the partial pressure of
ancient atmospheric carbon dioxide (p CO2) for the past 45 million years of Earth's history …

Dissolved oxygen (O2) is essential for most ocean ecosystems, fuelling organisms'
respiration and facilitating the cycling of carbon and nutrients. Oxygen measurements have …

The Cenomanian‐Turonian oceanic anoxic event (OAE2) is characterized by large
perturbations in the oxygen and sulfur cycles of the ocean, potentially resulting from …

The evolution of the Northern Hemisphere oceanic gateways has facilitated ocean
circulation changes and may have influenced climatic variations in the Cenozoic time (66 …

Paleoclimate studies suggest that increased global warmth during the Eocene epoch was
greatly amplified at high latitudes, a state that climate models cannot fully reproduce …

Understanding the role of sediment-water interactions in the oceanic cycling of neodymium
(Nd) isotopes is essential for its reliable use as a modern and palaeoceanographic tracer of …

Oceanic anoxic events (OAEs) are large-scale events of oxygen depletion in the deep ocean
that happened during pre-Cenozoic periods of extreme warmth. Here, to assess the role of …