[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 …
Cenozoic evolution of the steppe-desert biome in Central Asia
The origins and development of the arid and highly seasonal steppe-desert biome in Central
Asia, the largest of its kind in the world, remain largely unconstrained by existing records. It …
Asia, the largest of its kind in the world, remain largely unconstrained by existing records. It …
[HTML][HTML] Pattern and timing of diversification of Cetartiodactyla (Mammalia, Laurasiatheria), as revealed by a comprehensive analysis of mitochondrial genomes
The order Cetartiodactyla includes cetaceans (whales, dolphins and porpoises) that are
found in all oceans and seas, as well as in some rivers, and artiodactyls (ruminants, pigs …
found in all oceans and seas, as well as in some rivers, and artiodactyls (ruminants, pigs …
Global cooling during the Eocene-Oligocene climate transition
About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with
glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's …
glacial conditions on Antarctica characterized by substantial ice sheets. How Earth's …
Atmospheric carbon dioxide through the Eocene–Oligocene climate transition
Geological and geochemical evidence,, indicates that the Antarctic ice sheet formed during
the Eocene–Oligocene transition, 33.5–34.0 million years ago. Modelling studies, suggest …
the Eocene–Oligocene transition, 33.5–34.0 million years ago. Modelling studies, suggest …
Late Cretaceous–Neogene trends in deep ocean temperature and continental ice volume: Reconciling records of benthic foraminiferal geochemistry (δ18O and Mg …
We reconstruct trends in ice volume and deep ocean temperature for the past 108 Myr,
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …
resolving variations on timescales of∼ 2 Myr and longer. We use a sea level record as a …
Thresholds for Cenozoic bipolar glaciation
The long-standing view of Earth's Cenozoic glacial history calls for the first continental-scale
glaciation of Antarctica in the earliest Oligocene epoch (∼ 33.6 million years ago), followed …
glaciation of Antarctica in the earliest Oligocene epoch (∼ 33.6 million years ago), followed …
Late Eocene sea retreat from the Tarim Basin (west China) and concomitant Asian paleoenvironmental change
RE Bosboom, G Dupont-Nivet, AJP Houben… - Palaeogeography …, 2011 - Elsevier
The Paleogene sediments of the southwest Tarim Basin along the West Kunlun Shan in
western China include the remnants of the easternmost extent of a large epicontinental sea …
western China include the remnants of the easternmost extent of a large epicontinental sea …
Sensitivity of marginal basins in recording global icehouse and regional tectonic controls on sedimentation. Example of the Cergowa Basin,(Oligocene) Outer …
J Pszonka, M Wendorff, P Godlewski - Sedimentary Geology, 2023 - Elsevier
Global sea-level fall during the late Eocene-Oligocene icehouse, in conjunction with the
Alpine orogenesis, resulted in the epicontinental Paratethys Sea formed at the northern …
Alpine orogenesis, resulted in the epicontinental Paratethys Sea formed at the northern …
Antarctic glaciation caused ocean circulation changes at the Eocene–Oligocene transition
Two main hypotheses compete to explain global cooling and the abrupt growth of the
Antarctic ice sheet across the Eocene–Oligocene transition about 34 million years ago …
Antarctic ice sheet across the Eocene–Oligocene transition about 34 million years ago …