The middle Eocene (47.8-38 Ma) marks the transition from the early Cenozoic greenhouse into the late Cenozoic icehouse climate. The early Cenozoic was characterized by warm temperatures, high atmospheric CO2 concentration ( 1000 ppm) and a non-existent or minor cryosphere. The climatic cooling towards the major glaciation of Antarctica is only partially covered by sedimentary records from scientific deep-sea drilling, which allow for high- resolution paleoceanographic studies. In the context of anthropogenic CO2 emissions and consequent global warming, the study of the nature and causes of climatic variability and the role of the ocean in the climate system during greenhouse climate is one of the fundamental challenges of paleoclimatology. ...
The so-called ‘Middle Eocene Climatic Optimum’ (MECO, ~40 Ma) represents a ~500-750 kyr period of tr...
Studying past intervals of abrupt global warming and massive carbon release can improve our knowledg...
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2 concentrations ...
The middle Eocene (47.8-38 Ma) marks the transition from the early Cenozoic greenhouse into the late...
The middle Eocene (47.8-38 Ma) marks the transition from the early Cenozoic greenhouse into the late...
The late Palaeocene to late Eocene period of Earth's history is characterised by remarkable change. ...
Global cooling and continental-scale expansion of Antarctic ice sheets occurred approximately 34 mil...
The Middle Eocene (37 to 49 million years ago, Ma) was characterised by warmer global temperatures a...
The early Eocene climate optimum (EECO) was the time of peak Cenozoic warmth with ice free poles. Th...
The late Palaeocene to late Eocene period of Earth's history is characterised by remarkable change. ...
Understanding warm climate states is increasingly important as projections of anthropogenic climate ...
Falling atmospheric CO2 levels led to cooling through the Eocene and the expansion of Antarctic ice ...
The early Eocene represents an ideal case study to analyse the impact of enhanced global warming on ...
The warming trend that started in the latest Paleocene and culminated in the Early Eocene Climatic O...
The last hyperthermal event in the Eocene, the Late Lutetian Thermal Maximum or Chron C19r event, to...
The so-called ‘Middle Eocene Climatic Optimum’ (MECO, ~40 Ma) represents a ~500-750 kyr period of tr...
Studying past intervals of abrupt global warming and massive carbon release can improve our knowledg...
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2 concentrations ...
The middle Eocene (47.8-38 Ma) marks the transition from the early Cenozoic greenhouse into the late...
The middle Eocene (47.8-38 Ma) marks the transition from the early Cenozoic greenhouse into the late...
The late Palaeocene to late Eocene period of Earth's history is characterised by remarkable change. ...
Global cooling and continental-scale expansion of Antarctic ice sheets occurred approximately 34 mil...
The Middle Eocene (37 to 49 million years ago, Ma) was characterised by warmer global temperatures a...
The early Eocene climate optimum (EECO) was the time of peak Cenozoic warmth with ice free poles. Th...
The late Palaeocene to late Eocene period of Earth's history is characterised by remarkable change. ...
Understanding warm climate states is increasingly important as projections of anthropogenic climate ...
Falling atmospheric CO2 levels led to cooling through the Eocene and the expansion of Antarctic ice ...
The early Eocene represents an ideal case study to analyse the impact of enhanced global warming on ...
The warming trend that started in the latest Paleocene and culminated in the Early Eocene Climatic O...
The last hyperthermal event in the Eocene, the Late Lutetian Thermal Maximum or Chron C19r event, to...
The so-called ‘Middle Eocene Climatic Optimum’ (MECO, ~40 Ma) represents a ~500-750 kyr period of tr...
Studying past intervals of abrupt global warming and massive carbon release can improve our knowledg...
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2 concentrations ...