[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 …
Buffered, incomplete, and shredded: The challenges of reading an imperfect stratigraphic record
Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …
Orbital climate variability on the northeastern Tibetan Plateau across the Eocene–Oligocene transition
The first major build-up of Antarctic glaciation occurred in two consecutive stages across the
Eocene–Oligocene transition (EOT): the EOT-1 cooling event at~ 34.1–33.9 Ma and the Oi-1 …
Eocene–Oligocene transition (EOT): the EOT-1 cooling event at~ 34.1–33.9 Ma and the Oi-1 …
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 …
Expanded lacustrine sedimentation in the Qaidam Basin on the northern Tibetan Plateau: Manifestation of climatic wetting during the Oligocene icehouse
Abstract The Qaidam Basin in the core area of arid Inner Asia has been considered
undergoing continuous aridification over the Cenozoic. However, the Qaidam Basin is …
undergoing continuous aridification over the Cenozoic. However, the Qaidam Basin is …
Synchronous cooling and decline in monsoonal rainfall in northeastern Tibet during the fall into the Oligocene icehouse
The fall into the Oligocene icehouse is marked by a steady decline in global temperature
with punctuated cooling at the Eocene-Oligocene transition, both of which are well …
with punctuated cooling at the Eocene-Oligocene transition, both of which are well …
Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition
Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene
Transition (EOT) is one of the largest non-linear events in Earth's climate history. Declining …
Transition (EOT) is one of the largest non-linear events in Earth's climate history. Declining …
Carbonate stable and clumped isotopic evidence for late Eocene moderate to high elevation of the east-central Tibetan Plateau and its geodynamic implications
The topographic history of mountain belts reflects changes in lithospheric structure and
rheology and exerts an influence on climate. Although substantial progress has been made …
rheology and exerts an influence on climate. Although substantial progress has been made …
An abrupt decrease in Southern Hemisphere terrestrial temperature during the Eocene–Oligocene transition
Earth's climate transitioned from the greenhouse conditions of the Eocene to the icehouse of
the Oligocene∼ 34 million years ago. Global cooling was triggered by a decrease in …
the Oligocene∼ 34 million years ago. Global cooling was triggered by a decrease in …
Astronomically forced climate variability across the Eocene–Oligocene transition from a low latitude terrestrial record (Lühe Basin, South China)
K Xu, DB Kemp, J Ren, W Qian - Bulletin, 2023 - pubs.geoscienceworld.org
Across the late Eocene to early Oligocene, Earth's climate underwent a dramatic shift from
Greenhouse to Icehouse, known as the Eocene–Oligocene transition (EOT). This globally …
Greenhouse to Icehouse, known as the Eocene–Oligocene transition (EOT). This globally …