[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 …
[HTML][HTML] Reconstructions of Antarctic topography since the Eocene–Oligocene boundary
Accurate models of past Antarctic ice sheet behaviour require realistic reconstructions of the
evolution of bedrock topography. However, other than a preliminary attempt to reconstruct …
evolution of bedrock topography. However, other than a preliminary attempt to reconstruct …
Dynamic Antarctic ice sheet during the early to mid-Miocene
Geological data indicate that there were major variations in Antarctic ice sheet volume and
extent during the early to mid-Miocene. Simulating such large-scale changes is problematic …
extent during the early to mid-Miocene. Simulating such large-scale changes is problematic …
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 …
Solid Earth change and the evolution of the Antarctic Ice Sheet
Recent studies suggest that Antarctica has the potential to contribute up to~ 15 m of sea-
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …
Heterogeneity in global vegetation and terrestrial climate change during the late Eocene to early Oligocene transition
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 variability across the Eocene-Oligocene boundary climate transition
About 34 million years ago, Earth's climate cooled and an ice sheet formed on Antarctica as
atmospheric carbon dioxide (CO2) fell below~ 750 parts per million (ppm). Sedimentary …
atmospheric carbon dioxide (CO2) fell below~ 750 parts per million (ppm). Sedimentary …
Cenozoic climate changes: A review based on time series analysis of marine benthic δ18O records
The climate during the Cenozoic era changed in several steps from ice‐free poles and warm
conditions to ice‐covered poles and cold conditions. Since the 1950s, a body of information …
conditions to ice‐covered poles and cold conditions. Since the 1950s, a body of information …