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The Miocene: The future of the past
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 …
to today. Continental configurations and mountain topography transitioned toward modern …
[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 enigma of Oligocene climate and global surface temperature evolution
Falling atmospheric CO2 levels led to cooling through the Eocene and the expansion of
Antarctic ice sheets close to their modern size near the beginning of the Oligocene, a period …
Antarctic ice sheets close to their modern size near the beginning of the Oligocene, a period …
IPSL-CM5A2. An Earth System Model designed for multi-millennial climate simulations
Based on the CMIP5-generation previous IPSL earth system model, we designed a new
version, IPSL-CM5A2, aiming at running multi-millennial simulations typical of deep-time …
version, IPSL-CM5A2, aiming at running multi-millennial simulations typical of deep-time …
[HTML][HTML] The middle to late Eocene greenhouse climate modelled using the CESM 1.0. 5
The early and late Eocene have both been the subject of many modelling studies, but few
have focused on the middle Eocene. The latter still holds many challenges for climate …
have focused on the middle Eocene. The latter still holds many challenges for climate …
[HTML][HTML] Monitoring multidecadal coastline change and reconstructing tidal flat topography
Intertidal zones are vulnerable to both landward and seaward pressures, ie, sea level rise
and aquaculture expansion. Thus, the conservation of coastal habitats has reached …
and aquaculture expansion. Thus, the conservation of coastal habitats has reached …
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 …
Early Eocene ocean meridional overturning circulation: The roles of atmospheric forcing and strait geometry
Here, we compare the ocean overturning circulation of the early Eocene (47–56 Ma) in eight
coupled climate model simulations from the Deep‐Time Model Intercomparison Project …
coupled climate model simulations from the Deep‐Time Model Intercomparison Project …
Resilient Antarctic monsoonal climate prevented ice growth during the Eocene
Understanding the extreme greenhouse of the Eocene (56–34Ma ago) is key to anticipate
potential future conditions. During the Eocene, the Antarctic continent remained mostly ice …
potential future conditions. During the Eocene, the Antarctic continent remained mostly ice …
Drake Passage gateway opening and Antarctic Circumpolar Current onset 31 Ma ago: The message of foraminifera and reconsideration of the Neodymium isotope …
The establishment of the Antarctic Circumpolar Current (ACC) is one of the most important
events of the Cenozoic for both global oceanic circulation and climate. The onset of this …
events of the Cenozoic for both global oceanic circulation and climate. The onset of this …