Contrasting fast and slow intertropical convergence zone migrations linked to delayed Southern Ocean warming
Migrations of the intertropical convergence zone (ITCZ) have significant impacts on tropical
climate and society. Here we examine the ITCZ migration caused by CO2 increase using …
climate and society. Here we examine the ITCZ migration caused by CO2 increase using …
Modeling Past Hothouse Climates as a Means for Assessing Earth System Models and Improving the Understanding of Warm Climates
Simulating the warmth and equability of past hothouse climates has been a challenge since
the inception of paleoclimate modeling. The newest generation of Earth system models …
the inception of paleoclimate modeling. The newest generation of Earth system models …
Global vegetation zonation and terrestrial climate of the warm Early Eocene
The early Eocene is a key geological time interval to further our understanding of climate
change and biosphere variability under high atmospheric CO 2 concentrations of more than …
change and biosphere variability under high atmospheric CO 2 concentrations of more than …
Proto-monsoon rainfall and greening in Central Asia due to extreme early Eocene warmth
The dry continental interior of Asia has remained arid throughout most of its geological
history, yet the future of this unique ecosystem remains unclear. Here we use palynological …
history, yet the future of this unique ecosystem remains unclear. Here we use palynological …
DeepMIP-Eocene-p1: multi-model dataset and interactive web application for Eocene climate research
Paleoclimate model simulations provide reference data to help interpret the geological
record and offer a unique opportunity to evaluate the performance of current models under …
record and offer a unique opportunity to evaluate the performance of current models under …
Spatial and Temporal Patterns in Petrogenic Organic Carbon Mobilization During the Paleocene‐Eocene Thermal Maximum
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was a transient global warming
event and is recognized in the geologic record by a prolonged negative carbon isotope …
event and is recognized in the geologic record by a prolonged negative carbon isotope …
Dry hydroclimates in the late Palaeocene-early Eocene hothouse world
Extreme global warming can produce hydroclimate changes that remain poorly understood
for sub-tropical latitudes. Late Palaeocene-early Eocene (LPEE;~ 58-52 Ma) proto …
for sub-tropical latitudes. Late Palaeocene-early Eocene (LPEE;~ 58-52 Ma) proto …
[HTML][HTML] A paleoenvironmental and ecological analysis of biomarkers from the Eocene Fossil Basin, Green River Formation, USA
Exceptionally well-preserved fossil specimens in the Fossil Basin of the Green River
Formation (GRF) have made it the subject of extensive paleontological study, but the organic …
Formation (GRF) have made it the subject of extensive paleontological study, but the organic …
Biogeochemical responses to global warming during the Paleocene–Eocene Thermal Maximum in the eastern Tethys
Abstract The Paleocene–Eocene Thermal Maximum (PETM;∼ 56 Ma) represents a rapid
and sustained climatic perturbation that lasted for∼ 170 kyr and coincided with the …
and sustained climatic perturbation that lasted for∼ 170 kyr and coincided with the …
Orbital (hydro) climate variability in the ice‐free early Eocene Arctic
Abstract Early Eocene (∼ 56–48 Ma) climates are useful to investigate polar climate
dynamics in the absence of ice. We explore early Eocene orbital variability of Arctic climate …
dynamics in the absence of ice. We explore early Eocene orbital variability of Arctic climate …