[HTML][HTML] The Eocene–Oligocene transition: a review of marine and terrestrial proxy data, models and model–data comparisons
Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …
Weathering and the global carbon cycle: Geomorphological perspectives
The links between the weathering of silicate minerals, the global carbon cycle and climate
change are complex and involve a whole range of often inter-related tectonic, climatic …
change are complex and involve a whole range of often inter-related tectonic, climatic …
Onset of Antarctic Circumpolar Current 30 million years ago as Tasmanian Gateway aligned with westerlies
Earth's mightiest ocean current, the Antarctic Circumpolar Current (ACC), regulates the
exchange of heat and carbon between the ocean and the atmosphere, and influences …
exchange of heat and carbon between the ocean and the atmosphere, and influences …
Glacial weathering, sulfide oxidation, and global carbon cycle feedbacks
Connections between glaciation, chemical weathering, and the global carbon cycle could
steer the evolution of global climate over geologic time, but even the directionality of …
steer the evolution of global climate over geologic time, but even the directionality of …
Astronomical forcing and sedimentary noise modeling of lake-level changes in the Paleogene Dongpu Depression of North China
Challenges in interpreting continental sequence stratigraphy and typically uncertain
geochronology hinder the understanding of paleolake evolution and hydrocarbon …
geochronology hinder the understanding of paleolake evolution and hydrocarbon …
Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition
MJ Pound, U Salzmann - Scientific Reports, 2017 - nature.com
Rapid global cooling at the Eocene–Oligocene Transition (EOT),~ 33.9–33.5 Ma, is widely
considered to mark the onset of the modern icehouse world. A large and rapid drop in …
considered to mark the onset of the modern icehouse world. A large and rapid drop in …
Antarctic ice-sheet sensitivity to obliquity forcing enhanced through ocean connections
Deep sea geological records indicate that Antarctic ice-sheet growth and decay is strongly
influenced by the Earth's astronomical variations (known as Milankovitch cycles), and that …
influenced by the Earth's astronomical variations (known as Milankovitch cycles), and that …
Sea level and deep-sea temperature reconstructions suggest quasi-stable states and critical transitions over the past 40 million years
Sea level and deep-sea temperature variations are key indicators of global climate changes.
For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O …
For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O …
Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2
The greenhouse-to-icehouse climate transition from the Eocene into the Oligocene is well
documented by sea surface temperature records from the southwest Pacific and Antarctic …
documented by sea surface temperature records from the southwest Pacific and Antarctic …
Neogene ice volume and ocean temperatures: Insights from infaunal foraminiferal Mg/Ca paleothermometry
Antarctic continental‐scale glaciation is generally assumed to have initiated at the Eocene‐
Oligocene Transition, yet its subsequent evolution is poorly constrained. We reconstruct …
Oligocene Transition, yet its subsequent evolution is poorly constrained. We reconstruct …