[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 …
The Weddell Gyre, Southern Ocean: present knowledge and future challenges
Abstract The Weddell Gyre (WG) is one of the main oceanographic features of the Southern
Ocean south of the Antarctic Circumpolar Current which plays an influential role in global …
Ocean south of the Antarctic Circumpolar Current which plays an influential role in global …
The evolution of extant South American tropical biomes
C Jaramillo - New Phytologist, 2023 - Wiley Online Library
This review explores the evolution of extant South American tropical biomes, focusing on
when and why they developed. Tropical vegetation experienced a radical transformation …
when and why they developed. Tropical vegetation experienced a radical transformation …
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 …
Climatic and tectonic drivers of late Oligocene Antarctic ice volume
Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term
changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a …
changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a …
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 …
[HTML][HTML] Antarctic and global climate history viewed from ice cores
A growing network of ice cores reveals the past 800,000 years of Antarctic climate and
atmospheric composition. The data show tight links among greenhouse gases, aerosols and …
atmospheric composition. The data show tight links among greenhouse gases, aerosols and …
[HTML][HTML] Widespread Antarctic glaciation during the late Eocene
Marine sedimentary rocks drilled on the southeastern margin of the South Orkney
microcontinent in Antarctica (Ocean Drilling Program Leg 113 Site 696) were deposited …
microcontinent in Antarctica (Ocean Drilling Program Leg 113 Site 696) were deposited …